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The eruption plume of a volcano includes volcanic gas, ash, rock fragments, and air entrained into the plume.

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Chaz Stroman

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Volcanic activity as the lithosphere plate above a mantle plume continues to drift?

As the lithospheric plate moves over a stationary mantle plume, volcanic activity can occur at the hotspot created by the plume. As the plate drifts, new volcanic islands may form, while older ones become inactive and erode. This process leads to a chain of islands, such as the Hawaiian Islands, which illustrates the relationship between plate tectonics and volcanic activity. Overall, the continual movement of the plate results in a dynamic landscape shaped by both geological processes.


What happens as a tectonic plate moves over a plume?

A volcano. In the middle of an ocean, it also sometimes forms islands (like Hawaii)


Is it true that hotspots form where a plume of magma rises through the crust from mantle?

Yes, hotspots are geological phenomena where a plume of hot mantle material rises through the Earth's crust, creating localized volcanic activity. This results in the formation of volcanic centers and can lead to the creation of volcanic island chains, like the Hawaiian Islands.


What feature may for in an interpolate area over a rising plume of hot mantle material?

In an interpolated area over a rising plume of hot mantle material, one prominent feature that may form is a volcanic hotspot. This hotspot can lead to the creation of volcanic islands or chains, such as the Hawaiian Islands, as the tectonic plate moves over the stationary plume. Additionally, the intense heat and pressure can result in the melting of the crust, contributing to the formation of large igneous provinces or flood basalts.


A hot plume of mantle material which may extend to the core-mantle boundary produces a volcanic region a few hundred kilometers across called a?

A hot plume of mantle material that extends to the core-mantle boundary produces a volcanic region known as a "hotspot." These hotspots can lead to volcanic activity as the molten rock rises through the mantle and crust, resulting in the formation of islands or volcanic chains, such as the Hawaiian Islands. Hotspots are characterized by their ability to create volcanism independent of tectonic plate boundaries.

Related Questions

When A mantle plume extends up to the surface where there is a .?

When a mantle plume reaches the surface, it can create a hotspot, leading to volcanic activity. This can result in the formation of volcanic islands, like the Hawaiian Islands. Mantle plumes are a source of heat and material that contribute to the formation of new crust and landmasses.


Volcanic activity as the lithosphere plate above a mantle plume continues to drift?

As the lithospheric plate moves over a stationary mantle plume, volcanic activity can occur at the hotspot created by the plume. As the plate drifts, new volcanic islands may form, while older ones become inactive and erode. This process leads to a chain of islands, such as the Hawaiian Islands, which illustrates the relationship between plate tectonics and volcanic activity. Overall, the continual movement of the plate results in a dynamic landscape shaped by both geological processes.


What happens as a tectonic plate moves over a plume?

A volcano. In the middle of an ocean, it also sometimes forms islands (like Hawaii)


A mantle plume extends up to the surface where there is a what?

hot spot


What type of landform is formed by a mantle plume?

Hot spot and izzi rocks


Is it true that hotspots form where a plume of magma rises through the crust from mantle?

Yes, hotspots are geological phenomena where a plume of hot mantle material rises through the Earth's crust, creating localized volcanic activity. This results in the formation of volcanic centers and can lead to the creation of volcanic island chains, like the Hawaiian Islands.


What feature may for in an interpolate area over a rising plume of hot mantle material?

In an interpolated area over a rising plume of hot mantle material, one prominent feature that may form is a volcanic hotspot. This hotspot can lead to the creation of volcanic islands or chains, such as the Hawaiian Islands, as the tectonic plate moves over the stationary plume. Additionally, the intense heat and pressure can result in the melting of the crust, contributing to the formation of large igneous provinces or flood basalts.


What is the name of the cloud that volcanos make when they erupt?

The cloud of ash, gas, and rock fragments that is produced during a volcanic eruption is called a volcanic plume or eruption cloud.


Is a gas plume considered a volcanic eruption?

no


A hot plume of mantle material which may extend to the core-mantle boundary produces a volcanic region a few hundred kilometers across called a?

A hot plume of mantle material that extends to the core-mantle boundary produces a volcanic region known as a "hotspot." These hotspots can lead to volcanic activity as the molten rock rises through the mantle and crust, resulting in the formation of islands or volcanic chains, such as the Hawaiian Islands. Hotspots are characterized by their ability to create volcanism independent of tectonic plate boundaries.


How can one mantle plume form several volcanic islands?

Mantle plumes appear to remain nearly stationary. However, the lithospheric plate above a mantle plume continues to drift slowly. So, the volcano on the surface is eventually carried away from the mantle plume. The activity of the volcano stops because it has moved away from the hot spot that supplied it with magma. A new volcano forms, however, at the point on the plate's surface that is now over the mantle plume. Some mantle plumes are long and linear. As magma generated by these plumes rises through cracks in Earth's crust, a line of hotspot volcanoes forms. Unlike volcanoes that form individually as a plate moves over a mantle plume, hot-spot volcanoes that form in lines over a long plume do not have any particular age relationship to each another.Mantle plumes appear to remain nearly stationary. However, the lithospheric plate above a mantle plume continues to drift slowly. So, the volcano on the surface is eventually carried away from the mantle plume. The activity of the volcano stops because it has moved away from the hot spot that supplied it with magma. A new volcano forms, however, at the point on the plate's surface that is now over the mantle plume. Some mantle plumes are long and linear. As magma generated by these plumes rises through cracks in Earth's crust, a line of hotspot volcanoes forms. Unlike volcanoes that form individually as a plate moves over a mantle plume, hot-spot volcanoes that form in lines over a long plume do not have any particular age relationship to each another.


How did the Hawaiian chain island form?

The Hawaiian Island chain formed from a mantle plume and moving plates. The rising mantle plume causes crustal material to melt at depth, which results in volcanism and finally in the formation of a volcanic island. Since the Pacific Plate is in continuous (although slow) movement, the same mantle plume will cause volcanism subsequently in different places and this is expressed at the surface as a chain of volcanoes or volcanic islands.