Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Posting-Version: version B 2.10.1 exptools 1/6/84; site ihu1g.UUCP Path: utzoo!linus!decvax!harpo!ulysses!mhuxl!ihnp4!ihu1g!fish From: fish@ihu1g.UUCP (Bob Fishell) Newsgroups: net.misc,net.physics Subject: Re: What heats up the center of the earth? Message-ID: <277@ihu1g.UUCP> Date: Tue, 3-Apr-84 17:53:35 EST Article-I.D.: ihu1g.277 Posted: Tue Apr 3 17:53:35 1984 Date-Received: Thu, 5-Apr-84 03:21:55 EST References: <255@heurikon.UUCP> Organization: AT&T Bell Labs, Naperville, IL Lines: 23 You should properly be asking what keeps it from cooling off. The Earth was formed, along with the other planets of the Solar system, out of gravitational coalescence of floating gas, debris, dust, etc, as was the sun. It and many of the other planets have never cooled off from that time; originally, all the larger bodies in the Solar system were hot. Only the sun, and possibly Jupiter, were hot enough and heavy enough for sustained nuclear reactions to occur. This is why the sun shines and Jupiter appears to have an energy source at its core, while the other planets have cooled, or at least crusted over. This is an oversimplification; composition of the bodies is also a factor, but you get the idea. As to what keeps the Earth's core warm, all the silicate material in the planet's crust is a pretty good insulator. The planet doesn't radiate that heat very well, and in fact collects a good deal of what it does radiate from the sun. This does not necessarily imply a state of dynamic equilibrium, but the Earth is cooling only at a very slow rate. The USGS could probably give reasonable figures. -- Bob Fishell ihnp4!ihu1g!fish