Talk:Devils Tower National Monument

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[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)

[edit] Falling Rocks?

This article reads, "Rocks are continually breaking off and falling from the steep walls. Seldom do entire columns fall, but on rare occasions they do."

My family and I were out at the tower just today and one of the Park Rangers told us that the last rock to fall on the north side was about 10,000 years ago. Given the freeze-thaw attack that almost certainly occurs in the Wyoming climate, I didn't quite believe him.

He also said there was a column on the south side that leans about 1 cm. per year and will someday break off.

Can someone verify the frequency of spall from this monolith? Jeffcityjoe 05:33, 12 July 2007 (UTC)

[edit] Similar structures

I removed the section "Similar structures" (see below) because the lead sentence is clearly wrong. Devils Tower is phonolite porphyry, not basalt. The rock was intruded far below the surface and cooled very slowly. Some of the content after the second sentence may be useable, but as written, it is an invitation to add a long list of superficially similar features that are unrelated geologically.

Although the basaltic columns are impressive, they are not unique. Basalt columns are a common volcanic feature, and they occur on many scales (faster cooling produces smaller columns). Other notable sites include Fingal's Cave in Scotland, the Garni gorge in Armenia, the Cyclopean Isles near Sicily, Giant's Causeway in Ireland, Devils Postpile National Monument in California, Basalt Prisms in Hidalgo, Mexico, Organ Pipes National Park in Victoria (Australia), the "Organ Pipes" formation on Mount Cargill in New Zealand, Castellfollit de la roca in Catalonia, Spain and the "Columnar Cape" (Russian: Mis Stolbchaty) on Kunashir, the southernmost of the Kurile Islands in Russia.

Walter Siegmund (talk) 15:32, 24 September 2007 (UTC)

I support your removal of this section. Cheers Geologyguy 16:01, 24 September 2007 (UTC)

[edit] Name

The article says

If Colonel Dodge intended the name "Devils Tower" to refer to a single devil, then proper grammar would indicate that the monument be called "Devil's Tower". It has been said that the apostrophe was omitted due to a clerical error on early governmental papers, and the version without the apostrophe became its legal, and therefore official, name.

My understanding is that very, very few official geographical names in the United States take the possessive apostrophe, and those few (such as Martha's Vinyard) are grandfathered in; otherwise the possessive apostrophe is not permitted. So all this seems like groundless speculation. Herostratus (talk) 16:48, 4 February 2008 (UTC)

I've removed it and added sourcing to the USGS for the policy of apostrophe elimination. It has been standard for over a century, even though the original reason for adopting the policy is unclear (there are several obvious practical reasons). In general, speculating like this on Wikipedia is discouraged. --Dhartung | Talk 05:45, 2 May 2008 (UTC)
Your edit looks good to me.[1] Walter Siegmund (talk) 23:08, 2 May 2008 (UTC)