A volcano. In the middle of an ocean, it also sometimes forms islands (like Hawaii)
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∙ 14y agoWiki User
∙ 14y agovolcanoes will form. Possibly big enough to form islands, like Hawaii.
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∙ 9y agovolcanic hot spots form
When a volcanic island chain is formed, the tectonic plate moves over a hotspot in the Earth's mantle. The hotspot remains stationary while the plate moves, resulting in a series of volcanic islands forming in a line as the plate moves over the hotspot.
Tectonic plates that are located above mantle plumes are called hotspots. These hotspots are areas of volcanic activity that can create volcanic islands or seamounts as the tectonic plate moves over the stationary plume.
Yes, Hawaii is not located on a divergent boundary. The Hawaiian Islands were formed due to a hotspot, where a tectonic plate moves over a stationary mantle plume, creating a chain of volcanic islands.
Hot-spot volcanoes form at intraplate boundaries, where a plume of hot magma rises from deep within the mantle, creating volcanic activity away from tectonic plate boundaries.
Volcanoes at hot spots form due to magma plumes from deep within the Earth that rise and erupt through the crust. As the tectonic plate moves over the stationary hot spot, a chain of volcanoes is created, with the youngest volcano forming directly above the hot spot. Over time, as the plate continues to move, older volcanoes become more distant and inactive.
When a volcanic island chain is formed, the tectonic plate moves over a hotspot in the Earth's mantle. The hotspot remains stationary while the plate moves, resulting in a series of volcanic islands forming in a line as the plate moves over the hotspot.
The Hawaiian Islands are located over a hotspot, where a tectonic plate moves over a stationary mantle plume. This is not a plate boundary, but rather a volcanic hotspot chain that has formed the Hawaiian Islands as the Pacific Plate moves slowly over it.
mantle plume
The Hawaiian islands are the result of a hot spot beneath the Pacific Plate. Hot material rises from deep within the mantle and collects beneath the lithosphere. Some of it rises through the crust and erupts at the surface, forming volcanoes. Those volcanoes gradually build up into islands. As the plate moves over the hot spot the old volcanoes go extinct and new ones form.
Tectonic plates that are located above mantle plumes are called hotspots. These hotspots are areas of volcanic activity that can create volcanic islands or seamounts as the tectonic plate moves over the stationary plume.
Hot-spot volcanoes form at intraplate boundaries, where a plume of hot magma rises from deep within the mantle, creating volcanic activity away from tectonic plate boundaries.
Volcanoes at hot spots form due to magma plumes from deep within the Earth that rise and erupt through the crust. As the tectonic plate moves over the stationary hot spot, a chain of volcanoes is created, with the youngest volcano forming directly above the hot spot. Over time, as the plate continues to move, older volcanoes become more distant and inactive.
No, Yellowstone National Park is located on top of a hot spot, which is a plume of molten rock rising from the Earth's mantle. It is not located at a divergent plate boundary where tectonic plates are moving apart.
A mantle plume is a column of hot rock rising from deep within the Earth's mantle. As a tectonic plate moves over a stationary mantle plume, multiple volcanic islands can form successively as the plate shifts, creating a chain of volcanic activity. This process can lead to the creation of a volcanic island arc or a hot spot track.
Mountains can form over hot spots when a tectonic plate moves over a persistent plume of hot magma rising from deep within the Earth's mantle. As the plate moves, the magma pierces through its crust, causing volcanic activity that builds up over time to form mountains. This process can lead to the formation of volcanic chains or individual volcanoes, depending on the movement of the tectonic plate.
They can occur anywhere. For example the Hawaiian islands are caused by a hot spot thought to be created by a mantle plume and they are a very large distance away from any plate boundary. However some geophysicists also believe that Iceland sits atop a hotspot that is also caused by a mantle plume that coincidentally coincides with a tectonic plate boundary (the Mid-Atlantic-Ridge).
In the context of plate tectonics, a plume is a column of very hot magma, much hotter than the usual temperature of the mantle, that rises through the cooler magma because the heat causes it to expand and therefore to be less dense. When the rising magma reaches the crust, it exerts force on the crust and contributes to continental drift. It can also cause volcanoes. The Hawaiian chain is an example of islands that were produced by volcanoes that were all caused by the same plume. As the crustal plate moves, the plume strikes different parts of the crust.