Here's some more thoughts on the arch that "went missing".

http://crosscut.com/blog/#16664

T.

-----Original Message-----
>From: Gill Ediger <[email protected]>
>Sent: Aug 11, 2008 5:27 PM
>To: [email protected]
>Subject: [Texascavers] Freeze/thaw collapse
>
>At 11:00 AM 8/11/2008, Louise Power wrote:
>>On the news this weekend, they called it "geology at work." Hope 
>>nobody was hiking underneath when it happened.
>
>When Mt. St. Helens blew up people were all agast at the devistation 
>and destruction and how terrible it was to human and animal life. 
>That's a pretty biased and one-sided view and a slap in the face of 
>geology which was hard a work just tending to normal business.
>
>I call it "land building"--geology at work, doing what it's supposed 
>to be doing: Building mountains and then moving them to the sea--one 
>grain at a time if need be. Geology doesn't give a damn if anybody 
>was hiking under the arch at the time it fell or not. People are 
>mostly insignificant vectors in the overall scheme of geologic 
>things--they help out a bit by tumbling rocks down the hillside 
>(getting them closer to the sea) whilst road building or just hiking, 
>or they throw rocks into the river whilst entertaining themselves 
>skipping stones. Otherwise human beings are of little concern in 
>geologic time or to geologic forces. Future limestone will contain 
>rubber tires and lost boat motors and mafia exiles encased in 
>concrete blocks--stuff like that.
>
>Freeze/thaw cycles on the surface of the rock play an important part 
>in the first stages of rock degradation there, Fritz. At least in 
>places where it freezes--like Utah. But you can't discount the daily 
>expansion/contraction due to the temperature changes in the ambient 
>atmosphere around the arch when considering what actions weakened it 
>enough to make it fall. Daily expansion and contraction (over a range 
>on the order of 50 or more degrees) would, I think, play a lot larger 
>part in the eventual blowing apart of a (nominal) monolithic chunck 
>of extremely exposed sandstone along internal joints and other zones 
>of weakness by eventually crunching itself into smaller and 
>subsequently insubstantial pieces, at some point being unable to 
>support itself any longer.
>
>That global warming (even though it was introduced to this discussion 
>as a subtle joke unnoticed by some humor impaired readers) could have 
>a very real effect on the differential values of expansion and 
>contraction due to thermal changes in the dynamic atmosphere must be 
>considered, and in a big way--no matter what is causing global 
>warming this time around.
>
>Doing my part for global warming,
>--Ediger     
>
>
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