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  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake5.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake2.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosStewartLake3.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosStewartLake3.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosNoNameLake1.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake3.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake1.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosStewartLake2.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake4.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    JohnsonLakePano1.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosStewartLake3.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake5.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake2.jpg
  • The Pecos Wilderness is a protected wilderness area within the Santa Fe National Forest and Carson National Forest. The Pecos Wilderness lies within the Camino Real Ranger District of the Carson National Forest, and the Pecos Ranger District and Espanola Ranger District of the Santa Fe National Forest. The Pecos Wilderness includes the southernmost extension of the Rocky Mountains in the sub-range of the Sangre de Cristo Mountains of north central New Mexico. Covering an area of 223,667 acres it is the second largest wilderness in the state after the Gila Wilderness. The Wilderness boasts one of the highest concentrations of peaks exceeding 12,000 feet (3,700 m) in elevation in New Mexico, including Santa Fe Baldy, 12,622 feet (3,847 m), the highest point in Santa Fe County, and South Truchas Peak, 13,102 feet (3,993 m), the second highest peak in the state.
    PecosJohnsonLake3.jpg
  • Creek near Moraine Lake in Banff National Park. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    MoraineCreek2.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake_Panorama.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake6.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake1.jpg
  • Creek near Moraine Lake in Banff National Park. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    MoraineCreek1.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake5.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake4.jpg
  • Snow covered trees near Moraine Lake in Banff National Park. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    MoraineLakeTrees1.jpg
  • Skyline Lake, in Washington's Cascade Mountains, snowed in during winter<br />
.....<br />
Stevens Pass (elevation 4,056 ft) is a mountain pass through the Cascade Mountains located at the border of King County and Chelan County in Washington, United States. U.S. Highway 2 travels over the pass, reaching a maximum elevation of 4,061 feet. The Pacific Crest Trail crosses the highway at Stevens Pass. The BNSF Railway's Cascade Tunnel lies 1,180 feet below the pass summit. The pass is near Stevens Pass Ski Area, which is on Cowboy Mountain and Big Chief Mountain.<br />
.....<br />
Stevens Pass is named after John Frank Stevens, the first non-indigenous person to discover it. Native Americans familiar with the area knew of the pass, although very little is known about Native American routes through the mountains. An old native trail over nearby Cady Pass, connecting the North Fork Skykomish River and the Wenatchee River, had been known about and used by pioneers since the early 19th century. In 1872 Hubert C. Ward, who was exploring the area for the Northern Pacific Railway, heard from some Native Americans that there was a low pass at the head of Nason Creek, a tributary of the Wenatchee River, which led to one of the sources of the Skykomish River. Later, in 1887 Albert Bowman Rogers who, like Stevens, was working for the Great Northern Railway learned from Native Americans that the Skykomish River and Nason Creek had sources close to one another but that neither Native Americans nor whites visited the Nason Creek area. Neither Ward nor Rogers had time to fully explore the area. In 1890 John Stevens conducted a thorough survey, located the pass, and determined it to be the best suited for a railway crossing of the North Cascades. He wrote that there was no indication that the pass was used — there was no sign of any trails, blazes, campsites, or old campfires, for at least ten miles in either direction and that the area was thickly forested and covered with almost impenetrable brush. Steve
    SkylineLakeForest1.jpg
  • Skyline Lake, in Washington's Cascade Mountains, snowed in during winter<br />
.....<br />
Stevens Pass (elevation 4,056 ft) is a mountain pass through the Cascade Mountains located at the border of King County and Chelan County in Washington, United States. U.S. Highway 2 travels over the pass, reaching a maximum elevation of 4,061 feet. The Pacific Crest Trail crosses the highway at Stevens Pass. The BNSF Railway's Cascade Tunnel lies 1,180 feet below the pass summit. The pass is near Stevens Pass Ski Area, which is on Cowboy Mountain and Big Chief Mountain.<br />
.....<br />
Stevens Pass is named after John Frank Stevens, the first non-indigenous person to discover it. Native Americans familiar with the area knew of the pass, although very little is known about Native American routes through the mountains. An old native trail over nearby Cady Pass, connecting the North Fork Skykomish River and the Wenatchee River, had been known about and used by pioneers since the early 19th century. In 1872 Hubert C. Ward, who was exploring the area for the Northern Pacific Railway, heard from some Native Americans that there was a low pass at the head of Nason Creek, a tributary of the Wenatchee River, which led to one of the sources of the Skykomish River. Later, in 1887 Albert Bowman Rogers who, like Stevens, was working for the Great Northern Railway learned from Native Americans that the Skykomish River and Nason Creek had sources close to one another but that neither Native Americans nor whites visited the Nason Creek area. Neither Ward nor Rogers had time to fully explore the area. In 1890 John Stevens conducted a thorough survey, located the pass, and determined it to be the best suited for a railway crossing of the North Cascades. He wrote that there was no indication that the pass was used — there was no sign of any trails, blazes, campsites, or old campfires, for at least ten miles in either direction and that the area was thickly forested and covered with almost impenetrable brush. Steve
    SkylineLakeForest1.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    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.
    BeaversBendDusk2.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.
    MtAssiniboineLodgeNight2.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.
    MountAssiniboineTarn2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseClouds1.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.
    BeaversBendTrees11.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
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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.
    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
  • Les Baux-de-Provence is a commune in the Bouches-du-Rhône department in southern France, in the province of Provence. It has a spectacular position in the Alpilles mountains, set atop a rocky outcrop crowned with a ruined castle overlooking the plains to the south. Its names refers to its site — in Provençal, a baou is a rocky spur. The village gives its name to the aluminium ore Bauxite which was first discovered there in 1821 by geologist Pierre Berthier.
    LesBaux4.jpg
  • The Château de Beynac is a castle situated in the commune of Beynac-et-Cazenac, in the Dordogne département of France. The castle is one of the best-preserved and best known in the region.<br />
<br />
This Middle Ages construction, with its austere appearance, is perched on top of a limestone cliff, dominating the town and the north bank of the Dordogne River. The castle was built in the 12th century by the barons of Beynac (one of the four baronies of Périgord) to close the valley. The sheer cliff face being sufficient to discourage any assault from that side, the defences were built up on the plateau: double crenellated walls, double moats, one of which was a deepened natural ravine, double barbican.<br />
<br />
The oldest part of the castle is a large, square-shaped, Romanesque keep with vertical sides and few openings, held together with attached watch towers and equipped with a narrow spiral staircase terminating on a crenellated terrace. To one side, a residence of the same period is attached; it was remodelled and enlarged in the 16th and 17th centuries. On the other side is a partly 14th century residence side-by-side with a courtyard and a square plan staircase serving the 17th century apartments. The apartments have kept their woodwork and a painted ceiling from the 17th century. The Salle des États (States' Hall) has a Renaissance sculptured fireplace and leads into a small oratory entirely covered with 15th century frescoes, included a Pietà, a Saint Christopher, and a Last Supper in which Saint Martial (first bishop of Limoges) is the maître d'hôtel.<br />
<br />
At the time of the Hundred Years' War, the fortress at Beynac was in French hands. The Dordogne was the border between France and England. Not far away, on the opposite bank of the river, the Château de Castelnaud was held by the English. The Dordogne region was the theatre of numerous struggles for influence, rivalries and occasionally battles between the English and French supporters. However, the castles fell more of
    DJI_0275-HDR.jpg
  • The Château de Beynac is a castle situated in the commune of Beynac-et-Cazenac, in the Dordogne département of France. The castle is one of the best-preserved and best known in the region.<br />
<br />
This Middle Ages construction, with its austere appearance, is perched on top of a limestone cliff, dominating the town and the north bank of the Dordogne River. The castle was built in the 12th century by the barons of Beynac (one of the four baronies of Périgord) to close the valley. The sheer cliff face being sufficient to discourage any assault from that side, the defences were built up on the plateau: double crenellated walls, double moats, one of which was a deepened natural ravine, double barbican.<br />
<br />
The oldest part of the castle is a large, square-shaped, Romanesque keep with vertical sides and few openings, held together with attached watch towers and equipped with a narrow spiral staircase terminating on a crenellated terrace. To one side, a residence of the same period is attached; it was remodelled and enlarged in the 16th and 17th centuries. On the other side is a partly 14th century residence side-by-side with a courtyard and a square plan staircase serving the 17th century apartments. The apartments have kept their woodwork and a painted ceiling from the 17th century. The Salle des États (States' Hall) has a Renaissance sculptured fireplace and leads into a small oratory entirely covered with 15th century frescoes, included a Pietà, a Saint Christopher, and a Last Supper in which Saint Martial (first bishop of Limoges) is the maître d'hôtel.<br />
<br />
At the time of the Hundred Years' War, the fortress at Beynac was in French hands. The Dordogne was the border between France and England. Not far away, on the opposite bank of the river, the Château de Castelnaud was held by the English. The Dordogne region was the theatre of numerous struggles for influence, rivalries and occasionally battles between the English and French supporters. However, the castles fell more of
    Beynac1.jpg
  • The Château de Castelnaud is a medieval fortress in the commune of Castelnaud-la-Chapelle, overlooking the Dordogne River in Périgord, southern France. It was erected to face its rival, the Château de Beynac. The oldest documents mentioning it date to the 13th century, when it figured in the Albigensian Crusade; its Cathar castellan was Bernard de Casnac. Simon de Montfort took the castle and installed a garrison; when it was retaken by Bernard, he hanged them all. During the Hundred Years' War, the castellans of Castelnaud owed their allegiance to the Plantagenets, the sieurs de Beynac across the river, to the king of France. In later times it was abandoned bit by bit, until by the French Revolution it was a ruin. Today the picturesquely restored castle, a private property open to the public, houses a much-visited museum of medieval warfare, featuring reconstructions of siege engines, mangonneaux, and trebuchets. The castle is listed as a monument historique by the French Ministry of Culture.
    CastelnaudChateau1.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.
    NaisetMountainLight4.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 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.
    LakeMagogCreek1.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.
    LakeMagogMountainLight4.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.
    LakeMagogMountainLight3.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.
    NaisetMountainLight1.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).
    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). 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
  • 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.
    AssiniboineWinterTrees1.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.
    _A1A1012-2.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.
    MtAssiniboineHut3.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.
    LakeMagogCabins1.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.
    MtAssiniBoineCabin1.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.
    CanmoreHelicopter3.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseRedCanoes5.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseRedCanoes2.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    NaturalBridge2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorning1.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLakeCanoes3.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLake7.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLake3.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseMistyDawn2.jpg
  • Johnston Creek is a tributary of the Bow River in Canada's Rocky Mountains. The creek is located in Banff National Park. As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.
    JohnstonCanyon7.jpg
  • Johnston Creek is a tributary of the Bow River in Canada's Rocky Mountains. The creek is located in Banff National Park. As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.
    JohnstonCanyon2.jpg
  • Kananaskis Country is a park system situated to the west of Calgary, Alberta, Canada in the foothills and front ranges of the Canadian Rockies. Kananaskis Country can be accessed by three highways that run into or through the area: Highway 40, a 66 km (41 mi) segment of the Bighorn Highway and also known as Kananaskis Trail; Highway 66, a 28 km (17 mi) highway originating near Bragg Creek known as Elbow Falls Trail; and Highway 68, a 42 km (26 mi) gravel highway originating from the Trans-Canada Highway (Highway 1) known as Sibbald Creek Trail.<br />
<br />
An ecological and environmental research station of the University of Calgary is located nearby, at Barrier Lake. A "Tim Horton Children's Foundation" summer camp is also located in the area. Easter Seals Camp Horizon is also located within Kananaskis along Highway 66.<br />
<br />
The area is named for the Kananaskis River, which was named by John Palliser in 1858 after a Cree acquaintance.
    MountKidd2.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.
    MountAssiniboineTarn2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseMistyDawn1.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
  • 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
  • The Olympic Mountains is a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but the western slopes of the Olympics rise directly out of the Pacific Ocean and are the wettest place in the 48 contiguous states. On the wetter end of the spectrum, 140 and 170 inches (3,600 and 4,300 mm) of rain falls on the Hoh Rainforest annually. Conversely, areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Most of the mountains are protected within the bounds of the Olympic National Park. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
    MtOlympusWinterPan.jpg
  • Hayden Mountain in Colorado's Rocky Mountains
    HaydenPeak2.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
  • _Y6A3131-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.
    BeaversBendTrees7.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.
    GuadalupeMcKittrick4.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.
    BeaversBendTrees2.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees1.jpg
  • _Y6A3163-HDR.jpg
  • _Y6A3120.jpg
  • _Y6A2989-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
  • 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.
    GuadalupeMcKittrick4.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
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees11.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees7.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendTrees3.jpg
  • Beavers Bend State Park is a 1,300 acres Oklahoma state park located in McCurtain County. It is approximately 10.5 miles north of Broken Bow. It was established in 1937 and contains Broken Bow Lake. Built on the site of an old Choctaw settlement, Beavers Bend State Park was named after John T. Beavers, a Choctaw intermarried citizen. The "bend" in the park's name refers to an area of the park where a portion of Mountain Fork River meanders sharply, making an almost 180-degree turn. This area is commonly known as the River Bend, and is a popular area for trout fishing, canoe rentals, and swimming. Also in the River Bend area is the Broken Bow Hydroelectric Plant, which generates energy from the waters of Broken Bow Lake.<br />
The local rock formations are some of the most distinctive in the state of Oklahoma. Just north of Broken Bow, sedimentary rock has been thrust upward due to an ancient collision of the North American and South American Plates, forming what is now the Ouachita Mountains. Evidence of what is called the Ouachita orogeny can be seen all over the park, where some layers of rock can be seen tilted up at angles of about sixty-degrees. These geologic features can be easily viewed around Broken Bow Lake and Mountain Fork River, where erosion has left much of the rock exposed.
    BeaversBendDusk2.jpg
  • _Y6A3131-Edit.jpg
  • _Y6A2989-Edit.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
  • _Y6A3131-Edit.jpg
  • _Y6A3120.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.
    BeaversBendTrees1.jpg
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