Insights from previous karst studies of the relatively simple and stable carbonate islands of the Caribbean and Western Atlantic have been applied to develop the carbonate island karst model (CIKM), a general model with which we can interpret the karst of more complicated islands in the Western Pacific. This paper summarizes the karst of the five southernmost Mariana Islands in order of increasing complexity. All exhibit complicated histories of tectonic uplift and subsidence overprinted by glacio-eustasy. Each, however, is distinct and can be described in total or by subunit in terms of the four idealized carbonate island types defined in the CIKM: (1) simple carbonate island, (2) carbonate-cover island, (3) composite island, and (4) complex island. Aguijan is a simple carbonate island, but contains a probable phreatic-lift cave draining a confined aquifer. Tinian illustrates application of the CIKM to subunits: the northern lowland is a simple carbonate island area, while the southeastern ridge fits the carbonate-cover island category, and the central portion fits the composite island category. Rota is a composite island grading laterally from the volcanic core into a carbonate-cover island, thence to a simple carbonate island from the southwestern highland to the plains and terraces north and east. Northern Guam is a simple carbonate island ringing a carbonate-cover section, which contains a small composite island portion. Southern Guam exhibits composite and complex island features. Saipan is a complex island, where syndepositional volcaniclastic units interfingering with limestone are faulted to create isolated aquifers, including confined aquifers drained by phreatic-lift caves.

Abstract Lack of terrain data contributed significantly to the high costs of lives and operations during the Pacific campaign of World War II. After the war the U.S. Army Corps of Engineers contracted with the Military Geology Branch of the U.S. Geological Survey to gather detailed terrain information about the occupied islands under direct U.S. jurisdiction in the event they or comparable oceanic islands became sites of future military operations. The U.S. Geological Survey established a headquarters in Tokyo and initiated field studies of Okinawa during 1946. Subsequent detailed studies were launched at the Palau Islands (1947), Yap Islands (1947), Saipan (1948), Tinian (1949), Guam (1951), Pagan, Marianas Islands (1954), Truk (1954), Ishigaki and Miyako (1955), and the Marshall Islands (reconnaissance, 1951). Initial plans for detailed studies of all mandated islands were abandoned for lack of time, but members of the field parties briefly visited nearly all. Field teams included geologists, hydrologists, soils scientists, a plant ecologist, and a climatologist. The Tokyo office gathered and translated existing Japanese literature about the islands; more than 600 articles were translated. A by-product was the establishment of a joint U.S.-Japanese project to compile and publish a series of 1:250,000 geologic maps of formerly held Japanese territories, including Korea, Manchuria, northeast China, southern Sakhalin Island, and the Kuriles. Results of the field studies were published in a series of military geology folios composed of both basic and interpretive chapters. U.S. Geological Survey professional papers presented many of the scientific results.