It is a chain of Shield Volcanoes.
The Hawaiian Islands are the "hang loose" chain of shield volcanoes.
Hawaii is a famous example, it holds volcanoes and is on the fire chain, the fire chain is a chain of volcanoes on the bordering plate tectonics.
They are most often found in the Aleutian Island chain.
If it is a single island, it is simply known as a volcanic island! If however it is a chain or string of separate islands then it may be a volcanic island arc (these form parallel to trenches at subduction zones) or a volcanic island chain (these form where a mantle plume creates a hotspot and may be in the centre of a tectonic plate. A good example would be the Hawaiian island chain). They can also form a cluster of islands (an archipelago) such as the Canary Islands (again formed by hotspot volcanism) in the Atlantic of the coast of Morocco.
It is a chain of Shield Volcanoes.
The Hawaiian Islands are the "hang loose" chain of shield volcanoes.
Hawaii is a famous example, it holds volcanoes and is on the fire chain, the fire chain is a chain of volcanoes on the bordering plate tectonics.
They are most often found in the Aleutian Island chain.
Hawaii is actually a chain of volcanoes!
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.
If it is a single island, it is simply known as a volcanic island! If however it is a chain or string of separate islands then it may be a volcanic island arc (these form parallel to trenches at subduction zones) or a volcanic island chain (these form where a mantle plume creates a hotspot and may be in the centre of a tectonic plate. A good example would be the Hawaiian island chain). They can also form a cluster of islands (an archipelago) such as the Canary Islands (again formed by hotspot volcanism) in the Atlantic of the coast of Morocco.
Shield volcanoes are found worldwide, particularly:North AmericaSouth AmericaEuropeAfricaThey can form over hotspots (points where magma from below the surface wells up), such as the Hawaiian-Emperor seamount chain and the Galápagos Islands, or over more conventional rift zones, such as the Icelandic shields and the shield volcanoes of East Africa. Many shield volcanoes are found in ocean basins, such as Tamu Massif, the world's largest, although they can be found inland as well.
The Hawaiian Islands are formed from a chain of volcanoes, some still active.
hot spot volcanoes such as the Hawaiian island chain.
hot spot volcanoes such as the Hawaiian island chain.
Shield volcanoes, so named for their broad, shield-like profiles, are formed by the eruption of low-viscosity lava that can flow a great distance from a vent. They generally do not explode catastrophically. Since low-viscosity magma is typically low in silica, shield volcanoes are more common in oceanic than continental settings. The Hawaiian volcanic chain is a series of shield cones, and they are common in Iceland, as well.