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  • Snow and trees at the Tatoosh Range in Mount Rainier National Park in the winter.
    MountRainierTatooshWinter2.jpg
  • Mount Rainier National Park wilderness near Panhandle Gap along the Wonderland trail in winter
    SummerlandFryingpanCreek1.jpg
  • Snow and trees at the Tatoosh Range in Mount Rainier National Park in the winter.
    MountRainierTatooshWinter1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierHallwayTrees1.jpg
  • Bryce Canyon National Park is located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon which, despite its name, is not a canyon but a giant natural amphitheater created by erosion along the eastern side of the Paunsaugunt Plateau.  Seen here is the formation known as Thor's Hammer in the middle of winter.
    BryceThorsHammerSnow1-LAB-4000DPI.jpg
  • Bryce Canyon National Park is located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon which, despite its name, is not a canyon but a giant natural amphitheater created by erosion along the eastern side of the Paunsaugunt Plateau.  Seen here is the formation known as Thor's Hammer in the middle of winter.
    BryceThorsHammerSnow1-LAB-4000DPI.jpg
  • Fence on field in southern Oregon in the winter
    WinterFence1.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees4.jpg
  • Seen here in winter, Mount Baker, also known as Koma Kulshan or simply Kulshan, is an active glaciated andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. It is the second-most active volcano in the range after Mount Saint Helens.
    MtBakerSnow1.jpg
  • Winter below Snoqualmie Falls in Washington state, USA<br />
.....<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.
    SnoqualmieFallsRiverWinter1.jpg
  • The rising sun casts its first rays on the Border Peaks between USA and Canada in North Cascades national park in the midst of a very cold winter.
    MtBakerCascades1.jpg
  • Bryce Canyon National Park is located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon which, despite its name, is not a canyon but a giant natural amphitheater created by erosion along the eastern side of the Paunsaugunt Plateau.  Seen here is the formation known as Thor's Hammer in the middle of winter.
    BryceThorsHammerSnow1-LAB-4000DPI.jpg
  • Winter at Mount Rainier National Park administration building at Longmire, Washington
    MountRainierWinterHouse.jpg
  • Bryce Canyon in the winter
    BryceSunsetPointSnow1.jpg
  • Winter below Snoqualmie Falls in Washington state, USA<br />
.....<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.
    SnoqualmieFallsWinter1.jpg
  • Barn on field in southern Oregon in the winter
    WinterBarn1.jpg
  • Skyline Lake, in Washington's Cascade Mountains, snowed in during winter
    SkylineLake3.jpg
  • The setting sun casts its last rays on the Border Peaks between USA and Canada in North Cascades national park in the midst of a very cold winter.
    NorthCascadesPano1.jpg
  • Skyline Lake, in Washington's Cascade Mountains, snowed in during winter
    Skyline Lake 4-LAB.jpg
  • Bridge over Christine Falls in Mount Rainier National Park in winter
    MtRainierChristineFallsWinter2.jpg
  • Winter at Colchuck Lake
    EnchantmentsColchuckLake1.jpg
  • Skyline Lake, in Washington's Cascade Mountains, snowed in during winter
    Skyline Lake 1-LAB-New.jpg
  • The setting sun casts its last rays on the Border Peaks between USA and Canada in North Cascades national park in the midst of a very cold winter.
    MtBakerCascades2.jpg
  • Snow and trees along Mazama Ridge at Mount Rainier in the winter
    MazamaRidges2.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanWinter5.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanWinter3.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    HuangshanBench1.jpg
  • Mt Rainier and Kautz Creek in Winter
    MtRainierKautzCreek.jpg
  • Fryingpan Creek in winter
    SummerlandFryingpanCreek2.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierFrozenTrees.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierReflectionWinter2.jpg
  • Mt Rainier at Reflection Lakes in Winter
    RainierWinterPanorama1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    RainierFaceWinter.jpg
  • Frozen and snowy creek below Christine Falls in Mount Rainier National Park in winter
    MtRainierChristineIceStudy1.jpg
  • Hillside with burned in forest fire, in Oregon in winter
    SistersForestFire1.jpg
  • Hillside with burned in forest fire, in Oregon in winter
    SistersForestFire5.jpg
  • Hillside with burned in forest fire, in Oregon in winter
    SistersForestFire3.jpg
  • Hillside with burned in forest fire, in Oregon in winter
    SistersForestFire4.jpg
  • Hillside with burned in forest fire, in Oregon in winter
    SistersForestFire2.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.
    CraterLakeWinter5.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.
    CraterLakeWinter19.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.
    CraterLakeWinter10.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanWinter7.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.
    CraterLakeWinter16.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.
    CraterLakeWinter13.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.
    CraterLakeWinter11.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.
    CraterLakeWinter7.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.
    CraterLakeWinter6.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
  • Horses running on a snow covered field on a ranch in northeastern Wyoming
    SnowHorses1.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.
    CraterLakeWinter21.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.
    CraterLakeWinter9.jpg
  • Bryce Canyon National Park, a sprawling reserve in southern Utah, is known for crimson-colored hoodoos, which are spire-shaped rock formations. The park’s main road leads past the expansive Bryce Amphitheater, a hoodoo-filled depression lying below the Rim Trail hiking path. It has overlooks at Sunrise Point, Sunset Point, Inspiration Point and Bryce Point. Prime viewing times are around sunup and sundown.
    BryceThorsHammerSnow3-LAB.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees2.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierSnowDrift2.jpg
  • Barn near Leavenworth, Washington in winter
    LakeWenatcheeBarn1.jpg
  • Panoramic view in the winter from Bryce Canyon's Sunset Point. Bryce Canyon National Park, a sprawling reserve in southern Utah, is known for crimson-colored hoodoos, which are spire-shaped rock formations. The park’s main road leads past the expansive Bryce Amphitheater, a hoodoo-filled depression lying below the Rim Trail hiking path. It has overlooks at Sunrise Point, Sunset Point, Inspiration Point and Bryce Point. Prime viewing times are around sunup and sundown.
    BryceSunsetPointPan2-Flat.jpg
  • Marymere Falls, in Washington's Olympic National Park, covered in snow and ice during winter. Marymere Falls is located in Olympic National Park near Lake Crescent in Washington, United States. The falls are accessed by a one-mile, well maintained, dirt trail through old-growth lowland forest consisting of fir, cedar, hemlock, and alder trees. Falls creek descends from Aurora Ridge and tumbles over Marymere Falls and then flows into Barnes Creek. It has a height of 90 feet. The falls is one of the more popular attractions in the area, due to ease of access and proximity to U.S. Highway 101.
    MarymereFallsWinter1.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta4.jpg
  • Mount Hood, called Wy'east by the Multnomah tribe, is a stratovolcano in the Cascade Volcanic Arc of northern Oregon. It was formed by a subduction zone and rests in the Pacific Northwest region of the United States. It is located about 50 miles (80 km) east-southeast of Portland, on the border between Clackamas and Hood River counties. In addition to being Oregon's highest mountain, it is one of the loftiest mountains in the nation based on its prominence.
    MountHoodPeakWinter1.jpg
  • Hoodoos at Bryce Canyon's Sunset Point during winter. Bryce Canyon National Park, a sprawling reserve in southern Utah, is known for crimson-colored hoodoos, which are spire-shaped rock formations. The park’s main road leads past the expansive Bryce Amphitheater, a hoodoo-filled depression lying below the Rim Trail hiking path. It has overlooks at Sunrise Point, Sunset Point, Inspiration Point and Bryce Point. Prime viewing times are around sunup and sundown.
    BryceSnowHoodoos2-LAB.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees3.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierTatooshTrees1.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees5.jpg
  • The setting sun casts its last rays on the Border Peaks between USA and Canada in North Cascades national park in the midst of a very cold winter.
    MtBakerCascadesSunset2.jpg
  • Mount Rainier National Park wilderness near Panhandle Gap along the Wonderland trail in winter
    SummerlandFryingpanMoon1.jpg
  • Mount Rainier National Park wilderness near Panhandle Gap along the Wonderland trail in winter
    SummerlandCamp.jpg
  • Winter sunset at Bryce Canyon National Park, Sunrise Point. Bryce Canyon National Park, a sprawling reserve in southern Utah, is known for crimson-colored hoodoos, which are spire-shaped rock formations. The park’s main road leads past the expansive Bryce Amphitheater, a hoodoo-filled depression lying below the Rim Trail hiking path. It has overlooks at Sunrise Point, Sunset Point, Inspiration Point and Bryce Point. Prime viewing times are around sunup and sundown.
    BryceSnowHoodoos3-LAB.jpg
  • Winter sunset at Bryce Canyon National Park, Sunrise Point. Bryce Canyon National Park, a sprawling reserve in southern Utah, is known for crimson-colored hoodoos, which are spire-shaped rock formations. The park’s main road leads past the expansive Bryce Amphitheater, a hoodoo-filled depression lying below the Rim Trail hiking path. It has overlooks at Sunrise Point, Sunset Point, Inspiration Point and Bryce Point. Prime viewing times are around sunup and sundown.
    BryceSnowHoodoos3-LAB.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta5.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierTatooshTrees2.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierReflectionTrees2.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierBacklitDrift.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierSnowshoers2.jpg
  • Panoramic view in the winter from Bryce Canyon's Sunset Point. Bryce Canyon National Park, a sprawling reserve in southern Utah, is known for crimson-colored hoodoos, which are spire-shaped rock formations. The park’s main road leads past the expansive Bryce Amphitheater, a hoodoo-filled depression lying below the Rim Trail hiking path. It has overlooks at Sunrise Point, Sunset Point, Inspiration Point and Bryce Point. Prime viewing times are around sunup and sundown.
    BryceSunsetPointPan2-Flat.jpg
  • Winter sunset at Bryce Canyon National Park, Sunrise Point
    BryceSnowHoodoos3-LAB.jpg
  • Bryce Canyon's Paria Point in winter. Bryce Canyon National Park, a sprawling reserve in southern Utah, is known for crimson-colored hoodoos, which are spire-shaped rock formations. The park’s main road leads past the expansive Bryce Amphitheater, a hoodoo-filled depression lying below the Rim Trail hiking path. It has overlooks at Sunrise Point, Sunset Point, Inspiration Point and Bryce Point. Prime viewing times are around sunup and sundown.
    BrycePariaPointSnow1.jpg
  • Winter below Snoqualmie Falls in Washington state, USA<br />
.....<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.
    SnoqualmieFallsWinter2.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta6.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta3.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta2.jpg
  • Fence on field in southern Oregon in the winter
    WinterFence2.jpg
  • Barn near Leavenworth, Washington in winter
    LakeWenatcheeBarn2.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees1.jpg
  • Winter below Snoqualmie Falls in Washington state, USA
    SnoqualmieFallsRiverWinter2-HDR.jpg
  • Winter below Snoqualmie Falls in Washington state, USA<br />
.....<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.<br />
Snoqualmie Falls is a 268 ft (82 m) waterfall on the Snoqualmie River between Snoqualmie and Fall City, Washington, USA. It is one of Washington's most popular scenic attractions, but is perhaps best known internationally for its appearance in the cult television series Twin Peaks. More than 1.5 million visitors come to the Falls every year, where there is a two-acre (0.8 ha) park, an observation deck, and a gift shop.<br />
<br />
Most of the river is diverted into the power plants, but at times the river is high enough to flow across the entire precipice, which creates an almost blinding spray. High water occurs following a period of heavy rains or snow followed by warm rainy weather. This can occur during the rainy season which lasts from November through March. During high water, the falls take on a curtain form.
    SnoqualmieFallsRiverWinter2-HDR-Edit.jpg
  • Barn near Leavenworth, Washington in winter
    LakeWenatcheeBarn2.jpg
  • Marymere Falls, in Washington's Olympic National Park, covered in snow and ice during winter
    MarymereFallsWinter2a.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierChristineFallsWinter3.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierNationalParkInn1.jpg
  • Winter below Snoqualmie Falls in Washington state, USA
    SnoqualmieFallsRiverWinter2 (Blend).jpg
  • Lofoten is an archipelago and a traditional district in the county of Nordland, Norway. Lofoten is known for a distinctive scenery with dramatic mountains and peaks, open sea and sheltered bays, beaches and untouched lands. Though lying within the Arctic Circle, the archipelago experiences one of the world's largest elevated temperature anomalies relative to its high latitude.
    LofotenWinterDay3.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.
    LakeLouiseWinterMorning12.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.
    LakeLouiseWinterMorning2.jpg
  • Big Bend National Park in the U.S. state of Texas has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States. It contains more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. The national park covers 801,163 acres. A variety of Cretaceous and Cenozoic fossil organisms exist in abundance, and the park has artifacts estimated to be 9,000 years old. Historic buildings and landscapes offer graphic illustration of life along the international border in the 19th century. For more than 1,000 miles, the Rio Grande/Río Bravo forms the international boundary between Mexico and the United States, and Big Bend National Park administers approximately 118 miles along that boundary. The park was named after the area, which is bounded by a large bend in the river and Texas-Mexico border.
    BigBendChisosAgave4.jpg
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