page_title: Littoral cone
hierarchical_section_title: Littoral cone
caption_attribution_description: English: Glow of lava is reflected in steam plume at water’s edge east of Kupapa‘u Point. A littoral cone formed by spatter from steam explosions sits on top of the sea cliff to the right.
context_page_description: Littoral cones are a form of volcanic cone. They form from the interaction between lava flows and water. Steam explosions fragment the lava and the fragments can pile up and form a cone. Such cones usually form on aa lava flows, and typically require large lava flows to form. They have been found on Hawaii and elsewhere.
  Littoral cones are semicircular cones which are breached in the direction of the lava flow that created them. They are formed by mounds of clasts that appear like cones without a crater. Littoral cones are constructed by volcanic ash, lava bombs and lapilli. Their component material is usually poorly sorted and can feature agglutinated structures and layering. Sometimes spatter-fed lava flows occur on such cones. They are formed by degassed hyaloclastite. The most common form found on Hawaii involves two semicircles on both sides of the lava flow that generated them; some such cones on Hawaii form a complete rim with diameters of 200–400 metres. Puu Ki on Hawaii has nested craters on top of a lava tube. Typically such cones are not larger than 800 metres wide and 75 metres high.
context_section_description: Littoral cones are a form of volcanic cone. They form from the interaction between lava flows and water. Steam explosions fragment the lava and the fragments can pile up and form a cone. Such cones usually form on aa lava flows, and typically require large lava flows to form. They have been found on Hawaii and elsewhere.
  Littoral cones are semicircular cones which are breached in the direction of the lava flow that created them. They are formed by mounds of clasts that appear like cones without a crater. Littoral cones are constructed by volcanic ash, lava bombs and lapilli. Their component material is usually poorly sorted and can feature agglutinated structures and layering. Sometimes spatter-fed lava flows occur on such cones. They are formed by degassed hyaloclastite. The most common form found on Hawaii involves two semicircles on both sides of the lava flow that generated them; some such cones on Hawaii form a complete rim with diameters of 200–400 metres (660–1,310 ft). Puu Ki on Hawaii has nested craters on top of a lava tube. Typically such cones are not larger than 800 metres (2,600 ft) wide and 75 metres (246 ft) high. Other smaller cones on Hawaii have diameters of 40 metres (130 ft) and heights reaching 15 metres (49 ft).
  Littoral cones not primary volcanic vents and distinguishing between a littoral cone and a primary vent can be difficult. A littoral cone forms when lava flows from land into water. Interaction between the water and the lava leads to steam explosions. These explosions throw lava fragments into the air; under favourable circumstances these fragments pile up on land and form a cone. This activity may resemble that of fire fountaining. Repeated phases of magma-water mixing lead to the formation of bedded deposits. The steam explosions can lead to the formation of Pele's hair. The forming lava flows need to be sufficiently large; the minimum size of lava flows that have formed such cones in Hawaii is 38,000,000 cubic metres (50,000,000 cu yd). Of these, about 5-6% of their volume is converted to fragments. Usually littoral cones are formed by aa lava as their fragmented nature allows ideal water-lava interactions, but pahoehoe and intermediary lavas can also form littoral cones. Other properties such as the speed of the lava flow and the structure of the flow front also influence the formation of littoral cones. Larger lava flow rates generate larger cones. In some littoral cones on Hawaii that were formed by pahoehoe lava flows, the collapse of a lava bench and subsequent steam explosions formed the cones instead. Pyroclastic flows can also form littoral cones, one such cone has been found on Lombok and formed during the 1257 Samalas eruption.
  Pseudocraters and littoral cones have been found on Iceland, Hawaii, Cerro Azul in the Gálapagos Islands, Deception Island, Antarctica, and Medicine Lake Volcano, California. Sometimes the words "pseudocrater" and "littoral cone" are used as synonyms. Littoral cones are usually quickly removed by sea erosion; thus littoral cones are rare.
  Prehistorical littoral cones have been found on the coast of Hawaii, where the volcanoes Mauna Loa and Kilauea face the sea. They were named "littoral cones" by Wentworth in 1938. About 50 large cones are found on these two volcanoes and only three of them were formed during historical times; no such cones have been found on the other Hawaiian volcanoes. The Puu Oo and Mauna Ulu eruptions of Kilauea have also formed small littoral cones.
  Examples of littoral cones include Sand Hills (1840 eruption) on Kilauea in Hawaii, 'Au'au, Nā Pu'u a Pele, Pu'u Hou (1868 eruption) and Pu'u Kī (eruption 1300 years ago) at Mauna Loa on Hawaii, a cone close to Villamil at Sierra Negra, Galapagos, several cones south of Krýsuvík and Eldborg (1800 years ago) at Hengill both on Iceland, a cone in the Winter Water unit of the Columbia Plateau Basalts, Oregon, several cones along the shores of Lake Kivu, a cone at Becharof Lake, Alaska, Burilan and Devil Rock on Gaua, and Ponta de Ferraria (eruption 840 ± 60 years ago) on São Miguel Island,
caption: A littoral cone lies on the right, on top of the cliffs
exif: {}