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 such as the Hawaiian island chain.
One famous example of hot spots is the Hawaiian Islands. These islands were formed by a hot spot in the Earth's mantle that has created a chain of volcanic islands as the Pacific Plate moves over it. The most well-known island in this chain is Hawaii, which is home to the active volcano Kilauea.
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.
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.
The volcanoes in both Yellowstone and Hawaii are associated with hot spots. These are areas of especially hot mantle where some melting occurs. In Hawaii the hot spot melts oceanic crust, creating basaltic magma that most erupts effusively. In Yellowstone the hot spot melts continental crust, creating viscous rhyolitic magma that erupts explosively.
Volcanoes shot out magma which cooled down to make the Hawaiian Islands.
hot spot volcanoes such as the Hawaiian island chain.
One famous example of hot spots is the Hawaiian Islands. These islands were formed by a hot spot in the Earth's mantle that has created a chain of volcanic islands as the Pacific Plate moves over it. The most well-known island in this chain is Hawaii, which is home to the active volcano Kilauea.
cuz there wicked hot!
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.
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.
All of the active and inactive volcanoes that are part of the Hawaiian-Emperor Seamount chain are shield volcanoes. Shield volcanoes are the result of Hot Spot volcanism which is the type of volcanic force that created the Hawaiian islands.
The volcanoes in both Yellowstone and Hawaii are associated with hot spots. These are areas of especially hot mantle where some melting occurs. In Hawaii the hot spot melts oceanic crust, creating basaltic magma that most erupts effusively. In Yellowstone the hot spot melts continental crust, creating viscous rhyolitic magma that erupts explosively.
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.
Volcanoes are a special feature on Mars because they suggest that plate tectonics may have played a part in shaping Mars' geology in the past. There are volcano chains on mars similar to Hawaiian island chain. The chain of volcanoes is created from a hot spot underneath the plates as the plate moves across the hot spot a new volcano is formed until the plate moves again to create a new location for yet another volcano all of which are in a chain
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.
Hang Loose Chain is a group of young shield volcanoes located on the Big Island of Hawaii. They were formed by the eruptions of Mauna Loa and Kilauea volcanoes over the past few hundred years. The chain is characterized by low, broad volcanoes with gentle slopes, typical of shield volcanoes.