There's been a landslip from the bank behind the Uiskentuie Strand. This bank is comprised mainly of morainal material (sand and stones) left behind by a glacier and it was then cut back by the sea to the familiar steep slope. It rises at its highest point to about 90 feet, but most of it is about half that, including where the landslip has occurred.
Malcolm
Saturday 18 May 2013
Subscribe to:
Post Comments (Atom)
No comments:
Post a Comment