----- Original Message ----- From: Jeffrey Cross <jacross at lamar.ColoState.EDU> To: <geysers at wwc.edu> Sent: Thursday, July 28, 2005 1:27 PM Subject: [Geysers] Shoshone 17 July > Extremely low water was also noted in White Hot Spring, Sea Green Pool, and the UNNG > trumpet-shaped vent nearby, which has turned into a fumarole. > I agree, having been to Shoshone GB on July 16-- I got out my pictures from 2 years ago and started studying them however, to compare the water levels in Sea Green Pool from 2003 and 2005. I had to zoom in and closely examine the pictures in order to compare apples to apples, but the possible good news is that it does look to me like the 2005 picture shows slightly higher water levels that the 2003 picture.... just mere inches of difference. I have attached both pictures in hoping that someone might be able to confirm or deny, but in reducing the size of the images, some of the detail I can see on my computer screen has been lost in magnification. In the 2003 picture, the upper right corner of the actual pool corresponds to the upper left corner of the water level in the 2005 picture. There is some rust coloration on the roundish formations in the more recent image that do not appear to be present on the same formations from the 2003 pictures. Sea Green pool has not appeared to fluctuate in its water levels over the several minutes' observation I have dedicated to it on several occasions, but might it fluctuate over hours or days? Pictures taken the previous day on this year's backpacking trip (July 15) seem to show even higher water levels than on the 16th, but the west side of the pool was casting a shadow over the water surface on this day and the formations from pictures taken at that time are impossible to discern clearly. If the pool does fluctuate over hours or days, then all of this information may be of no great value, but is probably worth noting anyway. In other news, on the way out of Shoshone, we walked up to a major Lone Star eruption, and then hiked the little way to find Buried geyser. We sat and watched four eruptions, all of which seemed to be intermediates. All eruption durations (timed from first overflow to end of overflow into the runoff channel) ranged from 2 minutes 35 seconds to 3 minutes 5 seconds and all intervals (timed from end of end of overflow to beginning of overflow) ranged from 5-7 minutes. I also wish to thank Matthew McLean for directions and the downloaded picture 2 years ago to the hot spring with the complete bison skeleton in it. If I hadn't seen your picture we would never have found it this year as it looks like a pile of algae-covered rocks from every angle except directly facing it. I recognized the thermal feature from your picture but it still took a bit of searching around the pool to locate the skeleton. For the record, the skeleton sits on the shallow ledge on the west(ish) side of the hot spring called Great Crater. Great Crater is the very large spring to the east of Boiling Cauldron. Finding the poor deceased animal remains was the highlight of the trip for my 10 year old son. Mario Durrant _____________________________________________ > Geysers mailing list > Geysers at wwc.edu > https://mailman.wwc.edu/mailman/listinfo/geysers > -------------- next part -------------- A non-text attachment was scrubbed... Name: Sea Green Pool - Aug. 2003.JPG Type: application/octet-stream Size: 383635 bytes Desc: not available URL: </geyser-list/attachments/20050731/4021f7c9/attachment.obj> -------------- next part -------------- A non-text attachment was scrubbed... Name: Sea Green Pool - July 2005.JPG Type: application/octet-stream Size: 438797 bytes Desc: not available URL: </geyser-list/attachments/20050731/4021f7c9/attachment-0001.obj>