Rocky coastal regions can host caves produced by karst (dissolutional) processes, and
caves produced by pseudokarst (non-dissolutional) processes. On limestone coasts, which …

The island of Barbados is composed of a series of stepped Pleistocene carbonate terraces
that overlie Oligocene-Miocene chalk that is draped over deformed deep-sea clastics of …

Coastal karst cave development globally is biased towards the tropics and subtropics, where
carbonate deposition is ongoing, and therefore carbonate coasts are common. The …

Anchialine caves in coastal locations develop in two ways: by pseudokarst processes that
form talus caves, sea caves, tafoni, fissure caves and lava tubes, and by karst dissolutional …

Coastal caves are, by definition, caves that form along the coast as a result of the interaction
of terrestrial and marine processes. Sea level can fluctuate, both globally as well as locally …

Carbonate rock coasts are found world-wide, from continental shorelines of the Adriatic Sea
of Europe to the Yucatan Peninsula of North America, and on tropical islands from …

Pseudokarst caves form by fluid flow (rheogenic—lava tubes and glacier caves); particle
disarticulation (suffusion or piping caves, tafoni); by large-scale rock failure (fracture or …

Sea caves have been documented in all four states on the Pacific coast of the United States.
By far the most extensive written documentation, along with cave surveys, is from California …

Coastal areas on carbonate islands commonly contain two types of caves: sea caves
developed by wave erosion processes, and flank margin caves developed by dissolution at …

Blomstrandsøya, at Kongsfjord (780 57'N), Spitsbergen, is within the high arctic, a
completely permafrozen zone. The bedrock consists of Paleozoic marbles and has yielded a …