Great Urswick and Urswick Tarn looking to Daisy Hill and the
village's former iconic sycamores
Great Urswick is an ancient village nestling beneath steeply rising ground to the north and east, where
within living memory its original ancient field patterns ascended the sloping ground
approximating to a radiating
fan from the settlement below. The village occupies three sides of a
rare 5.63 hectare marl tarn, the heritage
bequeathed to the village by glacial action. The
possibility of cavern collapses in the limestone below the
tarn can not be ruled out as a reason contributing to its presence.
The water entering the tarn is from a limestone catchment
and most rises from springs at its bottom. As a marl tarn it has
taken on an importance in modern times as a site for ecological and
scientific research. Within the settlement, regard for the tarn is, for most, based on its
undoubted visual amenity. It is also valued as a
location for course fishing and bird watching. But its
real importance linking it to the initial establishment of a
settlement was the provision of a dependable supply of
water, water both for the inhabitants of the settlement and,
importantly, their livestock. It was not until around
1900 that mains water came to the village sourced from high
ground on the nearby Furness Fells where the catchment is over
a different geology which then ensured soft water being delivered to a parish
which up to that time had been accustomed to hard water from
its local limestone catchment.