File:P212915.jpg

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Canon Bridge, Hereford. Kettle hole in glacial moraine. The Canon Bridge area is underlain by gravels of the Devensian Kettle Moraine. This gives rise to a moundy topography with abundant kettle holes caused by the melting of sub-surface ice.

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current15:53, 14 May 2014Thumbnail for version as of 15:53, 14 May 20141,000 × 655 (208 KB)Dbk (Talk | contribs)Canon Bridge, Hereford. Kettle hole in glacial moraine. The Canon Bridge area is underlain by gravels of the Devensian Kettle Moraine. This gives rise to a moundy topography with abundant kettle holes caused by the melting of sub-surface ice.
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