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  • The raccoon, also known as the common raccoon, North American raccoon, northern raccoon and colloquially as coon, is a medium-sized mammal native to North America. The raccoon is the largest of the procyonid family, having a body length of 16 to 28 in and a body weight of 8 to 20 lb. Its grayish coat mostly consists of dense underfur which insulates against cold weather. Two of the raccoon's most distinctive features are its extremely dexterous front paws and its facial mask, which are themes in the mythology of several Native American tribes. Raccoons are noted for their intelligence, with studies showing that they are able to remember the solution to tasks for up to three years. The diet of the omnivorous raccoon, which is usually nocturnal, consists of about 40% invertebrates, 33% plant foods, and 27% vertebrates.<br />
The original habitats of the raccoon are deciduous and mixed forests, but due to their adaptability they have extended their range to mountainous areas, coastal marshes, and urban areas, where some homeowners consider them to be pests. As a result of escapes and deliberate introductions in the mid-20th century, raccoons are now also distributed across the European mainland, the Caucasus region and Japan.<br />
Though previously thought to be solitary, there is now evidence that raccoons engage in gender-specific social behavior. Related females often share a common area, while unrelated males live together in groups of up to four animals to maintain their positions against foreign males during the mating season, and other potential invaders.
    SpokaneRaccoon1.jpg
  • The Lincoln Memorial is an American memorial built to honor the 16th President of the United States, Abraham Lincoln. It is located on the National Mall in Washington, D.C. The architect was Henry Bacon, the sculptor of the main statue (Abraham Lincoln, 1920) was Daniel Chester French, and the painter of the interior murals was Jules Guerin. It is one of several monuments built to honor an American president.
    DCLincolnMemorial1.jpg
  • The Thomas Jefferson Memorial is a presidential memorial in Washington, D.C. that is dedicated to Thomas Jefferson, an American Founding Father and the third President of the United States. The neoclassical building was designed by John Russell Pope. It was built by Philadelphia contractor Tyler Nichols. Construction began in 1939, the building was completed in 1943, and the bronze statue of Jefferson was added in 1947.  <br />
The Jefferson Memorial is managed by the National Park Service under its National Mall and Memorial Parks division
    DCJeffersonMemorial3.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandRoad3.jpg
  • The Thomas Jefferson Memorial is a presidential memorial in Washington, D.C. that is dedicated to Thomas Jefferson, an American Founding Father and the third President of the United States. The neoclassical building was designed by John Russell Pope. It was built by Philadelphia contractor Tyler Nichols. Construction began in 1939, the building was completed in 1943, and the bronze statue of Jefferson was added in 1947.  <br />
The Jefferson Memorial is managed by the National Park Service under its National Mall and Memorial Parks division
    DCJeffersonMemorial1.jpg
  • Crooked River and Smith Rock<br />
.....<br />
Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
<br />
The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend2.jpg
  • Crooked River and Smith Rock<br />
.....<br />
Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
<br />
The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend1-LAB.jpg
  • Crooked River and Smith Rock<br />
.....<br />
Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
<br />
The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend2.jpg
  • Waterfront Park is an eight-acre (5 ha) park along approximately one-half mile of the Cooper River in Charleston, South Carolina. The park received the 2007 Landmark Award from the American Society of Landscape Architects and the National Trust for Historic Preservation. This award "recognizes a distinguished landscape architecture project completed between 15 and 50 years ago that retains its original design integrity and contributes significantly to the public realm of the community in which it is located..<br />
<br />
Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled dir
    CharlestonPineappleFountain11.jpg
  • Waterfront Park is an eight-acre (5 ha) park along approximately one-half mile of the Cooper River in Charleston, South Carolina. The park received the 2007 Landmark Award from the American Society of Landscape Architects and the National Trust for Historic Preservation. This award "recognizes a distinguished landscape architecture project completed between 15 and 50 years ago that retains its original design integrity and contributes significantly to the public realm of the community in which it is located..<br />
<br />
Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled dir
    CharlestonPineappleFountain9.jpg
  • Skyline Lake, in Washington's Cascade Mountains, snowed in during winter<br />
.....<br />
Stevens Pass (elevation 4,056 ft) is a mountain pass through the Cascade Mountains located at the border of King County and Chelan County in Washington, United States. U.S. Highway 2 travels over the pass, reaching a maximum elevation of 4,061 feet. The Pacific Crest Trail crosses the highway at Stevens Pass. The BNSF Railway's Cascade Tunnel lies 1,180 feet below the pass summit. The pass is near Stevens Pass Ski Area, which is on Cowboy Mountain and Big Chief Mountain.<br />
.....<br />
Stevens Pass is named after John Frank Stevens, the first non-indigenous person to discover it. Native Americans familiar with the area knew of the pass, although very little is known about Native American routes through the mountains. An old native trail over nearby Cady Pass, connecting the North Fork Skykomish River and the Wenatchee River, had been known about and used by pioneers since the early 19th century. In 1872 Hubert C. Ward, who was exploring the area for the Northern Pacific Railway, heard from some Native Americans that there was a low pass at the head of Nason Creek, a tributary of the Wenatchee River, which led to one of the sources of the Skykomish River. Later, in 1887 Albert Bowman Rogers who, like Stevens, was working for the Great Northern Railway learned from Native Americans that the Skykomish River and Nason Creek had sources close to one another but that neither Native Americans nor whites visited the Nason Creek area. Neither Ward nor Rogers had time to fully explore the area. In 1890 John Stevens conducted a thorough survey, located the pass, and determined it to be the best suited for a railway crossing of the North Cascades. He wrote that there was no indication that the pass was used — there was no sign of any trails, blazes, campsites, or old campfires, for at least ten miles in either direction and that the area was thickly forested and covered with almost impenetrable brush. Steve
    SkylineLakeForest1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendGrove1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees3.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendGrove1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees3.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees11.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendGrove1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees11.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendLeaves2.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    AboveCharleston5.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    AboveCharleston2.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    CharlestonHome1.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    CharlestonRainbowRow6.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    CharlestonRainbowRow5.jpg
  • Waterfront Park is an eight-acre (5 ha) park along approximately one-half mile of the Cooper River in Charleston, South Carolina. The park received the 2007 Landmark Award from the American Society of Landscape Architects and the National Trust for Historic Preservation. This award "recognizes a distinguished landscape architecture project completed between 15 and 50 years ago that retains its original design integrity and contributes significantly to the public realm of the community in which it is located..<br />
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Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled dir
    CharlestonPineappleFountain10.jpg
  • Waterfront Park is an eight-acre (5 ha) park along approximately one-half mile of the Cooper River in Charleston, South Carolina. The park received the 2007 Landmark Award from the American Society of Landscape Architects and the National Trust for Historic Preservation. This award "recognizes a distinguished landscape architecture project completed between 15 and 50 years ago that retains its original design integrity and contributes significantly to the public realm of the community in which it is located..<br />
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Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled dir
    CharlestonPineappleFountain8.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach9.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach8.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach6.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach4.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    _Y6A4829.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    _Y6A4825.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    CharlestonDockStreetTheatre1.jpg
  • Waterfront Park is an eight-acre (5 ha) park along approximately one-half mile of the Cooper River in Charleston, South Carolina. The park received the 2007 Landmark Award from the American Society of Landscape Architects and the National Trust for Historic Preservation. This award "recognizes a distinguished landscape architecture project completed between 15 and 50 years ago that retains its original design integrity and contributes significantly to the public realm of the community in which it is located..<br />
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Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled dir
    CharlestonPineappleFountain1.jpg
  • Frisco Heritage Museum in Frisco, Texas. Frisco is a city in Collin and Denton counties in Texas. It is part of the Dallas-Fort Worth metroplex, and is approximately 25 miles from both Dallas Love Field and Dallas/Fort Worth International Airport. Since 2003, Frisco has received the designation "Tree City USA" by the National Arbor Day Foundation. When the Dallas area was being settled by American pioneers, many of the settlers traveled by wagon trains along the old Shawnee Trail. This trail was also used for cattle drives north from Austin. This trail later became the Preston Trail, and later, Preston Road. Preston Road is one of the oldest north-south roads in all of Texas. With all of this activity, the community of Lebanon was founded along this trail and granted a U.S. post office in 1860. In 1902, a line of the St. Louis-San Francisco Railway was being built through the area, and periodic watering stops were needed along the route for the steam locomotives. The current settlement of Lebanon was on the Preston Ridge and was thus too high in elevation, so the watering stop was placed about four miles (6 km) to the west on lower ground. A community grew around this train stop. Residents of Lebanon actually moved their houses to the new community on logs. The new town was originally named Emerson, but the U.S. Postal Service rejected the name as being too similar to another town in Texas. In 1904, the residents chose Frisco City in honor of the St. Louis–San Francisco Railway on which the town was founded, later shortened to its present name. in Frisco, Texas. Frisco is a city in Collin and Denton counties in Texas. It is part of the Dallas-Fort Worth metroplex, and is approximately 25 miles from both Dallas Love Field and Dallas/Fort Worth International Airport. Since 2003, Frisco has received the designation "Tree City USA" by the National Arbor Day Foundation. When the Dallas area was being settled by American pioneers, many of the settlers traveled by wagon
    FriscoHeritageMuseum3.jpg
  • Frisco Heritage Museum in Frisco, Texas. Frisco is a city in Collin and Denton counties in Texas. It is part of the Dallas-Fort Worth metroplex, and is approximately 25 miles from both Dallas Love Field and Dallas/Fort Worth International Airport. Since 2003, Frisco has received the designation "Tree City USA" by the National Arbor Day Foundation. When the Dallas area was being settled by American pioneers, many of the settlers traveled by wagon trains along the old Shawnee Trail. This trail was also used for cattle drives north from Austin. This trail later became the Preston Trail, and later, Preston Road. Preston Road is one of the oldest north-south roads in all of Texas. With all of this activity, the community of Lebanon was founded along this trail and granted a U.S. post office in 1860. In 1902, a line of the St. Louis-San Francisco Railway was being built through the area, and periodic watering stops were needed along the route for the steam locomotives. The current settlement of Lebanon was on the Preston Ridge and was thus too high in elevation, so the watering stop was placed about four miles (6 km) to the west on lower ground. A community grew around this train stop. Residents of Lebanon actually moved their houses to the new community on logs. The new town was originally named Emerson, but the U.S. Postal Service rejected the name as being too similar to another town in Texas. In 1904, the residents chose Frisco City in honor of the St. Louis–San Francisco Railway on which the town was founded, later shortened to its present name. in Frisco, Texas. Frisco is a city in Collin and Denton counties in Texas. It is part of the Dallas-Fort Worth metroplex, and is approximately 25 miles from both Dallas Love Field and Dallas/Fort Worth International Airport. Since 2003, Frisco has received the designation "Tree City USA" by the National Arbor Day Foundation. When the Dallas area was being settled by American pioneers, many of the settlers traveled by wagon
    FriscoHeritageMuseum1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees5.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendFog1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A9052.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees7.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendLeaves1.jpg
  • The raccoon, also known as the common raccoon, North American raccoon, northern raccoon and colloquially as coon, is a medium-sized mammal native to North America. The raccoon is the largest of the procyonid family, having a body length of 16 to 28 in and a body weight of 8 to 20 lb. Its grayish coat mostly consists of dense underfur which insulates against cold weather. Two of the raccoon's most distinctive features are its extremely dexterous front paws and its facial mask, which are themes in the mythology of several Native American tribes. Raccoons are noted for their intelligence, with studies showing that they are able to remember the solution to tasks for up to three years. The diet of the omnivorous raccoon, which is usually nocturnal, consists of about 40% invertebrates, 33% plant foods, and 27% vertebrates.<br />
The original habitats of the raccoon are deciduous and mixed forests, but due to their adaptability they have extended their range to mountainous areas, coastal marshes, and urban areas, where some homeowners consider them to be pests. As a result of escapes and deliberate introductions in the mid-20th century, raccoons are now also distributed across the European mainland, the Caucasus region and Japan.<br />
Though previously thought to be solitary, there is now evidence that raccoons engage in gender-specific social behavior. Related females often share a common area, while unrelated males live together in groups of up to four animals to maintain their positions against foreign males during the mating season, and other potential invaders.
    SpokaneRaccoon2.jpg
  • Skyline Lake, in Washington's Cascade Mountains, snowed in during winter<br />
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Stevens Pass (elevation 4,056 ft) is a mountain pass through the Cascade Mountains located at the border of King County and Chelan County in Washington, United States. U.S. Highway 2 travels over the pass, reaching a maximum elevation of 4,061 feet. The Pacific Crest Trail crosses the highway at Stevens Pass. The BNSF Railway's Cascade Tunnel lies 1,180 feet below the pass summit. The pass is near Stevens Pass Ski Area, which is on Cowboy Mountain and Big Chief Mountain.<br />
.....<br />
Stevens Pass is named after John Frank Stevens, the first non-indigenous person to discover it. Native Americans familiar with the area knew of the pass, although very little is known about Native American routes through the mountains. An old native trail over nearby Cady Pass, connecting the North Fork Skykomish River and the Wenatchee River, had been known about and used by pioneers since the early 19th century. In 1872 Hubert C. Ward, who was exploring the area for the Northern Pacific Railway, heard from some Native Americans that there was a low pass at the head of Nason Creek, a tributary of the Wenatchee River, which led to one of the sources of the Skykomish River. Later, in 1887 Albert Bowman Rogers who, like Stevens, was working for the Great Northern Railway learned from Native Americans that the Skykomish River and Nason Creek had sources close to one another but that neither Native Americans nor whites visited the Nason Creek area. Neither Ward nor Rogers had time to fully explore the area. In 1890 John Stevens conducted a thorough survey, located the pass, and determined it to be the best suited for a railway crossing of the North Cascades. He wrote that there was no indication that the pass was used — there was no sign of any trails, blazes, campsites, or old campfires, for at least ten miles in either direction and that the area was thickly forested and covered with almost impenetrable brush. Steve
    SkylineLakeForest1.jpg
  • Crooked River and Smith Rock<br />
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Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
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The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend1-LAB.jpg
  • The Lincoln Memorial is an American memorial built to honor the 16th President of the United States, Abraham Lincoln. It is located on the National Mall in Washington, D.C. The architect was Henry Bacon, the sculptor of the main statue (Abraham Lincoln, 1920) was Daniel Chester French, and the painter of the interior murals was Jules Guerin. It is one of several monuments built to honor an American president.
    DCLincolnMemorial2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees11.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees7.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees4.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A8758.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees11.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees7.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees4.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendGrove1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A8758.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A8758.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    AboveCharleston3.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach5.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach3.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach2.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    _Y6A4756-2.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    CharlestonDockStreetTheatre2.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    AboveCharleston6.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    CharlestonRainbowRow1.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
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Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    CharlestonBroadStreet2.jpg
  • Frisco Heritage Museum in Frisco, Texas. Frisco is a city in Collin and Denton counties in Texas. It is part of the Dallas-Fort Worth metroplex, and is approximately 25 miles from both Dallas Love Field and Dallas/Fort Worth International Airport. Since 2003, Frisco has received the designation "Tree City USA" by the National Arbor Day Foundation. When the Dallas area was being settled by American pioneers, many of the settlers traveled by wagon trains along the old Shawnee Trail. This trail was also used for cattle drives north from Austin. This trail later became the Preston Trail, and later, Preston Road. Preston Road is one of the oldest north-south roads in all of Texas. With all of this activity, the community of Lebanon was founded along this trail and granted a U.S. post office in 1860. In 1902, a line of the St. Louis-San Francisco Railway was being built through the area, and periodic watering stops were needed along the route for the steam locomotives. The current settlement of Lebanon was on the Preston Ridge and was thus too high in elevation, so the watering stop was placed about four miles (6 km) to the west on lower ground. A community grew around this train stop. Residents of Lebanon actually moved their houses to the new community on logs. The new town was originally named Emerson, but the U.S. Postal Service rejected the name as being too similar to another town in Texas. In 1904, the residents chose Frisco City in honor of the St. Louis–San Francisco Railway on which the town was founded, later shortened to its present name. in Frisco, Texas. Frisco is a city in Collin and Denton counties in Texas. It is part of the Dallas-Fort Worth metroplex, and is approximately 25 miles from both Dallas Love Field and Dallas/Fort Worth International Airport. Since 2003, Frisco has received the designation "Tree City USA" by the National Arbor Day Foundation. When the Dallas area was being settled by American pioneers, many of the settlers traveled by wagon
    FriscoHeritageMuseum2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees3.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendPano1-Edit.jpg
  • Agave americana, common names sentry plant, century plant, maguey, or American aloe, is a species of flowering plant in the family Agavaceae, native to Mexico, and the United States in New Mexico, Arizona and Texas. Today, it is cultivated worldwide as an ornamental plant. It has become naturalized in many regions, including the West Indies, parts of South America, the southern Mediterranean Basin, and parts of Africa, India, China, Thailand, and Australia. Despite the common name "American aloe", it is not closely related to plants in the genus Aloe.
    GuadalupeMcKittrickAgave1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees3-New.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A9044.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A8879-Edit.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendGrove1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees5.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees6.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees10.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees3.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A9025-Edit.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    _A1A9011-HDR.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees8.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendLeaves2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendCypresses1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees4.jpg
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