Show Navigation
Newest galleries All Galleries
Add to Cart Download

CANADA: Yukon: Whitehorse, Dawson, Klondike Highway

77 images Created 28 Aug 2019

Loading ()...

  • Trapper George Johnston bought his dream car in 1928, a four cylinder Model AB Chevrolet sedan, shipped by steamer from Whitehorse several hundred miles via the Yukon and Teslin Rivers to Teslin village. The local Taylor & Drury store fueled it with naphtha. At first, his only road was 78 miles of frozen Taslin Lake. For his taxi service in Teslin, George Johnston built a 3- to 5-mile road, which later became part of the Alaska Highway. The car is now displayed in the George Johnston Museum, Alaska Highway, Teslin, Yukon, Canada. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez).
    1906AKH-0996.jpg
  • Trapper George Johnston bought his dream car in 1928, a four cylinder Model AB Chevrolet sedan, shipped by steamer from Whitehorse several hundred miles via the Yukon and Teslin Rivers to Teslin village. The local Taylor & Drury store fueled it with naphtha. At first, his only road was 78 miles of frozen Taslin Lake. For his taxi service in Teslin, George Johnston built a 3- to 5-mile road, which later became part of the Alaska Highway. The car is now displayed in the George Johnston Museum, Alaska Highway, Teslin, Yukon, Canada. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez).
    1906AKH-0997.jpg
  • Inland Tlingit ceremonial garments and masks. George Johnston Museum, Alaska Highway, Teslin, Yukon, Canada. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez).
    1906AKH-0998.jpg
  • Animal pelts, locked moose antlers, snowshoes, traps at George Johnston Museum, Alaska Highway, Teslin, Yukon, Canada. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez).
    1906AKH-1016.jpg
  • The view from Miles Canyon Suspension Bridge, near Whitehorse, capital and largest city of the Yukon, Canada. At Miles Canyon and the former Whitehorse Rapids downstream, the Yukon River cuts through 8-million-year-old lava flows, the Miles Canyon Basalts. Salmon pooling above and below the rapids attracted humans who left tools here 2500 years ago, and likely other people arriving 8000-9000 years ago after the retreat of glaciers. These narrow cliffs and rapids also established the upstream terminus for paddle-wheelers during the Klondike Gold Rush, eventually helping establish the City of Whitehorse. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. The town was named for the former Whitehorse Rapids (now drowned by a hydroelectric dam), whose pale-colored glacially silted waters resemble the mane of a white horse. The Yukon River originates in British Columbia and flows into the Bering Sea in Alaska. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1036.jpg
  • Tom hikes along Miles Canyon, near Whitehorse, capital and largest city of the Yukon, Canada. At Miles Canyon and the former Whitehorse Rapids downstream, the Yukon River cuts through 8-million-year-old lava flows, the Miles Canyon Basalts. Salmon pooling above and below the rapids attracted humans who left tools here 2500 years ago, and likely other people arriving 8000-9000 years ago after the retreat of glaciers. These narrow cliffs and rapids also established the upstream terminus for paddle-wheelers during the Klondike Gold Rush, eventually helping establish the City of Whitehorse. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. The town was named for the former Whitehorse Rapids (now drowned by a hydroelectric dam), whose pale-colored glacially silted waters resemble the mane of a white horse. The Yukon River originates in British Columbia and flows into the Bering Sea in Alaska. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1043.jpg
  • Miles Canyon, near Whitehorse, capital and largest city of the Yukon, Canada. At Miles Canyon and the former Whitehorse Rapids downstream, the Yukon River cuts through 8-million-year-old lava flows, the Miles Canyon Basalts. Salmon pooling above and below the rapids attracted humans who left tools here 2500 years ago, and likely other people arriving 8000-9000 years ago after the retreat of glaciers. These narrow cliffs and rapids also established the upstream terminus for paddle-wheelers during the Klondike Gold Rush, eventually helping establish the City of Whitehorse. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. The town was named for the former Whitehorse Rapids (now drowned by a hydroelectric dam), whose pale-colored glacially silted waters resemble the mane of a white horse. The Yukon River originates in British Columbia and flows into the Bering Sea in Alaska. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1050.jpg
  • Miles Canyon Suspension Bridge, near Whitehorse, capital and largest city of the Yukon, Canada. At Miles Canyon and the former Whitehorse Rapids downstream, the Yukon River cuts through 8-million-year-old lava flows, the Miles Canyon Basalts. Salmon pooling above and below the rapids attracted humans who left tools here 2500 years ago, and likely other people arriving 8000-9000 years ago after the retreat of glaciers. These narrow cliffs and rapids also established the upstream terminus for paddle-wheelers during the Klondike Gold Rush, eventually helping establish the City of Whitehorse. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. The town was named for the former Whitehorse Rapids (now drowned by a hydroelectric dam), whose pale-colored glacially silted waters resemble the mane of a white horse. The Yukon River originates in British Columbia and flows into the Bering Sea in Alaska. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002). This image was stitched from multiple overlapping photos.
    1906AKH-1053-p1-Pano.jpg
  • The SS Klondike No. 2 sternwheeler, launched at Whitehorse in 1937, was the largest vessel ever to sail the Canadian portion of the Yukon River. The SS Klondike No 2 moved silver-lead ore, freight, and passengers primarily between Whitehorse and Dawson, until retirement in 1955 ended the era of commercial steamboats in the Yukon. It's now a National Historic Site in Whitehorse, the capital and largest city of Yukon, Canada. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. Whitehorse lies on the Yukon River, which originates in British Columbia, is light-colored from glacial runoff, and meets the Bering Sea in Alaska. Whitehorse was named after the White Horse Rapids for their resemblance to the mane of a white horse, near Miles Canyon, before the river was dammed. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically and popularly called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1066.jpg
  • Bunks. The SS Klondike No. 2 sternwheeler, launched at Whitehorse in 1937, was the largest vessel ever to sail the Canadian portion of the Yukon River. The SS Klondike No 2 moved silver-lead ore, freight, and passengers primarily between Whitehorse and Dawson, until retirement in 1955 ended the era of commercial steamboats in the Yukon. It's now a National Historic Site in Whitehorse, the capital and largest city of Yukon, Canada. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. Whitehorse lies on the Yukon River, which originates in British Columbia, is light-colored from glacial runoff, and meets the Bering Sea in Alaska. Whitehorse was named after the White Horse Rapids for their resemblance to the mane of a white horse, near Miles Canyon, before the river was dammed. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically and popularly called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1084.jpg
  • A coffee pot warms on engine machinery. The SS Klondike No. 2 sternwheeler, launched at Whitehorse in 1937, was the largest vessel ever to sail the Canadian portion of the Yukon River. The SS Klondike No 2 moved silver-lead ore, freight, and passengers primarily between Whitehorse and Dawson, until retirement in 1955 ended the era of commercial steamboats in the Yukon. It's now a National Historic Site in Whitehorse, the capital and largest city of Yukon, Canada. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. Whitehorse lies on the Yukon River, which originates in British Columbia, is light-colored from glacial runoff, and meets the Bering Sea in Alaska. Whitehorse was named after the White Horse Rapids for their resemblance to the mane of a white horse, near Miles Canyon, before the river was dammed. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically and popularly called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1089.jpg
  • Galley. The SS Klondike No. 2 sternwheeler, launched at Whitehorse in 1937, was the largest vessel ever to sail the Canadian portion of the Yukon River. The SS Klondike No 2 moved silver-lead ore, freight, and passengers primarily between Whitehorse and Dawson, until retirement in 1955 ended the era of commercial steamboats in the Yukon. It's now a National Historic Site in Whitehorse, the capital and largest city of Yukon, Canada. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. Whitehorse lies on the Yukon River, which originates in British Columbia, is light-colored from glacial runoff, and meets the Bering Sea in Alaska. Whitehorse was named after the White Horse Rapids for their resemblance to the mane of a white horse, near Miles Canyon, before the river was dammed. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically and popularly called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1094.jpg
  • The SS Klondike No. 2 sternwheeler, launched at Whitehorse in 1937, was the largest vessel ever to sail the Canadian portion of the Yukon River. The SS Klondike No 2 moved silver-lead ore, freight, and passengers primarily between Whitehorse and Dawson, until retirement in 1955 ended the era of commercial steamboats in the Yukon. It's now a National Historic Site in Whitehorse, the capital and largest city of Yukon, Canada. Whitehorse was incorporated in 1950 at kilometer 1426 (Historic Mile 918) on the Alaska Highway. Whitehorse lies on the Yukon River, which originates in British Columbia, is light-colored from glacial runoff, and meets the Bering Sea in Alaska. Whitehorse was named after the White Horse Rapids for their resemblance to the mane of a white horse, near Miles Canyon, before the river was dammed. The name Yukon comes from a Gwich'in phrase meaning white water river. Although historically and popularly called "Yukon Territory", the territory is now officially called "Yukon" (after the federal government's Yukon Act in 2002).
    1906AKH-1107.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
  • The American Scimitar Cat (Homotherium serum) lived in the Yukon and Beringia 80,000–20,000 years ago, and other areas on earth from 4 million–12,000 years ago. (The Scimitar Cat's fangs, or maxillary canine teeth, are shorter than those of the head shown below of a Sabre-toothed Cat, a close relative which has never been found in Beringia.) Yukon Beringia Interpretive Centre, in Whitehorse, capital and largest city of the Yukon, Canada. During the ice ages, Beringia's climate alternated between warm interglacial and cold glacial periods. During glacial periods, sea levels dropped 120 meters, exposing a land bridge that was up to 1000 kilometers (620 miles) wide. Beringia, like most of Siberia and all of North and Northeast China, was a grassland steppe. Fossils found on both sides of the Bering Land Bridge show that since the time of the dinosaurs, it was a major route for the exchange of plants and animals between Asia and North America. Swedish botanist Eric Hultén coined the term Beringia in 1937. Beringia is the land and ocean area bounded on the west by the Lena River in Russia; on the east by the Mackenzie River in Canada; on the north by 72 degrees north latitude in the Chukchi Sea; and on the south by the tip of the Kamchatka Peninsula. It includes the Chukchi Sea, the Bering Sea, the Bering Strait, the Chukchi and Kamchatka Peninsulas in Russia plus Alaska in the United States.
    1906AKH-1125.jpg
  • Jefferson's Ground Sloth (Megalonyx jeffersoni) was endemic to North America from 10 million–11,000 years ago, and became extinct in Yukon 75,000 years ago. Yukon Beringia Interpretive Centre, in Whitehorse, capital and largest city of the Yukon, Canada. During the ice ages, Beringia's climate alternated between warm interglacial and cold glacial periods. During glacial periods, sea levels dropped 120 meters, exposing a land bridge that was up to 1000 kilometers (620 miles) wide. Beringia, like most of Siberia and all of North and Northeast China, was a grassland steppe. Fossils found on both sides of the Bering Land Bridge show that since the time of the dinosaurs, it was a major route for the exchange of plants and animals between Asia and North America. Swedish botanist Eric Hultén coined the term Beringia in 1937. Beringia is the land and ocean area bounded on the west by the Lena River in Russia; on the east by the Mackenzie River in Canada; on the north by 72 degrees north latitude in the Chukchi Sea; and on the south by the tip of the Kamchatka Peninsula. It includes the Chukchi Sea, the Bering Sea, the Bering Strait, the Chukchi and Kamchatka Peninsulas in Russia plus Alaska in the United States.
    1906AKH-1128.jpg
  • Five Finger Rapids on the Yukon River makes a good walking break for drivers along the Klondike Highway north of Carmacks, Yukon, Canada. Four islands divide the river into five narrow channels of which only the eastern is passable. Whitehorse-bound sternwheelers during the Klondike Gold Rush in 1898 had to winch themselves over the 1-2 foot drop until the underwater obstacle was blasted away. These rapids are mentioned in Jack London's novel "The Call of the Wild". In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City. In Alaska, the Highway is marked as Alaska Route 98 (as in "route of 1898"). This image was stitched from multiple overlapping photos.
    1906AKH-1154-Pano.jpg
  • Robert Service Cabin, in Dawson City, Klondike Highway, Yukon, Canada. Robert William Service (1874–1958) was a British-Canadian poet and writer, often called "the Bard of the Yukon". He lived in this rented cabin 1909–1912.
    1906AKH-1169.jpg
  • Jack London's Cabin replica in Dawson City, Yukon, Canada. Jack London (1876–1916) was an American novelist, journalist, and social activist. At age 21, he spent a difficult winter 1897–1898 prospecting for gold from in a rented cabin on the North Fork of Henderson Creek, 120 km south of Dawson City, just prior to the gold rush of 1898. While he didn’t strike it rich, he later turned his Klondike adventures into fame and fortune with legendary short stories and books. His most famous works include "The Call of the Wild" and "White Fang", both set during the Klondike Gold Rush. A pioneer in the world of commercial magazine fiction, he was one of the first writers to become a worldwide celebrity and earn a fortune from writing. He was also an innovator in the genre that would later become known as science fiction. Born as John Griffith Chaney, his last name become London through his mother's remarriage during his first year of life. He began calling himself Jack as a boy. London's cabin, abandoned after the Gold Rush, was re-discovered by trappers in 1936 who noted London's signature on the back wall. Yukon author Dick North organized a search in 1965 and eventually had the cabin dismantled and shipped out. Two replicas were made from the original logs. One is shown here in Dawson City, while the other was re-assembled at Jack London Square in Oakland, California, London's hometown.
    1906AKH-1176.jpg
  • Interior of Jack London's Cabin replica in Dawson City, Yukon, Canada. Jack London (1876–1916) was an American novelist, journalist, and social activist. At age 21, he spent a difficult winter 1897–1898 prospecting for gold from in a rented cabin on the North Fork of Henderson Creek, 120 km south of Dawson City, just prior to the gold rush of 1898. While he didn’t strike it rich, he later turned his Klondike adventures into fame and fortune with legendary short stories and books. His most famous works include "The Call of the Wild" and "White Fang", both set during the Klondike Gold Rush. A pioneer in the world of commercial magazine fiction, he was one of the first writers to become a worldwide celebrity and earn a fortune from writing. He was also an innovator in the genre that would later become known as science fiction. Born as John Griffith Chaney, his last name become London through his mother's remarriage during his first year of life. He began calling himself Jack as a boy. London's cabin, abandoned after the Gold Rush, was re-discovered by trappers in 1936 who noted London's signature on the back wall. Yukon author Dick North organized a search in 1965 and eventually had the cabin dismantled and shipped out. Two replicas were made from the original logs. One is shown here in Dawson City, while the other was re-assembled at Jack London Square in Oakland, California, London's hometown. This image was stitched from multiple overlapping photos.
    1906AKH-1178-p1-Pano.jpg
  • St Andrews Church, 1901, Dawson City, Klondike Highway, Yukon, Canada. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1196.jpg
  • Old wood roof shingles. St Andrews Church, 1901, Dawson City, Klondike Highway, Yukon, Canada. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1208.jpg
  • Dawson City Museum. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1212.jpg
  • Cleopatra statue in Dawson City Museum. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1226.jpg
  • Antique tobacco and cigarette tins in Dawson City Museum, including Prince Albert in a can. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1228.jpg
  • 3rd Avenue Complex, Dawson City: permafrost has wreaked havoc on these three unrestored 1901 buildings, once a hotel, photography studio and hardware store. Heated buildings placed on frozen ground caused footings to sink at different rates into the melting muck. Eventually the town learned to elevate buildings on blocks. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1238.jpg
  • Masonic Temple building. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1245.jpg
  • Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1246.jpg
  • 1900s wood fruit boxes: Tartan, Lincoln, Victoria, Venice Cove, Sunny Heights, and Princess brands. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1255.jpg
  • Old wood siding with badly peeling paint. Dawson City, Yukon, Canada.
    1906AK2-060.jpg
  • A yellowjacket (a yellow and black striped wasp) crawls on old wood siding with badly peeling paint. Dawson City, Yukon, Canada.
    1906AKH-1277.jpg
  • Small green house on wheels. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1279.jpg
  • Preserved historic 1922-1951 sternwheel paddle steamer, SS Keno National Historic Site of Canada, at dry dock along the Yukon River in Dawson City, Yukon, Canada. The vessel was built in 1922 in Whitehorse by the British Yukon Navigation Company, a subsidiary of the White Pass and Yukon Route railway company. It mostly transported silver, zinc and lead ore down the Stewart River from mines in the Mayo district to the confluence of the Yukon and Stewart rivers at Stewart City. It was retired from commercial service in 1951 due to the extension and improvement of the Klondike Highway in the years after World War II. About 250 sternwheelers served the Yukon River and its tributaries. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1284.jpg
  • Despite the suggestive mannequin, the 1898 Flora Dora Hotel was unlikely a brothel. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1287.jpg
  • Preserved historic 1922-1951 sternwheel paddle steamer, SS Keno National Historic Site of Canada, at dry dock along the Yukon River in Dawson City, Yukon, Canada. The vessel was built in 1922 in Whitehorse by the British Yukon Navigation Company, a subsidiary of the White Pass and Yukon Route railway company. It mostly transported silver, zinc and lead ore down the Stewart River from mines in the Mayo district to the confluence of the Yukon and Stewart rivers at Stewart City. It was retired from commercial service in 1951 due to the extension and improvement of the Klondike Highway in the years after World War II. About 250 sternwheelers served the Yukon River and its tributaries. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1291.jpg
  • Preserved historic 1922-1951 sternwheel paddle steamer, SS Keno National Historic Site of Canada, at dry dock along the Yukon River in Dawson City, Yukon, Canada. The vessel was built in 1922 in Whitehorse by the British Yukon Navigation Company, a subsidiary of the White Pass and Yukon Route railway company. It mostly transported silver, zinc and lead ore down the Stewart River from mines in the Mayo district to the confluence of the Yukon and Stewart rivers at Stewart City. It was retired from commercial service in 1951 due to the extension and improvement of the Klondike Highway in the years after World War II. About 250 sternwheelers served the Yukon River and its tributaries. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City. This image was stitched from multiple overlapping photos.
    1906AKH-1302-p1-Pano.jpg
  • Built from 1998-2001, the Klondike Spirit paddlewheeler has offered narrated cruises on the Yukon River since 2007 from Dawson City (www.klondikespirit.com), in Yukon, Canada. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1319.jpg
  • Old rust pattern. Paddlewheel graveyard, Yukon River Campground, Dawson City, Yukon, Canada. Explore the ruins of seven historic paddlewheel boats discarded in the woods along the banks of the Yukon River. Directions: On foot or auto, take the free George Black Ferry to West Dawson and the Top of the World Highway. Turn right into Yukon River campground and park at its northern end. Walk through the yellow gate, turn left, and walk downstream a few minutes to the Paddlewheel graveyard. Please respect this site, which is protected under the Yukon Historic Resources Act. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AK2-062.jpg
  • Old rust pattern. Paddlewheel graveyard, Yukon River Campground, Dawson City, Yukon, Canada. Explore the ruins of seven historic paddlewheel boats discarded in the woods along the banks of the Yukon River. Directions: On foot or auto, take the free George Black Ferry to West Dawson and the Top of the World Highway. Turn right into Yukon River campground and park at its northern end. Walk through the yellow gate, turn left, and walk downstream a few minutes to the Paddlewheel graveyard. Please respect this site, which is protected under the Yukon Historic Resources Act. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AK2-073.jpg
  • Paddlewheel graveyard, Yukon River Campground, Dawson City, Yukon, Canada. Explore the ruins of seven historic paddlewheel boats discarded in the woods along the banks of the Yukon River. Directions: On foot or auto, take the free George Black Ferry to West Dawson and the Top of the World Highway. Turn right into Yukon River campground and park at its northern end. Walk through the yellow gate, turn left, and walk downstream a few minutes to the Paddlewheel graveyard. Please respect this site, which is protected under the Yukon Historic Resources Act. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1363.jpg
  • Paddlewheel graveyard, Yukon River Campground, Dawson City, Yukon, Canada. Explore the ruins of seven historic paddlewheel boats discarded in the woods along the banks of the Yukon River. Directions: On foot or auto, take the free George Black Ferry to West Dawson and the Top of the World Highway. Turn right into Yukon River campground and park at its northern end. Walk through the yellow gate, turn left, and walk downstream a few minutes to the Paddlewheel graveyard. Please respect this site, which is protected under the Yukon Historic Resources Act. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1388.jpg
  • Red fox (Vulpes vulpes), West Dawson, Yukon, Canada. The red fox is one of the most widely distributed members of the order Carnivora, found across the entire Northern Hemisphere from the Arctic Circle to North Africa, North America and Eurasia. It comes in many colorings and sub-species. This versatile animal has colonized many suburban and urban areas.
    1906AKH-1401.jpg
  • Red fox (Vulpes vulpes), West Dawson, Yukon, Canada. The red fox is one of the most widely distributed members of the order Carnivora, found across the entire Northern Hemisphere from the Arctic Circle to North Africa, North America and Eurasia. It comes in many colorings and sub-species. This versatile animal has colonized many suburban and urban areas.
    1906AKH-1403.jpg
  • Red fox (Vulpes vulpes), West Dawson, Yukon, Canada. The red fox is one of the most widely distributed members of the order Carnivora, found across the entire Northern Hemisphere from the Arctic Circle to North Africa, North America and Eurasia. It comes in many colorings and sub-species. This versatile animal has colonized many suburban and urban areas.
    1906AKH-1405.jpg
  • Built from 1998-2001, the Klondike Spirit paddlewheeler has offered narrated cruises on the Yukon River since 2007 from Dawson City (www.klondikespirit.com), in Yukon, Canada. In Yukon, the free George Black Ferry (at right in background of photo) connects Dawson City to West Dawson and the Top of the World Highway, which goes to the Yukon-Alaska border. It is a drive-on/drive-off single deck ferry, operating 24 hours per day in summer. The remote 65-mile Top of the World Highway connects the Klondike Loop from Dawson City with the Taylor Highway (which links Chicken, Eagle and the Alaska Highway). Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1419.jpg
  • In Yukon, Canada, the free George Black Ferry connects Dawson City to West Dawson and the Top of the World Highway, which goes to the Yukon-Alaska border. It is a drive-on/drive-off single deck ferry, operating 24 hours per day in summer. The remote 65-mile Top of the World Highway connects the Klondike Loop from Dawson City with the Taylor Highway (which links Chicken, Eagle and the Alaska Highway). Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AKH-1421.jpg
  • Dredge No. 4, a National Historic Site of Canada, was the largest wooden-hulled dredge in North America. Operating from 1913 until 1959, it recovered 8 metric tones of gold. After nearly 30 years on the Klondike River, it was re-built near the mouth of Bonanza Creek to run for another 18 years before sinking where seen now, along Bonanza Creek Road 13 kilometres (8.1 mi) south of the Klondike Highway near Dawson City, Yukon, Canada. A hydro-electric dam 60 km away powered the massive water pumps, winches, and 72-bucket line to sluice gold from river gravel, 24-7 from late April or early May until late November each season, and sometimes throughout winter. Vast river beds were upended into tailing piles, including 26 homes, as the ongoing Placer Mining Act gave mining rights precedence over surface rights. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City. This image was stitched from multiple overlapping photos.
    1906AKH-1437-p1-Pano.jpg
  • These patterns were eaten by the common aspen leaf miner or aspen serpentine leafminer (Phyllocnistis populiella), a moth larvae of the family Gracillariidae. Kluane National Park and Reserve, Yukon, Canada. Hike Sheep Creek trail (10-15 km with 500-1200 m gain, or 1700-4000 ft) for spectacular views of the Slim's River Valley and surrounding mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge.Kluane National Park and Reserve, Yukon, Canada. Hike Sheep Creek trail (10-15 km with 500-1200 m gain, or 1700-4000 ft) for spectacular views of the Slim's River Valley and surrounding mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge.
    1906AKH-2858.jpg
  • Kluane National Park and Reserve, Yukon, Canada. Hike Sheep Creek trail (10-15 km with 500-1200 m gain, or 1700-4000 ft) for spectacular views of the Slim's River Valley and surrounding mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge.
    1906AKH-2878.jpg
  • Dryas octopetala (also known as mountain avens, white dryas, or white dryad) is an Arctic–alpine flowering plant in the family Rosaceae. Photographed in Kluane National Park and Reserve, Yukon, Canada. This small prostrate evergreen subshrub forms large colonies. Its name octopetala derives from the Greek octo (eight) and petalon (petal). Its eight petals are an unusual number in the Rosaceae family, where five is normal, though flowers with up to 16 petals also occur naturally. Hike Sheep Creek trail (10-15 km with 500-1200 m gain, or 1700-4000 ft) for spectacular views of the Slim's River Valley and surrounding mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge.
    1906AKH-2889.jpg
  • Kluane National Park and Reserve, 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 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. This image was stitched from multiple overlapping photos.
    1906AKH-2903-p1-Pano.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
  • A row of red peaks in Kluane National Park and Reserve, Yukon, Canada. Hike Sheep Creek trail (10-15 km with 500-1200 m gain, or 1700-4000 ft) for spectacular views of the Slim's River Valley and surrounding mountains, plus Kluane Lake seen from Soldier's Summit on Tachal Dahl (Sheep Mountain) Ridge. This image was stitched from multiple overlapping photos.
    1906AKH-2978-p3-Pano.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
  • 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.
    1906AKH-3045.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.
    1906AKH-3051.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
  • 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. This image was stitched from multiple overlapping photos.
    1906AKH-3064-65-Pano.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.
    1906AKH-3071.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.
    1906AKH-3083.jpg
  • "Tourists Crossing" sign shows a bear delightfully chasing a person with camera. Cottonwood RV Park, Kluane Lake, Yukon, Canada.
    1906AKH-3115.jpg
  • Kathleen Lake, near Haines Junction, Kluane National Park & Reserve, Yukon, Canada. This image was stitched from multiple overlapping photos.
    1906AKH-3120-p1-Pano.jpg
  • White Pass (elevation 873 m or 2864 ft) is in the Boundary Ranges of the Coast Mountains on the border of Alaska, USA and the province of British Columbia, Canada. The White Pass Trail (or Dead Horse Trail) was one of the two main passes used by prospectors during the Klondike Gold Rush. It leads from Skagway, Alaska, to the chain of lakes at the headwaters of the Yukon River: Crater Lake, Lake Lindeman, and Bennett Lake.
    1906AKH-5694.jpg
  • White Pass (elevation 873 m or 2864 ft) is in the Boundary Ranges of the Coast Mountains on the border of Alaska, USA and the province of British Columbia, Canada. The White Pass Trail (or Dead Horse Trail) was one of the two main passes used by prospectors during the Klondike Gold Rush. It leads from Skagway, Alaska, to the chain of lakes at the headwaters of the Yukon River: Crater Lake, Lake Lindeman, and Bennett Lake.
    1906AKH-5703.jpg
  • A pond at White Pass reflects mountains of the Boundary Ranges of the Coast Mountains, at Outhouse Hill Pullout on South Klondike Highway, British Columbia, Canada. The White Pass Trail (or Dead Horse Trail) was one of the two main passes used by prospectors during the Klondike Gold Rush. It leads from Skagway, Alaska, to the chain of lakes at the headwaters of the Yukon River: Crater Lake, Lake Lindeman, and Bennett Lake. Skagway was founded in 1897 on the Alaska Panhandle. The 98-mile/158-km South Klondike Highway (Skagway-Carcross Road) connects Skagway over White Pass via British Columbia to the Alaska Highway, in the Yukon southeast of Whitehorse.
    1906AKH-5710.jpg
  • Mountains of the Boundary Ranges of the Coast Mountains rise above Summit Lake at White Pass, at Summit Creek Pullout on South Klondike Highway, in British Columbia, Canada. The White Pass Trail (or Dead Horse Trail) was one of the two main passes used by prospectors during the Klondike Gold Rush. It leads from Skagway, Alaska, to the chain of lakes at the headwaters of the Yukon River: Crater Lake, Lake Lindeman, and Bennett Lake. Skagway was founded in 1897 on the Alaska Panhandle. The 98-mile/158-km South Klondike Highway (Skagway-Carcross Road) connects Skagway over White Pass via British Columbia to the Alaska Highway, in the Yukon southeast of Whitehorse. This image was stitched from multiple overlapping photos.
    1906AKH-5746-p1-Pano.jpg
  • Mountains & trees reflect abstractly in Windy Arm of Tagish Lake, South Klondike Highway, Yukon, Canada.
    1906AKH-5763.jpg
  • Ruins of Venus Silver Mine on Windy Arm of Tagish Lake, Yukon, Canada. The 98-mile/158-km South Klondike Highway (Skagway-Carcross Road) connects Skagway over White Pass via British Columbia to the Alaska Highway in the Yukon southeast of Whitehorse. This image was stitched from multiple overlapping photos.
    1906AKH-5779-p1-Pano.jpg
  • Ruins of Venus Silver Mine on Windy Arm of Tagish Lake, Yukon, Canada. The 98-mile/158-km South Klondike Highway (Skagway-Carcross Road) connects Skagway over White Pass via British Columbia to the Alaska Highway in the Yukon southeast of Whitehorse.
    1906AKH-5796.jpg
  • Ruins of Venus Silver Mine on Windy Arm of Tagish Lake, Yukon, Canada. The 98-mile/158-km South Klondike Highway (Skagway-Carcross Road) connects Skagway over White Pass via British Columbia to the Alaska Highway in the Yukon southeast of Whitehorse.
    1906AKH-5821.jpg
  • Carcross Sand Dunes, Yukon, Canada. Mountainous rain shadow makes this area arid. Although some have called it the "world's smallest desert" (1 square mile of sand dunes), the Carcross Dunes are actually too humid to be a true desert. Its sand comes mainly from nearby Bennett Lake, a former bed of a Pleistocene glacial lake. The exceptionally rare Baikal Sedge grows here (normally found only on the coast of Lake Baikal in Siberia).
    1906AKH-5834.jpg
  • Watson Lake signpost forest, began 1942 in Yukon, Canada. The Sign Post Forest is one of the most famous landmarks along the Alaska Highway. Started by a homesick GI in 1942, the number of signs has snowballed. Private Carl Lindley, serving with the 341st Engineers during World War II, was assigned light duty while recovering from an injury and erected the signpost for his hometown: "Danville, Ill. 2835 miles". Visitors may add their own signs to the over 80,000 already present. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez). This image was stitched from multiple overlapping photos.
    1906AKH-5903-p1-Pano.jpg
  • Watson Lake signpost forest, began 1942 in Yukon, Canada. The Sign Post Forest is one of the most famous landmarks along the Alaska Highway. Started by a homesick GI in 1942, the number of signs has snowballed. Private Carl Lindley, serving with the 341st Engineers during World War II, was assigned light duty while recovering from an injury and erected the signpost for his hometown: "Danville, Ill. 2835 miles". Visitors may add their own signs to the over 80,000 already present. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez).
    1906AKH-5929.jpg
  • Watson Lake signpost forest, began 1942 in Yukon, Canada. The Sign Post Forest is one of the most famous landmarks along the Alaska Highway. Started by a homesick GI in 1942, the number of signs has snowballed. Private Carl Lindley, serving with the 341st Engineers during World War II, was assigned light duty while recovering from an injury and erected the signpost for his hometown: "Danville, Ill. 2835 miles". Visitors may add their own signs to the over 80,000 already present. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez).
    1906AKH-5963.jpg
  • Watson Lake signpost forest, began 1942 in Yukon, Canada. The Sign Post Forest is one of the most famous landmarks along the Alaska Highway. Started by a homesick GI in 1942, the number of signs has snowballed. Private Carl Lindley, serving with the 341st Engineers during World War II, was assigned light duty while recovering from an injury and erected the signpost for his hometown: "Danville, Ill. 2835 miles". Visitors may add their own signs to the over 80,000 already present. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez). This image was stitched from multiple overlapping photos.
    1906AKH-5976-p1-Pano.jpg
  • Watson Lake signpost forest, began 1942 in Yukon, Canada. The Sign Post Forest is one of the most famous landmarks along the Alaska Highway. Started by a homesick GI in 1942, the number of signs has snowballed. Private Carl Lindley, serving with the 341st Engineers during World War II, was assigned light duty while recovering from an injury and erected the signpost for his hometown: "Danville, Ill. 2835 miles". Visitors may add their own signs to the over 80,000 already present. The Alaska Highway was built as a military road during World War II in just 9 months in 1942, to link existing airfields via Canada to the territory of Alaska. The ALCAN Highway (a military acronym for Alaska-Canada) opened to the public in 1948. It begins in Dawson Creek, British Columbia, and runs via Whitehorse, Yukon to Delta Junction, Alaska. The "Alaskan Highway" is comprised of British Columbia Highway 97, Yukon Highway 1 and Alaska Route 2. While the ALCAN measured 2700 kilometers (1700 mi) upon completion in 1942, by 2012 it was rerouted and shortened to 2232 km (1387 mi). Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Delta Junction, at the end of the highway, claims "Historic Milepost 1422" where the Alaska Highway meets the Richardson Highway, which continues 96 mi (155 km) to the city of Fairbanks at Historic Milepost 1520, often (but unofficially) regarded as the northern portion of the Alaska Highway (although its Mileposts are measured from Valdez).
    1906AKH-6002.jpg
  • From May 27-July 3, 2019, we drove our new RV about 6200 miles from Seattle to Denali National Park via Cassiar Highway, Klondike Highway, and Alaska Highway; then looped back via Parks Highway, Glenn Highway, Alaska Highway, Jasper National Park, and Mt Robson.
    1906-AKMap2_Seattle-to-Alaska.jpg
View: 100 | All
  • Facebook
  • Twitter
x

Portfolio of Tom Dempsey / PhotoSeek.com

  • Portfolio
  • BLOG — PhotoSeek HOME
  • ALL IMAGES + captions
    • Worldwide favorites
    • ALL GALLERIES
    • Lightbox
  • SEARCH
  • CART
  • How to buy my images
  • Camera reviews
  • ABOUT