Article View: sci.misc
Article #337max. mountain height; was Re: alternative to plate tectonics
From: cdaf
Date: Fri, 12 Dec 1986 23:50
Date: Fri, 12 Dec 1986 23:50
24 lines
1930 bytes
1930 bytes
In article <648@bath63.ux63.bath.ac.uk> ma_jpb@ux63.bath.ac.uk (Bennett) writes:
>[...]
> Given we can work out the kinetic
>energy of the plate, we can calculate the height of the mountains this would
>raise if converted to potential energy with 100% efficiency.
There seems to be a limit to the height of the mountains. If I remember
correctly from freshman physics, Everest is close to the theoretical height
of a mountain. This is because the intense pressure sustained by the rock
supporting the mountain has brought it to nearly melting temperatures.
Obviously this is only applicable to the rock deep inside the base region of
the mountain, upon which most of the stress falls.
I'm lead to wonder whether a molten inner base of a mountain (due to stress)
would cause the mountain to collapse, or if the molten portion could be
successfully contained by the less-strained base of the mountain?
-charles
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Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Path: arc1-ca.pugleaf.net!utzoo!watmath!clyde!cuae2!ihnp4!inuxc!iuvax!cdaf From: cdaf@iuvax.UUCP Newsgroups: sci.misc Subject: max. mountain height; was Re: alternative to plate tectonics Message-ID: <2207@iuvax.UUCP> Date: Fri, 12-Dec-86 18:50:34 EST Article-I.D.: iuvax.2207 Posted: Fri Dec 12 18:50:34 1986 Date-Received: Mon, 15-Dec-86 20:50:31 EST References: <531@weitek.UUCP> <1272@cit-vax.Caltech.Edu> <1273@cit-vax.Caltech.Edu> <648@bath63.ux63.bath.ac.uk> Reply-To: cdaf@iuvax.UUCP (Charles Daffinger) Organization: Indiana University, Bloomington Lines: 24 Keywords: plate tectonics, continental drift