Carey Islands

Last updated • 3 min readFrom Wikipedia, The Free Encyclopedia
Carey Islands
Native name:
Kitsissut
Bjorlingo.png
View of Björling Island
Greenland edcp location map.svg
Red pog.svg
Carey Islands
Carey Islands (Greenland)
Geography
Location Baffin Bay, Greenland
Coordinates 76°40′00″N72°30′00″W / 76.666667°N 72.5°W / 76.666667; -72.5
ArchipelagoCarey Islands
Total islands6
Major islandsNordvestø
Highest elevation300 m (1000 ft)
Administration
Greenland
Municipality Avannaata
Demographics
Populationuninhabited
Northwestern Greenland location map.png
Cercle rouge 100%25.svg
Location of the Carey Islands

The Carey Islands (Danish : Carey Øer; Greenlandic : Kitsissut) are an island group off Baffin Bay, in Avannaata municipality, northwest Greenland. Located relatively far offshore the Carey Islands are the westernmost point of Greenland as a territory. The sea surrounding the islands is clogged by ice most of the year.

Contents

Geography

The archipelago consists of six desolate islands, a few small islets and a number of rocks awash. [1] It is located about 100 kilometres (62 mi) to the west of Thule Air Base and 50 kilometres (31 mi) to the SW of Cape Parry. [2]

The nearest settlement is Moriusaq to the east on the coast of Greenland, abandoned since 2007.

Islands

Main islands

  • Nordvestø, Isbjørneø and Mellemø form a compact cluster at the NW end of the archipelago.
    • Nordvestø, the biggest island with a length of 4.5 kilometres (2.8 mi) and a width of nearly 3 kilometres (1.9 mi). This island's western landhead is the westernmost point of Greenland. Its highest point is 225 metres (738 ft).
    • Isbjørneø and Mellemø, lying close to the east and forming a natural harbour between them and Nordvestø.
  • Bordø and Björlingø, located further to the east; the latter has a 300 metres (980 ft) high peak and is named after Johan Alfred Björling.
  • Fireø, lying in the southern area of the group.

Islets

  • Hollænderhatten and Tyreøjet are two small islets to the east of Fireø having a diameter of a few hundred metres. there are also numerous other islets and rocks, especially in the western sector of the archipelago. [3]

Climate

Climate data for Kitsissut, Greenland (2009-2020)
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °C (°F)0.1
(32.2)
0.6
(33.1)
2.9
(37.2)
−0.1
(31.8)
8.9
(48.0)
10.5
(50.9)
13.1
(55.6)
10.4
(50.7)
8.0
(46.4)
2.4
(36.3)
1.6
(34.9)
−0.5
(31.1)
13.1
(55.6)
Mean daily maximum °C (°F)−14.7
(5.5)
−15.8
(3.6)
−16.4
(2.5)
−10.0
(14.0)
−2.8
(27.0)
2.2
(36.0)
6.2
(43.2)
5.0
(41.0)
0.6
(33.1)
−3.8
(25.2)
−9.1
(15.6)
−13.0
(8.6)
−6.0
(21.2)
Daily mean °C (°F)−16.6
(2.1)
−17.7
(0.1)
−18.2
(−0.8)
−11.6
(11.1)
−4.0
(24.8)
0.7
(33.3)
4.4
(39.9)
3.7
(38.7)
−0.3
(31.5)
−5.0
(23.0)
−10.9
(12.4)
−14.8
(5.4)
−7.5
(18.5)
Mean daily minimum °C (°F)−18.4
(−1.1)
−19.4
(−2.9)
−20.1
(−4.2)
−13.4
(7.9)
−5.4
(22.3)
−0.7
(30.7)
2.8
(37.0)
2.3
(36.1)
−1.3
(29.7)
−6.2
(20.8)
−12.5
(9.5)
−16.6
(2.1)
−9.1
(15.6)
Record low °C (°F)−33.4
(−28.1)
−28.4
(−19.1)
−32.7
(−26.9)
−26.7
(−16.1)
−15.0
(5.0)
−6.0
(21.2)
−2.3
(27.9)
−2.4
(27.7)
−6.2
(20.8)
−15.6
(3.9)
−23.9
(−11.0)
−30.3
(−22.5)
−33.4
(−28.1)
Average relative humidity (%)75.474.174.475.580.587.486.588.781.579.577.376.179.7
Source: DMI (humidity 2011-2020) [4]

Important Bird Area

The island group has been designated an Important Bird Area (IBA) by BirdLife International because it supports a breeding population of some 6,700 pairs of thick-billed murres, as well as other seabirds including glaucous gulls, razorbills, black guillemots and Atlantic puffins. [5]

History

The islands had been inhabited by the Inuit in the past; remains of their dwellings were found by Clements Markham in August 1851. [6]

The Carey Islands' were named by the 1616 Bylot-Baffin Arctic expedition after Allwin Carey, one of the financiers of the venture. [7]

Swedish naturalists Alfred Björling and Evald Kallstenius stopped at the Carey Islands in 1892 during an expedition on schooner Ripple to pick up supplies at a cache there. The Ripple, however, was driven on shore and wrecked. The men attempted to sail a small sloop back to Etah, but were forced to return to the Carey Islands. [8]

According to letters left by members of the ill-fated expedition in a cairn on the islands, the remaining four men attempted to sail their open boat 80 miles to Ellesmere Island:

Forced by bad weather to linger on this island for a long time, I now set out on the tour to the Eskimos... on Ellesmere Island. As I hope that a whaler will visit the Carey Islands next summer to rescue me and my companions, I will try to reach the islands again before July 1. We are now five men, of which one is dying. [9]

In June 1893, the crew of the Scottish whaler Aurora spotted a wreck on the Carey Islands. They found the Ripple, a man's body buried under a pile of stones, and Björling's letters. [9] No trace of the other four men, or the small boat, was ever found.

See also

Related Research Articles

<span class="mw-page-title-main">Geography of Greenland</span>

Greenland is located between the Arctic Ocean and the North Atlantic Ocean, northeast of Canada and northwest of Iceland. The territory comprises the island of Greenland—the largest island in the world—and more than a hundred other smaller islands. Greenland has a 1.2-kilometer-long (0.75 mi) border with Canada on Hans Island. A sparse population is confined to small settlements along certain sectors of the coast. Greenland possesses the world's second-largest ice sheet.

<span class="mw-page-title-main">Northwest Passage</span> Sea route north of North America

The Northwest Passage (NWP) is the sea lane between the Atlantic and Pacific oceans through the Arctic Ocean, along the northern coast of North America via waterways through the Arctic Archipelago of Canada. The eastern route along the Arctic coasts of Norway and Siberia is accordingly called the Northeast Passage (NEP). The various islands of the archipelago are separated from one another and from Mainland Canada by a series of Arctic waterways collectively known as the Northwest Passages, Northwestern Passages or the Canadian Internal Waters.

<span class="mw-page-title-main">Ellesmere Island</span> Island of the Arctic Archipelago in Nunavut, Canada

Ellesmere Island is Canada's northernmost and third largest island, and the tenth largest in the world. It comprises an area of 196,236 km2 (75,767 sq mi), slightly smaller than Great Britain, and the total length of the island is 830 km (520 mi).

<span class="mw-page-title-main">Baffin Bay</span> Marginal sea between Greenland and Baffin Island, Canada

Baffin Bay, located between Baffin Island and the west coast of Greenland, is defined by the International Hydrographic Organization as a marginal sea of the Arctic Ocean. It is sometimes considered a sea of the North Atlantic Ocean. It is connected to the Atlantic via Davis Strait and the Labrador Sea. The narrower Nares Strait connects Baffin Bay with the Arctic Ocean. The bay is not navigable most of the year because of the ice cover and high density of floating ice and icebergs in the open areas. However, a polynya of about 80,000 km2 (31,000 sq mi), known as the North Water, opens in summer on the north near Smith Sound. Most of the aquatic life of the bay is concentrated near that region.

<span class="mw-page-title-main">Devon Island</span> Uninhabited island in Nunavut, Canada

Devon Island is an island in Canada and the largest uninhabited island in the world. It is located in Baffin Bay, Qikiqtaaluk Region, Nunavut, Canada. It is one of the largest members of the Arctic Archipelago, the second-largest of the Queen Elizabeth Islands, Canada's sixth-largest island, and the 27th-largest island in the world. It has an area of 55,247 km2 (21,331 sq mi). The bedrock is Precambrian gneiss and Paleozoic siltstones and shales. The highest point is the Devon Ice Cap at 1,920 m (6,300 ft) which is part of the Arctic Cordillera. Devon Island contains several small mountain ranges, such as the Treuter Mountains, Haddington Range and the Cunningham Mountains. The notable similarity of its surface to that of Mars has attracted interest from scientists.

<span class="mw-page-title-main">Bylot Island</span> Uninhabited island off Baffin Island in Nunavut Territory, Canada

Bylot Island lies off the northern end of Baffin Island in Nunavut Territory, Canada. Eclipse Sound to the southeast and Navy Board Inlet to the southwest separate it from Baffin Island. Parry Channel lies to its northwest. At 11,067 km2 (4,273 sq mi) it is ranked 71st largest island in the world and Canada's 17th largest island. The island measures 180 km (110 mi) east to west and 110 km (68 mi) north to south and is one of the largest uninhabited islands in the world. While there are no permanent settlements on this Canadian Arctic island, Inuit from Pond Inlet and elsewhere regularly travel to Bylot Island. An Inuit seasonal hunting camp is located southwest of Cape Graham Moore.

<span class="mw-page-title-main">Disko Bay</span> Bay on the western coast of Greenland

Disko Bay is a large bay on the western coast of Greenland. The bay constitutes a wide southeastern inlet of Baffin Bay.

<span class="mw-page-title-main">Lomonosov Ridge</span> Underwater ridge of continental crust in the Arctic Ocean

The Lomonosov Ridge is an unusual underwater ridge of continental crust in the Arctic Ocean. It spans 1,800 kilometres (1,100 mi) between the New Siberian Islands over the central part of the ocean to Ellesmere Island of the Canadian Arctic Archipelago. The ridge divides the Arctic Basin into the Eurasian Basin and the Amerasian Basin. The width of the Lomonosov Ridge varies from 60 to 200 kilometres. It rises 3,300 to 3,700 metres above the 4,200-metre (13,800 ft) deep seabed. The minimum depth of the ocean above the ridge is less than 400 metres (1,300 ft). Slopes of the ridge are relatively steep, broken up by canyons, and covered with layers of silt. It is an aseismic ridge.

<span class="mw-page-title-main">Kane Basin</span> Arctic waterway lying between Greenland and Canada

Kane Basin is an Arctic waterway lying between Greenland and Ellesmere Island, Canada's northernmost. It links Smith Sound to Kennedy Channel and forms part of Nares Strait. It is approximately 180 km (110 mi) in length and 130 km (81 mi) at its widest.

<span class="mw-page-title-main">Cape Alexander, Greenland</span>

Cape Alexander is a headland in the Baffin Bay, northwest Greenland, Avannaata municipality. It is one of the important landmarks of Greenland.

<span class="mw-page-title-main">Wilczek Land</span> Island in the Arctic Ocean

Wilczek Land, is an island in the Arctic Ocean at 80.58°N 60.5°E. At 2,000 km2 (770 sq mi) it is the second-largest island in Franz Josef Land, in Arctic Russia.

<span class="mw-page-title-main">Nordenskiöld Archipelago</span> Cluster of islands in the eastern region of the Kara Sea

The Nordenskiöld Archipelago or Nordenskjold Archipelago is a large and complex cluster of about 90 islands in the eastern region of the Kara Sea. Its eastern limit lies 120 km (75 mi) west of the Taymyr Peninsula. The archipelago is part of the Taymyrsky Dolgano-Nenetsky District of the Krasnoyarsk Krai administrative division of Russia.

<span class="mw-page-title-main">Etah, Greenland</span> Place in Greenland, Kingdom of Denmark

Etah is an abandoned settlement in the Avannaata municipality in northern Greenland. It was a starting point of discovery expeditions to the North Pole and the landing site of the last migration of the Inuit from the Canadian Arctic.

<span class="mw-page-title-main">Björling–Kallstenius Expedition</span>

.

<span class="mw-page-title-main">Timeline of European exploration</span>

This timeline of European exploration lists major geographic discoveries and other firsts credited to or involving Europeans during the Age of Discovery and the following centuries, between the years AD 1418 and 1957.

<span class="mw-page-title-main">Geography of Franz Josef Land</span>

The Geography of Franz Josef Land refers to an island group belonging to Arkhangelsk Oblast of Russia. It is situated in the Barents Sea of the Arctic, north of Novaya Zemlya and east of Svalbard. At latitudes between 80.0° and 81.9° north, it is the most northerly group of islands associated with Eurasia. The extreme northernmost point is Cape Fligely on Rudolf Island. The archipelago consists of 191 ice-covered islands with a total area of 16,134 km2 (6,229 sq mi). It is currently uninhabited. The archipelago is only 900 to 1,110 km from the North Pole, and the northernmost islands are closer to the Pole than any other land except for Canada's Ellesmere Island and Greenland. The largest island is Zemlya Georga which measures 110 km (68 mi) from end to end. The highest point in the archipelago is on Ostrov Viner-Neyshtadt which reaches 620 m (2,034 ft) above sea level. The central cluster of large islands in the midst of the archipelago forms a compact whole, known as Zichy Land, where islands are separated from each other by very narrow sounds that are frozen most of the year.

<span class="mw-page-title-main">Johan Alfred Björling</span> Swedish botanist and Arctic explorer

Johan Alfred Björling was a Swedish botanist and Arctic explorer. He led the ill-fated Swedish NW Greenland Expedition, also known as Björling–Kallstenius Expedition, in 1892.

<span class="mw-page-title-main">Thomas Abernethy (explorer)</span> Scottish seafarer and polar explorer (1803–1860)

Thomas Abernethy was a Scottish seafarer, gunner in the Royal Navy, and polar explorer. Because he was neither an officer nor a gentleman, he was little mentioned in the books written by the leaders of the expeditions he went on, but was praised in what was written. In 1857, he was awarded the Arctic Medal for his service as an able seaman on the 1824–25 voyage of HMS Hecla, the first of his five expeditions for which participants were eligible for the award. He was in parties that, for their time, reached the furthest north, the furthest south (twice), and the nearest to the South Magnetic Pole. In 1831, along with James Clark Ross's team of six, Abernethy was in the first party ever to reach the North Magnetic Pole.

<span class="mw-page-title-main">Canadian Arctic Rift System</span> North American geological structure

The Canadian Arctic Rift System is a major North American geological structure extending from the Labrador Sea in the southeast through Davis Strait, Baffin Bay and the Arctic Archipelago in the northwest. It consists of a series of interconnected rifts that formed during the Paleozoic, Mesozoic and Cenozoic eras. Extensional stresses along the entire length of the rift system have resulted in a variety of tectonic features, including grabens, half-grabens, basins and faults.

References

  1. "Carey Øer". Mapcarta. Retrieved 10 April 2016.
  2. Carey Islands, Greenland
  3. Sailing Directions (Enroute), Pub. 181: Greenland and Iceland (PDF). Sailing Directions . United States National Geospatial-Intelligence Agency. 2017. p. 70.
  4. "Climatological Standard Normals 1991-2020 – Greenland" (PDF). Danish Meteorological Institute . Retrieved February 14, 2024.
  5. "Carey Islands". BirdLife Data Zone. BirdLife International. 2021. Retrieved 28 November 2021.
  6. Clements Robert Markham: Franklin’s footsteps. Chapman and Hall, London 1853, p. 115.
  7. Thomas Rundall. Narratives of Voyages towards the North-west, in search of a Passage to Cathay and India, 1496 to 1631. The Hakluyt Society, London 1849, S. 141.
  8. Mowat, Farley (1967). The Polar Passion: The Quest for the North Pole . Toronto: McClelland and Stewart Limited.
  9. 1 2 Harper, Ken. (Oct 7, 2005) Nunatsiaq News: "Taissumani: A Day in Arctic History Oct. 12, 1892 - The Disappearance of Bjorling and Kallstenius"