Comment:
This wide-angle photograph is taken from the lower northern slope of
Beacon Hill, the largest drumlin in rural Low Furness. Mere
Tarn is a small but permanent body of open water which is drained
from the surrounding bedrock of limestone and from the elevated
ground of the encircling drumlins. The drumlins were deposited
when the last ice age melted from around 14000 years ago and consist
of debris carried by glacial events and movement from the valleys
around Coniston in the Lake District approximately 28 km to the
north. In the distance behind Mere Tarn is the village of
Scales and a short distance south of Mere Tarn is Gleaston Castle.
The castle no doubt used as its water supply a constantly flowing
emergence from the western side of Beacon Hill which is in close
proximity to the castle.