Image:Toreva block bench in White Rock Canyon.jpg

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[edit] Summary

A large Toreva block bench several hundred feet below the level of the parent cliff in White Rock Canyon. In this case, the weaker base is the Tesuque Formation, the stronger overburden is the Cerros del Rio basalts, and the eroding agent is the Rio Grande River. I took this photo myself on 20 August 2006.

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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. Subject to disclaimers. This file is licensed under the Creative Commons Attribution ShareAlike license versions 2.5, 2.0, and 1.0. You may select the license of your choice.

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• (del) (cur) 03:50, 28 September 2006 . . Chyeburashka (Talk | contribs) . . 3072×2304 (1,993,147 bytes) (A large Toreva block bench several hundred feet below the level of the parent cliff in White Rock Canyon. In this case, the weaker base is the Tesuque Formation, the stronger overburden is the Cerros del Rio basalts, and the eroding agent is the Rio Grand)
• (del) (rev) 03:00, 21 August 2006 . . Chyeburashka (Talk | contribs) . . 640×480 (192,480 bytes) (A large Toreva block bench several hundred feet below the level of the parent cliff in White Rock Canyon. In this case, the weaker base is the Tesuque Formation, the stronger overburden is the Cerros del Rio basalts, and the eroding agent is the Rio Gran)

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• Image:Toreva block bench in White Rock Canyon.jpg

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