The pacific plate moves towards the northwest. the plate moves the older volcanoes with it and so the hot spot produces new volcanoes.
Volcanic arcs form at plate subduction zones. Island arcs are volcanic islands that form over "hot spots" in the Earth's mantle. Because the islands are moving with the oceanic plate, they eventually are removed from the hot spot, forming a chain of islands in the direction of the plate movement.
It leaves an island arc or chain if the hot spot is in the ocean. A great example of this is the Hawaiian Island chain. There is another hot spot in the North American plate which now resides in Yellowstone National park. This hot spot simply leaves a chain of extinct volcanic areas as the continental plate moves over it.
hot spot volcanoes such as the Hawaiian island chain.
When a volcanic island chain is formed, the tectonic plate moves over a hotspot in the Earth's mantle. The hotspot remains stationary while the plate moves, resulting in a series of volcanic islands forming in a line as the plate moves over the hotspot.
Probably the pacific Plate. The permanent hot spots are revealed by chains of volcanic islands. The chain itself reveals the direction the plate is moving.
An island chain is a chain of islands that form in the middle of a plate. Example: Hawaii An island arc is a string of islands that form on a plate boundary. Example: Japan
Volcanic arcs form at plate subduction zones. Island arcs are volcanic islands that form over "hot spots" in the Earth's mantle. Because the islands are moving with the oceanic plate, they eventually are removed from the hot spot, forming a chain of islands in the direction of the plate movement.
Volcanic arcs form at plate subduction zones. Island arcs are volcanic islands that form over "hot spots" in the Earth's mantle. Because the islands are moving with the oceanic plate, they eventually are removed from the hot spot, forming a chain of islands in the direction of the plate movement.
The Hawaiian Island-Emperor Seamount Chain is primarily located on the Pacific Plate. This volcanic chain was formed as the Pacific Plate moved over a stationary hotspot in the Earth's mantle, resulting in the creation of the Hawaiian Islands and the seamounts to the northwest. The chain extends from the islands of Hawaii to the northwest, where it transitions into the Emperor Seamounts.
Easter Island is located on a hot spot, which is not a plate boundary. The hot spot has created a chain of volcanic islands, with Easter Island being one of them.
It leaves an island arc or chain if the hot spot is in the ocean. A great example of this is the Hawaiian Island chain. There is another hot spot in the North American plate which now resides in Yellowstone National park. This hot spot simply leaves a chain of extinct volcanic areas as the continental plate moves over it.
hot spot volcanoes such as the Hawaiian island chain.
When a volcanic island chain is formed, the tectonic plate moves over a hotspot in the Earth's mantle. The hotspot remains stationary while the plate moves, resulting in a series of volcanic islands forming in a line as the plate moves over the hotspot.
Probably the pacific Plate. The permanent hot spots are revealed by chains of volcanic islands. The chain itself reveals the direction the plate is moving.
A Hot spot is stationary in time and burns though the solid lithosphere creating an island through volcanic eruptions. The lithosphere is separated into plates that move around so if a hot spot occurs under an oceanic plate it forms a island and as the plate moves (and the hot spot does not) it forms a chain of islands (as the plate moves over the hot spot). This is how the Hawaiian chain is formed.
Volcanic arcs form at plate subduction zones. Island arcs are volcanic islands that form over "hot spots" in the Earth's mantle. Because the islands are moving with the oceanic plate, they eventually are removed from the hot spot, forming a chain of islands in the direction of the plate movement.
The growth of the Hawaiian island chain is primarily due to the movement of the Pacific tectonic plate over a hotspot in the Earth's mantle. As the plate moves, volcanic activity at the hotspot creates new islands, with the oldest islands in the chain found in the northwest and the youngest in the southeast.