Hilina Slump
http://dbpedia.org/resource/Hilina_Slump an entity of type: Thing
Le Hilina Slump (« effondrement de Hilina ») est un glissement de terrain d'un volume de 20 km3 sur l'île de Hawaï qui se décroche du versant sud du Kīlauea et glisse progressivement dans l'océan Pacifique à une vitesse moyenne de dix centimètres par an.
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The Hilina Slump, on the south flank of the Kīlauea Volcano on the southeast coast of the Big Island of Hawaiʻi, is the most notable of several landslides that ring each of the Hawaiian Islands. These landslides are the means by which material deposited at a volcano's vents are transferred downward and seaward, eventually spilling onto the seabed to broaden the island.
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Hilina Slump
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Hilina Slump
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The Hilina Slump, on the south flank of the Kīlauea Volcano on the southeast coast of the Big Island of Hawaiʻi, is the most notable of several landslides that ring each of the Hawaiian Islands. These landslides are the means by which material deposited at a volcano's vents are transferred downward and seaward, eventually spilling onto the seabed to broaden the island. Kīlauea's entire south flank, extending out to Cape Kumukahi, is currently sliding seaward, with some parts of the central portion (over looking the Hilina slump) moving as much as 10 centimeters (3.9 inches) per year, pushed by the forceful injection of magma and pulled by gravity. Current movement of the Hilina slump and recent volcanic activity, coupled with evidence of massive submarine slides in the geological past, has led to claims that megatsunamis might result if the south flank of Kīlauea should suddenly fail.
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Le Hilina Slump (« effondrement de Hilina ») est un glissement de terrain d'un volume de 20 km3 sur l'île de Hawaï qui se décroche du versant sud du Kīlauea et glisse progressivement dans l'océan Pacifique à une vitesse moyenne de dix centimètres par an.
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