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  • Saint Nicholas Anapafsa Monastery (Agio Nikolaou Anapafsa) was built in the 1500s on a rock pinnacle at Meteora, Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-44-09_Anapafsa-Monastery.jpg
  • Varlaam Monastery was founded on a rock pinnacle in 1517 AD at Meteora, Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-43-27_Varlaam-Monastery.jpg
  • Grand Meteora Monastery (Holy Monastery of Great Meteoron) was built in the mid 1300s on a rock pinnacle in Greece, Europe. It was restored and embellished in 1483 and 1552, and is the largest monastery at Meteora. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-44-10_Grand-Meteora-Monastery.jpg
  • Varlaam Monastery was founded on a rock pinnacle in 1517 AD at Meteora, Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-44-06_Varlaam-Monastery-_rock-...jpg
  • House isolated by lava field in Hawaii Volcanoes National Park, just west of Kalapana, Hawaii, USA. In the background, on Kilauea volcano's south flank, smoke rises from lava flowing from Pu'u O'o crater, which has been erupting continuously since 1983, making it the world's longest-lived rift-zone (flank) eruption of the last 200 years. The eruption has consumed 189 buildings and 8.7 miles of highway. Since 1987, the coastal highway has been closed, buried under lava up to 115 feet thick. After June 30, 2016, the County of Hawaii opened a section of the emergency road/Highway 130 to lava viewing (8 miles round trip, open 3pm-9pm), limiting vehicles to bicycles (rented at the roadblock in Kalapana for $15+ for 3 hours), local residents' cars, and emergency vehicles. See updates at: USGS Hawaiian Volcano Observatory (HVO) http://hvo.wr.usgs.gov and www.hawaiicounty.gov/lava-viewing/. Kilauea is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. This image was stitched from multiple overlapping images.
    1701HAW-2990-91-Pano.jpg
  • A isolated metal door to nowhere remains in a field on historic Maria Island National Park, Tasmania, Australia.
    04AUS-30052_door-to-nowhere_Maria-Is...jpg
  • Two bald eagles perch on a tree branch growing on an isolated sea stack rock, in Tillamook Bay, near Bay City, on the Oregon coast, USA.
    08ORC-639.jpg
  • Horses graze on a ranch preserved in Cades Cove, an isolated valley located in the East Tennessee section of Great Smoky Mountains National Park, USA. Cades Cove was once home to numerous settlers. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife. Cades Cove is a type of valley known as a "limestone window," created by erosion that removed the older Precambrian sandstone, exposing the younger Paleozoic limestone beneath. The weathering of the limestone produced deep, fertile soil, making Cades Cove attractive to early farmers. More weather-resistant formations, such as the Cades sandstone which comprises Rich Mountain to the north and the Elkmont and Thunderhead sandstones which comprise the Smokies crest to the south have surrounded the cove, leaving it relatively isolated within the Great Smokies.
    08TN-2162_Cades-Cove.jpg
  • "Helmets Recommended" for bicyclists sign in Cades Cove, an isolated valley located in the East Tennessee section of Great Smoky Mountains National Park, USA. Cades Cove was once home to numerous settlers. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife. Cades Cove is a type of valley known as a "limestone window," created by erosion that removed the older Precambrian sandstone, exposing the younger Paleozoic limestone beneath. The weathering of the limestone produced deep, fertile soil, making Cades Cove attractive to early farmers. More weather-resistant formations, such as the Cades sandstone which comprises Rich Mountain to the north and the Elkmont and Thunderhead sandstones which comprise the Smokies crest to the south have surrounded the cove, leaving it relatively isolated within the Great Smokies.
    08TN-2164_Bicycle-Helmets-Recommende...jpg
  • 2017 statue of William H. Seward (1801-1872) in Juneau, Alaska, USA. As US Secretary of State, William H. Seward oversaw the Alaska purchase, transferred from the Russian Empire in 1867. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-219.jpg
  • A hat (Xaadas) made of split spruce roots with painted clan crest by late 1800s Haida Gwaii. Alaska State Museum, Juneau. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-164.jpg
  • A dilapidated wood door ages at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2666_Bodie-CA.jpg
  • During the decline of the gold mining town Bodie, a newspaper article illustrates "Home Lessons in the Latest Dances" with a couple doing an extreme waltz bend, tango whirl & twirl, split, and wriggle bend (from the San Francisco Chronicle, February 1, 1914). At the Bodie Museum and Visitor Center, view this and many other curious artifacts of bygone eras. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2595_Bodie-CA.jpg
  • Glass reflecting an abstract pattern of cumulus clouds obscures rows of bottles seen behind. These prominent windows front the finest home in Bodie, owned by James Stuart Cain from the 1890s - 1940s. Bodie is now California's official state gold rush ghost town. Jessie McGath originally built this house for his new wife in 1879, and JS Cain bought it in the 1890s. Cain moved to Bodie when he was 25 and built an empire starting with putting lumber barges on Mono Lake and transporting timber to support mine shafts, stoke boilers for machinery, build & heat buildings, and cook food. Cain eventually took control of the Stamp Mill though court action and went on to be the principal property owner and one of the richest men in town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2562_Bodie-CA.jpg
  • Ancient Puebloan kiva for religious rituals. Casa Rinconada, occupied about AD 1140-1200, is an isolated great kiva (out of four in Chaco Canyon), built 63 feet (19 m) in diameter with a circular inner bench, masonry firebox, masonry vaults, 34 niches, four large pits for seating roof supports, plus an unusual 39-foot (12 m) passage dug underground through sandstone and shale. Chaco Culture National Historical Park hosts the densest and most exceptional concentration of pueblos in the American Southwest and is a UNESCO World Heritage Site. Chaco Canyon is in remote northwestern New Mexico, between Albuquerque and Farmington, USA. From 850 AD to 1250 AD, Chaco Canyon advanced then declined as a major center of culture for the Ancient Pueblo Peoples. Chacoans quarried sandstone blocks and hauled timber from great distances, assembling fifteen major complexes that remained the largest buildings in North America until the 1800s. Climate change may have led to its abandonment, beginning with a 50-year drought starting in 1130.
    1403NM-0672_Casa-Rinconada_Chaco.jpg
  • See Glacier Peak (elevation 10,541 feet) from atop Beckler Peak Trail, 7.4 miles round trip with 2200 feet gain, in Mount Baker-Snoqualmie National Forest, Washington, USA. Glacier Peak, located in Glacier Peak Wilderness, is the most isolated of the five major stratovolcanoes (composite volcanoes) of the Cascade Volcanic Arc in Washington. See vistas of  the town of Skykomish, Skykomish Valley, and Alpine Lakes, Wild Sky, and Henry M. Jackson Wilderness. Directions: Drive US Highway 2 to near Milepost 52, and turn north onto Forest Service Road 6066. Drive 6.6 miles on a gravel road to the Jennifer Dunn Trailhead.
    1208BEC-020_Glacier-Peak.jpg
  • A replica of the original cantilever drive-through barn at Tipton Place, at Cades Cove, an isolated valley located in the East Tennessee section of Great Smoky Mountains National Park, USA. Cades Cove was once home to numerous settlers. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife.
    08TN-2243_Cades-Cove-cantilever-barn.jpg
  • The overhang in cantilever barns provided shelter for animals and farm equipment. Cable Mill Historic Area, Cades Cove, Tennessee. Cades Cove, once home to numerous settlers, is an isolated valley located in Great Smoky Mountains National Park, USA. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife.
    08TN-2224_Cades-Cove.jpg
  • This old barn allows driving through the center in order to more easily transfer hay to the loft. Draft animals and milk cows were fed the hay in the stalls below during winter months. Cable Mill Historic Area, Cades Cove, Tennessee. Cades Cove, once home to numerous settlers, is an isolated valley located in Great Smoky Mountains National Park, USA. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife.
    08TN-2211_Cades-Cove.jpg
  • Hanging Rock State Park, Stokes County, North Carolina, USA.  The eroded quartzite knob called Hanging Rock rises to 2150 feet elevation. The park is 30 miles (48 km) north of Winston-Salem, and approximately 2 miles (3.2 km) from Danbury. Hanging Rock State Park is located in the Sauratown Mountain Range, which is made up of monadnocks (or inselbergs, isolated hills) that are separated from the nearby Blue Ridge Mountains. Prominent peaks in the Sauratown range rise from 1,700 feet (520 m) to more than 2,500 feet (760 m) in elevation and stand in contrast to the surrounding countryside, which averages only 800 feet (240 m) in elevation. Named for the Saura Native Americans who were early inhabitants of the region, the Sauratown Mountains are the erosion-resistant quartzite remnants of mountains pushed up between 250 and 500 million years ago.
    08NC-2177-p1_Hanging-Rock-SP_NC.jpg
  • Look across miles of autumn orange and red foliage at Hanging Rock State Park, Stokes County, North Carolina, USA. The eroded quartzite knob called Hanging Rock rises to 2150 feet elevation. The park is 30 miles (48 km) north of Winston-Salem, and approximately 2 miles (3.2 km) from Danbury. Hanging Rock State Park is located in the Sauratown Mountain Range, which is made up of monadnocks (or inselbergs, isolated hills) that are separated from the nearby Blue Ridge Mountains. Prominent peaks in the Sauratown range rise from 1,700 feet (520 m) to more than 2,500 feet (760 m) in elevation and stand in contrast to the surrounding countryside, which averages only 800 feet (240 m) in elevation. Named for the Saura Native Americans who were early inhabitants of the region, the Sauratown Mountains are the erosion-resistant quartzite remnants of mountains pushed up between 250 and 500 million years ago. Panorama stitched from 2 overlapping photos.
    08NC-2135+2137pan_Hanging-Rock.jpg
  • The White Pass and Yukon Route is a narrow-gauge railroad built in 1900 linking the port of Skagway, Alaska, with Whitehorse, the capital of Yukon in Canada. Recapturing the Gold Rush era, it is the most popular land excursion from Alaska cruises. Isolated from any other railroad system, its equipment, freight and passengers are ferried by ship via the Port of Skagway, and by road at a few stops. It was built 1898-1900 during the Klondike Gold Rush to reach the goldfields, and became the primary route to the interior of the Yukon, replacing the Chilkoot Trail and other routes. The route continued operation until 1982, and in 1988 was partially revived as a heritage railway. Skagway was founded in 1897 on the Alaska Panhandle. Half of Alaska's total visitors come via cruise ships. Klondike Gold Rush National Historical Park commemorates the late 1890s Gold Rush with three units in Municipality of Skagway Borough: Historic Skagway; the White Pass Trail; and Dyea Townsite and Chilkoot Trail. (A fourth unit is in Pioneer Square National Historic District in Seattle, Washington.)
    1906AKH-5670.jpg
  • Lupine flowers in Mendenhall River Greenbelt near Brotherhood Bridge, in Juneau, capital city of Alaska, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-323.jpg
  • The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-306.jpg
  • Nature is reclaiming historic Treadwell Mine, which operated from 1882-1922 in Juneau, Alaska, USA. Walk the intriguing Treadwell Mine Historic Trail 3 miles south of Douglas Bridge next to Savikko Park. Formerly the largest gold mine in the world, this mini-town peaked in the 1880s, but was abandoned after partially sliding into the sea on April 21, 1917, when a massive cave-in flooded three of four underground mines 2300 feet deep, due to an extreme high tide and failure of unstable underground rock pillars. Now, spooky reminders poke through the forest on well-signposted and interpreted trail: the concrete New Office Building; 1917 slide site; "glory hole", and the restored shell of Treadwell pumphouse. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat.
    1906AKH-4900.jpg
  • Treadwell Mine office building dates from 1882-1922, in Juneau, Alaska, USA. Walk the intriguing Treadwell Mine Historic Trail 3 miles south of Douglas Bridge next to Savikko Park. Formerly the largest gold mine in the world, this mini-town peaked in the 1880s, but was abandoned after partially sliding into the sea on April 21, 1917, when a massive cave-in flooded three of four underground mines 2300 feet deep, due to an extreme high tide and failure of unstable underground rock pillars. Now, spooky reminders poke through the forest on well-signposted and interpreted trail: the concrete New Office Building; 1917 slide site; "glory hole", and the restored shell of Treadwell pumphouse. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat.
    1906AKH-4880.jpg
  • See cruise ships in Gastineau Channel from the walkways of Mayor Bill Overstreet Park, Juneau, Alaska, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers. This image was stitched from multiple overlapping photos.
    1906AK2-181-p3-Pano.jpg
  • Nature expert and sculptor R.T. "Skip" Wallen created "Tahku", an impressive 6.5-ton, 25-foot tall breaching humpback whale statue with fountains and lights, completed in 2018 in Overstreet Park along the Seawalk near Juneau-Douglas Bridge, in Juneau, Alaska, USA. Tahku celebrates 50 years of Alaska statehood 1959-2009. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-201.jpg
  • Nature expert and sculptor R.T. "Skip" Wallen created "Tahku", an impressive 6.5-ton, 25-foot tall breaching humpback whale statue with fountains and lights, completed in 2018 in Overstreet Park along the Seawalk near Juneau-Douglas Bridge, in Juneau, Alaska, USA. Tahku celebrates 50 years of Alaska statehood 1959-2009. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-197.jpg
  • Sheet'ka Kwaan Tlingit ceremonial Chilkat robe (naaxein), a diving whale with head down and tail up in center panel in Alaska State Museum, Juneau, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-172.jpg
  • Frog hat (Xixch'i s'aaxw) from Sitka, Kiks.adi Clan, Sheet'ka Kwaan, Tlingit, displayed in Alaska State Museum, Juneau, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-174.jpg
  • Late 1800s bentwood chest by Captain Carpenter (Heiltsuk) of British Columbia, shown in Alaska State Museum, Juneau, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-170.jpg
  • A Tlingit dressed in ceremonial eagle headdress carries a shield-shaped copper plate (Tinaa), symbolizing wealth. The earliest coppers were hammered from raw copper obtained by the Eyak living along the Copper River, and later copper sheeting was traded by Euro-American seafarers who sailed in copper-clad ships. Displayed in the Alaska State Museum, Juneau, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-168.jpg
  • Early 1900s Xeitl X'een (Thunderbird screen) from Thunderbird House, Shangookeidi clan, Yakutat Tlingit. Alaska State Museum, Juneau. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AK2-156.jpg
  • Sealaska Heritage Institute building, Juneau, capital city of Alaska, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AKH-4779.jpg
  • Peaks above Mendenhall Lake at sunset, seen from Auke Lake in Juneau, Alaska, USA. The City and Borough of Juneau is the capital city of Alaska and the second largest city in the USA by area (only Sitka is larger). This unified municipality lies on Gastineau Channel in the Alaskan panhandle. Juneau has been the capital of Alaska since 1906, when the government of what was the District of Alaska was moved from Sitka. The city is named after a gold prospector from Quebec, Joe Juneau. Isolated by rugged terrain on Alaska's mainland, Juneau can only be reached by plane or boat. Downtown Juneau sits at sea level under steep mountains up to 4000 feet high, topped by Juneau Icefield and 30 glaciers.
    1906AKH-3956.jpg
  • Dall sheep (Ovis dalli, or thinhorn sheep) on Tachal Dahl (Sheep Mountain) Ridge, St. Elias Mountains, in Kluane National Park and Reserve, Yukon, Canada. Hike Sheep Creek trail (10-15 km with 500-1200 m gain) for spectacular views of the Slims River Valley and surrounding mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge. In a startling case of global warming, over 4 days in spring 2016, the Slims River suddenly disappeared, leaving windswept mud flats creating clouds of dust in the formerly clear air. With its main water supply cut off, Kluane Lake will be isolated within a few years, shrinking below its outflow into the Kluane River (which flows into the Donjek River, White River, Yukon River, and eventually the Bering Sea). Kluane Lake chemistry and fish populations are rapidly changing. For the last 300 years, abundant meltwater from the Kaskawulsh Glacier has been channeled by ice dam to drain via the 150-meter wide Slims River, north into Kluane Lake. Between 1956 and 2007, the Kaskawulsh glacier retreated by 600-700m, which most scientists attribute to anthropogenic climate change. Meltwater flooding from accelerating retreat in 2016 carved a new channel through a large ice field, diverting all flows to the Kaskawulsh River, a tributary of the Alsek, which flows into the Gulf of Alaska.
    1906AKH-3058.jpg
  • Wind sweeps clouds of dust over Kluane Lake from the A'ay Chu (Slims River Valley), dried since 2016 glacial meltwater diversion, seen from Tachal Dahl (Sheep Mountain) Ridge, St. Elias Mountains, Yukon, Canada. Hike Sheep Creek trail (10-15 km with 500-1200 m gain or 1700-4000 ft) for spectacular views of the Slims River Valley and surrounding St. Elias Mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge. In a startling case of climate change, over 4 days in spring 2016, the Slims River suddenly disappeared, leaving windswept mud flats creating clouds of dust in the formerly clear air. With its main water supply diminished to a trickle, Kluane Lake may become an isolated basin within a few years, shrinking below its outflow into the Kluane River (which flows into the Donjek River, White River, Yukon River, and eventually the Bering Sea). Kluane Lake chemistry and fish populations are rapidly changing. For the last 300 years, abundant meltwater from the Kaskawulsh Glacier has been channeled by ice dam to drain via the 150-meter wide Slims River, north into Kluane Lake. Between 1956 and 2007, the Kaskawulsh glacier retreated by 655m, which most scientists attribute to human-caused climate change. Meltwater flooding from accelerating retreat in 2016 carved a new channel through a large ice field, diverting most flows to the Kaskawulsh River, a tributary of the Alsek, which flows into the Gulf of Alaska. Read more at: https://projects.thestar.com/climate-change-canada/yukon/.
    1906AKH-2990.jpg
  • Wind sweeps clouds of dust over Kluane Lake from the A'ay Chu (Slims River Valley), dried since 2016 glacial meltwater diversion, seen from Tachal Dahl (Sheep Mountain) Ridge, St. Elias Mountains, Yukon, Canada. Hike Sheep Creek trail (10-15 km with 500-1200 m gain or 1700-4000 ft) for spectacular views of the Slims River Valley and surrounding St. Elias Mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge. In a startling case of climate change, over 4 days in spring 2016, the Slims River suddenly disappeared, leaving windswept mud flats creating clouds of dust in the formerly clear air. With its main water supply diminished to a trickle, Kluane Lake may become an isolated basin within a few years, shrinking below its outflow into the Kluane River (which flows into the Donjek River, White River, Yukon River, and eventually the Bering Sea). Kluane Lake chemistry and fish populations are rapidly changing. For the last 300 years, abundant meltwater from the Kaskawulsh Glacier has been channeled by ice dam to drain via the 150-meter wide Slims River, north into Kluane Lake. Between 1956 and 2007, the Kaskawulsh glacier retreated by 655m, which most scientists attribute to human-caused climate change. Meltwater flooding from accelerating retreat in 2016 carved a new channel through a large ice field, diverting most flows to the Kaskawulsh River, a tributary of the Alsek, which flows into the Gulf of Alaska. Read more at: https://projects.thestar.com/climate-change-canada/yukon/. This image was stitched from multiple overlapping photos captured in June 2019 by Tom Dempsey / PhotoSeek.com.
    1906AKH-2973-p1-p1-Pano.jpg
  • Woolly Mammoth skeleton at the Yukon Beringia Interpretive Centre, in Whitehorse, capital and largest city of the Yukon, Canada. An adult woolly mammoth stood over 3 meters tall and consumed 200 kilograms of grass each day. The tusks of an adult bull mammoth could exceed 3.5 metres long and weigh more than 100 kilograms each. Extremely well-preserved remains found frozen in permafrost have revealed the complete sequence of mammoth DNA, including hair colour and blood proteins. Not all mammoths were brunettes. Thick fur, small ears and a short tail helped them minimize heat loss. Woolly mammoths disappeared from Yukon around 12,000 years ago, at the end of the last glacial period, except for an isolated group which survived on an island off northern Siberia until 4000 years ago.
    1906AKH-1113.jpg
  • Dusty, dilapidated living room. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-5190_Bodie-CA.jpg
  • A pattern of overlapping sheets of iron siding rusts at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-5197_Bodie-CA.jpg
  • An old window reflects cumulus clouds at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-5189_Bodie-CA.jpg
  • A worn hat hangs on an old chair in a dilapidated room. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-5188_Bodie-CA.jpg
  • Historic wallpaper. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-5174.jpg
  • An old window reflects cumulus clouds at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-5182_Bodie-CA.jpg
  • Dilapidated window and rusted iron siding at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2529_Bodie-CA.jpg
  • Methodist Church at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2537_Bodie-CA.jpg
  • A big, discarded mining flywheel rusts in a field at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2517_Bodie-CA.jpg
  • Prominent windows front the home of James Stuart Cain, who was eventually the principal property owner in Bodie, which is now California's official state gold rush ghost town. Jessie McGath built this house for his new wife in 1879. In the 1890s, JS Cain bought it to live there with his wife until the 1940s. Cain moved to Bodie when he was 25 and built an empire starting with putting lumber barges on Mono Lake and transporting timber to support mine shafts, stoke boilers for machinery, build & heat buildings, and cook food. Cain and a business partner leased a block of land from the Standard Consolidated Mining Company which yielded $90,000 in gold in just 90 days. Cain eventually took control of the Stamp Mill though court action and went on to be one of the richest men in town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2766_Bodie-CA.jpg
  • Glass reflecting blue sky obscures rows of bottles seen behind. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2767_Bodie-CA.jpg
  • Behind glass reflecting Bodie ghost town is a dress form in Boone Store and Warehouse (built 1879). This building was owned by Harvey Boone (a direct descendent of Daniel Boone), who may have owned a business longer than anyone else in town. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2757_Bodie-CA.jpg
  • A billiard table collects dust in the Wheaton & Hollis Hotel at Bodie, California's official state gold rush ghost town. In 1885-86, this building served as the United States Land Office. Later, it was the office for the Power Company, then the Bodie Store, and finally the Hotel. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2744_Bodie-CA.jpg
  • A reflection of wood siding obscures clothes hung in a bedroom within an old house at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2735_Bodie-CA.jpg
  • An old yellowed wooden globe has lost its maps, in Bodie Schoolhouse (which was originally the 1879 Bon Ton Lodging House). Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2742_Bodie-CA.jpg
  • Ramshackle wood door. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2732_Bodie-CA.jpg
  • Ramshackle houses line Green Street in Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2714-p1_Bodie-CA.jpg
  • Dilapidated wood and iron siding ages at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2691_Bodie-CA.jpg
  • Dilapidated wood and iron siding ages at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2694_Bodie-CA.jpg
  • Dilapidated doors and interior of a ramshackle building at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2667_Bodie-CA.jpg
  • Orange-yellow mine tailings cover the hillside above a ramshackle cabin at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold and silver ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962. This panorama was stitched from 5 overlapping photos.
    1507CAL-2682_Bodie-CA.jpg
  • The Standard Stamp Mill and associated buildings are preserved at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. In the 1870s, the Bunker Hill Mine, later renamed the Standard Mining Company, made a rich strike of gold and silver ore yielding nearly $15 million over the next 25 years. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2663_Bodie-CA.jpg
  • See a model excavator and textbooks through the window of Bodie Schoolhouse (which was originally the 1879 Bon Ton Lodging House). Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2653_Bodie-CA.jpg
  • Tall grass reclaims ramshackle outhouses at Bodie gold mining ghost town 1859-1942, California, USA. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2650_Bodie-CA.jpg
  • Tall grass reclaims ramshackle outhouses at Bodie gold mining ghost town 1859-1942, California, USA. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2649_Bodie-CA.jpg
  • A reflection of wood siding obscures clothes hung in a bedroom within an old house at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2628_Bodie-CA.jpg
  • Dusty, dilapidated living room. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2631_Bodie-CA.jpg
  • Bodie ghost town buildings reflect in a window fronting the Wheaton and Hollis Hotel. A sign visible indoors reads "Bodie Hotel -- Meals at all Hours". In 1885-86, this building served as the United States Land Office. Later, it was the office for the Power Company, then the Bodie Store, and finally the Hotel. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2638_Bodie-CA.jpg
  • 1927 Dodge Graham blue truck at antique gas station in Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2625_Bodie-CA.jpg
  • The gray-metal-sided Standard Stamp Mill is preserved at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. In the 1870s, the Bunker Hill Mine, later renamed the Standard Mining Company, made a rich strike of gold and silver ore yielding nearly $15 million in 25 years. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2626_Bodie-CA.jpg
  • 1927 Dodge Graham blue truck at antique gas station in Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2624_Bodie-CA.jpg
  • Rusty iron siding frames a window & door at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2615_Bodie-CA.jpg
  • Java coffee artifact, in Boone Store and Warehouse built 1879 in Bodie, California's official state gold rush ghost town. This building was owned by Harvey Boone (a direct descendent of Daniel Boone), who may have owned a business longer than anyone else in town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2623_Bodie-CA.jpg
  • An historic ore wagon decays outside of the Miner's Union Hall, at the corner of Green Street and Main Street in Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2613_Bodie-CA.jpg
  • An historic glass hearse (funeral carriage) is displayed in the Miners Union Hall (which has been turned into the park's Museum & Visitor Center) at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2597_Bodie-CA.jpg
  • Rustic wagon. Bodie is California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2585_Bodie-CA.jpg
  • Bottles collect dust on a bar counter in Dechambeau Hotel at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2589_Bodie-CA.jpg
  • Glass reflecting an abstract pattern of cumulus clouds obscures rows of bottles seen behind. These prominent windows front the finest home in Bodie, owned by James Stuart Cain from the 1890s - 1940s. Bodie is now California's official state gold rush ghost town. Jessie McGath originally built this house for his new wife in 1879, and JS Cain bought it in the 1890s. Cain moved to Bodie when he was 25 and built an empire starting with putting lumber barges on Mono Lake and transporting timber to support mine shafts, stoke boilers for machinery, build & heat buildings, and cook food. Cain eventually took control of the Stamp Mill though court action and went on to be the principal property owner and one of the richest men in town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962. This image was stitched from two photos to increase pixel count and potential print size.
    1507CAL-2563-64pan_Bodie-CA.jpg
  • Prominent windows front the finest home in Bodie, owned by James Stuart Cain from the 1890s - 1940s. Bodie is now California's official state gold rush ghost town. Jessie McGath originally built this house for his new wife in 1879, and JS Cain bought it in the 1890s. Cain moved to Bodie when he was 25 and built an empire starting with putting lumber barges on Mono Lake and transporting timber to support mine shafts, stoke boilers for machinery, build & heat buildings, and cook food. Cain eventually took control of the Stamp Mill though court action and went on to be the principal property owner and one of the richest men in town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2566_Bodie-CA.jpg
  • A window distorts a reflection of an old wagon at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2583_Bodie-CA.jpg
  • Old organ in Methodist Church at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2540_Bodie-CA.jpg
  • An old window reflects the Methodist Church steeple at Bodie, California's official state gold rush ghost town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    1507CAL-2544_Bodie-CA.jpg
  • Casa Rinconada, occupied about AD 1140-1200, is an isolated great kiva (out of four in Chaco Canyon), built 63 feet (19 m) in diameter with a circular inner bench, masonry firebox, masonry vaults, 34 niches, four large pits for seating roof supports, plus an unusual 39-foot (12 m) passage dug underground through sandstone and shale. Chaco Culture National Historical Park hosts the densest and most exceptional concentration of pueblos in the American Southwest and is a UNESCO World Heritage Site. Chaco Canyon is in remote northwestern New Mexico, between Albuquerque and Farmington, USA. From 850 AD to 1250 AD, Chaco Canyon advanced then declined as a major center of culture for the Ancient Pueblo Peoples. Chacoans quarried sandstone blocks and hauled timber from great distances, assembling fifteen major complexes that remained the largest buildings in North America until the 1800s. Climate change may have led to its abandonment, beginning with a 50-year drought starting in 1130. This panorama was stitched from 13 overlapping photos.
    1403NM-0701-713pan_Casa-Rinconada_Ch...jpg
  • Casa Rinconada, occupied about AD 1140-1200, is an isolated great kiva (out of four in Chaco Canyon), built 63 feet (19 m) in diameter with a circular inner bench, masonry firebox, masonry vaults, 34 niches, four large pits for seating roof supports, plus an unusual 39-foot (12 m) passage dug underground through sandstone and shale. Chaco Culture National Historical Park hosts the densest and most exceptional concentration of pueblos in the American Southwest and is a UNESCO World Heritage Site. Chaco Canyon is in remote northwestern New Mexico, between Albuquerque and Farmington, USA. From 850 AD to 1250 AD, Chaco Canyon advanced then declined as a major center of culture for the Ancient Pueblo Peoples. Chacoans quarried sandstone blocks and hauled timber from great distances, assembling fifteen major complexes that remained the largest buildings in North America until the 1800s. Climate change may have led to its abandonment, beginning with a 50-year drought starting in 1130. This panorama was stitched from 5 overlapping photos.
    1403NM-0692-698pan_Casa-Rinconada_Ch...jpg
  • T-shaped passage into ancient stone kiva. Casa Rinconada, occupied about AD 1140-1200, is an isolated great kiva (out of four in Chaco Canyon), built 63 feet (19 m) in diameter with a circular inner bench, masonry firebox, masonry vaults, 34 niches, four large pits for seating roof supports, plus an unusual 39-foot (12 m) passage dug underground through sandstone and shale. Chaco Culture National Historical Park hosts the densest and most exceptional concentration of pueblos in the American Southwest and is a UNESCO World Heritage Site. Chaco Canyon is in remote northwestern New Mexico, between Albuquerque and Farmington, USA. From 850 AD to 1250 AD, Chaco Canyon advanced then declined as a major center of culture for the Ancient Pueblo Peoples. Chacoans quarried sandstone blocks and hauled timber from great distances, assembling fifteen major complexes that remained the largest buildings in North America until the 1800s. Climate change may have led to its abandonment, beginning with a 50-year drought starting in 1130.
    1403NM-0690_Casa-Rinconada_Chaco.jpg
  • The Pacific Ocean erodes sea stacks from the rocky coast at Cleone, north of Mendocino, California, USA. A lone house sits on an isolated headland above pounding surf.
    1212CA-3142.jpg
  • The weird rock spires of Meteora rise above the village of Kastraki, near Kalambaka, in central Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-43-22_Kastraki-village-weird-r...jpg
  • Fantastic rock spires of Meteora rise above a blue house with red tile roof in Kastraki, near Kalambaka, in central Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    01GRE-41-35_Blue-house-Meteora-pinna...jpg
  • Fantastic rock spires of Meteora rise above a house in Kastraki, near Kalambaka, in central Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-41-23_house_rock-towers-Meteor...jpg
  • Fantastic rock spires of Meteora rise above Kastraki, near Kalambaka, in central Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-41-16_rock-formations-Meteora.jpg
  • Roussanou Monastery (Holy Monastery of St. Barbara) was founded in 1545 AD and now hosts a Greek Orthodox Convent at Meteora, Greece, Europe. Meteora (which means "suspended in the air") is a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-44-19_Roussanou-Monastery-rock...jpg
  • Varlaam Monastery was founded on a rock pinnacle in 1517 AD at Meteora, Greece, Europe. Meteora (which means "suspended in the air") a complex of six Eastern Orthodox Christian monasteries built by medieval monks on natural rock pillars near Kalambaka, in central Greece, Europe. The sandstone and conglomerate of Meteora were formed in the cone of a river delta estuary emerging into a sea about 60 million years ago, then later uplifted and eroded into pinnacles. The isolated monasteries of Meteora helped keep alive Greek Orthodox religious traditions and Hellenic culture during the turbulent Middle Ages and Ottoman Turk occupation of Greece (1453-1829). UNESCO honored Meteora as a World Heritage Site in 1988. Visit early in the morning and in the off season to avoid crowds.
    01GRE-43-36_Varlaam-Monastery-Meteor...jpg
  • A Common Wombat (Vombatus ursinus) is shown at Bonorong Wildlife Park, Briggs Road, Brighton, Tasmania, Australia. Wombats are burrowing grass eaters, and can be thought of as the marsupial ecological equivalent of a bear. Wombats are found in forested, mountainous, and heathland areas of southeast Australia including Tasmania, plus an isolated group in Epping Forest National Park in central Queensland. The three living species of wombats are marsupial mammals in the Vombatidae family. They dig extensive burrow systems with rodent-like front teeth and powerful claws. Their unusual backwards-facing pouch avoids gathering dirt onto its young. Although mainly crepuscular and nocturnal, wombats also venture out to feed on cool or overcast days. Wombats are herbivores, mostly eating grasses, sedges, herbs, bark and roots.
    04AUS-30203_Wombat_Bonorong-WP.jpg
  • Trees frame a romantic church isolated on a lake island. The town of Bled and glacial formed Lake Bled (Slovene: Blejsko jezero) are popular tourist sites in the Julian Alps in northwestern Slovenia. The lake surrounds Bled Island (Blejski otok, the only natural island in Slovenia), upon which stands the Pilgrimage Church of the Assumption of Mary (Slovenian: Cerkev Marijinega vnebovzetja), built in the 15th century and now popular for romantic weddings. Lake Bled hosted the World Rowing Championships in 1966, 1979, 1989, and 2011.The lake is 35 kilometers from Ljubljana International Airport.
    11SLO-9261.jpg
  • Trees frame a romantic church isolated on a lake island. The town of Bled and glacial formed Lake Bled (Slovene: Blejsko jezero) are popular tourist sites in the Julian Alps in northwestern Slovenia. The lake surrounds Bled Island (Blejski otok, the only natural island in Slovenia), upon which stands the Pilgrimage Church of the Assumption of Mary (Slovenian: Cerkev Marijinega vnebovzetja), built in the 15th century and now popular for romantic weddings. Lake Bled hosted the World Rowing Championships in 1966, 1979, 1989, and 2011.The lake is 35 kilometers from Ljubljana International Airport.
    11SLO-9257.jpg
  • Nailed wood siding warps and weathers to a brown patina in Bodie State Historic Park. Bodie is California's official state gold rush ghost town. It lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, CA, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962.
    96CAL-09-32_weathered-wood-siding_Bo...jpg
  • A replica of the original cantilever barn at Tipton Place, at Cades Cove, an isolated valley located in the East Tennessee section of Great Smoky Mountains National Park, USA. Cades Cove was once home to numerous settlers. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife.
    08TN-2241_Cades-Cove-cantilever-barn.jpg
  • A modern barn at Cades Cove, an isolated valley located in the East Tennessee section of Great Smoky Mountains National Park, USA. Cades Cove was once home to numerous settlers. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife.
    08TN-2238_Cades-Cove.jpg
  • A modern barn at Cades Cove, an isolated valley located in the East Tennessee section of Great Smoky Mountains National Park, USA. Cades Cove was once home to numerous settlers. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife.
    08TN-2236_Cades-Cove.jpg
  • Old farm equipment at Cable Mill Historic Area, Cades Cove, Tennessee. Cades Cove, once home to numerous settlers, is an isolated valley located in Great Smoky Mountains National Park, USA. Today Cades Cove is the most popular destination for visitors to the park, attracting over two million visitors a year, due to its well preserved homesteads, scenic mountain views, and abundant display of wildlife.
    08TN-2228_Cades-Cove.jpg
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