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Blokk (geologi)

En blokk er, i geologisk betyding, sedimentære partikler med kornstørrelse over 256 mm i diameter.[1]

Blokktransport assosieres med svært energirike miljø. I dag ser man blokktransport i forbindelse med isbreer, massestrømmer, skred, fluvial transport og på spesielle strender.[trenger referanse]

Innen kvartærgeologi snakker man om blokkmark, en type dekke som kjennetegnes av store blokker med lite eller ingen finmateriale mellom blokkene.[1]

Referanser

[rediger | rediger kilde]
  1. ^ a b Sigmond, Ellen M. O. (2013). Norsk geologisk ordbok med engelsk-norsk ordliste. Trondheim: Akademika. ISBN 978-82-321-0151-1. 
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Blokk (geologi)
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