Xref: utzoo sci.bio:1449 sci.misc:2295 sci.research:464 Path: utzoo!utgpu!attcan!uunet!husc6!psuvax1!rutgers!mit-eddie!uw-beaver!cornell!rochester!pt.cs.cmu.edu!speech2.cs.cmu.edu!jgk From: jgk@speech2.cs.cmu.edu (Joe Keane) Newsgroups: sci.bio,sci.misc,sci.research Subject: Re: The Loch Ness Monster Keywords: Nessie Loch Ness passages Message-ID: <2576@pt.cs.cmu.edu> Date: 4 Aug 88 03:21:04 GMT References: <861@altger.UUCP> <31293@cca.CCA.COM> <2160@alliant.Alliant.COM> <34997@aero.ARPA> <7481@cit-vax.Caltech.Edu> <1507@aplcomm.jhuapl.edu> <7497@cit-vax.Caltech.Edu> Sender: netnews@pt.cs.cmu.edu Organization: Carnegie Mellon Computer Science Lines: 13 In article <7497@cit-vax.Caltech.Edu> wen-king@cit-vlsi.UUCP (Wen-King Su) writes: >Thanks for the number. If sea wather is 1.025 times heavier than fresh >water, then Loch Ness can be in equilibrium at 52 feet above sea level >if the hole is 2028 feet below sea level. We don't need equilibrium. If the hole were above that depth, fresh water would flow out of the loch. This isn't a problem as long as the flow is less than that of the various rivers which feed the loch. So let's go over there and measure the amount of water flowing in and out of the loch by the expected routes. If there were a discrepancy, we'd have evidence for the hole. --Joe