Torngat orogeny
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The Torngat Mountains are a mountain range on the Labrador Peninsula at the northern tip of Newfoundland and Labrador and eastern Quebec. They are part of the
Arctic Cordillera The Arctic Cordillera is a terrestrial ecozone in northern Canada characterized by a vast, deeply dissected chain of mountain ranges extending along the northeastern flank of the Canadian Arctic Archipelago from Ellesmere Island to the northeas ...
.Park Wardens - Arctic Cordillera
The mountains form a peninsula that separates
Ungava Bay Ungava Bay (french: baie d'Ungava, ; iu, ᐅᖓᕙ ᑲᖏᖅᓗᒃ/) is a bay in northeastern Canada separating Nunavik (far northern Quebec) from Baffin Island. Although not geographically apparent, it is considered to be a marginal sea of the ...
from the Atlantic Ocean.


Etymology

The name ''Torngat'' is derived from an
Inuktitut Inuktitut (; , syllabics ; from , "person" + , "like", "in the manner of"), also Eastern Canadian Inuktitut, is one of the principal Inuit languages of Canada. It is spoken in all areas north of the tree line, including parts of the provinces o ...
word meaning ''place of spirits'', sometimes interpreted as ''place of evil spirits''.


Geography

The Torngat Mountains have a substantial geographical extent. About 56% of the range is located in Quebec, 44% is in Labrador, and the remainder, less than 1%, is located on
Killiniq Island Killiniq Island (English: ''ice floes'') is a remote island in southeastern Nunavut and northern Newfoundland and Labrador, Canada. Located at the extreme northern tip of Labrador between Ungava Bay and the Labrador Sea, it is notable in that it c ...
in
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'' ...
. At least 2% of the mountain chain is under water, and poorly surveyed. The Torngat Mountains cover , including lowland areas and extend over from Cape Chidley in the north to Hebron Fjord in the south. The Torngat Mountains have the highest peaks of eastern continental Canada. The highest point is Mount Caubvick (also known as
Mont D'Iberville Mount Caubvick (known as Mont D'Iberville in Quebec) is a mountain located in Canada on the border between Labrador and Quebec in the Selamiut Range of the Torngat Mountains. It is the highest point in mainland Canada east of the Canadian Rockies ...
) at . There are no trees in the Torngat Mountains because the mountains lie in an arctic tundra climate and are therefore above the tree line.
Permafrost Permafrost is ground that continuously remains below 0 °C (32 °F) for two or more years, located on land or under the ocean. Most common in the Northern Hemisphere, around 15% of the Northern Hemisphere or 11% of the global surface ...
is continuous on the Quebec side of the border, and it is extensive but discontinuous on the eastern Atlantic side. The terrain is over above sea level and is predominantly rocky desert.


Geology

Precambrian The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the ...
gneisses that comprise the Torngat Mountains are among the oldest on Earth and have been dated at roughly 3.6 to 3.9 billion years old. Geologists recognize the gneisses of the Torngats as a part of the
Canadian Shield The Canadian Shield (french: Bouclier canadien ), also called the Laurentian Plateau, is a geologic shield, a large area of exposed Precambrian igneous and high-grade metamorphic rocks. It forms the North American Craton (or Laurentia), the anc ...
or Laurentian Upland, which, composing the very old North American Craton, split from the continent of
Rodinia Rodinia (from the Russian родина, ''rodina'', meaning "motherland, birthplace") was a Mesoproterozoic and Neoproterozoic supercontinent that assembled 1.26–0.90 billion years ago and broke up 750–633 million years ago. were probably ...
roughly 750 million years ago to form the geologic core of
North America North America is a continent in the Northern Hemisphere and almost entirely within the Western Hemisphere. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and the Car ...
. However, the mountain-building or
orogeny Orogeny is a mountain building process. An orogeny is an event that takes place at a convergent plate margin when plate motion compresses the margin. An ''orogenic belt'' or ''orogen'' develops as the compressed plate crumples and is uplifted t ...
of the Torngats took place much more recently, and is characteristic of the folding and faulting that defines the series of geological events known as
Arctic Cordillera The Arctic Cordillera is a terrestrial ecozone in northern Canada characterized by a vast, deeply dissected chain of mountain ranges extending along the northeastern flank of the Canadian Arctic Archipelago from Ellesmere Island to the northeas ...
. This, according to some, makes the Torngats, as mountains, "distinct compared to the surrounding Precambrian Canadian Shield," though they are ultimately composed of shield rock. Evidence of this dramatic cordilleran folding and faulting characterizing the Torngat Mountains can be seen distinctly in rocks where the North American Craton long ago collided with the Nain Craton, later exposed in cross-section by glacial scouring, especially at Saglek Fjord.


Glaciation

The ranges of the Torngat Mountains are separated by deep fjords and finger lakes surrounded by sheer rock walls. The fjords were produced by glaciation. The Laurentide Ice Sheet covered most of the mountains at least once, however during the last ice age the coverage was more limited. Currently, there are over 100 active small mountain
glaciers 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 over many years, often centuries. It acquires distinguishing features, such as ...
in the Torngat Mountains with a total of about 195 ice masses in the region.


Ecology


Flora

The Torngat Mountain tundra is characterized by sparse cover of arctic sedges, grass, lichen, and moss. Patches of mixed arctic evergreen and deciduous shrubs can be found on sheltered south-facing slopes, increasing in prevalence as one moves south.


Fauna

The tundra provides seasonal habitat for
caribou Reindeer (in North American English, known as caribou if wild and ''reindeer'' if domesticated) are deer in the genus ''Rangifer''. For the last few decades, reindeer were assigned to one species, ''Rangifer tarandus'', with about 10 subspe ...
, polar bears, and the only tundra-dwelling black bears in the world. In addition, the coastal area of this ecoregion lies along the Atlantic migratory flyway.


Conservation

The
Torngat Mountains National Park Reserve Torngat Mountains National Park () is a Canadian national park located on the Labrador Peninsula in the province of Newfoundland and Labrador. The park encompasses of mountainous terrain between Northern Quebec and the Labrador Sea. It is the l ...
was announced on 1 December 2005. It aims to protect wildlife (caribou, polar bears,
peregrine falcon The peregrine falcon (''Falco peregrinus''), also known as the peregrine, and historically as the duck hawk in North America, is a Cosmopolitan distribution, cosmopolitan bird of prey (Bird of prey, raptor) in the family (biology), family Falco ...
and golden eagle among others), while offering wilderness-oriented recreational activities.


In popular culture

In the CBC Series ''Geological Journey'' the Torngat mountains are feature

Notably, a billion-year-old coal seam (based on algae, not peat swamps) was discovered in the Torngat mountains on the Newfoundland Coast as part of the filming of the series. ''Backcountry Magazine'' ran a feature story written by Drew Pogge in 2009 on steep skiing in the Torngat Mountains, notably first descents in Nachvak and Saglek fjords, as well as on the Caubvick massif.


See also

* List of ecoregions in Canada (WWF) * Torngat Mountains National Park * Kuururjuaq National Park


References


Further reading

* Ives, J. D. 1957. "Glaciation of the Torngat Mountains, Northern Labrador". ''Arctic''. 10, no. 2: 67–87. * Kobalenko, Jerry. 2007. "Ghost Coast - Kayaking the Foreboding Fiords of Torngat Mountains National Park". ''Canadian Geographic''. 127, no. 3: 38. * Schaefer, James A, and Stuard N Luttich. 1998. "Articles - Movements and Activity of Caribou, Rangifer Tarandus Caribou, of the Torngat Mountains, Northern Labrador and Quebec". ''The Canadian Field-Naturalist''. 112, no. 3: 486. * Way, R.G., Bell, T. and Barrand, N.E. 2014. "An inventory and topographic analysis of glaciers in the Torngat Mountains, northern Labrador, Canada". ''Journal of Glaciology''. 60, no. 223: 945–956. * Perkins, Robert "Against Straight Lines/Alone in Labrador" 1983 Perkins sets off on a journey in 1979 to remote Labrador crossing the Torngat Mountains from Atlantic Ocean to Ungavava Bay.


External links


Torngat MountainsGreat photos of the mountain rangeTales from the Torngats, August 2004Alexander Forbes Collection: Aerial photo survey of Labrador from 1931, 1932, and 1935 expeditions
- University of Wisconsin-Milwaukee Libraries Digital Collections
Torngat Mountains: Canada's newest national park
{{Authority control Labrador Mountain ranges of Newfoundland and Labrador Mountain ranges of Quebec Arctic Cordillera Physiographic sections Landforms of Nord-du-Québec