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Mohorovičić-diskontinuiteten

Världskarta som visar jordskorpans tjocklek, från Moho till den fasta berggrundens yta.

Mohorovičić-diskontinuiteten (IPA: moxoroʋitʃitɕ), vanligtvis känd som Moho, betecknar gränsen mellan jordskorpan och manteln. Namngiven efter den kroatiske seismologen Andrija Mohorovičić.

Mohorovičić-diskontinuiteten är belägen 5–10 kilometer under djuphavsbottnen och 20–90 kilometer under kontinentalplattorna och det är i genomsnitt 35 kilometer mellan Moho och jordskorpans yta.[1]

Mohole kallades ett år 1966 nedlagt amerikanskt projekt i syfte att borra genom jordskorpan ner till manteln.[2]

Referenser

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  1. ^ James Stewart Monroe, Reed Wicander (2008). The Changing Earth: Exploring Geology and Evolution (5). Cengage Learning. sid. 216. ISBN 0-495-55480-4. http://books.google.com/?id=jFPMa4MxwJkC&pg=PA216 
  2. ^ Bra Böckers lexikon, 1978
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Mohorovičić-diskontinuiteten
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