Talk:Devils Tower National Monument
From Wikipedia, the free encyclopedia
Devil's Tower National Monument, Devil's Tower
[edit] Odd erosion pattern
Can anyone explain why the top third of the tower is visibly much more eroded than the relatively-pristine lower two-thirds? If the tower was exposed by erosion of surrounding soft material, wouldn't there be a gradual change in the amount of erosion from the most-eroded top to the least-eroded bottom? And, can I justifiably eroded put any more erosions in this paragraph? —The preceding unsigned comment was added by 86.31.127.7 (talk) 05:19, 31 January 2007 (UTC).
[edit] Origin
Devil's Tower has, indeed, a volcanic origin. It was most likely, a "caldera" similar to Kilauea's, without having an external flow and, therefore, without any volcanic material around its crater. Most "calderas" have little gases and hot lava may erupt to a certain altitude, but always falling inside the crater. This process explains absence of volcanic debris around Devil's Tower. --Fev 04:08, 10 August 2006 (UTC)
[edit] Formation theory dissent, or original research?
The following two sentences require citation:
"The current popular theory, that the tower is an intrusive feature, does not really hold up under scrutiny. If the tower formed as an intrusion, then the columns should radiate out from the center instead of rising steeply."
These statements are preceded by:
"Geologists agree that Devils Tower was formed by the intrusion of igneous material."
They are then followed by:
"Geologists agree that the igneous material intruded and then cooled..."
This seeems contradictory. If geologists generally agree on a theory of formation which includes intrusion, then that "current popular theory" does indeed "hold up under scrutiny". There is room here for dissent, of course, but unless a dissenting theory has been published by geologists in a scientific journal, it would seem to violate WP:NOR. -Tobogganoggin talk 04:01, 3 January 2007 (UTC)