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  • 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).
    SunburstPeak3.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).
    SunburstPeak2.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).
    SunburstPeak1.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).
    SunburstPeak1.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).
    SunburstPeak1.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).
    SunburstPeak2-2.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.
    SunburstLarchTrees1.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.
    SunburstLarchTrees1.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.
    MtAssinniboine4.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.
    MtAssinniboine5.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.
    MtAssinniboine6.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.
    MtAssinniboine2.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.
    MtAssinniboine5.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnSunburst1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnSunburst1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice1.jpg
  • The Basilica di Santa Maria del Fiore (English: Basilica of Saint Mary of the Flower) is the main church of Florence, Italy. The Duomo, as it is ordinarily called, was begun in 1296 in the Gothic style to the design of Arnolfo di Cambio and completed structurally in 1436 with the dome engineered by Filippo Brunelleschi. The exterior of the basilica is faced with polychrome marble panels in various shades of green and pink bordered by white and has an elaborate 19th-century Gothic Revival façade by Emilio De Fabris.<br />
The cathedral complex, located in Piazza del Duomo, includes the Baptistery and Giotto's Campanile. The three buildings are part of the UNESCO World Heritage Site covering the historic centre of Florence and are a major attraction to tourists visiting the region of Tuscany. The basilica is one of Italy's largest churches, and until development of new structural materials in the modern era, the dome was the largest in the world. It remains the largest brick dome ever constructed.<br />
The cathedral is the mother church of the Roman Catholic Archdiocese of Florence, whose archbishop is currently Giuseppe Betori.
    DuomoSunburst1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssinniboine1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssinniboine1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssiniboine-Pano1.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence3.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick3.jpg
  • Cowboy on horse silhouetted against the rising sun and morning sky in eastern Wyoming
    CowboySunrise1.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendSantaElena3.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendBalancedRock2.jpg
  • Mesa Arch at sunrise, Island in the Sky district of Canyonlands National Park, Utah. Mesa Arch is a pothole arch in Canyonlands National Park, Utah. Canyonlands National Park is a U.S. National Park located in southeastern Utah near the town of Moab. It preserves a colorful landscape eroded into countless canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964. The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the rivers themselves. While these areas share a primitive desert atmosphere, each retains its own character. Two large river canyons are carved into the Colorado Plateau by the Colorado River and Green River. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
    MesaArch1.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei8.jpg
  • Cowboy and his horse at sunrise on a ranch in northweastern Wyoming
    CowboyAntlers1.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendBalancedRock1.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendSouthRimSunset3.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence3.jpg
  • Cowboy on horse at sunrise on a ranch in Hulett, Wyoming
    CowboySunrise5.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick3.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick3.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach15.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • Mesa Arch at sunrise, Island in the Sky district of Canyonlands National Park, Utah. Mesa Arch is a pothole arch in Canyonlands National Park, Utah. Canyonlands National Park is a U.S. National Park located in southeastern Utah near the town of Moab. It preserves a colorful landscape eroded into countless canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964. The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the rivers themselves. While these areas share a primitive desert atmosphere, each retains its own character. Two large river canyons are carved into the Colorado Plateau by the Colorado River and Green River. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
    MesaArch2.jpg
  • Mesa Arch at sunrise, Island in the Sky district of Canyonlands National Park, Utah. Mesa Arch is a pothole arch in Canyonlands National Park, Utah. Canyonlands National Park is a U.S. National Park located in southeastern Utah near the town of Moab. It preserves a colorful landscape eroded into countless canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964. The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the rivers themselves. While these areas share a primitive desert atmosphere, each retains its own character. Two large river canyons are carved into the Colorado Plateau by the Colorado River and Green River. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
    MesaArch3.jpg
  • Basilica in Guanajuato, Mexico<br />
------<br />
Guanajuato is a city and municipality in central Mexico and the capital of the state of the same name. It is part of the macroregion of Bajío. It is in a narrow valley, which makes its streets narrow and winding. Most are alleys that cars cannot pass through, and some are long sets of stairs up the mountainsides. Many of the city’s thoroughfares are partially or fully underground. The historic center has numerous small plazas and colonial-era mansions, churches and civil constructions built using pink or green sandstone.<br />
<br />
The origin and growth of Guanajuato resulted from the discovery of minerals in the mountains surrounding it. The mines were so rich that the city was one of the most influential during the colonial period. One of the mines, La Valenciana, accounted for two-thirds of the world’s silver production at the height of its production.<br />
<br />
The city is home to the Mummy Museum, which contains naturally mummified bodies that were found in the municipal cemetery between the mid 19th and 20th centuries. It is also home to the Festival Internacional Cervantino, which invites artists and performers from all over the world as well as Mexico. Guanajuato was the site of the first battle of the Mexican War of Independence between insurgent and royalist troops at the Alhóndiga de Granaditas. The city was named a World Heritage Site in 1988.
    GuanajuatoBasilica1.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.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
    GlacierLakeMcDonald7.jpg
  • Cowboy and his horse at sunrise on a ranch in northweastern Wyoming
    CowboyAntlers1.jpg
  • Cowboy on horse at sunrise on a ranch in Hulett, Wyoming
    CowboySunrise5.jpg
  • Cowboy on horse silhouetted against the rising sun and morning sky in eastern Wyoming
    CowboySunrise1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence1.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendSantaElena3.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendBalancedRock2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendBalancedRock1.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence1-2.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach14.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach1.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach6.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendSantaElena3.jpg
  • Mesa Arch at sunrise, Island in the Sky district of Canyonlands National Park, Utah. Mesa Arch is a pothole arch in Canyonlands National Park, Utah. Canyonlands National Park is a U.S. National Park located in southeastern Utah near the town of Moab. It preserves a colorful landscape eroded into countless canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964. The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the rivers themselves. While these areas share a primitive desert atmosphere, each retains its own character. Two large river canyons are carved into the Colorado Plateau by the Colorado River and Green River. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
    MesaArchSunrise1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssiniboine3.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssiniboine2.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick3.jpg
  • Mesa Arch at sunrise, Island in the Sky district of Canyonlands National Park, Utah. Mesa Arch is a pothole arch in Canyonlands National Park, Utah. Canyonlands National Park is a U.S. National Park located in southeastern Utah near the town of Moab. It preserves a colorful landscape eroded into countless canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964. The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the rivers themselves. While these areas share a primitive desert atmosphere, each retains its own character. Two large river canyons are carved into the Colorado Plateau by the Colorado River and Green River. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
    MesaArch3.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees5.jpg
  • Mykonos windmills - The windmills are a defining feature of the Mykonian landscape. There are many dotted around the island, but most are concentrated in the main town of Chora. The famous "Kato Mili" in Chora (Greek for lower mills), stand in a row on a hill overlooking the sea to harness the strong northern winds. Capped with wood and straw, the windmills were built by the Venetians in the 16th century to mill flour and remained in use until the early 20th century. Many have been refurbished and restored to serve as homes to locals and vaults to numerous Mykonian heritage documents.
    MykonosWindmills3.jpg
  • Cowboy and his horse at sunrise on a ranch in northweastern Wyoming
    CowboyAntlers1-Edit-2.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick3.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendBalancedRock1.jpg
  • McKittrick Canyon is a scenic canyon within the Guadalupe Mountains of West Texas and Eddy County, New Mexico. The steep towering walls of McKittrick Canyon protect a rich riparian oasis in the midst of the Chihuahuan Desert.
    GuadalupeMcKittrick2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendSantaElena3.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach11.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach4.jpg
  • Mesa Arch at sunrise, Island in the Sky district of Canyonlands National Park, Utah. Mesa Arch is a pothole arch in Canyonlands National Park, Utah. Canyonlands National Park is a U.S. National Park located in southeastern Utah near the town of Moab. It preserves a colorful landscape eroded into countless canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964. The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the rivers themselves. While these areas share a primitive desert atmosphere, each retains its own character. Two large river canyons are carved into the Colorado Plateau by the Colorado River and Green River. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
    MesaArch2.jpg
  • Mesa Arch at sunrise, Island in the Sky district of Canyonlands National Park, Utah. Mesa Arch is a pothole arch in Canyonlands National Park, Utah. Canyonlands National Park is a U.S. National Park located in southeastern Utah near the town of Moab. It preserves a colorful landscape eroded into countless canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964. The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the rivers themselves. While these areas share a primitive desert atmosphere, each retains its own character. Two large river canyons are carved into the Colorado Plateau by the Colorado River and Green River. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
    MesaArch1.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendSantaElena3.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendBalancedRock2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendSantaElena3.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach13.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach12.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach5.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendBalancedRock1.jpg
  • Central Park is an urban park in middle-upper Manhattan, within New York City.  The Park was established in 1857 on 778 acres of city-owned land. In 1858, Frederick Law Olmsted and Calvert Vaux, a landscape architect and an architect, respectively, won a design competition to improve and expand the park with a plan they titled the "Greensward Plan". Construction began the same year and the park's first area was opened to the public in the winter of 1858. Construction continued during the American Civil War farther south. Central Park was designated a National Historic Landmark (listed by the U.S. Department of the Interior and administered by the National Park Service) in 1962. The Park was managed for decades by the New York City Department of Parks and Recreation, and is currently managed by the Central Park Conservancy under contract with the municipal government in a public-private partnership.
    NYC_CentralPark1.jpg
  • The Washington Monument is an obelisk near the west end of the National Mall in Washington, D.C., built to commemorate the first U.S. president, General George Washington. The monument, made of marble, granite, and bluestone gneiss, is both the world's tallest stone structure and the world's tallest obelisk, standing 555 feet 5⅛ inches (169.294 m)
    DCWashingtonMonument4.jpg
  • Wildflower meadow in the Tatoosh Range in Mount Rainier national park, Washington
    MtRainierPinnacleMeadow1.jpg
  • Wildflower meadow in the Tatoosh Range in Mount Rainier national park, Washington
    MtRainierPinnacleMeadow1.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.
    MtAssiniboineHut5.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.
    MtAssiniboineHut1.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
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