<HTML><HEAD> <META charset=US-ASCII http-equiv=Content-Type content="text/html; charset=US-ASCII"> <META content="MSHTML 6.00.2800.1264" name=GENERATOR></HEAD> <BODY style="FONT-SIZE: 10pt; FONT-FAMILY: Arial; BACKGROUND-COLOR: #ffffff"> <DIV> <DIV>In a message dated 1/31/2005 17:54:24 PM Pacific Standard Time, jacross@lamar.ColoState.EDU writes:</DIV> <BLOCKQUOTE style="PADDING-LEFT: 5px; MARGIN-LEFT: 5px; BORDER-LEFT: blue 2px solid"><FONT face=Arial>1) When Giantess registers on the seismograph, how big of an eartuquake<BR>does it create?  M 2.0?  1.0?<BR><BR>2) Years ago I remember hearing that prior to Giant Geyser's eruptions,<BR>the platform would shake and pound.  Yet I have not heard anybody mention<BR>this for perhaps the last 15 years.  Did this really happen?  And if so,<BR>does it still happen?<BR><BR>3) Does anyone have the URL for the Yellowstone photo files?  It appeared<BR>on the list last winter, but I have since lost it.</FONT></BLOCKQUOTE></DIV> <DIV> </DIV> <DIV>1. No idea from here.</DIV> <DIV> </DIV> <DIV>2. Since I (ah, hem) have yet to be there for the beginning of an eruption, I cannot say if things shake and pound. But I do recall numerous early describtions of such, from Grand and Beehive and almost everything else. And I have yet to experience any such. Writer's license, I think.</DIV> <DIV> </DIV> <DIV>3. <A href="http://www.nps.gov/yell/slidefile/thermalfeatures/">www.nps.gov/yell/slidefile/thermalfeatures/</A> gets you to the start of all the thermal stuff.</DIV> <DIV> </DIV> <DIV>Scott Bryan</DIV></BODY></HTML>