what type of plate boundary is in iceland?
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Iceland sits spanning the Mid-Atlantic Ridge tectonic plate boundary which separates the Eurasian and the North American plates.
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The two types of plate boundaries that are most likely to produce volcanic activity are divergent plate boundaries and convergent plate boundaries. At a divergent boundary, tectonic plates move apart from one another.
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Each of these types of plate boundaries is associated with different geological features. Typically, a convergent plate boundary—such as the one between the Indian Plate and the Eurasian Plate—forms towering mountain ranges, like the Himalaya, as Earth's crust is crumpled and pushed upward.
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It is located 5 km (3.1 mi) off the island's southern Atlantic coast about 120 km southeast of Reykjavik, Iceland's capital city. The icecap of the glacier covers an active volcano 1,666 meters (5,466 ft) in height, its crater is 3–4 kilometers (1.9–2.5 mi) in diameter.
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Subduction zones are plate tectonic boundaries where two plates converge, and one plate is thrust beneath the other. This process results in geohazards, such as earthquakes and volcanoes.
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convergent plate boundary. [ kən-vûr′jənt ] A tectonic boundary where two plates are moving toward each other. If the two plates are of equal density, they usually push up against each other, forming a mountain chain.
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The Reykjanes Ridge (RR) separates the North American and Eurasian plates in the north Atlantic south of Iceland (Fig. 1). It is the longest oblique spreading ridge in the world, extending about 900 km from Iceland to the Bight transform fault near 56.5°N.
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Most active divergent plate boundaries occur between oceanic plates and exist as mid-oceanic ridges. Divergent boundaries also form volcanic islands, which occur when the plates move apart to produce gaps that molten lava rises to fill.
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['Convergent boundaries: where two plates are colliding. Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust. ... ', 'Divergent boundaries – where two plates are moving apart. ... ', 'Transform boundaries – where plates slide passed each other.']
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The location where two plates meet is called a plate boundary. Plate boundaries are commonly associated with geological events such as earthquakes and the creation of topographic features such as mountains, volcanoes, mid-ocean ridges, and oceanic trenches.
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Subduction zones are plate tectonic boundaries where two plates converge, and one plate is thrust beneath the other. This process results in geohazards, such as earthquakes and volcanoes. ... The largest earthquakes on Earth occur at the interface between the two plates, called the megathrust.
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['Hot spots,', 'Divergent plate boundaries (such as rifts and mid-ocean ridges), and.', 'Convergent plate boundaries (subduction zones)']
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At a convergent plate boundary, when one plate is oceanic, there are large volcanoes. These volcanoes are found in lines that outline the subduction zone. Earthquakes also happen in these zones. The Aleutian Islands that border southern Alaska are an island arc.
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Natural phenomena such as earthquakes, mountain formation, and volcanoes occur at plate boundaries. Mountains are usually formed at what are called convergent plate boundaries, meaning a boundary at which two plates are moving towards one another. This type of boundary eventually results in a collision.
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Most divergent plate boundaries are underwater and form submarine mountain ranges called oceanic spreading ridges. While the process of forming these mountain ranges is volcanic, volcanoes and earthquakes along oceanic spreading ridges are not as violent as they are at convergent plate boundaries.
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The mainland of Iceland is just a few degrees south of the Arctic Circle. The Arctic Circle does, however, pass through Grímsey Island, which lies only 40 kilometers (25 miles) off the North coast of Iceland.
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Volcanoes and earthquakes are most likely to form along plate boundaries.