The western Pacific region contains 22 independent island countries and territories spread over an area of 27.8 million km 2 . Pacific peoples have lived here for as long as 50,000 yr, developing isolated cultures with close relationships to the environment. Although food security is adequate, the region suffers from persistent poverty that places many in a precarious position. Beginning in the 1920s, geological surveys conducted pioneering studies geared toward development. Beginning in the mid-1990s, many aid donors shifted their focus away from science, leading to a depletion of geo-science capacity. Lately, regional organizations have made considerable headway in expanding scientific capacity. The Geoscience Division of the Secretariat of the Pacific Community plays a significant role in helping the region attract geoscience-related aid funding and stitching the dispersed geoscience communities together. Universities in the region, assisted by geoscientists abroad and private employers, are also playing a role. This paper describes three examples of how geoscience can contribute to inclusive sustainable development. One example explores deep-sea minerals as a new source of wealth generation and the challenges the region faces in developing capacity and addressing the environmental concerns of this new revenue stream. A second project in Kiribati has moved aggregate extraction from beaches only 3 m above sea level to sediment-rich lagoons, providing new options for the future. Lastly, the promises and benefits of sustainable geothermal and ocean thermal technology are described.

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.