File:Layering in tuff - geograph.org.uk - 1373512.jpg

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English: Layering in tuff — Wales.
  • Tuffs of the Ordovician Lower Rhyolitic Tuff Formation outcrop in resistant strata that have been polished by ice moving down from Cwm Uchaf.
  • Layering in these re-worked tuffs is evident because of the enhanced weathering of certain layers and features within the layers. The outcome is a rock with neat holes up to 50mm in diameter arranged in parallel bands.
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Source From geograph.org.uk
Author Jonathan Wilkins
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Jonathan Wilkins / Layering in tuff / 
Jonathan Wilkins / Layering in tuff
Camera location53° 04′ 52.6″ N, 4° 03′ 28″ W  Heading=135° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location53° 04′ 52.6″ N, 4° 03′ 28″ W  Heading=135° 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.
Attribution: Jonathan Wilkins
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current15:12, 28 February 2011Thumbnail for version as of 15:12, 28 February 2011640 × 480 (94 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Layering in tuff Tuffs of the Ordovician Lower Rhyolitic Tuff Formation outcrop in resistant strata that have been polished by ice moving down from Cwm Uchaf. Layering in these re-worked tuffs is ev

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