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Few areas of science can have changed as fast as geology has in the past forty years. In the first half of the last century geologists were divided, often bitterly, between the drifters and those who believed that the Earth and its continents were static. Neither side of this debate foresaw that the application of methods from physics, chemistry and mathematics to these speculations would revolutionize the study of all aspects of the Earth Sciences, and would lead to accurate and detailed reconstructions of world geography at former times, as well as to an understanding of the origin of the forces that maintain the continental movements.
Geomagnetism is the study of the earth's magnetic field: its measurement, variation in time and space, origins, and its use in helping us to understand more about our Earth. Paleomagnetism is the study of the record left in the rocks; it has contributed much to our understanding of the geomagnetic field's past behavior and many other aspects of geology and earth history.
The term ‘geomorphology’ arose in the Geological Survey in the USA in the 1880s and was possibly coined by those two great pioneers, J.W. Powell and WJ McGee. In 1891 McGee wrote: ‘The phenomena of degradation form the subject of geomorphology, the novel branch of geology.’ He plainly regarded geomorphology as being that part of geology which enabled the practitioner to reconstruct
Geographic Information Systems date from the 1960s, when computers were mostly seen as devices for massive computation. Very significant technical problems had to be solved in those early days: how did one convert the contents of a paper map to digital form (by building an optical scanner from scratch); how did one store the result on magnetic tape (in the form of a linear sequence of records representing the geometry of each boundary line as sequences of vertices); and how did one compute the areas of patches (using an elegant algorithm involving trapezia). Most of the early research was about algorithms, data structures, and indexing schemes, and, thus, had strong links to emerging research agendas in computer science.
The field of hydrological science deals with the occurrence, distribution, movement, and properties of water on the earth. The science of hydrology holds a unique and central place in the field of earth system science, intimately linked with other water-related disciplines such as meteorology, climatology, geomorphology, hydrogeology, and ecology. Beyond basic scientific interest, water quantity and water quality have become two of the most pressing environmental issues of our time.
The Encyclopedia of Islands is a comprehensive, complete, and authoritative reference dealing with all of the physical and biological aspects of islands and island habitats. Articles are written by researchers and scientifi c experts and provide a broad overview of the current state of knowledge on these fascinating places. Biologists, ecologists, geologists, climatologists, oceanographers, geographers, and zoologists have contributed reviews intended for students as well as the interested general public. In order for the reader to easily use this reference, the following summary describes the features, reviews the organization and format of the articles, and is a guide to the many ways to maximize the utility of this Encyclopedia. <...>
Accuracy is a measure of how close a measured value of a variable is to its true value. In the context of the mathematical geosciences, it could also be a measure of how close an estimated value of a variable is to the unknown true value at a given location when the estimate is obtained as some function of the measured data values.
This volume is offered in tribute to the memory of Rhodes W. Fairbridge, Senior Editor of the Encyclopedia of Earth Sciences Series, who sadly passed away before this encyclopedia could be completed. It was upon his recommendation and inspiration that this project was undertaken. Rhodes Fairbridge took a keen interest in paleoclimatology, which ties together many aspects of the geosciences. He wrote several articles especially for this encyclopedia, including a detailed history of paleoclimatology and “Earth Laws and Paleoclimatology”, which summarizes many of the ideas he had covered in his long and distinguished career. He was way ahead of his time in his early acceptance of Wegener's theory of continental drift, the role of orbital cycles in climate change (i.e., the Milankovitch theory), solar influences on climate, and recognition of general aridity during glacial periods.
The great 19th-century geologist and natural historian, Charles Lyell (1830), is generally credited as being the author of the concept of Uniformitarianism (see History of Quaternary Science). Simply stated, this concept says that ‘‘the present is the key to the past.’’ In other words, we may interpret the ancient history of the planet through our understanding of modern-day processes. This concept represented a major step forward in scientific thought, greatly influencing contemporary scientists, such as Charles Darwin (see History of Quaternary Science).