Tanquary Fiord


Tanquary Fiord is a fjord on the north coast of the Arctic Archipelago's Ellesmere Island, Nunavut, Canada. It is located in the Quttinirpaaq National Park and extends in a north-westerly direction from Greely Fiord.

History

methods suggest that between 10,000 and 4,100 BP, occurred, followed by a period of glacial readvance and the formation of ice shelves until 2,400 BP. Until 1,400 BP, a period of glacial retreat occurred, and since then glacial readvance and nearby ice rises have marked the area.
Radiocarbon analysis of charcoal undertaken by the Geological Survey of Canada has shown that Inuit were present at Tanquary Fiord around 1070 BP at the latest.

Geography

The head of the Tanquary Fiord is the convergence point of four river valleys, three of which end in a floodplain and one in a river delta. Carbon dating findings show that the fjord was free of glacial ice approximately 6,500 years ago. In the past 40 years, the terminal points of side glaciers have receded.
Tanquary Fiord has 65 frost-free days per year, which is remarkable for its latitude. Summer temperatures of have been recorded.

Human activity

In 1963, the Defence Research Board began 'Operation Tanquary' in the area, with a focus on oceanography. The operation concluded in 1972. As the fjord is in a remote location, there is little human habitation. A Warden Station is staffed by Parks Canada during the summer months, and Tanquary Fiord Airport is located nearby. It is possible to reach the area via charter aircraft, or increasingly, via icebreaker cruise ships. In 1947, a meteorological station was installed at Eureka, about southwest of the fiord.