AGSO


Book Description




Survival in the South Pacific


Book Description

The true story of a young pilot who disappeared on a routine mission, resulting in a rescue attempt on a remote and inhospitable island in the South Pacific. In September 1943, as America began advancing from its foothold on Guadalcanal, a young American airman was lost in heavy weather over the South Pacific on what was expected to be a routine flight. In examining that loss and the events leading up to a rescue attempt on an island in the South Pacific, and bringing together societies utterly alien to each other, Survival in the South Pacific brings together the big themes of the Pacific War. Lieutenant Leonard Richardson and his comrades had been swept from their homes across America, trained at speed for war, and dispatched to one of the remotest places on the globe. American war plans in place when Pearl Harbor was attacked poorly reflected the capabilities of its military, and the limits imposed by America’s far-flung and indefensible territories. The “Germany First” policy had resulted in a deeply uncertain future for forces in the South Pacific and Australia—the United States was unprepared for the global war that came to it in late 1941, even as the pipeline of men and materiel began to fill. Young Allied and Japanese aviators, sailors, and soldiers, were not the only ones thrown into the swirling maelstrom of war that had engulfed the Pacific—the indigenous islanders were also immersed in a new reality. In bringing together individual stories of men at war, this book gives a new perspective on the Pacific War.










Volcanoes of the World


Book Description

This impressive scientific resource presents up-to-date information on ten thousand years of volcanic activity on Earth. In the decade and a half since the previous edition was published new studies have refined assessments of the ages of many volcanoes, and several thousand new eruptions have been documented. This edition updates the book’s key components: a directory of volcanoes active during the Holocene; a chronology of eruptions over the past ten thousand years; a gazetteer of volcano names, synonyms, and subsidiary features; an extensive list of references; and an introduction placing these data in context. This edition also includes new photographs, data on the most common rock types forming each volcano, information on population densities near volcanoes, and other features, making it the most comprehensive source available on Earth’s dynamic volcanism.




Encyclopedia of Geology


Book Description

Encyclopedia of Geology, Second Edition presents in six volumes state-of-the-art reviews on the various aspects of geologic research, all of which have moved on considerably since the writing of the first edition. New areas of discussion include extinctions, origins of life, plate tectonics and its influence on faunal provinces, new types of mineral and hydrocarbon deposits, new methods of dating rocks, and geological processes. Users will find this to be a fundamental resource for teachers and students of geology, as well as researchers and non-geology professionals seeking up-to-date reviews of geologic research. Provides a comprehensive and accessible one-stop shop for information on the subject of geology, explaining methodologies and technical jargon used in the field Highlights connections between geology and other physical and biological sciences, tackling research problems that span multiple fields Fills a critical gap of information in a field that has seen significant progress in past years Presents an ideal reference for a wide range of scientists in earth and environmental areas of study




Intra-oceanic Subduction Systems


Book Description

Recycling of oceanic plate back into the Earth's interior at subduction zones is one of the key processes in Earth evolution. Volcanic arcs, which form above subduction zones, are the most visible manifestations of plate tectonics, the convection mechanism by which the Earth loses excess heat. They are probably also the main location where new continental crust is formed, the so-called 'subduction factory' About 400f modern subduction zones on Earth are intra-oceanic. These subduction systems are generally simpler than those at continental margins as they commonly have a shorter history of subduction and their magmas are not contaminated by ancient sialic crust. They are therefore the optimum locations for studies of mantle processes and magmatic addition to the crust in subduction zones.