Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Path: utzoo!watmath!clyde!cbatt!ihnp4!islenet!bob From: bob@islenet.UUCP (Bob Cunningham) Newsgroups: net.politics,net.sci Subject: Re: Re: Nuclear power and Alternatives: Geothermal Message-ID: <2792@islenet.UUCP> Date: Thu, 11-Sep-86 07:22:38 EDT Article-I.D.: islenet.2792 Posted: Thu Sep 11 07:22:38 1986 Date-Received: Sun, 14-Sep-86 06:14:26 EDT References: <715@curly.ucla-cs.ARPA> <953@whuts.UUCP> <2431@ihlpg.UUCP> <959@whuts.UUCP> <727@riccb.UUCP> Organization: Hawaii Institute of Geophysics Lines: 20 Xref: watmath net.politics:19106 net.sci:1590 > The main problem with geothermal wells is that you tend to have to dig > VERY deep wells. Few places exist where magma is close enough to the > surface to heat groundwater... It's surprising how many places are suitable: portions of the U.S. Pacific northwest, California, Japan, etc. along the "ring of fire" circling the Pacific Ocean, plus the Hawaiian islands (where there is very active development of geothermal sources). Not so surprisingly (given the geological conditions) those are precisely areas where coal generally isn't. The temperature difference doesn't have to be extreme, remember that ocean thermal energy conversion technology works with a relatively small thermal difference (though it does require lots of water, and thus its usefulness is primarily confined to ocean & nearshore sites between 35 degrees north or south of the Equator). -- Bob Cunningham {humu|ihnp4}!{islenet|uhmanoa}!bob cunninghamr%haw.sdscnet@LLL-MFE.ARPA Hawaii Institute of Geophysics, University of Hawaii