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  • Seattle skyline at dawn on a winter day in February
    SeattleSunrise2.jpg
  • Denver is the largest city and capital of the State of Colorado. Denver is nicknamed the Mile-High City because its official elevation is exactly one mile (5,280 feet) above sea level, making it one of the highest major cities in the United States. Denver is ranked as a beta world city by the Globalization and World Cities Research Network. With a 2013 estimated population of 649,495, Denver ranks as the 22nd-most populous U.S. city.<br />
<br />
Denver City was founded in November 1858 as a mining town during the Pike's Peak Gold Rush in western Kansas Territory. That summer, a group of gold prospectors from Lawrence, Kansas, had arrived and established Montana City on the banks of the South Platte River. This was the first settlement in what was later to become the city of Denver. The site faded quickly, however, and by the summer of 1859 it was abandoned in favor of Auraria (named after the gold mining town of Auraria, Georgia), and St. Charles City.
    DenverMNS2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • Lake McDonald is the largest lake in Glacier National Park. It is located ain Flathead County in the U.S. state of Montana. Lake McDonald is approximately 10 miles long, and over a mile wide and 472 feet deep, filling a valley formed by a combination of erosion and glacial activity. Lake McDonald lies at an elevation of 3,153 feet and is on the west side of the Continental Divide. The Going-to-the-Sun Road parallels the lake along its southern shoreline. The surface area of the lake is 6,823 acres.<br />
<br />
The lake is home to numerous native species of trout, and other game fish. Catchable species include, but are not limited to - westslope cutthroat trout, rainbow trout, bull trout (char), lake trout (char), Lake Superior whitefish, mountain whitefish, kokanee salmon (landlocked sockeye), and suckers. However, the lake is nutrient-poor and is not considered a prime fishing destination. Grizzly bears, black bear, moose, and mule deer are found in many places near the lake but are most common on the north shore. The lake is surrounded by a dense coniferous forest dominated by various species of spruce, fir, and larch. At the westernmost section of the lake in Apgar there is a National Park Service visitor center, limited lodging and dining facilities as well as outboard powerboats available for rental. Lake McDonald Lodge is the largest lodging facility on the lake and is approximately 5 miles east along the Going-to-the-Sun Road.<br />
<br />
Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land enco
    GlacierMcDonald3.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald1.jpg
  • The Brooklyn Bridge is one of the oldest suspension bridges in the United States. Completed in 1883, it connects the New York City boroughs of Manhattan and Brooklyn by spanning the East River. With a main span of 1,595.5 feet (486.3 m), it was the longest suspension bridge in the world from its opening until 1903, and the first steel-wire suspension bridge.
    NYCBrooklynBridge5.jpg
  • HanaBayBacklight1.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • Lake McDonald is the largest lake in Glacier National Park. It is located ain Flathead County in the U.S. state of Montana. Lake McDonald is approximately 10 miles long, and over a mile wide and 472 feet deep, filling a valley formed by a combination of erosion and glacial activity. Lake McDonald lies at an elevation of 3,153 feet and is on the west side of the Continental Divide. The Going-to-the-Sun Road parallels the lake along its southern shoreline. The surface area of the lake is 6,823 acres.<br />
<br />
The lake is home to numerous native species of trout, and other game fish. Catchable species include, but are not limited to - westslope cutthroat trout, rainbow trout, bull trout (char), lake trout (char), Lake Superior whitefish, mountain whitefish, kokanee salmon (landlocked sockeye), and suckers. However, the lake is nutrient-poor and is not considered a prime fishing destination. Grizzly bears, black bear, moose, and mule deer are found in many places near the lake but are most common on the north shore. The lake is surrounded by a dense coniferous forest dominated by various species of spruce, fir, and larch. At the westernmost section of the lake in Apgar there is a National Park Service visitor center, limited lodging and dining facilities as well as outboard powerboats available for rental. Lake McDonald Lodge is the largest lodging facility on the lake and is approximately 5 miles east along the Going-to-the-Sun Road.<br />
<br />
Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land enco
    GlacierMcDonald3.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells2.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.
    BigBendSouthRim2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald1.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens2.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens9.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens8.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens5.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens2.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens2.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens10.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens9.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens4.jpg
  • Seattle skyline at dawn on a winter day in February
    SeattleSunrise2-2.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens1-Edit.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens8.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens7-Edit.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens6.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens5.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens3.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens2.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens10.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens1-Edit.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens6.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens4.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens3.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens5.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens7-Edit.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens2.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
  • Cracked earth and bushes in Valley of the Gods, Utah
    ValleyOfTheGods2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells3.jpg
  • Canyon with multiple waterfalls in the Southern Region of Iceland
    Sigoldugljufur1.jpg
  • Saltö dock in Karlskona, Sweden<br />
.....<br />
Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaSaltö1.jpg
  • Urban buildings in Karlskona, Sweden<br />
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Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaBridge1.jpg
  • Typical Swedish small cottages in Karlskona, Sweden<br />
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Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaBrandaholm2.jpg
  • Looking across the Borgmästarfjärden bay in Karlskrona, Sweden<br />
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Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    Karlskrona-Pano1.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
  • The Roman Forum, also known by its original Latin designation, is located between the Palatine Hill and the Capitoline Hill of the city of Rome, Italy.
    _A1A3362.jpg
  • Positano is a village and comune on the Amalfi Coast (Costiera Amalfitana), in Campania, Italy, mainly in an enclave in the hills leading down to the coast. <br />
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Positano was a port of the Amalfi Republic in medieval times, and prospered during the sixteenth and seventeenth centuries. By the mid-nineteenth century, however, the town had fallen on hard times. More than half the population emigrated, mostly to America.<br />
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Positano was a relatively poor fishing village during the first half of the twentieth century. It began to attract large numbers of tourists in the 1950s, especially after John Steinbeck published his essay about Positano in Harper's Bazaar in May, 1953: "Positano bites deep", Steinbeck wrote. "It is a dream place that isn’t quite real when you are there and becomes beckoningly real after you have gone."
    PositanoCoast1.jpg
  • Trevi Fountain (Italian: Fontana di Trevi) is a fountain in the Trevi district in Rome, Italy, designed by Italian architect Nicola Salvi and completed by Pietro Bracci. Standing 86 ft high and 161.3 ft wide, it is the largest Baroque fountain in the city and one of the most famous fountains in the world. The fountain has appeared in several notable films, including Federico Fellini's La Dolce Vita, and is a popular tourist attraction. The backdrop for the fountain is the Palazzo Poli, given a new façade with a giant order of Corinthian pilasters that link the two main stories. Taming of the waters is the theme of the gigantic scheme that tumbles forward, mixing water and rockwork, and filling the small square. Tritons guide Oceanus' shell chariot, taming hippocamps.<br />
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In the centre a robustly-modelled triumphal arch is superimposed on the palazzo façade. The centre niche or exedra framing Oceanus has free-standing columns for maximal light and shade. In the niches flanking Oceanus, Abundance spills water from her urn and Salubrity holds a cup from which a snake drinks. Above, bas reliefs illustrate the Roman origin of the aqueducts.<br />
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The tritons and horses provide symmetrical balance, with the maximum contrast in their mood and poses (by 1730, rococo was already in full bloom in France and Germany).
    RomeTrevi4.jpg
  • The Mausoleum of Hadrian, usually known as the Castel Sant'Angelo, is a towering cylindrical building in Rome, central Italy, initially commissioned by the Roman Emperor Hadrian as a mausoleum for himself and his family.
    RomeCastelStAngelo2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
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The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
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The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLakeMcDonald3.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
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The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei4.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
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The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei8.jpg
  • Denver is the largest city and capital of the State of Colorado. Denver is nicknamed the Mile-High City because its official elevation is exactly one mile (5,280 feet) above sea level, making it one of the highest major cities in the United States. Denver is ranked as a beta world city by the Globalization and World Cities Research Network. With a 2013 estimated population of 649,495, Denver ranks as the 22nd-most populous U.S. city.<br />
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Denver City was founded in November 1858 as a mining town during the Pike's Peak Gold Rush in western Kansas Territory. That summer, a group of gold prospectors from Lawrence, Kansas, had arrived and established Montana City on the banks of the South Platte River. This was the first settlement in what was later to become the city of Denver. The site faded quickly, however, and by the summer of 1859 it was abandoned in favor of Auraria (named after the gold mining town of Auraria, Georgia), and St. Charles City.
    DenverMNS1.jpg
  • Monte Fitz Roy (also known as Cerro Chaltén, Cerro Fitz Roy, or simply Mount Fitz Roy) is a mountain located near El Chaltén village, in the Southern Patagonian Ice Field in Patagonia, on the border between Argentina and Chile. First climbed in 1952 by French alpinists Lionel Terray and Guido Magnone, it remains among the most technically challenging mountains on Earth for mountaineers. Monte Fitz Roy is the basis for the Patagonia clothing logo following Yvon Chouinard's ascent and subsequent film in 1968.
    MtFitzRoyRiver3.jpg
  • Monte Fitz Roy (also known as Cerro Chaltén, Cerro Fitz Roy, or simply Mount Fitz Roy) is a mountain located near El Chaltén village, in the Southern Patagonian Ice Field in Patagonia, on the border between Argentina and Chile. First climbed in 1952 by French alpinists Lionel Terray and Guido Magnone, it remains among the most technically challenging mountains on Earth for mountaineers. Monte Fitz Roy is the basis for the Patagonia clothing logo following Yvon Chouinard's ascent and subsequent film in 1968.
    MtFitzRoyRiverPano1.jpg
  • Lake McDonald is the largest lake in Glacier National Park. It is located ain Flathead County in the U.S. state of Montana. Lake McDonald is approximately 10 miles long, and over a mile wide and 472 feet deep, filling a valley formed by a combination of erosion and glacial activity. Lake McDonald lies at an elevation of 3,153 feet and is on the west side of the Continental Divide. The Going-to-the-Sun Road parallels the lake along its southern shoreline. The surface area of the lake is 6,823 acres.<br />
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The lake is home to numerous native species of trout, and other game fish. Catchable species include, but are not limited to - westslope cutthroat trout, rainbow trout, bull trout (char), lake trout (char), Lake Superior whitefish, mountain whitefish, kokanee salmon (landlocked sockeye), and suckers. However, the lake is nutrient-poor and is not considered a prime fishing destination. Grizzly bears, black bear, moose, and mule deer are found in many places near the lake but are most common on the north shore. The lake is surrounded by a dense coniferous forest dominated by various species of spruce, fir, and larch. At the westernmost section of the lake in Apgar there is a National Park Service visitor center, limited lodging and dining facilities as well as outboard powerboats available for rental. Lake McDonald Lodge is the largest lodging facility on the lake and is approximately 5 miles east along the Going-to-the-Sun Road.<br />
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Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land enco
    GlacierMcDonald4.jpg
  • First light over Monument Valley from atop Hunts Mesa
    HuntsMesaPano1.jpg
  • Sand Springs in Monument Valley, shadow of nearby tree
    MonumentValleySandSprings1.jpg
  • Canyon near El Chalten in Los Glaciares National Park.
    ElCanon1-Oloneo.jpg
  • Iguazu Falls, Iguazú Falls, Iguassu Falls or Iguaçu Falls are waterfalls of the Iguazu River on the border of the Argentine province of Misiones and the Brazilian state of Paraná. The falls divide the river into the upper and lower Iguazu. The Iguazu River rises near the city of Curitiba. The river flows through Brazil for most of its course, although most of the falls are on the Argentine side. Below its confluence with the San Antonio River, the Iguazu River forms the boundary between Argentina and Brazil.<br />
The name "Iguazu" comes from the Guarani or Tupi words "y", meaning "water", and "ûasú ", meaning "big". Legend has it that a god planned to marry a beautiful woman named Naipí, who fled with her mortal lover Tarobá in a canoe. In rage, the god sliced the river, creating the waterfalls and condemning the lovers to an eternal fall. The first European to find the falls was the Spanish conquistador Álvar Núñez Cabeza de Vaca in 1541.
    _D3_5431-Edit.jpg
  • Seattle skyline at dawn on a winter day in February
    SeattleDowntownSunrise3.jpg
  • Dramatic sunrise over Hana Bay on the northeast coast of Maui, Hawaii, in the town of Hana<br />
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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.
    HanaBayClouds1.jpg
  • "Korsvirkeshus" type house in central Ystad in the southern province of Skåne in Sweden<br />
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Ystad is a town, and the seat of Ystad Municipality, Skåne County, Sweden, with 18,350 inhabitants in 2010. The settlement dates back to the 11th century and the town has become a busy ferryport, local administrative centre and tourist attraction. It is associated with the fictional detective Kurt Wallander whose stories, by Henning Mankell, are set primarily in Ystad and nearby communities. In 1285, the town's name was written Ystath. Its original meaning is not fully understood, but the "y" is probably related to an old word for the yew tree, while -stad is town, or place. In Danish times before 1658 the spelling was Ysted.
    YstadStreet1.jpg
  • The Taj Mahal is a white marble mausoleum located in Agra, Uttar Pradesh, India. It was built by Mughal emperor Shah Jahan in memory of his third wife, Mumtaz Mahal. The Taj Mahal is widely recognized as "the jewel of Muslim art in India and one of the universally admired masterpieces of the world's heritage". Taj Mahal is regarded by many as the finest example of Mughal architecture, a style that combines elements from Islamic, Persian, Ottoman Turkish and Indian architectural styles. In 1983, the Taj Mahal became a UNESCO World Heritage Site. While the white domed marble mausoleum is the most familiar component of the Taj Mahal, it is actually an integrated complex of structures. The construction began around 1632 and was completed around 1653, employing thousands of artisans and craftsmen. The construction of the Taj Mahal was entrusted to a board of architects under imperial supervision, including Abd ul-Karim Ma'mur Khan, Makramat Khan, and Ustad Ahmad Lahauri. Lahauri is generally considered to be the principal designer.
    TajMahalMist2.jpg
  • The Taj Mahal is a white marble mausoleum located in Agra, Uttar Pradesh, India. It was built by Mughal emperor Shah Jahan in memory of his third wife, Mumtaz Mahal. The Taj Mahal is widely recognized as "the jewel of Muslim art in India and one of the universally admired masterpieces of the world's heritage". Taj Mahal is regarded by many as the finest example of Mughal architecture, a style that combines elements from Islamic, Persian, Ottoman Turkish and Indian architectural styles. In 1983, the Taj Mahal became a UNESCO World Heritage Site. While the white domed marble mausoleum is the most familiar component of the Taj Mahal, it is actually an integrated complex of structures. The construction began around 1632 and was completed around 1653, employing thousands of artisans and craftsmen. The construction of the Taj Mahal was entrusted to a board of architects under imperial supervision, including Abd ul-Karim Ma'mur Khan, Makramat Khan, and Ustad Ahmad Lahauri. Lahauri is generally considered to be the principal designer.
    TajMahalMist1.jpg
  • Baloon at the Plano Baloon Festival in Plano, Texas
    BlackBaloon.jpg
  • Horse stable and the South and North Sister peaks in Oregon behind it
    SistersStable1.jpg
  • Ranch and the South and North Sister peaks in Oregon behind it
    SistersRanch4.jpg
  • Seattle skyline at dawn on a winter day in February
    SeattleDowntownSunrisePan2.jpg
  • Steptoe Butte is a quartzite island jutting out of the silty loess of the Palouse hills in Whitman County, Washington. It is contained by Steptoe Butte State Park. The rock that forms the butte is over 400 million years old, in contrast with the 15–7 million year old Columbia River basalts that underlie the rest of the Palouse. Steptoe Butte has become an archetype, as isolated protrusions of bedrock, such as summits of hills or mountains, in lava flows have come to be called steptoes.
    PalouseDawn.jpg
  • Seattle skyline at dawn on a winter day in February
    SeattleDowntownSunrisePan2.jpg
  • Moored gondolas at Piazza San Marco in Venice, Italy<br />
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Venice is a city in northeastern Italy sited on a group of 118 small islands separated by canals and linked by bridges. It is located in the marshy Venetian Lagoon which stretches along the shoreline, between the mouths of the Po and the Piave Rivers. Venice is renowned for the beauty of its setting, its architecture and its artworks. The city in its entirety is listed as a World Heritage Site, along with its lagoon. Venice is the capital of the Veneto region. In 2009, there were 270,098 people residing in Venice's comune. Although there are no historical records that deal directly with the founding of Venice, tradition and the available evidence have led several historians to agree that the original population of Venice consisted of refugees from Roman cities near Venice such as Padua, Aquileia, Treviso, Altino and Concordia (modern Portogruaro) and from the undefended countryside, who were fleeing successive waves of Germanic and Hun invasions. Some late Roman sources reveal the existence of fishermen on the islands in the original marshy lagoons. They were referred to as incolae lacunae ("lagoon dwellers"). The traditional founding is identified with the dedication of the first church, that of San Giacomo at the islet of Rialto (Rivoalto, "High Shore"), which is said to have been at the stroke of noon on 25 March 421.
    VeniceStMarksGondolas1.jpg
  • The hilly landscape surrounding the Tuscan town of San Gimignano
    VecchioMannegioSunrise2.jpg
  • Pienza, a town and comune in the province of Siena, in the Val d'Orcia in Tuscany (central Italy), between the towns of Montepulciano and Montalcino, is the "touchstone of Renaissance urbanism"
    PienzaDuomo1.jpg
  • The fountain Fontana del Moro on Rome's Piazza Navona
    RomeNavonaFountain1.jpg
  • Sand dunes at Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles4.jpg
  • The Plaza Mayor is a major public space in the heart of Madrid, the capital of Spain. It was once the centre of Old Madrid. It was first built (1580–1619) during the Habsburg period of Philip III's reign. Only a few Spanish blocks away is another famous plaza, the Puerta del Sol. The Plaza Mayor is for the people of Madrid and tourists to shop, walk around, eat, and enjoy the outdoors. The Plaza Mayor dates back to the 15th century where it was originally called the "Plaza del Arrabal" and was used as the main market of the town. In 1561, the plaza was transferred to the city of Madrid. King Philip II commissioned Classical architect Juan de Herrera to remodel the area. Construction did not begin until Philip III's reign in 1617. Juan Gómez de Mora continued on the architectural renovation, and was finished two years later in 1619. The Plaza Mayor has suffered 3 major fires in its history. The first was in 1631. Juan Gómez de Mora took on the reconstructions of the plaza following this fire. The second of the fires occurred in 1670, with the architect Tomás Román in charge of the reconstruction. The last fire consumed a third of the square and took place in 1790. Today, the Plaza Mayor's architecture is credited to Juan de Villanueva. He handled the reconstruction following the massive fire in 1790. Prior to this, the buildings that enclosed the square were five stories. Juan de Villanueva lowered the square's surrounding buildings to three stories, closed the corners and created large entrances into the squares. Construction after Juan de Villanueva's death by Antonio López Aguado and Custodio Moreno and was finished in 1854.
    MadridPlazaMayor3.jpg
  • The Plaza Mayor is a major public space in the heart of Madrid, the capital of Spain. It was once the centre of Old Madrid. It was first built (1580–1619) during the Habsburg period of Philip III's reign. Only a few Spanish blocks away is another famous plaza, the Puerta del Sol. The Plaza Mayor is for the people of Madrid and tourists to shop, walk around, eat, and enjoy the outdoors. The Plaza Mayor dates back to the 15th century where it was originally called the "Plaza del Arrabal" and was used as the main market of the town. In 1561, the plaza was transferred to the city of Madrid. King Philip II commissioned Classical architect Juan de Herrera to remodel the area. Construction did not begin until Philip III's reign in 1617. Juan Gómez de Mora continued on the architectural renovation, and was finished two years later in 1619. The Plaza Mayor has suffered 3 major fires in its history. The first was in 1631. Juan Gómez de Mora took on the reconstructions of the plaza following this fire. The second of the fires occurred in 1670, with the architect Tomás Román in charge of the reconstruction. The last fire consumed a third of the square and took place in 1790. Today, the Plaza Mayor's architecture is credited to Juan de Villanueva. He handled the reconstruction following the massive fire in 1790. Prior to this, the buildings that enclosed the square were five stories. Juan de Villanueva lowered the square's surrounding buildings to three stories, closed the corners and created large entrances into the squares. Construction after Juan de Villanueva's death by Antonio López Aguado and Custodio Moreno and was finished in 1854.
    MadridPlazaMayor2.jpg
  • Sailboat off the shore of Orcas Island in the San Juan Islands in Washington state
    OrcasSailboat.jpg
  • The Palouse is a region of the northwestern United States, encompassing parts of southeastern Washington, north central Idaho and, in some definitions, extending south into northeast Oregon. It is a major agricultural area, primarily producing wheat and legumes.
    PalousePanorama1.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.
    HamnoyDawn1.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.
    Hamnoy3.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
  • Slickrock ridges at White Pocket
    WhitePocketSunrise1.jpg
  • Rock formations in the White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketTree4.jpg
  • Sunrise at the far end of Hunt's Mesa above Monument Valley, Arizona
    MonumentValleyFirstRays1.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles2.jpg
  • Sand dunes at Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles4.jpg
  • First light at Yei-bi-Chai rocks in Monument Valley
    MonumentValleyYeibicheiSunrise2.jpg
  • First light at Yei-bi-Chai rocks in Monument Valley
    MonumentValleyYeibicheiSunrise3.jpg
  • Canyon with multiple waterfalls in the Southern Region of Iceland
    Sigoldugljufur3.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
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A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
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Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells6.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
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A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
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Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells5.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells4.jpg
  • Canyon with multiple waterfalls in the Southern Region of Iceland
    Sigoldugljufur2.jpg
  • Canyon with multiple waterfalls in the Southern Region of Iceland
    Sigoldugljufur3.jpg
  • Urban buildings in Karlskona, Sweden<br />
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Karlskrona is a locality and the seat of Karlskrona Municipality, Blekinge County, Sweden. It is also the capital of Blekinge County. Karlskrona is known as Sweden's only baroque city and is host to Sweden's only remaining naval base and the headquarters of the Swedish Coast Guard. The city of Karlskrona is spread over 30 islands in the eastern part of Blekinge archipelago, Trossö being the main one; another is Saltö. The islet of Stumholmen was formerly property of the Navy and today it houses the National Naval Museum (Marinmuseum). Outside the city lies the archipelago of Karlskrona, the most southern of the Swedish archipelagos. Several islands are connected to the city by ferries. The city was founded in 1680 when the Royal Swedish Navy was relocated from the Stockholm area to the Trossö island which had up until then been used chiefly for farming and grazing. At the time Sweden was the dominant military power in the Baltic sea region, but needed a better strategic location against Denmark, since southern parts of Sweden had been conquered only a few decades ago (see the Torstenson War). The Swedish fleet tended to get stuck in the ice during winter while located to Stockholm and was therefore moved south. The island had a very strategic position with short sailing distances to the German and Baltic provinces. The city name means Karl's Crown in honour of King Karl XI of Sweden, the name being inspired by the name of the city Landskrona.
    KarlskronaBridge1.jpg
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