A volcanic hot spot forms from upwelling magma usually due to the subduction of a tectonic plate. As plates move over this area new volcanoes are formed.
+++
A hot spot alone is the top of a convection plume in the Mantle, not above subduction. This type of hot spot can lead to continental rifting.
Metamorphic rocks at hot spots will form mostly by contact and hydrothermal metamorphism as a result of exposure to heat from magma and interaction with hot water respectively.
Volcanoes located at hot spots form by lying directly above columns of hot rock that rise through Earth's mantle. As a tectonic plate moves over a mantle plume, rising magma causes a chain of volcanic islands to form.
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.
Hot mantle rock rises to fill rift zones. When rock rises, a decrease in pressure causes hot mantle rock to melt and form magma.
They form volcanic mountains by heating magma that breaks through the crust. On the oceanic plates, these crustal hot spots can form chains of volcanic islands such as the Hawaiian Islands.
The flow of molten magma is what causes varying hot spots on Earth. Hot spots are also known to heat water beneath the ground.
Metamorphic rocks at hot spots will form mostly by contact and hydrothermal metamorphism as a result of exposure to heat from magma and interaction with hot water respectively.
Magma from deep within the mantle melts through the crust which is what causes hot spot volcanoes to form
Volcanoes located at hot spots form by lying directly above columns of hot rock that rise through Earth's mantle. As a tectonic plate moves over a mantle plume, rising magma causes a chain of volcanic islands to form.
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.
Hot mantle rock rises to fill rift zones. When rock rises, a decrease in pressure causes hot mantle rock to melt and form magma.
They form volcanic mountains by heating magma that breaks through the crust. On the oceanic plates, these crustal hot spots can form chains of volcanic islands such as the Hawaiian Islands.
They are explained as 'hot spots' in the Earth's mantle, such as Yellowstone and the Hawaiian Island Chain, where heat from the Earth's interior is rising in a suspected current to the always moving crust.
magma from hot spots in the crust
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, hot spots can form in both oceanic and continental crust. Hot spots are areas of high volcanic activity that are thought to be caused by a deep-seated mantle plume that rises to the surface, creating a localized area of magma upwelling. These hot spots can create volcanic islands, such as the Hawaiian Islands, regardless of whether they are in oceanic or continental crust.
Metamorphic rocks are formed by continental plates colliding. These are Himalayan or Alps mountains. Sedimentary rock is also made into mountains when it is pushed up where tectonic plates collide.