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Post by retaja5e on Nov 16, 2014 13:09:08 GMT
Pillow lava: Pillow lavas are volumetrically the most abudant type because they are erupted at mid-ocean ridges and because they make up the submarine portion of seamounts and large intraplate volcanoes, like the Hawaii-Emperor seamounts chain. Pahoehoe: Pahoehoe is the second most abundant type of lava flow. Pahoehoe lava is characterized by a smooth, billowy, or ropy surface. Pahoehoe flows tend be relatively thin, from a few inches to a few feet thick Volcanoes.docx (122.16 KB) Done By: Retaj Ali Hussain G5E
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