They were named " littoral cones " by Wentworth in 1938.
2.
Littoral cones not primary volcanic Pele's hair.
3.
The Puu Oo and Mauna Ulu eruptions of Kilauea have also formed small littoral cones.
4.
Littoral cones are semicircular cones which are breached in the direction of the lava flow that created them.
5.
Pseudocraters and littoral cones have been found on Iceland, Hawaii, sea erosion; thus littoral cones are rare.
6.
Pseudocraters and littoral cones have been found on Iceland, Hawaii, sea erosion; thus littoral cones are rare.
7.
Prehistorical littoral cones have been found on the coast of Hawaii, where the volcanoes Mauna Loa and Kilauea face the sea.
8.
Pyroclastic flows can also form littoral cones, one such cone has been found on Lombok and formed during the 1257 Samalas eruption.
9.
Littoral cones are another hydrovolcanic feature, generated by the explosive deposition of basaltic tephra ( although they are not truly volcanic vents ).
10.
Other properties such as the speed of the lava flow and the structure of the flow front also influence the formation of littoral cones.
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