Comment:
This sizeable limestone erratic has dropped out of an eroded drumlin
and now sits on the shoreline of Morecambe Bay at Aldingham adjacent
to the still eroding drumlin which defines the boundary of the bay
at this point. It is almost certain that the erratic was
originally part of the exposed bedrock on what is now known as
Birkrigg Common 3.3 km to the north and approximately 130 m higher
than the shoreline. The striation marks and rounding bear
witness to the wearing action of the abrasive ice and embedded rock
debris as it passed by the rock when still part of the bedrock mass.
The rougher surfaces have escaped the abrasion by originally being
down-flow to the ice movement. Given that this is no longer
the case as the erratic sits on the beach, it indicates that after
it eventually capitulated to the great forces of the ice movement
and snapped off the bedrock, it must have rotated prior to settling
in its present position,