Cave passages formed by a newly recognised type of mass movement: a gull tear (UBSS Proceedings v.24(2))
Proceedings » Volume 24 » Sub-volume 2
Self,C.A., 2008. Cave passages formed by a newly recognised type of mass movement: a gull tear.
UBSS Proceedings, 24(2) , pp 101-106 Download PDF.
Abstract: Sally's Rift is the most extensive landslip cave in the Great Oolite limestone of the Cotswolds. The cave was originally thought to be a simple rectilinear network, but new calculations show that it cannot have formed by mass movement in any single direction. A sequence of gulls leads almost directly into the hillside along an axis of mass movement spreading, whereby the rock masses on either side have moved in divergent directions – a gull tear.