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Hydrothermal vents are distributed along the Earth's plate boundaries, although they may also be found at intra-plate locations such as hotspot volcanoes. As of 2009 there were approximately 500 known active submarine hydrothermal vent fields, with about half visually observed at the seafloor and the other half suspected from water column ...
[1] [20] Its potential habitat across all Indian Ocean hydrothermal vent fields has been estimated to be at most 0.27 square kilometres (67 acres), while the three known sites at which it has been found, between which only negligible migration occurs, [38] add up to 0.0177 square kilometres (4.4 acres), [1] or less than one-fifth of a football ...
A volcanic plug, also called a volcanic neck or lava neck, is a volcanic object created when magma hardens within a vent on an active volcano. When present, a plug can cause an extreme build-up of high gas pressure if rising volatile -charged magma is trapped beneath it, and this can sometimes lead to an explosive eruption.
The secondary defense involves pushing away from the bottom of the seafloor and then drifting back down once the threat has dissipated. V. hydrothermalis uses its front arms (I dorsal and II dorsolateral) to detect and catch prey. The back arms (III ventrolateral and IV ventral) function to support the weight of the vent octopus and move it ...
Researchers speculate that Davidson Seamount is an ideal habitat for deep-sea corals and sponges because it has favorable bottom rock (bare lava rock), a steady food supply (supplied by a water current favoring the seamount; see the section above), and has not been disturbed by strong bottom currents than often bother other seafloor areas. [7]
The federal agency warned people to stay away from the bottom of ravines in case of mud and debris flows on the volcano prompted by heavy rain. Satellite footage shows the Popocatepetl volcano ...
A volcano needs a reservoir of molten magma (e.g. a magma chamber), a conduit to allow magma to rise through the crust, and a vent to allow the magma to escape above the surface as lava. The erupted volcanic material (lava and tephra) that is deposited around the vent is known as a volcanic edifice, typically a volcanic cone or mountain. [2] [22]
Mauna Kea (/ ˌ m ɔː n ə ˈ k eɪ ə, ˌ m aʊ n ə-/, [6] Hawaiian: [ˈmɐwnə ˈkɛjə]; abbreviation for Mauna a Wākea) [7] is a dormant shield volcano on the island of Hawaiʻi. [8] Its peak is 4,207.3 m (13,803 ft) above sea level, making it the highest point in Hawaii and the island with the second highest high point, behind New Guinea, the world's largest tropical island with ...