HRS 8023 Boulders excavated from river bed Roeburndale below Salter
The boulders are mainly Carboniferous and local geology. They were transported from nearby fells by extreme rain weather events, in 1967 such a flood destroyed a nearby bridge. The rocks consist of sandstones, gritstones and local fossiliferous shales with plant remains.
No EXIF information is available
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Keywords:boulders, flash floods, floods, geology, lancashire, river, roeburndale, streams
