Peak Island (Nunavut)

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Peak Island
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Peak Island
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Peak Island
Geography
Location Frobisher Bay
Coordinates 63°23′00″N67°53′00″W / 63.38333°N 67.88333°W / 63.38333; -67.88333 (Peak Island) Coordinates: 63°23′00″N67°53′00″W / 63.38333°N 67.88333°W / 63.38333; -67.88333 (Peak Island)
Archipelago Arctic Archipelago
Administration
Canada
Nunavut Nunavut
Region Qikiqtaaluk
Demographics
PopulationUninhabited

Peak Island is one of the many uninhabited Canadian arctic islands in Qikiqtaaluk Region, Nunavut. It is a Baffin Island offshore island located in Frobisher Bay, southeast of Iqaluit. It is just east of the larger Culbertson Island. Other islands in the immediate vicinity include Low Island, Mark Island, McAllister Island, and Precipice Island. [1]

Related Research Articles

Topographic prominence Vertical measurement of the independence of a summit

In topography, prominence measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's key col is a unique point on this contour line and the parent peak is some higher mountain, selected according to various criteria.

Dobrudzha Glacier Glacier in Antarctica

Dobrudzha Glacier is situated on the southeast side of Tangra Mountains, Burgas Peninsula, eastern Livingston Island in the South Shetland Islands, northeast of Magura Glacier, southeast of Iskar Glacier and southwest of Ropotamo Glacier. It is bounded by Ruse Peak and Asen Peak to the north and by Kuber Peak to the west and flows southeastward into Bransfield Strait. The glacier is named after the Dobrudzha region in northeastern Bulgaria.

Kaliakra Glacier Glacier in Antarctica

Kaliakra Glacier is a glacier in northeastern Livingston Island, Antarctica extending 3.8 nautical miles in east-west direction and 4.3 nautical miles in north-south direction, and situated southeast of Saedinenie Snowfield, southwest of Panega Glacier, north of Struma Glacier and upper Huron Glacier, and northeast of Perunika Glacier. It is bounded by Melnik Ridge and Bowles Ridge to the south, by Hemus Peak, Gurev Gap, Gleaner Heights, Elhovo Gap, Leslie Hill, Leslie Gap and Radnevo Peak to the west, and Miziya Peak and Samuel Peak to the north. The glacier drains eastwards into Moon Bay south of Perperek Knoll and north of Sindel Point.

Magura Glacier Glacier in Antarctica

Magura Glacier on the southeast side of Tangra Mountains on Livingston Island in the South Shetland Islands, Antarctica is located to the north of M'Kean Point, northeast of Srebarna Glacier, south of Iskar Glacier and southwest of Dobrudzha Glacier. It is bounded by Great Needle Peak to the west, Vitosha Saddle, Vihren Peak and Helmet Peak to the northwest, Plovdiv Peak and Shishman Peak to the north, and Devin Saddle and Kuber Peak to the northeast. The glacier extends 3.5 km in southwest-northeast direction and 1.9 km in northwest-southeast direction, and flows southeastward into Bransfield Strait.

Musala Glacier Glacier located in Antarctica

Musala Glacier on Greenwich Island in the South Shetland Islands, Antarctica is situated northeast of Targovishte Glacier, east-northeast of Zheravna Glacier and southeast of Fuerza Aérea Glacier. It is bounded by St. Kiprian Peak to the south, Vratsa Peak to the southwest, central Breznik Heights to the west, and Ilarion Ridge bordering Hardy Cove to the northeast, extends 2 nautical miles in east-west direction and 1.2 nautical miles in north-south direction, and drains eastwards into Bransfield Strait north of Fort Point.

Prespa Glacier

Prespa Glacier on Rozhen Peninsula, Livingston Island in the South Shetland Islands, Antarctica is situated east-northeast of Tarnovo Ice Piedmont, east of the head of Charity Glacier, southeast of Ruen Icefall and southwest of Macy Glacier. It is bounded to the east by Needle Peak and Ludogorie Peak, to the northwest by St. Cyril Peak and St. Methodius Peak, and to the southwest by Shumen Peak and Yambol Peak, and flows southeastward into Bransfield Strait between Gela Point and Samuel Point. The feature extends 3.5 km in east-west direction and 2.5 km in north-south direction. The glacier is named after Prespa Peak in the Rhodope Mountains, Bulgaria.

Strandzha Glacier Glacier in Antarctica

Strandzha Glacier is located on Burgas Peninsula, eastern Livingston Island in the South Shetland Islands, Antarctica northeast of Ropotamo Glacier, south of Sopot Ice Piedmont and southwest of Pautalia Glacier. It is bounded by Delchev Peak to the west, Spartacus Peak, Trigrad Gap and Yavorov Peak to the northwest, and by Elena Peak to the north, extends 1.6 km in northeast-southwest direction and 800 m in northwest-southeast direction, and flows southeastward into Bransfield Strait.

Targovishte Glacier Glacier in Antarctica

Targovishte Glacier is situated in Breznik Heights on Greenwich Island in the South Shetland Islands, Antarctica, east of Zheravna Glacier and southwest of Musala Glacier. It is bounded by Viskyar Ridge to the west, Vratsa Peak to the northeast, and Drangov Peak and Ziezi Peak to the east, extending 700 m in east-west direction and 1.6 km in north-south direction, and draining southwards into Bransfield Strait northeast of Sartorius Point.

Ultra-prominent peak Mountain summit with a topographic prominence of 1,500 metres (4,900 ft) or more

An ultra-prominent peak, or Ultra for short, is a mountain summit with a topographic prominence of 1,500 metres (4,900 ft) or more; it is also called a P1500. The prominence of a peak is the minimum height of climb to the summit on any route from a higher peak, or from sea level if there is no higher peak. There are approximately 1,524 such peaks on Earth. Some well-known peaks, such as the Matterhorn and Eiger, are not Ultras because they are connected to higher mountains by high cols and therefore do not achieve enough topographic prominence.

Topographic isolation Topography measuring minimum distance to a point of equal elevation

The topographic isolation of a summit is the minimum distance to a point of equal elevation, representing a radius of dominance in which the peak is the highest point. It can be calculated for small hills and islands as well as for major mountain peaks and can even be calculated for submarine summits.

Chuprene Glacier Glacier in Antarctica

Chuprene Glacier is a 2.1 nautical miles long glacier draining the northwest slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Bistra Glacier, southwest of Yablanitsa Glacier and northwest of Krivodol Glacier, Pashuk Glacier and Rupite Glacier, and flows southwest of Drinov Peak and Popovo Saddle, and west of Slatina Peak and Varshets Saddle southwestward along the northwest slopes of Antim Peak and Evlogi Peak into Drake Passage south of Villagra Point and north of Garmen Point. Bulgarian early mapping in 2009. The glacier is named after the settlement of Chuprene in northwestern Bulgaria.

Mountains are listed according to various criteria:

Kennedy Island Conservancy

Kennedy Island Conservancy protects all 4,970 hectares of Kennedy Island in British Columbia, Canada. The island contains many cultural modified trees and other cultural values and is a gathering location for First Nations travelling upon the Skeena River.

References

  1. "Peak Island". travelingluck.com. Retrieved 2009-07-12.