A hot spot, unlike other forms of volcanism that rely on plate subduction, is due to rising heat from a specific location in the mantle which is very localized, not broadly regionalized. The Hawaiian Islands are a great example of the resultant landforms created by a hot spot that exists under oceanic crust. While the crust moves over the hot spot due to plate tectonics, volcanic mountains build up on the ocean floor, eventually breaching the surface of the water. As the crust moves away, the existing volcanic mountains become inactive and are replaced with newer volcanic mountains, the older ones slowly eroding below the surface of the ocean.
A hot spot is an area of volcanic activity that occurs independently of tectonic plate boundaries. As a tectonic plate moves over a hot spot, a linear chain of volcanoes forms on the plate surface. The most well-known example of this is the Hawaiian Islands.
hot spot volcanoes such as the Hawaiian island chain.
The place where volcanoes form in the middle of plates is called a hot spot. Hot spots are areas of high volcanic activity caused by a rising plume of hot mantle material that melts through the Earth's crust, creating volcanic eruptions. An example of a hot spot is the Hawaiian Islands.
No. Katmai is associated with a subduction zone.
No, the Emperor Seamount Chain is not divergent. It is actually a series of volcanic seamounts and underwater mountains that were formed by a hot spot, which is an upwelling of molten rock from deep within the Earth's mantle.
Volcanoes shot out magma which cooled down to make the Hawaiian Islands.
hot spot volcanoes such as the Hawaiian island chain.
A hot spot is an area of volcanic activity that occurs independently of tectonic plate boundaries. As a tectonic plate moves over a hot spot, a linear chain of volcanoes forms on the plate surface. The most well-known example of this is the Hawaiian Islands.
The place where volcanoes form in the middle of plates is called a hot spot. Hot spots are areas of high volcanic activity caused by a rising plume of hot mantle material that melts through the Earth's crust, creating volcanic eruptions. An example of a hot spot is the Hawaiian Islands.
No. Katmai is associated with a subduction zone.
AnswerHawaii is a volcanic chain of islands formed over a 'hot spot' in the Earth's mantle. As the Pacific tectonic plate slowly moves over the hot spot, volcanoes rise from the seafloor, forming the islands. A new, future Hawaiian island is rising from the seafloor at this time. As the islands move away from the hot spot, the volcanoes become dormant, resulting in a chain of eroding mountains.
its a hot spot
Yes, it is not uncommon to find volcanoes at hot spots.
No, the Emperor Seamount Chain is not divergent. It is actually a series of volcanic seamounts and underwater mountains that were formed by a hot spot, which is an upwelling of molten rock from deep within the Earth's mantle.
Such volcanoes are hot spot volcanoes.
A hot spot is not on a volcano, it is something that can lead to volcano formation. The deeper you go into the earth, the hotter it gets. Sometimes especially hot material wells up from deep within the mantle in what is called a mantle plume. As the plume nears the crust some of it melts. This magma can rise through the crust to form volcanoes.
Hot spot volcanoes are not associated with plate interactions.