Suffosion is one of the two geological processes by which subsidence sinkholes or dolines are formed, the other being due to collapse of an underlying cave or void,[1] with most sinkholes formed by the suffosion process.[2] Suffosion sinkholes are normally associated with karst topography although they may form in other types of rock including chalk, gypsum and basalt. In the karst of the UK's Yorkshire Dales, numerous surface depressions known locally as "shakeholes" are the result of glacial till washing into fissures in the underlying limestone.[citation needed]
- ^ Waltham, T.; Bell, T.; Culshaw, M. (2005). Sinkholes and Subsidence. Berlin: Springer. ISBN 978-3540207252.
- ^ "Dolines and sinkholes". British Geological Survey. Retrieved February 21, 2011.