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Akshayuk Pass
Akshayuk Pass formerly Pangnirtung Pass is a mountain pass in the Baffin Mountains of Nunavut, Canada. It is found within Auyuittuq National Park. To the southwest is Mount Thor, about , and Pangnirtung, about and to the northeast is Qikiqtarjuaq, about . Geography Akshayuk Pass is located in Baffin Island's Cumberland Peninsula. It is a Auyuittuq National Park
at Travel Nunavut
long along a spectacular valley through the southern Baffin Mountains. Summit Lake is the highest point on the pass. Akshayuk Pass is an ancient

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Baffin Island
Baffin Island (formerly Baffin Land), in the Canadian territory of Nunavut, is the largest island in Canada and the fifth-largest island in the world. Its area is , slightly larger than Spain; its population was 13,039 as of the 2021 Canadian census; and it is located at . It also contains the city of Iqaluit, the capital of Nunavut. Name The Inuktitut name for the island is , which means "very big island" ( "island" + "very big") and in Inuktitut syllabics is written as . This name is used for the administrative region the island is part of ( Qikiqtaaluk Region), as well as in multiple places in Nunavut and the Northwest Territories, such as some smaller islands: Qikiqtaaluk in Baffin Bay and Qikiqtaaluk in Foxe Basin. Norse explorers referred to it as ("stone land"). In 1576, English seaman Martin Frobisher made landfall on the island, naming it "Queen Elizabeth's Foreland" and Frobisher Bay is named after him. The island is named after English explorer William Baff ...
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Baffin Mountains
The Baffin Mountains are a mountain range running along the northeastern coast of Baffin Island and Bylot Island, Nunavut, Canada. The ice-capped mountains are part of the Arctic Cordillera and have some of the highest peaks of eastern North America, reaching a height of above sea level. While they are separated by bodies of water to make Baffin Island, they are closely related to the other mountain ranges that make the much larger Arctic Cordillera mountain range. Terrain The highest point is Mount Odin at while Mount Asgard (''Sivanitirutinguak'') at is perhaps the best known. The highest point in the northern Baffin Mountains is Qiajivik Mountain at . There are no trees in the Baffin Mountains because they are north of the Arctic tree line. Rocks that compose the Baffin Mountains are primarily deeply dissected granitic rocks. They were covered with ice until about 1500 years ago, and vast parts of them are still ice-covered. Geologically, the Baffin Mountains form the easte ...
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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ...
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Nunavut
Nunavut ( , ; iu, ᓄᓇᕗᑦ , ; ) is the largest and northernmost Provinces and territories of Canada#Territories, territory of Canada. It was separated officially from the Northwest Territories on April 1, 1999, via the ''Nunavut Act'' and the ''Nunavut Land Claims Agreement, Nunavut Land Claims Agreement Act'', which provided this territory to the Inuit for independent government. The boundaries had been drawn in 1993. The creation of Nunavut resulted in the territorial evolution of Canada, first major change to Canada's political map in half a century since the province of Newfoundland and Labrador, Newfoundland was admitted in 1949. Nunavut comprises a major portion of Northern Canada and most of the Arctic Archipelago. Its vast territory makes it the list of the largest country subdivisions by area, fifth-largest country subdivision in the world, as well as North America's second-largest (after Greenland). The capital Iqaluit (formerly Frobisher Bay), on Baffin Islan ...
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Auyuittuq National Park
Auyuittuq National Park ( iu, ᐊᐅᔪᐃᑦᑐᖅ, , "the land that never melts") is a national park located on Baffin Island's Cumberland Peninsula, in the Qikiqtaaluk Region of Nunavut, the largest political subdivision of Canada. The park was initially known as ''Baffin Island National Park'' when it was established in 1972, but the name was changed in 1976 to its current name to better reflect the region and its history. It features many terrains of Arctic wilderness, such as fjords, glaciers, and ice fields. Although Auyuittuq was established in 1972 as a national park reserve, it was upgraded to a full national park in 2000. Location and access Auyuittuq National Park is located on the Cumberland Peninsula of Baffin Island in Nunavut. The park is located within the Arctic Circle. The park covers The Municipality of Pangnirtung website states that the park measures . and is located partially within the Penny Highlands and contains the Penny Ice Cap. The Penny Ice Cap, mad ...
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Mount Thor
Mount Thor, officially gazetted as Thor Peak ( iu, ᙯᕐᓱᐊᓗᒃ ''Qaisualuk'' "huge bedrock" or iu, ᑭᒍᑎᙳᐊᖅ ''Kigutinnguaq'' "tooth-like"), is a mountain with an elevation of located in Auyuittuq National Park, on Baffin Island, Nunavut, Canada. The mountain is located northeast of Pangnirtung and features Earth's greatest vertical drop of , with the cliff overhanging at an average angle of 15 degrees from vertical. Despite its remoteness, this feature makes the mountain a popular rock climbing site. Camping is allowed, with several designated campsites located throughout the length of Akshayuk Pass. For climbers looking to scale Mount Thor, there is an established campsite a few kilometres north of its base, complete with windbreaks and emergency shelters. The English naming of the mountain originates from Thor, the Norse thunder god. Geography Mount Thor is part of the Baffin Mountains which in turn form part of the Arctic Cordillera mountain range. The mo ...
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Pangnirtung
Pangnirtung (or Pang, also Pangniqtuuq, in syllabics: ᐸᖕᓂᖅᑑᖅ ) is an Inuit hamlet, in the Qikiqtaaluk Region of the Canadian territory of Nunavut, located on Baffin Island. Pangnirtung is situated on a coastal plain at the coast of Pangnirtung Fjord, a fjord In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Ice ... which eventually merges with Cumberland Sound. As of January 2022, the mayor is Stevie Komoartok. Name There is some confusion about the village name. Residents say the real name is ''Pangniqtuuq'', which means "the place of many bull caribou". Early in 2005 residents voted against officially changing the name of the village to the native one, as Pangnirtung has achieved an international reputation. Its residents have created high-quality traditional arts in scul ...
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Qikiqtarjuaq
Qikiqtarjuaq (; formerly known as Broughton Island until November 1998 ,) is a community located on Broughton Island in the Qikiqtaaluk Region of Nunavut, Canada. The island is known for Arctic wildlife (ring seals, polar bears, bowhead whales, narwhals), bird watching (Qaqulluit National Wildlife Area), and as the northern access point for Auyuittuq National Park (see also Pangnirtung) Qikiqtarjuaq hosts an annual "Suicide Prevention Walk". Local participants would walk a total distance of across the tundra from Kivitoo, an old whaling station. Today the walk is much shorter than the original two and a half days, but it is still meant to promote hope among the community. The community hosts a two-week celebration over the Christmas and New Year period every year. Visitors are warmly welcomed and encouraged to join the festivities and games. Near Qikiqtarjuaq was the home of FOX-5, a Distant Early Warning Line and now a North Warning System site. In July 2011, Qikiqtarjuaq ...
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Cumberland Peninsula
Cumberland Peninsula is a peninsula in the southeastern part of Baffin Island in Nunavut, Canada. It is located between 64°56' and 67°57' north latitude, and 61°56' to 68° west longitude. The Arctic Circle crosses the peninsula, with the Labrador Sea to the southeast, and the Davis Strait to the east, which lies between the peninsula and Greenland. The Cumberland Sound lies to the southwest, separating the Cumberland Peninsula from the Hall Peninsula, which is also part of Baffin Island. The Cumberland Peninsula is part of the Arctic Tundra biome—the world's coldest and driest biome—as is the rest of Baffin Island. The terrain is mountainous, and Mt. Odin, near the Arctic Circle, rises . The peninsula is home to Pangnirtung, which lies on the southwest coast, and the Auyuittuq National Park. References Further reading * Dyke, Arthur S., John T. Andrews, and Gifford H. Miller. ''Quaternary Geology of Cumberland Peninsula, Baffin Island, District of Franklin''. Ottawa ...
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Stream Bed
A stream bed or streambed is the bottom of a stream or river (bathymetry) or the physical confine of the normal water flow (Channel (geography), channel). The lateral confines or channel margins are known as the stream Bank (geography), banks or river banks, during all but flood stage. Under certain conditions a river can branch from one stream bed to multiple stream beds. A flood occurs when a stream overflows its banks and flows onto its flood plain. As a general rule, the bed is the part of the stream channel, channel up to the normal water line, and the banks are that part above the normal water line. However, because water flow varies, this differentiation is subject to local interpretation. Usually, the bed is kept clear of terrestrial vegetation, whereas the banks are subjected to water flow only during unusual or perhaps infrequent high water stages and therefore might support vegetation some or much of the time. The nature of any stream bed is always a function of th ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ...
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Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ...
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