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What is Greenland's natural environment like?
What plants grow in Greenland?
How many species of plants are in Greenland?
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Plants such as broccoli, radishes, spinach, leeks, lettuce, turnips, chervil, potatoes and parsley are grown up to considerable latitudes, while the very south of the country also rears asters, Nemophila, mignonette, rhubarb, sorrel and carrots. [3]
Greenland’s flora ranges widely – from lush thickets and beautiful flower meadows to sparse vegetation on rocks and steppes. There are a number of different plant communities and types of nature in Greenland, each characterised by different plants and flowers.
Greenland’s natural environment is shaped by the extreme Arctic climate. Most of the vegetation on the island exists on the tundra, away from the ice sheets. Low-growing plants like dwarf...
- Aaron Sidder
Greenland (Greenlandic: Kalaallit Nunaat, pronounced [kalaːɬːit nʉnaːt]; Danish: Grønland, pronounced [ˈkʁɶnˌlænˀ]) is a North American autonomous territory of the Kingdom of Denmark.
- Overview
- Land
Greenland, the world’s largest island, lying in the North Atlantic Ocean. Greenland (Kalaallit Nunaat) is noted for its vast tundra and immense glaciers.
Although Greenland remains part of the Kingdom of Denmark, the island’s home-rule government is responsible for most domestic affairs. The Greenlandic people are primarily Inuit who, depending upon the region they are from, call themselves Kalaallit (West Greenlanders), Inugguit (from Thule district), or Iit (East Greenlanders). They call their homeland Kalaallit Nunaat (“Country of the Greenlanders”). The capital of Greenland is Nuuk (Godthåb).
More than three times the size of the U.S. state of Texas, Greenland extends about 1,660 miles (2,670 km) from north to south and more than 650 miles (1,050 km) from east to west at its widest point. Two-thirds of the island lies within the Arctic Circle, and the island’s northern extremity extends to within less than 500 miles (800 km) of the North Pole. Greenland is separated from Canada’s Ellesmere Island to the north by only 16 miles (26 km). The nearest European country is Iceland, lying about 200 miles (320 km) across the Denmark Strait to the southeast. Greenland’s deeply indented coastline is 24,430 miles (39,330 km) long, a distance roughly equivalent to Earth’s circumference at the Equator.
A submarine ridge no deeper than 600 feet (180 metres) connects the island physically with North America. Structurally, Greenland is an extension of the Canadian Shield, the rough plateau of the Canadian North that is made up of hard Precambrian rocks.
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Islands and Archipelagos
Greenland’s major physical feature is its massive ice sheet, which is second only to Antarctica’s in size. The Greenland Ice Sheet has an average thickness of 5,000 feet (1,500 metres), reaches a maximum thickness of about 10,000 feet (3,000 metres), and covers more than 700,000 square miles (1,800,000 square km)—over four-fifths of Greenland’s total land area. Layers of snow falling on its barren, windswept surface become compressed into ice layers, which constantly move outward to the peripheral glaciers; the Jakobshavn Glacier, often moving 100 feet (30 metres) a day, is among the world’s fastest glaciers. The remaining ice-free land area occupies the country’s coastal areas and consists largely of highlands; mountain chains parallel the island’s east and west coasts, rising to 12,139 feet (3,700 metres) at Gunnbjørn Mountain in the southeast. These highlands notwithstanding, most parts of the rock floor underlying the Greenland Ice Sheet are in fact at or slightly beneath current sea levels.
Long, deep fjords reach far into both the east and west coasts of Greenland in complex systems, offering magnificent, if desolate, scenery. Along many parts of the coast, the ice sheet fronts directly on the sea, with large chunks breaking off the glaciers and sliding into the water as icebergs.
Mar 15, 2021 · This material contains a stratigraphic record of glaciation and vegetation in northwestern Greenland spanning the Pleistocene. Enriched stable isotopes of pore-ice suggest precipitation at lower elevations implying ice-sheet absence.
The vegetation is generally sparse, with the only patch of forested land being found in Nanortalik Municipality in the extreme south near Cape Farewell. The climate is arctic to subarctic , with cool summers and cold winters.
