convergent boundaries
Archipelagos are usually volcanic, forming along island arcs produced by subduction zones (or hot spots). They formed by tectonic activities when a tectonic plate moves over a hot- spot. the lava gets pushed and when there is enough, it rises to the surface of the water. as it cools it forms a pile (an island). the volcanic activity then stops but the plate carries on moving. so when it starts again, a new island is formed.... There are other processes involved in their construction: erosion, deposition and land elevation.
Magma gushes out of the earth and then it cools and becomes a volcano.
Hot spot volcanos. As these age they can become island chains and eventually subsurface seamount arcs if the hot spot is in the ocean.
Earthquakes are caused by strike-slip faults, which are the grinding of two tectonic plates past each other. Volcanoes are commonly caused at convergent subduction zones causing volcanic arcs or sometimes island arcs. This is not the only case of volcano formation however. Mountains are formed at continental-continental convergent boundaries at the pushing upward of tectonic plates. This would be the only case of mountain building. That is how the Himalayas formed, and Mt. Everest is still actually inching higher every year.
A compass is mainly used to draw perfect circles, but it can also be used to draw arcs of different sizes.
COnvERgEnT BounDarY
I thought the same which forms mountain ranges, 'constructive' plates.Volcanic Island arcs are found along subduction zones, wich occur at convergent boundaries.
A convergent plate boundary where subduction occurs.
constructive plate boundaries cause volcanoes.
Volcanic arcs form at plate subduction zones. Island arcs are volcanic islands that form over "hot spots" in the Earth's mantle. Because the islands are moving with the oceanic plate, they eventually are removed from the hot spot, forming a chain of islands in the direction of the plate movement.
They are where mid-ocean ridges occur. Island arcs are common features of convergent boundaries where two ocean plates meet. The boundary where two plates slide past each other, is a transform boundary. The density of the plates, is important at subduction zones, where the denser plate sinks below the less-dense plate, which is also a feature of convergent plates. Tectonic plates are part of the lithosphere, which floats on the asthenosphere.
Ocean Trenches, Island Arcs, Volcanic Mountain Chains, Magmatic Arcs.
This happens in front of Island Arcs and in at destructive plate boundaries.
Ocean Trenches, Island Arcs, Volcanic Mountain Chains, Magmatic Arcs.
Island arcs are formed from the subduction and melting of oceanic crust as it descends into the mantle underneath a less dense oceanic crust at a convergent plate boundary. The subduction results in the creation of undersea volcanoes which then rise above sea level. The resulting volcanoes create a string of islands called an island arc. The curve of an island arc echoes the curve of its deep-ocean trench.
Several things are characteristic of plate boundaries. Mountain and volcanoes are common at converging plate boundaries, as well as faults and earthquakes. mid oceanic ridges form when the edges of oceanic tectonic plates spread appart from each other. Island arcs form near the edges of a subducting tectonic plate.
Volcanic arcs form at plate subduction zones. Island arcs are volcanic islands that form over "hot spots" in the Earth's mantle. Because the islands are moving with the oceanic plate, they eventually are removed from the hot spot, forming a chain of islands in the direction of the plate movement.