See more from this Division: Topical Sessions
See more from this Session: From San Salvador and Beyond: A Tribute to Don and Kathy Gerace and the Development of the Gerace Research Centre
Abstract:
The early karst research on San Salvador attempted unsuccessfully to apply continental models, which considered old, diagenetically-mature carbonates with significant imposed structure and adjacent non-carbonate lithologies. The first breakthrough, the flank margin cave model, explained the largest caves of San Salvador as the result of water mixing at the fresh-water lens boundaries, in a laminar-flow environment within young, porous, diagenetically-immature carbonates. A Friends Of Karst meeting at the GRC in 1988, and a Karst Waters Institute Paleokarst meeting there in 1995 presented these ideas to the karst science community, opening a new karst frontier.
Island karst research has advanced to successively more complex island settings: Isla de Mona, Puerto Rico, an uplifted carbonate island; the Mariana Islands, tectonically active with mixed carbonate and non-carbonate lithologies; and to the New Zealand and Croatian coasts with diagenetically-mature coastal carbonates. The result has been the development of the Carbonate Island Karst Model (CIKM), which takes into account the complexities of tectonics, geochemistry, rock maturity, and non-carbonate lithologies to explain island caves and karst globally. The karst of San Salvador Island is the gold standard base line of the CIKM.
See more from this Division: Topical Sessions
See more from this Session: From San Salvador and Beyond: A Tribute to Don and Kathy Gerace and the Development of the Gerace Research Centre