 | |
| Continent | Europe |
|---|---|
| Region | Northern Europe |
| Coordinates | 65°00′N18°00′W / 65.000°N 18.000°W /65.000; -18.000 |
| Area | Ranked 106 |
| • Total | 103,001 km2 (39,769 sq mi) |
| • Land | 97.33% |
| • Water | 2.67% |
| Coastline | 4,970 km (3,090 mi) |
| Borders | None |
| Highest point |
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| Lowest point |
|
| Longest river |
|
| Largest lake |
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| Climate | Subpolar oceanic climate, Tundra |
| Terrain | Plateau interspersed with mountain peaks, volcanic peaks, icefields and a coast deeply indented by bays and fjords |
| Natural resources | Marine life, diatomite, hydrothermal power |
| Natural hazards | Volcanism, earthquakes, avalanches, and glacial lake outburst flooding |
| Environmental issues | Air pollution, climate change, desertification, hazardous wastes, marine dumping |
| Exclusive economic zone | 751,345 km2 (290,096 sq mi) |
Iceland is anisland country at the confluence of theNorth Atlantic andArctic oceans, east ofGreenland and immediately south of theArctic Circle, atop theconstructive boundary of the northernMid-Atlantic Ridge. The island country is the world's18th largest in area and one mostsparsely populated. It is the westernmost European country when not including Greenland and has more land covered byglaciers thancontinental Europe. Its total size is 103,125 km2 (39,817 sq mi) and possesses anexclusive economic zone of 751,345 km2 (290,096 sq mi).
Iceland is an island country in Northern Europe, straddling the Eurasian and North American plates between theGreenland Sea and the North Atlantic Ocean, northwest of theBritish Isles.
Extent (locations outside mainland in parentheses)
Area:
Maritime claims:
Elevation extremes:
Natural resources:
Iceland consists of eight geographical regions,Capital Region, Southern Peninsula, West, Westfjords, Northwest, Northeast, East and South.[1] Twenty per cent of the land is used forgrazing, while only one per cent is cultivated. Iceland has lost most of the woodland that previously covered large areas of the country, but an ambitiousreforestation program is currently underway.[2] Fossilized tree pollen and descriptions by the early settlers indicate that prior to human settlement, now thought to have occurred from around AD 800 onwards,[3][4] trees covered between thirty and forty per cent of the island. Today, however, there are only small patches of the originalbirch forests left, the most prominent beingHallormsstaðaskógur andVaglaskógur. The country of Iceland contains 36 islands. The longest river on the island isÞjórsá at 230 kilometres (143 miles). Iceland hasthree national parks:Vatnajökull National Park,Snæfellsjökull National Park, andÞingvellir National Park.[5] The inhabited areas are on the coast, particularly in the southwest, while the central highlands are all but uninhabited. The island's terrain is mostly plateau interspersed with mountain peaks, icefields and a coast deeply indented by bays and fjords.
TheHighlands make up about half of Iceland's land area, which is of recent volcanic origin and consists of a mountainouslava desert (highest elevation 2,110 m (6,923 ft) above sea level) and other wastelands. The area is mostly uninhabited and uninhabitable.
TheWestfjords region is composed of a large, mountainous peninsula on Iceland's northwestern coast. The coastline is marked by numerous fjords as its name suggests. The peninsula contains Iceland's northernmost glacier, Drangajökull.
TheSouthern Peninsula, also known as theReykjanes Peninsula, is located in the southwestern corner of Iceland. The area contains little vegetation because of activevolcanism and large lava fields. There arehot springs andsulphur springs in the southern portion of the peninsula, in theKleifarvatn lake and theKrýsuvíkgeothermal area.
Home to Iceland's capital,Reykjavík, theCapital Region is the most densely populated area in Iceland. It is located on the southwest coast of the island near the Southern Peninsula. The majority of Reykjavík is located on theSeltjarnarnes peninsula. MountEsja, at 914 metres (2,999 ft), is the highest mountain in the vicinity of Reykjavík. Several natural harbours exist and provide good fishing grounds.[6]
Located in the western portion of the island and north of the Capital Region. InHvalfjörður fjord rests the second-tallest waterfall in Iceland,Glymur. West is also home toBorgarfjörður, a fjord with volcanic activity such asDeildartunguhver, a powerful hotspring. The 804-metre (2,638 ft) Hafnarfjall Mountain rises over the landscape.[7]
The southern portion of Iceland contains some of its most notable volcanoes such as Hekla, Eldgjá, and Katla. Alongside the volcanoes exist numerous glaciers such as Vatnajökull, Mýrdalsjökull, and Eyjafjallajökull. Basalt columns andblack sand beaches are examples of the volcanic activity of the area. The area also contains mountain ranges and Iceland's highest peak,Hvannadalshnjúkur, as well as theVestmannaeyjar (Westman Islands) archipelago.
East Iceland contains the majority of the island's vegetation and birch forests.
Atlantic contains large amounts of ice.
Around 10.2 per cent of the total land area is covered byglaciers, although these are retreating at an accelerating rate.[8] The four largest Icelandic glaciers are:
Other notable glaciers include:
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Because of the moderating influence of theNorth Atlantic Current, theclimate is temperate and characterized by damp, cool summers and relatively mild but windy winters. Reykjavík has an average temperature of 12 °C (53.6 °F) in July and 1 °C (34 °F) in January[9] It has aKöppen Climate Classification of Subpolar oceanic climate (Cfc) with most of the island classified as Tundra (ET).
Iceland has extensivevolcanic andgeothermal activity. Therift associated with the Mid-Atlantic Ridge, which marks the division between theEurasian Plate andNorth Americantectonic plates, runs across Iceland from the southwest to the northeast. This geographic feature is prominent at theÞingvellir National Park, where thepromontory creates an extraordinary naturalamphitheatre. The site was the home of Iceland's parliament, theAlþing, which was first convened in 930. It is a common misconception that Þingvellir is at the juncture between the North American and Eurasian continental plates. However, they are in fact at the juncture of the North American continental plate and a smaller plate (approx. 10,000 km2) called the Hreppar Microplate (Hreppaflekinn).[10] From 1963 to 1967, the island ofSurtsey was created on the southwest coast by a volcanic eruption.
A geologically young land, Iceland is located on both theIceland hotspot and the Mid-Atlantic Ridge, which runs right through it. This location means that the island is highly geologically active with earthquakes and volcanoes, notably Hekla, Eldgjá, Herðubreið and Eldfell. Eyjafjallajökull (1,666 m)erupted in 2010, disrupting European air traffic.[11] To demonstrate the geothermal activity, theIcelandic Meteorological Office said that during a single week in February 2021, around 17,000 earthquakes have hit the southwestern region ofReykjanes.[12]
Iceland has manygeysers, includingGeysir, from which the English wordgeyser is derived. With the widespread availability ofgeothermal power, and the harnessing of many rivers and waterfalls forhydroelectricity, most residents have access to inexpensive hot water, heating, and electricity. The island is composed primarily ofbasalt, a low-silicalava associated witheffusive volcanism as has occurred also in Hawaii. Iceland, however, has a variety of volcanic types (composite and fissure), many producing more evolved lavas such asrhyolite andandesite. Iceland has hundreds of volcanoes, with approximately 30 active volcanic systems.[13]
Party to:
Signed, but not ratified:
Media related toGeography of Iceland at Wikimedia Commons
This article incorporatespublic domain material fromThe World Factbook.CIA.
