File:Granite Dells, North of Prescott, Arizona (101308458).jpg

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The Granite Dells is a geological feature north of Prescott, Arizona. The Dells consist of exposed bedrock and large boulders of granite that have eroded into an unusual lumpy, rippled appearance. Watson Lake and Willow Lake are small man-made reservoirs in this formation.

The Peavine National Recreation Trail follows the former railbed of the Santa Fe, Prescott & Phoenix Railway through the Granite Dells. This winding portion of the railroad was known as the "Peavine" because its twisting curves resembled that of a pea vine. It connects to the Iron King Trail, which follows the route of the old Prescott & Eastern Railroad through the eastern Granite Dells. Both are rail trail conversions.

The precambrian Dells' granite has been dated at 1.4 billion years old. Its pluton was intruded at a depth of around one or two miles (1.6 to 3.2 km). These cover rocks have since been eroded away. Weathering along joints produced the rounded boulders and other unusual rock formations that characterize the Granite Dells. This process is called spheroidal weathering, and is common in granitic terrains.

The Dells' granite has an unusually high uranium content, and thus homes built over the granite should be checked for radon leaking from the granite.

en.wikipedia.org/wiki/Granite_Dells

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Source Granite Dells, North of Prescott, Arizona
Author Ken Lund from Reno, Nevada, USA
Camera location34° 36′ 02.07″ N, 112° 25′ 30.56″ W Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
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This image was originally posted to Flickr by Ken Lund at https://flickr.com/photos/75683070@N00/101308458. It was reviewed on 3 December 2015 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-sa-2.0.

3 December 2015

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current21:40, 3 December 2015Thumbnail for version as of 21:40, 3 December 20151,600 × 1,200 (1.55 MB)INeverCry (talk | contribs)Transferred from Flickr via Flickr2Commons

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