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Ralph, you graciously pointed it out to me here in 2010. I actually
have a set of photos from that day I would like to get to you. If
you would email your snail mail address, I can get them shipped off
to you.<br>
<br>
Janet White<br>
<a class="moz-txt-link-abbreviated" href="mailto:janet@snowmoon.us">janet@snowmoon.us</a> <br>
<br>
<div class="moz-cite-prefix">On 2/8/2013 10:47 AM, Ralph Taylor
wrote:<br>
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<p class="MsoNormal"><span
style="font-size:11.0pt;font-family:"Calibri","sans-serif";color:#1F497D">I
do not seem to have digital images of Anemone, and have not
had time to dig through thousands of slides. The third vent
is currently sintered closed. It is in a line through the
south and north vents, and is the deepest of the
indentations in the rings of geyserite around “Big Anemone”,
about two or three feet to the northwest of Big Anemone.
The last time I looked (during the summer of 2011 while
cleaning the thermal features on Geyser Hill) the old third
vent was covered by smooth white sinter and it had trapped
some sandy particles. Some 15 or 20 years ago there was a
patch of dark microbial mat that occasionally bubbled during
eruptions, but I have not seen that for many years.<o:p></o:p></span></p>
<p class="MsoNormal"><span
style="font-size:11.0pt;font-family:"Calibri","sans-serif";color:#1F497D"><o:p> </o:p></span></p>
<p class="MsoNormal"><span
style="font-size:11.0pt;font-family:"Calibri","sans-serif";color:#1F497D">If
you stand on the boardwalk at the point nearest the vent of
Big Anemone the location of the third vent is at about the
four o’clock position.<o:p></o:p></span></p>
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style="font-size:11.0pt;font-family:"Calibri","sans-serif";color:#1F497D"><o:p> </o:p></span></p>
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