It is near the middle of the volcano
the islands of hawaii
A hot spot is formed on a point of the earths surface where strong upward convection currents or plumes of hot magma in the upper mantle push up below the plates of the lithosphere causing volcanic activity. no it doesn'twhen the mantle is weak
Magma forms at a hot spot due to the upwelling of hot mantle material from deep within the Earth. This heat source causes rock to melt, creating magma that can eventually make its way to the surface, forming volcanic eruptions. Hot spots are often associated with mantle plumes that bring heat from the core-mantle boundary to the surface.
The mantle hot spot located closest to a mid-ocean ridge is the Iceland hot spot. It is situated beneath the island of Iceland, which is positioned on the Mid-Atlantic Ridge. This unique location allows for volcanic activity driven by the hot spot to occur alongside the tectonic processes of the ridge, resulting in significant geological features and frequent eruptions. The interaction between the hot spot and the mid-ocean ridge is a prime example of how mantle plumes can influence plate tectonics.
A hot spot is an area where extra hot mantle material wells up from deep inside the mantle, forming magma that can lead to the formation of volcanoes. An eruption is an event in which a volcano ejects ash, gas, or molten rock. Most volcanoes are not associated with hot spots.
A geological hot spot is where hot magma rises from the earth's mantle, which creates volcanic activity.
A hot spot in the Earth's mantle.
a hot spot :)
Hot Spot
the islands of hawaii
Magma from deep within the mantle melts through the crust which is what causes hot spot volcanoes to form
A hot spot is formed on a point of the earths surface where strong upward convection currents or plumes of hot magma in the upper mantle push up below the plates of the lithosphere causing volcanic activity. no it doesn'twhen the mantle is weak
A hot spot. An example of a hot spot are the islands in Hawaii which were made from hot spots.
Magma forms at a hot spot due to the upwelling of hot mantle material from deep within the Earth. This heat source causes rock to melt, creating magma that can eventually make its way to the surface, forming volcanic eruptions. Hot spots are often associated with mantle plumes that bring heat from the core-mantle boundary to the surface.
The mantle hot spot located closest to a mid-ocean ridge is the Iceland hot spot. It is situated beneath the island of Iceland, which is positioned on the Mid-Atlantic Ridge. This unique location allows for volcanic activity driven by the hot spot to occur alongside the tectonic processes of the ridge, resulting in significant geological features and frequent eruptions. The interaction between the hot spot and the mid-ocean ridge is a prime example of how mantle plumes can influence plate tectonics.
mauna kea was born when a hot part of the mantle melted a hole in the lithospheric ocean crust and formed a hot spot this hot spot constantly is feeding fresh hot magma from the mantle in what is thought to be the meeting of two convection cells flowing opposite direction's.
A hot spot is an area where extra hot mantle material wells up from deep inside the mantle, forming magma that can lead to the formation of volcanoes. An eruption is an event in which a volcano ejects ash, gas, or molten rock. Most volcanoes are not associated with hot spots.