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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 (fr)
  • Hilina Slump (en)
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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. (fr)
  • 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. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/black_pog.svg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Hilina_Pali.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Kilauea-pp1801_4-2_excerpt.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Kilauea_cross-section_pp963.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Kilauea_gps-pp1801_1-13.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/USGS_Kīlauea_Hilina_slump.jpg
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