Old Crow, Yukon

Flying to the Yukon is as easy as any other major travel destination. Once in the Yukon you can camp under the midnight sun. Fish at a four-star lodge. Float the Yukon River. Mush a dog team. Enjoy world class musicians and artisans. Relax on the deck of a secluded log cabin. Catch the gambling nightlife in Dawson City. Whatever your Yukon dream, our site will provide you with the information, tips and ideas that will help make it a reality. With multiple trip options, you can make your Alaskan journey your own and ensure you return home with unique personal memories that will last a lifetime.

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No new mining; closed. TMAC has now reached commercial production in Transportation[ edit ] Northern Transportation Company Limited , owned by Norterra, a holding company that was, until April 1, , jointly owned by the Inuvialuit of the Northwest Territories and the Inuit of Nunavut.

Gold Run tephra has been found at Thistle Creek, Sixtymile River, and the Klondike goldfields of west-central Yukon, Canada. It is a hornblende-bearing rhyolitic tephra with thicknesses of up to 10 cm at each site, suggesting a widespread distribution across interior Alaska and the Yukon Territory, given the long distance to the nearest volcanic centre.

From to Designation Level: Municipal in Whitehorse The Log Skyscrapers are a municipally designated site consisting of two multi-storied log buildings and single lot at Lambert Street in downtown Whitehorse, Yukon Construction Period: Municipal Log Skyscraper One, Log Skyscraper Two and lot are municipally designated for their historic and architectural significance. The Log Skyscrapers are associated with events during and immediately after World War Two, when Yukon transportation systems were being redeveloped and the City of Whitehorse was quickly growing to become the capital city.

During the war, a large influx of military personnel and construction workers arrived to work on three major construction projects; the Alaska Highway, the North West Staging Route airports and the Canol Pipeline. Builder Martin Berrigan responded to the need in by constructing the Log Skyscrapers, the first privately built multiple-dwelling rental accommodation in Whitehorse.

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Most of the grid power is hydroelectric power through the north-south grid from dams near Mayo , Whitehorse and Aishihik Lake. After the local hydroelectric power plant for the gold dredges was shut down in , YEC provided electrical power from local diesel generators. In YEC connected Dawson to its grid system.

Since then the diesel generators function as a backup to the grid. The area’s creeks were quickly staked and most of the thousands who arrived in the spring of for the Klondike Gold Rush found that there was very little opportunity to benefit directly from gold mining. Many instead became entrepreneurs to provide services to miners.

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See Article History Canadian territorial flag that is a vertically striped tricolour of green, white, and blue, with the Yukon coat of arms and floral emblem in the centre. The flag was adopted by the Territorial Council in In heraldry , a pale is a central vertical stripe on a shield, normally covering one-third or less of the area. The central emblem is the official Yukon coat of arms, which was granted to the territory on February 24, , by royal warrant.

This coat of arms was designed by Commander Alan B. Beddoe, whereas the flag was the concept of Mr. Lynn Lambert, a student at Haines Junction. The crest in the coat of arms features a Malamute dog, which was widely used in the opening of the mineral-rich Yukon territory to European habitation. The wavy vertical stripe on the shield stands for the Yukon River , the red triangles suggest mountains, and the gold disks refer to gold and other minerals.

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Radiocarbon dates reveal that Lupinus arcticus plants were grown from modern not Pleistocene seeds New Phytologist, In , Porsild et al. These seeds were recovered from an ancient rodent burrow in frozen silt Five modern and four fossil samples from arctic ground squirrel caches and nests provide information on late Pleistocene vegetation in Eastern Beringia. Modern arctic ground squirrel caches from Alaska’s arctic tundra were dominated by willow and grass leaves and grass seeds and bearberries, which were widespread in the local vegetation as confirmed by vegetation surveys.

Late Pleistocene caches from Interior Alaska were primarily composed of steppe and dry tundra graminoid and herb seeds. Graminoid cuticle analysis of fossil leaves identified Calamagrostis canadensis, Koeleria sp.

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History[ edit ] A large number of apparently human modified animal bones have been discovered in the Old Crow area, notably at Bluefish Caves , located near the shores of the Arctic Ocean, that have been dated to 25, , years ago by carbon dating , several thousand years earlier than generally accepted human habitation of North America. The town was named after him. The people of Old Crow are dependent on the Porcupine caribou herd for food and clothing. Many citizens of Old Crow believe the herd is being seriously threatened by oil-drilling in the ANWR and have been heavily involved in lobbying to prevent it.

Transportation[ edit ] Old Crow Airport provides year-round transportation to other communities. During winter time, a temporary winter road is sometimes built to transport freight into Old Crow; it is not annual, but only when a significant need arises such as a major building project.

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Sulphide mineralogy in unoxidized mantos, Fe-silicate alteration zones and in veins and stockwork consists mainly of pyrrhotite, pyrite, arsenopyrite, marcasite, and chalcopyrite. Minor amounts of native bismuth are present in all ore types. Gangue minerals are mainly carbonates calcite and ankerite , and quartz. Additionally, Fe-silicate alteration zones have locally abundant magnetite and Fe-amphibole. The area was affected by two episodes of folding, followed by two of faulting.

All units exposed in the area are affected by the deformation. The two phases of folds have coincident, E-W-trending axes, and are distinguished on the basis of their vergence and nature of the axial planar foliation.

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Although considerable debate still occurs amongst scientists about when the first people arrived in North America, current scientific conscensus places their arrival around 15, years ago. Several lines of evidence have helped scientists reach this conclusion. Some of the best sources of evidence are the similarities in DNA and blood types of aboriginal people across the Americas and people in Asia. The earliest evidence of people in the Arctic region dates to around 35, years ago at the Yana River Site in northern Siberia during a relatively warm period of the Ice Age.

Small groups of people slowly made their way across Eurasia into Beringia and North America around 15, years ago.

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Buried in the cave deposits are the bones of long-gone animals, some with marks made by stone tools wielded by possibly North America’s earliest humans. The Bluefish Caves contain some of the oldest, undisturbed archaeological evidence in Canada that points to the earliest traces of human migration across the Beringia land mass. The Bluefish Caves lie in a region that was part of the dry land mass that is now mostly underwater. Excavations of the caves by archaeologists from to produced some large animal bones with butchering marks that may have been made with stone tools.

This conclusion led to great controversy in the archaeological community, primarily because there was no evidence of similar sites in the region. And there were also concerns over the striations and anthropogenic signature on the bone evidence that yielded the dates. The bulk of archaeological evidence suggests that the first peopling of North America occurred ca.

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