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<DIV>Radiator is not down the slope -- it was, after all, in the old parking
area, and the vent is little more than a hole and not an open
crater. Judging by the photos, this appears to be Bank Geyser.</DIV>
<DIV> </DIV>
<DIV>Scott Bryan</DIV>
<DIV> </DIV>
<DIV>
<DIV>In a message dated 10/9/2012 8:01:52 P.M. US Mountain Standard Time,
wolveslax65@comcast.net writes:</DIV>
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<DIV>Gazers, </DIV>
<DIV> </DIV>
<DIV> The past few times I have been in the UGB I have seen
a geyser (more of a bulger though) on the downward slope off of the Daisy
complex. This spring was the first time I had seen the feature. It was when
waiting at Daisy one morning and the rangers came up to make there first
prediction of the day for Daisy. One of the rangers noticed a bulging of water
over the top of the ridge when positioned by the information sign at the south
viewing area. After some discussion we came to the conclusion it was Radiator
Geyser. Currently I believe that is correct but now I am a but uncertain about
if the feature is Bank Geyser or Radiator Geyser. From the description
in T. Scott Bryan’s book the location fits better with Radiator but the
behavior fits more with Bank. I have attached a few pictures that I took
of it but they are not very good (date taken 9/22/2012). Also if anybody has
pictures or helpful discussion or descriptions of Bank or Radiator to compare
with the current feature that would be awesome.</DIV>
<DIV> </DIV>
<DIV>Thanks,</DIV>
<DIV> </DIV>
<DIV>Will
Boekel</DIV></DIV></DIV><BR><BR>_______________________________________________<BR>Geysers
mailing
list<BR>Geysers@lists.wallawalla.edu<BR>https://lists.wallawalla.edu/mailman/listinfo/geysers</FONT></BLOCKQUOTE></DIV></FONT></BODY></HTML>