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, and therefore the site of coastal cave development changes through time. Coastal caves form for two main reasons. First, wave and salt attack on any rocky coast can excavate simple hollows and chambers, called sea caves or littoral caves, in a variety of rock materials. Second, on limestone coasts, the dissolution of the rock by the mixing of freshwater and seawater can create complex cave systems called flank margin caves. Blue holes also form in limestone coastal regions from a variety of processes. Safe cave exploration in any environment requires ...
Mixing between meteoric water and sea water produces brackish to saline water in many coastal aquife...
Coastal lagoons are inland water bodies, found on all continents, usually oriented parallel to the c...
Caves and associated dissolution features provide a valuable resource and geological record for pale...
Coastal karst cave development globally is biased towards the tropics and subtropics, where carbonat...
Caves on carbonate islands are useful indicators of past sea level because cave formation is depende...
The coastal scenery of the Northeastern Adriatic sea is widely interested by caves and related coast...
Underwater caves may yield valuable information on changes in sea level, as they can track the posit...
This chapter presents a simple model for environmental succession in coastal karst basins (CKB) unde...
Flank margin caves owe their formation to fresh and marine water mixing, inducing corrosion processe...
Extensive flooded cave systems are developed in a zone 8–12 km inland of the east coast of the Yucat...
Almost 20% of Italy is characterized by the outcropping of carbonate massifs ranging in age from Cam...
Coastal karst is characterized by special geomorphologic and hydrodynamic conditions as well as by p...
San Salvador (Bahamas) is a carbonate island with dozens of flank margin caves formed in the phreati...
Marine caves are unique and vulnerable habitats, threatened by multiple global and local disturbance...
Coastal karst areas often host many indices of past sea level changes, such as marine terraces, foss...
Mixing between meteoric water and sea water produces brackish to saline water in many coastal aquife...
Coastal lagoons are inland water bodies, found on all continents, usually oriented parallel to the c...
Caves and associated dissolution features provide a valuable resource and geological record for pale...
Coastal karst cave development globally is biased towards the tropics and subtropics, where carbonat...
Caves on carbonate islands are useful indicators of past sea level because cave formation is depende...
The coastal scenery of the Northeastern Adriatic sea is widely interested by caves and related coast...
Underwater caves may yield valuable information on changes in sea level, as they can track the posit...
This chapter presents a simple model for environmental succession in coastal karst basins (CKB) unde...
Flank margin caves owe their formation to fresh and marine water mixing, inducing corrosion processe...
Extensive flooded cave systems are developed in a zone 8–12 km inland of the east coast of the Yucat...
Almost 20% of Italy is characterized by the outcropping of carbonate massifs ranging in age from Cam...
Coastal karst is characterized by special geomorphologic and hydrodynamic conditions as well as by p...
San Salvador (Bahamas) is a carbonate island with dozens of flank margin caves formed in the phreati...
Marine caves are unique and vulnerable habitats, threatened by multiple global and local disturbance...
Coastal karst areas often host many indices of past sea level changes, such as marine terraces, foss...
Mixing between meteoric water and sea water produces brackish to saline water in many coastal aquife...
Coastal lagoons are inland water bodies, found on all continents, usually oriented parallel to the c...
Caves and associated dissolution features provide a valuable resource and geological record for pale...