Hawaii Hotspot Volcano
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In the geologic future loihi may eventually become fused with the island of hawaii which itself is composed of five volcanoes knitted together kohala mauna kea hualalai mauna loa.
Hawaii hotspot volcano. The southeasternmost part of the island of hawaii presently overlies the hot spot and still taps the magma source to feed its active volcanoes. After moving over the hotspot volcanic activity wanes maui and eventually ceases. Its molten rock fuels the eruption of this islands four active.
The hawaiian islandsthe emperor seamount chain develops as volcanoes form above the hawaiian hotspot and then ride away on top of the pacific plate. Loeihi seamount the active submarine volcano off the island of hawaiis south coast may mark the beginning of the zone of magma formation at the southeastern edge of the hot spot. Hot spot volcanism can occur in the middle of tectonic plates.
Over millions of years these layers form mountains of volcanic rock that eventually break the surface of the pacific ocean forming islands. The hawaii hotspot is a volcanic hotspot located near the namesake hawaiian islands in the northern pacific ocean. Under the hawaiian islands there is a volcanic hot spot a hole in the earths crust that allows lava to surface and layer.
Mauna loa volcano is the largest volcano on earth. One of the best known and intensively studied hotspots in the world the hawaii plume is responsible for the creation of the hawaiianemperor seamount chain a 6200 kilometer 3900 mi mostly undersea volcanic mountain range. An island emerges as lava erupts on the seafloor loihi and eventually piles up above sea level hawaii.
With the possible exception of maui the other hawaiian islands have moved northwestward beyond the hot spot they were successively cut off from the sustaining magma. Mauna loa erupted in 1984 and kilauea is considered to be one of the most active volcanoes on earth today. To the hotspot theory assuming loihi continues to grow it will become the next island in the hawaiian chain.
The hotspot is thought to lurk for now below the archipelagos youngest and most active landmass the big island of hawaii. This does not appear to be the case in the galapagos instead there is evidence of concurrent volcanism over a wide area. In hawaii the evidence suggests that each volcano has a distinct period of activity as the hotspot moves under that portion of the pacific plate before becoming dormant and then extinct and eroding under the ocean.
Today the big island of hawaii sits over the hot spot and has the only active volcanoes in that island group. Konala hualaiai mauna kea mauna loa and kilauea volcanoes have built the island over the last 500000 years. Only two of hawaiis volcanoes are active today mauna loa and kiluaea.
Thats unlike traditional volcanism which takes place at plate boundaries.
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