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  • Conifers and blueberry shrubs in fall color at Mount Baker in Washington state, USA
    MtBakerTrees1_Blend.jpg
  • Conifers and blueberry shrubs in fall color at a tarn near Mount Shuksan in Washington state, USA
    MtBakerTarn1.jpg
  • Conifers and blueberry shrubs in fall color at Mount Baker in Washington state, USA
    MtBakerTrees1_Blend.jpg
  • Conifers and blueberry shrubs in fall color at a tarn near Mount Shuksan in Washington state, USA
    MtBakerTarn1.jpg
  • Conifers and blueberry shrubs in fall color at Mount Baker in Washington state, USA
    MtBakerTrees1_Blend.jpg
  • Conifers and blueberry shrubs in fall color at a tarn near Mount Shuksan in Washington state, USA
    MtBakerTarn1.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.
    JohnstonCanyon10.jpg
  • Forest at Sol Duc Falls in Olympic National Park, Washington
    SolDucEnchantedForest3.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). 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.
    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
  • 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.
    LakeLouiseWinterMorning2.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
  • 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
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Sol Duc Falls in Olympic National Park, The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucFallsBridge1.jpg
  • Small creek near Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucCascades6.jpg
  • Creek entering Perfection Lake in the Enchantment Lakes area of Alpine Lakes Wilderness, Washington
    EnchantmentsPerfectionLake1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • The Stuart Range is a mountain range in central Washington, USA. The range lies within the eastern extent of the Cascade Range immediately southwest of Leavenworth and runs east-west. The western peaks make up a single sharp ridge. The eastern half of the range splits into two parallel ridges, the northern of which is known as the Enchantment Peaks. Between these ridges lies the Enchantment Basin, which holds the dozens of tarns known as the Enchantment Lakes. Collectively, the basin and the encircling eastern peaks of the Stuart Range make up The Enchantments, a well-known backpacking destination. The south face of the Stuart Range falls off steeply to Ingalls Creek, beyond which rise the roughly parallel Wenatchee Mountains
    EnchantmentsAnnapurna1.jpg
  • Mountain Larches at Prusik Peak
    EnchantmentsInspirationLake2.jpg
  • Heather Pass, along Maple PAss / Lake Ann trail in the North Cascades National Park.
    HeatherPass1.jpg
  • Creek entering Perfection Lake in the Enchantment Lakes area of Alpine Lakes Wilderness, Washington
    EnchantmentsPerfectionLake1.jpg
  • Carpet of lupines on 1st Burroughs Mountain in Mount Rainier National Park in Western Washington, USA<br />
.....<br />
Mount Rainier National Park is a United States National Park located in southeast Pierce County and northeast Lewis County in Washington state. It was established on March 2, 1899 as the fifth national park in the United States. The park encompasses 236,381 acres including all of Mount Rainier, a 14,411-foot stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet. The highest point in the Cascade Range, around it are valleys, waterfalls, subalpine meadows, old-growth forest and more than 25 glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends.<br />
<br />
Mount Rainier is circled by the Wonderland Trail and is covered by several glaciers and snowfields totaling some 35 square miles. Carbon Glacier is the largest glacier by volume in the contiguous United States, while Emmons Glacier is the largest glacier by area. About 1.8 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for mountaineering with some 10,000 attempts per year with approximately 50% making it to the summit.
    MountRainierSunrise1stBurrough2.jpg
  • Mount Rainier National Park, Washington
    _MG_7024.jpg
  • Mountain Larches at Blue Lake in North Cascades National Park, Washington.  North Cascades National Park is a U.S. National Park located in the state of Washington. The park is the largest of the three National Park Service units that comprise the North Cascades National Park Service Complex. Several national wilderness areas and British Columbia parkland adjoin the National Park. The park features rugged mountain peaks and protects portions of the North Cascades range. Nearly all of the national park is protected as the Stephen Mather Wilderness, so there are few maintained buildings and roads within the North and South units of the Park. The park is most popular with backpackers and mountain climbers. One of the most popular destinations in the park is Cascade Pass, which was used as a travel route by Native Americans. It can be accessed by a four-mile (6 km) trail at the end of a gravel road. The North and South Picket Ranges, Mount Triumph, as well as Eldorado Peak and the surrounding mountains, are popular with climbers due to glaciation and technical rock. Mount Shuksan, in the northwest corner of the park, is one of the most photographed mountains in the country and the second highest peak in the park 9,127 ft or 2,782 m.
    Blue Lake and Spires 5.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanPictureLake1.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassFall1.jpg
  • Sequoia and King Canyon National Park, California
    SequoiaForest2.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • Gnome Tarn and Prusik Peak in the Enchantment Lakes area of Alpine Lakes Wilderness, Washington
    EnchantmentsPrussikSunset2.jpg
  • Sunrise at tarn in the Enchantments Lakes wilderness
    EnchantmentsGnomeTarnPink2.jpg
  • Mountain tarn reflecting Mount Rainier at dawn, Mount Rainier national park, Washington, USA
    MtRainierPlummerPeakTarn3.jpg
  • Sol Duc Falls in Olympic National Park, in autumn.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucFallsAutumn1.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    SahaleArm1.jpg
  • Mountain Larches at Prusik Peak
    EnchantmentsInspirationLake2.jpg
  • Mountain Larches at Blue Lake in North Cascades National Park, Washington.  North Cascades National Park is a U.S. National Park located in the state of Washington. The park is the largest of the three National Park Service units that comprise the North Cascades National Park Service Complex. Several national wilderness areas and British Columbia parkland adjoin the National Park. The park features rugged mountain peaks and protects portions of the North Cascades range. Nearly all of the national park is protected as the Stephen Mather Wilderness, so there are few maintained buildings and roads within the North and South units of the Park. The park is most popular with backpackers and mountain climbers. One of the most popular destinations in the park is Cascade Pass, which was used as a travel route by Native Americans. It can be accessed by a four-mile (6 km) trail at the end of a gravel road. The North and South Picket Ranges, Mount Triumph, as well as Eldorado Peak and the surrounding mountains, are popular with climbers due to glaciation and technical rock. Mount Shuksan, in the northwest corner of the park, is one of the most photographed mountains in the country and the second highest peak in the park 9,127 ft or 2,782 m.
    Blue Lake and Spires 5.jpg
  • Mount Rainier at sunset with a slightly lenticular cloud above its peak.  Seen from the east side near Tipsoo Lake.
    MountRainierTipsooSunset1.jpg
  • Meadows carpeted with lupines at Sunrise in Mount Rainier National Park
    MountRainierSunriseMeadow2.jpg
  • High Box peak seen from a tarn at Rampart Lakes in the Alpine Lakes Wilderness area of Washington state
    RampartsLakesTarn1.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassFall1.jpg
  • Shoreline of Blue Lake, North Cascades
    BlueLakeBush1.jpg
  • Larch trees at Enchantment Lakes
    EnchantmentsTamaracks1.jpg
  • Mountain tarn reflecting Mount Rainier at dawn, Mount Rainier national park, Washington, USA
    MtRainierPlummerPeakTarn2.jpg
  • Tamaracks reflecting in Lake Leprechaun in Washington's Enchantment Lakes wilderness area
    EnchantmentsLeprechaun.jpg
  • Prusik Peak from Gnome Tarn in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnSunrise1.jpg
  • Prusik Peak from an icy Gnome Tarn in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnIce1.jpg
  • Waterfall along Asgaard pass route to the Enchantment Lakes in Washington with Dragontail Peak in the background
    AsgaardWaterfall1.jpg
  • Crater Lake National Park is a United States National Park located in southern Oregon. Established in 1902, Crater Lake National Park is the fifth oldest national park in the United States and the only one in the state of Oregon. The park encompasses the caldera of Crater Lake, a remnant of a destroyed volcano, Mount Mazama, and the surrounding hills and forests.<br />
The lake is 1,943 feet deep at its deepest point, which makes it the deepest lake in the United States, the second deepest in North America and the ninth deepest in the world. Crater Lake is often referred to as the seventh deepest lake in the world, but this former listing excludes the approximately 3,000-foot depth of subglacial Lake Vostok in Antarctica, which resides under nearly 13,000 feet of ice, and the recent report of a 2,740-foot maximum depth for Lake O'Higgins/San Martin, located on the border of Chile and Argentina. However, when comparing its average depth of 1,148 feet to the average depth of other deep lakes, Crater Lake becomes the deepest in the Western Hemisphere and the third deepest in the world. The impressive average depth of this volcanic lake is due to the nearly symmetrical 4,000-foot deep caldera formed 7,700 years ago during the violent climactic eruptions and subsequent collapse of Mount Mazama and the relatively moist climate that is typical of the crest of the Cascade Range.<br />
The caldera rim ranges in elevation from 7,000 to 8,000 feet. The United States Geological Survey benchmarked elevation of the lake surface itself is 6,178 feet. This National Park encompasses 183,225 acres. Crater Lake has no streams flowing into or out of it. All water that enters the lake is eventually lost from evaporation or subsurface seepage. The lake's water commonly has a striking blue hue, and the lake is re-filled entirely from direct precipitation in the form of snow and rain.
    CraterLakeWinter2.jpg
  • Mount Rainier at sunset with a slightly lenticular cloud above its peak.  Seen from the east side near Tipsoo Lake.
    MountRainierTipsooSunset1.jpg
  • Mountain Larches at Lake Ann in the North Cascades National Park
    LakeAnn1.jpg
  • Heather Pass, along Maple PAss / Lake Ann trail in the North Cascades National Park.
    HeatherPass2.jpg
  • Larch trees at Crystal Lake in the Enchantment Lakes wilderness
    EnchantmentsCrystalLake1.jpg
  • Boulders along lake in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnRocks1.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.
    LakeMagogMountainLight1.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).
    SunburstPeak2.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.
    LakeMagogCabins2.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 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.
    SunburstLarchTrees1.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.
    MoraineLakeClouds3.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.
    LakeLouiseWinterMorningPano1-Edit.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.
    LakeLouiseWinterMorning10.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.
    LakeLouiseWinterMorning9-Edit.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.
    LakeLouiseWinterMorning3.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.
    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.
    MoraineLake6.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.
    MoraineLake4.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.
    MoraineLake2.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.
    JohnstonCanyon4.jpg
  • Prusik Peak from Gnome Tarn in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnClouds1.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).
    SunburstPeak1.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
  • 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.
    JohnstonCanyon3.jpg
  • Mount Rainier at sunset with a slightly lenticular cloud above its peak.  Seen from the east side near Tipsoo Lake.
    MountRainierTipsooSunset1.jpg
  • Mountain Larches at Lake Ann in the North Cascades National Park
    LakeAnn1.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanFall3.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierTipsoo9.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassTrees1.jpg
  • Carpet of lupines on 1st Burroughs Mountain in Mount Rainier National Park in Western Washington, USA<br />
.....<br />
Mount Rainier National Park is a United States National Park located in southeast Pierce County and northeast Lewis County in Washington state. It was established on March 2, 1899 as the fifth national park in the United States. The park encompasses 236,381 acres including all of Mount Rainier, a 14,411-foot stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet. The highest point in the Cascade Range, around it are valleys, waterfalls, subalpine meadows, old-growth forest and more than 25 glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends.<br />
<br />
Mount Rainier is circled by the Wonderland Trail and is covered by several glaciers and snowfields totaling some 35 square miles. Carbon Glacier is the largest glacier by volume in the contiguous United States, while Emmons Glacier is the largest glacier by area. About 1.8 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for mountaineering with some 10,000 attempts per year with approximately 50% making it to the summit.
    MountRainierSunrise1stBurrough2.jpg
  • Mountain tarn reflecting Mount Rainier at dawn, Mount Rainier national park, Washington, USA
    MtRainierPlummerPeakTarn1.jpg
  • Mount Rainier National Park, Washington
    _MG_7024.jpg
  • Waterfall along Asgaard pass route to the Enchantment Lakes in Washington with Dragontail Peak in the background
    EnchantmentsAsgaardPassTree.jpg
  • Prusik Peak from Gnome Tarn in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnSunrise1.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanWinter5.jpg
  • Mountain Larches at Blue Lake
    Blue Lake and Spires 2.jpg
  • Shoreline of Blue Lake, North Cascades
    BlueLakeBush1.jpg
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