It is an undersea volcanco. Yes its apart of the hawaiian chain
The Loihi volcano is a type of volcano known as a shield, undersea volcano or a seamount. Such volcanoes form over hotspots while the sea floor moves over it.
KilaueaAnswerPericutin came up through a cornfield in Mexico in 1943. It now stands about 424 meters (1391 feet) above the level of the cornfield.
The plate tectonics theory is not relevant to the formation of the Hawaiian Islands, but the theory explains why the islands formed in a chain. According to the theory, the plates move constantly. This caused the islands to form in a chain, as the hot spot under them does not move.
The Hawaiian Islands are the "hang loose" chain of shield volcanoes.
The American islands that are actually an underwater chain of volcanoes are the Hawaiian Islands. These islands were formed by volcanic activity from the Hawaiian-Emperor seamount chain. The islands of Hawaii, Maui, Oahu, Kauai, and others are all part of this volcanic chain.
Loihi is a seamount; specifically an underwater volcano. It is definitely part of the Hawaiian chain.
The Loihi volcano is a type of volcano known as a shield, undersea volcano or a seamount. Such volcanoes form over hotspots while the sea floor moves over it.
The Hawaiian Islands are formed from a chain of volcanoes, some still active.
A new Hawaiian island, Loihi, will break the surface in roughly 18,000 years. Assuming that the USA and it's states are still intact at this time, Loihi will be a new island of the state of Hawaii.
Get back into formation, soldier! Volcanic activity is central to the formation of new islands in the Hawaiian chain.
KilaueaAnswerPericutin came up through a cornfield in Mexico in 1943. It now stands about 424 meters (1391 feet) above the level of the cornfield.
Yes. Currently a volcano named Loihi is building up off the coast of the big island. In a few hundred thousand years it will reach the ocean surface and form a new island.
Yes, south and east of the Hawaiian Island chain, a new island is being formed by volcanic activity, and has already been dubbed 'Loihi'. On the Big Island, both Mauna Loa and Kilauea are active volcanoes.
The youngest volcano of the Hawaiian chain is Loihi at about 400,000 years old. This volcano has not yet emerged above the ocean surface and remains at about 3,000 feet below sea level. It is expected to emerge as an island in a few tens of thousands of years.
Over very long periods of time, there may be the formation of a chain of volcanoes or volcanic islands. The Hawaiian Islands formed this way.
The Hawaiian Island chain formed from a mantle plume and moving plates. The rising mantle plume causes crustal material to melt at depth, which results in volcanism and finally in the formation of a volcanic island. Since the Pacific Plate is in continuous (although slow) movement, the same mantle plume will cause volcanism subsequently in different places and this is expressed at the surface as a chain of volcanoes or volcanic islands.
The plate tectonics theory is not relevant to the formation of the Hawaiian Islands, but the theory explains why the islands formed in a chain. According to the theory, the plates move constantly. This caused the islands to form in a chain, as the hot spot under them does not move.