Towards the end of the Ice Age, Pendle has its own small glaciers. The evidence for this was a glacial moraine situated near Stainscombe Dole Hall. Unfortunately, the moraine was leveled during renovation work on the hall. The moraine can be seen on the right of this photo.
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Keywords:devensian, geology, glaciation, glaciation, ice age, lancashire, moraines, pendle, ribble valley, sabden, stainscombe dole hall
