At the end of the Ice Age event there was a period of intense cold. This resulted in freeze-thaw action on rocks producing large amounts of scree and in the Conwy and Sychnant areas, huge boulders were spilt by this action.
No EXIF information is available
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Keywords:conwy mountain, cymru, freeze-thaw, geology, ice, ice age, snowdonia, split rocks, sychnant, wales
