Pumice raft

Pumice rafts from the eruption of Fukutoku-Okanoba submarine volcano in 1986, seen from a ship
A piece of pumice

A pumice raft is a floating raft of pumice created by some eruptions of submarine volcanoes or coastal subaerial volcanoes.

Pumice rafts have unique characteristics, such as the highest surface-area-to-volume ratio known for any rock type, long term flotation and beaching in the tidal zone, exposure to a variety of conditions, including dehydration, and an ability to absorb many potentially advantageous elements/compounds. For at least these reasons, astrobiologists have proposed pumice rafts as a possible ideal substrate for the origin of life.[1]

Biologists have suggested that animals and plants have migrated from island to island on pumice rafts.[2][3]

  1. ^ Martin D. Brasier, Richard Matthewman, Sean McMahon and David Wacey. "Pumice as a Remarkable Substrate for the Origin of Life" Astrobiology. August 31, 2011
  2. ^ New Island and Pumice Raft, Tonga, NASA Earth Observatory photo with commentary, August 2006
  3. ^ Nunn, Patrick D. (2008). Vanished Islands and Hidden Continents of the Pacific. University of Hawai'i Press. p. 59. ISBN 978-0-8248-3219-3.

Pumice raft

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