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  • 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.
    BeaversBendTrees7.jpg
  • Lofoten is an archipelago and a traditional district in the county of Nordland, Norway. Lofoten is known for a distinctive scenery with dramatic mountains and peaks, open sea and sheltered bays, beaches and untouched lands. Though lying within the Arctic Circle, the archipelago experiences one of the world's largest elevated temperature anomalies relative to its high latitude.
    ReineStillness1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald1.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
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald1.jpg
  • Dock and buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSaltö6.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald1.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.
    BeaversBendTrees7.jpg
  • Dock and buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSalto6.jpg
  • The river Arno and Ponte Vecchio bridge in Firenze (Florence), Italy.<br />
-----<br />
Captured with a Canon 5D Mk III camera and Canon EF 24-105/4L IS lens  <br />
-----<br />
Florence (Italian: Firenze) is the capital city of the Italian region of Tuscany and of the province of Florence. The Ponte Vecchio ("Old Bridge") is a Medieval stone closed-spandrel segmental arch bridge over the Arno River, in Florence, Italy, noted for still having shops built along it, as was once common. Butchers initially occupied the shops; the present tenants are jewellers, art dealers and souvenir sellers. The Ponte Vecchio's two neighbouring bridges are the Ponte Santa Trinita and the Ponte alle Grazie. The bridge spans the Arno at its narrowest point where it is believed that a bridge was first built in Roman times, when the via Cassia crossed the river at this point. The Roman piers were of stone, the superstructure of wood. The bridge first appears in a document of 996. After being destroyed by a flood in 1117 it was reconstructed in stone but swept away again in 1333 save two of its central piers, as noted by Giovanni Villani in his Nuova Cronica. It was rebuilt in 1345, Giorgio Vasari recorded the tradition in his day, that attributed its design to Taddeo Gaddi, besides Giotto one of the few artistic names of the trecento still recalled two hundred years later. Modern historians present Neri di Fioravanti as a possible candidate. Sheltered in a little loggia at the central opening of the bridge is a weathered dedication stone, which once read Nel trentatrè dopo il mille-trecento, il ponte cadde, per diluvio dell' acque: poi dieci anni, come al Comun piacque, rifatto fu con questo adornamento. The Torre dei Mannelli was built at the southeast corner of the bridge to defend it.<br />
The bridge consists of three segmental arches: the main arch has a span of 30 meters (98 ft) the two side arches each span 27 meters (88 ft). The rise of the arches is between 3.5 and 4.4 meters (11½ to 14½ feet), and the spa
    PonteVecchio3.jpg
  • The river Arno and Ponte Vecchio bridge in Firenze (Florence), Italy.<br />
-----<br />
Captured with a Canon 5D Mk III camera and Canon EF 24-105/4L IS lens  <br />
-----<br />
Florence (Italian: Firenze) is the capital city of the Italian region of Tuscany and of the province of Florence. The Ponte Vecchio ("Old Bridge") is a Medieval stone closed-spandrel segmental arch bridge over the Arno River, in Florence, Italy, noted for still having shops built along it, as was once common. Butchers initially occupied the shops; the present tenants are jewellers, art dealers and souvenir sellers. The Ponte Vecchio's two neighbouring bridges are the Ponte Santa Trinita and the Ponte alle Grazie. The bridge spans the Arno at its narrowest point where it is believed that a bridge was first built in Roman times, when the via Cassia crossed the river at this point. The Roman piers were of stone, the superstructure of wood. The bridge first appears in a document of 996. After being destroyed by a flood in 1117 it was reconstructed in stone but swept away again in 1333 save two of its central piers, as noted by Giovanni Villani in his Nuova Cronica. It was rebuilt in 1345, Giorgio Vasari recorded the tradition in his day, that attributed its design to Taddeo Gaddi, besides Giotto one of the few artistic names of the trecento still recalled two hundred years later. Modern historians present Neri di Fioravanti as a possible candidate. Sheltered in a little loggia at the central opening of the bridge is a weathered dedication stone, which once read Nel trentatrè dopo il mille-trecento, il ponte cadde, per diluvio dell' acque: poi dieci anni, come al Comun piacque, rifatto fu con questo adornamento. The Torre dei Mannelli was built at the southeast corner of the bridge to defend it.<br />
The bridge consists of three segmental arches: the main arch has a span of 30 meters (98 ft) the two side arches each span 27 meters (88 ft). The rise of the arches is between 3.5 and 4.4 meters (11½ to 14½ feet), and the spa
    PonteVecchio2.jpg
  • The river Arno and Ponte Vecchio bridge in Firenze (Florence), Italy.<br />
-----<br />
Captured with a Canon 5D Mk III camera and Canon EF 24-105/4L IS lens  <br />
-----<br />
Florence (Italian: Firenze) is the capital city of the Italian region of Tuscany and of the province of Florence. The Ponte Vecchio ("Old Bridge") is a Medieval stone closed-spandrel segmental arch bridge over the Arno River, in Florence, Italy, noted for still having shops built along it, as was once common. Butchers initially occupied the shops; the present tenants are jewellers, art dealers and souvenir sellers. The Ponte Vecchio's two neighbouring bridges are the Ponte Santa Trinita and the Ponte alle Grazie. The bridge spans the Arno at its narrowest point where it is believed that a bridge was first built in Roman times, when the via Cassia crossed the river at this point. The Roman piers were of stone, the superstructure of wood. The bridge first appears in a document of 996. After being destroyed by a flood in 1117 it was reconstructed in stone but swept away again in 1333 save two of its central piers, as noted by Giovanni Villani in his Nuova Cronica. It was rebuilt in 1345, Giorgio Vasari recorded the tradition in his day, that attributed its design to Taddeo Gaddi, besides Giotto one of the few artistic names of the trecento still recalled two hundred years later. Modern historians present Neri di Fioravanti as a possible candidate. Sheltered in a little loggia at the central opening of the bridge is a weathered dedication stone, which once read Nel trentatrè dopo il mille-trecento, il ponte cadde, per diluvio dell' acque: poi dieci anni, come al Comun piacque, rifatto fu con questo adornamento. The Torre dei Mannelli was built at the southeast corner of the bridge to defend it.<br />
The bridge consists of three segmental arches: the main arch has a span of 30 meters (98 ft) the two side arches each span 27 meters (88 ft). The rise of the arches is between 3.5 and 4.4 meters (11½ to 14½ feet), and the spa
    _D3_6491.jpg
  • The river Arno and Ponte Vecchio bridge in Firenze (Florence), Italy.<br />
-----<br />
Captured with a Canon 5D Mk III camera and Canon EF 24-105/4L IS lens  <br />
-----<br />
Florence (Italian: Firenze) is the capital city of the Italian region of Tuscany and of the province of Florence. The Ponte Vecchio ("Old Bridge") is a Medieval stone closed-spandrel segmental arch bridge over the Arno River, in Florence, Italy, noted for still having shops built along it, as was once common. Butchers initially occupied the shops; the present tenants are jewellers, art dealers and souvenir sellers. The Ponte Vecchio's two neighbouring bridges are the Ponte Santa Trinita and the Ponte alle Grazie. The bridge spans the Arno at its narrowest point where it is believed that a bridge was first built in Roman times, when the via Cassia crossed the river at this point. The Roman piers were of stone, the superstructure of wood. The bridge first appears in a document of 996. After being destroyed by a flood in 1117 it was reconstructed in stone but swept away again in 1333 save two of its central piers, as noted by Giovanni Villani in his Nuova Cronica. It was rebuilt in 1345, Giorgio Vasari recorded the tradition in his day, that attributed its design to Taddeo Gaddi, besides Giotto one of the few artistic names of the trecento still recalled two hundred years later. Modern historians present Neri di Fioravanti as a possible candidate. Sheltered in a little loggia at the central opening of the bridge is a weathered dedication stone, which once read Nel trentatrè dopo il mille-trecento, il ponte cadde, per diluvio dell' acque: poi dieci anni, come al Comun piacque, rifatto fu con questo adornamento. The Torre dei Mannelli was built at the southeast corner of the bridge to defend it.<br />
The bridge consists of three segmental arches: the main arch has a span of 30 meters (98 ft) the two side arches each span 27 meters (88 ft). The rise of the arches is between 3.5 and 4.4 meters (11½ to 14½ feet), and the spa
    _D3_6490.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.
    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.
    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.
    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.
    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.
    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
  • Wichita Mountains Wildlife Refuge, located in southwestern Oklahoma near Lawton, has protected unique wildlife habitats since 1901 and is the oldest managed wildlife facility in the United States Fish and Wildlife Service system. Measuring about 59,020 acres (238.8 km2), the Refuge hosts a great diversity of species: 806 plant species, 240 species of birds, 36 fish, and 64 reptiles and amphibians are present. The refuge's location in the geologically unique Wichita Mountains and its areas of undisturbed mixed grass prairie make it an important conservation area. The Wichitas are approximately 500 million years old.
    _D3_4480.jpg
  • Wichita Mountains Wildlife Refuge, located in southwestern Oklahoma near Lawton, has protected unique wildlife habitats since 1901 and is the oldest managed wildlife facility in the United States Fish and Wildlife Service system. Measuring about 59,020 acres (238.8 km2), the Refuge hosts a great diversity of species: 806 plant species, 240 species of birds, 36 fish, and 64 reptiles and amphibians are present. The refuge's location in the geologically unique Wichita Mountains and its areas of undisturbed mixed grass prairie make it an important conservation area. The Wichitas are approximately 500 million years old.
    QuanahParkerLake1.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 />
<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 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
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn3.jpg
  • Dock and buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSalto5.jpg
  • Deer Harbor is an unincorporated community on Orcas Island in San Juan County, Washington, United States. As with most San Juan Islands communities, Deer Harbor is known for its recreation and tourism, including kayaking, whale watching, and fishing. Many people fish for Dungeness crab, Rock crab, and shrimp.
    OrcasChairs3.jpg
  • Lofoten is an archipelago and a traditional district in the county of Nordland, Norway. Lofoten is known for a distinctive scenery with dramatic mountains and peaks, open sea and sheltered bays, beaches and untouched lands. Though lying within the Arctic Circle, the archipelago experiences one of the world's largest elevated temperature anomalies relative to its high latitude.
    Hamnoy2.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn3.jpg
  • Boulders along lake in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnRocks1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.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
  • Boulders along lake in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnRocks1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierDrSmet1.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
  • Boulders along lake in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnRocks1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.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
  • Urban buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaTrossö7.jpg
  • Dock in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSaltö7.jpg
  • Urban buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaBridge1.jpg
  • Urban buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaTrossö3.jpg
  • Urban buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaBridge1.jpg
  • Typical Swedish small cottages in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaBrandaholm2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald4.jpg
  • MtRainierTipsoo2.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.
    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.
    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.
    _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.
    BeaversBendLeaves1.jpg
  • Deer Harbor is an unincorporated community on Orcas Island in San Juan County, Washington, United States. As with most San Juan Islands communities, Deer Harbor is known for its recreation and tourism, including kayaking, whale watching, and fishing. Many people fish for Dungeness crab, Rock crab, and shrimp.
    OrcasChairs1 (Topaz).jpg
  • Mount Rainier National Park is a United States National Park located in southeast Pierce County and northeast Lewis County in Washington state. It was established on March 2, 1899 as the fifth national park in the United States. The park encompasses 236,381 acres including all of Mount Rainier, a 14,410-foot (4,390 m) stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet (490 m) to over 14,000 feet (4,300 m). The highest point in the Cascade Range, around it are valleys, waterfalls, subalpine wildflower meadows, old growth forest and more than 25 glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends. <br />
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Mount Rainier is circled by the Wonderland Trail and is covered by several glaciers and snowfields totaling some 35 square miles (91 km2). Carbon Glacier is the largest glacier by volume in the continental United States, while Emmons Glacier is the largest glacier by area. About 1.8 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for mountain climbing with some 10,000 attempts per year with approximately 50% making it to the summit. The park contains outstanding subalpine meadows and 91,000 acres (370 km2) of old growth forests.
    MtRainierLowerTipsoo1.jpg
  • Deer Harbor is an unincorporated community on Orcas Island in San Juan County, Washington, United States. As with most San Juan Islands communities, Deer Harbor is known for its recreation and tourism, including kayaking, whale watching, and fishing. Many people fish for Dungeness crab, Rock crab, and shrimp.
    OrcasChairs1 (Topaz).jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
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The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
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The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald6.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge4.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
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The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
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Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
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Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta4.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls7.jpg
  • Deer Harbor is an unincorporated community on Orcas Island in San Juan County, Washington, United States. As with most San Juan Islands communities, Deer Harbor is known for its recreation and tourism, including kayaking, whale watching, and fishing. Many people fish for Dungeness crab, Rock crab, and shrimp.
    OrcasDeerHarbor1.jpg
  • Deer Harbor is an unincorporated community on Orcas Island in San Juan County, Washington, United States. As with most San Juan Islands communities, Deer Harbor is known for its recreation and tourism, including kayaking, whale watching, and fishing. Many people fish for Dungeness crab, Rock crab, and shrimp.
    OrcasChairs2.jpg
  • Deer Harbor is an unincorporated community on Orcas Island in San Juan County, Washington, United States. As with most San Juan Islands communities, Deer Harbor is known for its recreation and tourism, including kayaking, whale watching, and fishing. Many people fish for Dungeness crab, Rock crab, and shrimp.
    OrcasDeerHarbor1.jpg
  • Sailboat off the shore of Orcas Island in the San Juan Islands in Washington state
    OrcasSailboat.jpg
  • Tufa formations reflecting in Mono Lake in California's Owens Valley, located just east of Yosemite National Park near the town of Lee Vining.
    MonoLakeGlowingTufa.jpg
  • Sailboats in Ystad, Sweden marina<br />
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Ystad is a town, and the seat of Ystad Municipality, Skåne County, Sweden, with 18,350 inhabitants in 2010. The settlement dates back to the 11th century and the town has become a busy ferryport, local administrative centre and tourist attraction. It is associated with the fictional detective Kurt Wallander whose stories, by Henning Mankell, are set primarily in Ystad and nearby communities. In 1285, the town's name was written Ystath. Its original meaning is not fully understood, but the "y" is probably related to an old word for the yew tree, while -stad is town, or place. In Danish times before 1658 the spelling was Ysted.
    YstadSailboats1.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.
    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.
    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.
    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.
    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.
    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
  • Boulders along lake in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnRocks1.jpg
  • Dock and buildings in Karlskona, Sweden<br />
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Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSalto5.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls3.jpg
  • Mount Rainier National Park, Washington
    _MG_7024.jpg
  • Dock and buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSaltö4.jpg
  • Dock and buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSaltö3.jpg
  • Urban buildings in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaTrosso7.jpg
  • Dock and buildings in Karlskona, Sweden<br />
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Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSalto8.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
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The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
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The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierDrSmet3.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald3.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
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald4.jpg
  • Larch trees at Crystal Lake in the Enchantment Lakes wilderness
    ColchuckLakeReflection1.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.
    _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.
    _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.
    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
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