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  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs3.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnAfterglow.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnSunburst1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnLight1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnLight1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnAfterglow.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnSunburst1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs2.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnLight1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnAfterglow.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCove2-2.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCove2.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnAfterglow.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnRipples.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs3.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs2.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs3.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs1.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs3.jpg
  • The Lime Kiln light, a name derived from the lime kilns built nearby in the 1860s, was first established in 1914. It was the last major light established in Washington. The lighthouse was updated five years later with a 38-foot octagonal concrete tower rising from the fog signal building. A fourth-order Fresnel lens was first exhibited from the new tower on June 30, 1919. The Coast Guard automated the Lime Kiln Lighthouse in August 1962, using photoelectric cells to turn the light on at dusk and off during daylight hours. In 1998, the drum lens was replaced with a modern optic, flashing a white light once every 10 seconds. Sitting on the rocky shoreline at a height of 55 feet, the beacon is visible for 17 miles.
    LimeKilnCliffs2.jpg
  • Griffith Park is a large municipal park at the eastern end of the Santa Monica Mountains, in the Los Feliz neighborhood of Los Angeles, California. The park covers 4,310 acres of land, making it one of the largest urban parks in North America. It is the second-largest city park in California, after Mission Trails Preserve in San Diego, and the 11th largest municipally-owned park in the United States. It has also been referred to as the Central Park of Los Angeles but is much larger, more untamed, and rugged than its New York City counterpart.
    HollywoodHills1.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseRedCanoes5.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorning3.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.
    LakeLouiseRedCanoes2.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
  • West Point lighthouse in Seattle's Discovery Park
    West Point Lighthouse2.jpg
  • West Point lighthouse in Seattle's Discovery Park
    West Point Lighthouse3.jpg
  • Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    _D3_4097.jpg
  • West Point lighthouse in Seattle's Discovery Park
    West Point Lighthouse2.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanFall3.jpg
  • West Point lighthouse in Seattle's Discovery Park
    West Point Lighthouse1.jpg
  • Ridges in the sand at Seattle's Discovery Park.  Low tide exposes a wide beach with West Point Lighthouse in the background.
    DiscoveryParkLowTide3.jpg
  • West Point lighthouse in Seattle's Discovery Park
    West Point Lighthouse2.jpg
  • Sunrise at Koki Beach in the town of Hana in Hawaii's Maui island<br />
..... <br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Wailuku is the seat of Maui County and is the third-largest CDP as of 2010. Other significant places include Kīhei (including Wailea and Makena in the Kihei Town CDP, which is the second-most-populated CDP in Maui); Lahaina (including Kāʻanapali and Kapalua in the Lahaina Town CDP); Makawao; Pāʻia; Kula; Haʻikū; and Hāna. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    KokiBeachSunrise4.jpg
  • Palm trees on Promenade des Anglais in Nice, France on the French riviera
    NiceBeachSunsetPalms1.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.
    BigBendSantaElena2.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.
    BigBendSantaElena1.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.
    BigBendSantaElena1.jpg
  • Wichita Mountains Wildlife Refuge, located in southwestern Oklahoma near Lawton, has protected unique wildlife habitats since 1901 and is the oldest managed wildlife facility in the United States Fish and Wildlife Service system. Measuring about 59,020 acres (238.8 km2), the Refuge hosts a great diversity of species: 806 plant species, 240 species of birds, 36 fish, and 64 reptiles and amphibians are present. The refuge's location in the geologically unique Wichita Mountains and its areas of undisturbed mixed grass prairie make it an important conservation area. The Wichitas are approximately 500 million years old.
    _D3_4480.jpg
  • Wichita Mountains Wildlife Refuge, located in southwestern Oklahoma near Lawton, has protected unique wildlife habitats since 1901 and is the oldest managed wildlife facility in the United States Fish and Wildlife Service system. Measuring about 59,020 acres (238.8 km2), the Refuge hosts a great diversity of species: 806 plant species, 240 species of birds, 36 fish, and 64 reptiles and amphibians are present. The refuge's location in the geologically unique Wichita Mountains and its areas of undisturbed mixed grass prairie make it an important conservation area. The Wichitas are approximately 500 million years old.
    QuanahParkerLake1.jpg
  • 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.
    LakeLouiseRedCanoes1.jpg
  • Heceta Head State Park (which includes Devils Elbow State Park) is located in a cove at the mouth of Cape Creek.  The light at top of 56-foot tower was illuminated in 1894.
    HecetaHeadLighthouse2.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.
    MoraineLakeClouds2.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.
    LakeLouiseWinterMorning6.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.
    LakeLouiseWinterMorning5.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
  • 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.
    MoraineLake8.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.
    MoraineLake5.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLake3.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseMistyDawn1.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.
    LakeLouiseMistyDawn3.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
  • 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.
    LakeLouiseCanoes2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseRedCanoes5.jpg
  • 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.
    MoraineLakeCanoes2.jpg
  • Heceta Head State Park (which includes Devils Elbow State Park) is located in a cove at the mouth of Cape Creek.  The light at top of 56-foot tower was illuminated in 1894.
    HecetaHeadLighthouse2.jpg
  • Sunset over Lago Pehoe and the Los Cuernos peaks in Torres del Paine National Park, Patagonia, Chile. Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    LagoPehoe2.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanFall3.jpg
  • Reflection in the Colorado River at the side canyon called National Canyon
    GrandCanyonNationalReflection1.jpg
  • Colorado River at North Canyon
    GrandCanyonNorthCanyon1.jpg
  • Reflection in the Colorado River at the side canyon called National Canyon
    GrandCanyonNationalReflection1.jpg
  • Heceta Head State Park (which includes Devils Elbow State Park) is located in a cove at the mouth of Cape Creek.  The light at top of 56-foot tower was illuminated in 1894.
    HecetaHeadLighthouse2.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake
    MtShuksanPictureLake1.jpg
  • Heceta Head State Park (which includes Devils Elbow State Park) is located in a cove at the mouth of Cape Creek.  The light at top of 56-foot tower was illuminated in 1894.
    HecetaHeadLighthouse3.jpg
  • Colorado River at North Canyon
    GrandCanyonNorthCanyon2.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. 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
  • Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    LosCuernosDawn2.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.
    MtShuksanPictureLake7.jpg
  • Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    _D3_4109.jpg
  • West Point lighthouse in Seattle's Discovery Park
    West Point Lighthouse1.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
  • The sun is setting behind the Los Cuernos in Torres del Paine, Chile.  Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    LagoPehoe1-Oloneo.jpg
  • Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    LosCuernosDawnPanorama.jpg
  • Sunset over Lago Pehoe and the Los Cuernos peaks in Torres del Paine National Park, Patagonia, Chile. Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    LagoPehoe3.jpg
  • Torres del Paine National Park is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes. The park is located 112 km (70 mi) north of Puerto Natales and 312 km (194 mi) north of Punta Arenas. The park borders Bernardo O'Higgins National Park to the west and the Los Glaciares National Park to the north in Argentine territory.<br />
Torres del Paine National Park is part of the Sistema Nacional de Áreas Silvestres Protegidas del Estado de Chile (National System of Protected Forested Areas of Chile). In 2006, it measured approximately 242,242 hectares. It is one of the largest and most visited parks in Chile. The park averages around 150,000 visitors a year, of which 60% are foreign tourists, who come from all over the world.<br />
The park is one of the 11 protected areas of the Magallanes Region and Chilean Antarctica (together with four national parks, three national reserves, and three national monuments). Together, the protected forested areas comprise about 51% of the land of the region.<br />
The Torres del Paine are the peaks of the mountain range, Cerro Paine. They extend 3,050 meters above sea level, and are joined by the Cuernos del Paine. The area also boasts valleys, rivers such as the Paine, lakes, and glaciers. The well-known lakes include Grey, Pehoé, Nordenskiöld, and Sarmiento. The glaciers, including Grey, Pingo, Tyndall, and Geikie, belong to the Southern Patagonia Ice Field.
    _D3_4113.jpg
  • OahuSunsetReflection2.jpg
  • Rocks on Sunset Beach on Oahu, Hawaii
    OahuSunsetBeach3.jpg
  • Black sand beach in Hana Bay on the northeast coast of Maui, in the town of Hana.<br />
.....<br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    HanaPalmTrees2.jpg
  • Heceta Head State Park (which includes Devils Elbow State Park) is located in a cove at the mouth of Cape Creek.  The light at top of 56-foot tower was illuminated in 1894.
    HecetaHeadMoon2.jpg
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