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In the 400 years of its modern history the Netherlands has produced a distinguished array of eminent mathematicians, scientists and medical researchers including many Nobel-prize winners and other internationally recognised figures, from Stevin, Snel, and Huygens in the 17th century to Lorentz, Kammerlingh Onnes, Buys Ballot, De Vries, de Sitter, and Oort in the 19th and 20th centuries. Yet it has often been noted that the history of science in the Netherlands is underepresented in the international literature. The handbook A History of Science in The Netherlands aims to correct this situation by providing a chronological and thematic survey of the field from the 16th century to the present, essays on selected aspects of science in the Netherlands, and reference biographies of about 65 important Dutch scientists. Written by more than 10 experts from Europe and North America, the handbook is the standard English-language reference work for the field.
A witty, irreverent guide to the birth, development, and state-of-the-art of one of the most important theories in Earth Science. The book explains how modern plate tectonics accounts for phenomena such as great earthquakes, tsunamis, volcanic eruptions, and how it controls conditions at the Earth's surface, including global geography and climate.
This book deals with sedimentary sulfides which are the most abundant authigenic minerals in sediments. Special emphasis is given to the biogeochemistry that plays such a central role in the formation of sedimentary sulfides. It will be of interest to scientists in a number of disciplines, including geology, microbiology, chemistry and environmental science. The sulfur system is important to environmental scientists considering the present and future effects of pollution and anoxia. The development of the sulfur system – particularly the characteristics of ocean anoxia over the last 200 Ma – is useful in predicting the future fate of the Earth surface system as well as in understanding the past. The biochemistry and microbiology of the sulfur system are key to understanding microbial ecology and the evolution of life. - First monograph on sedimentary sulfides, covering the ancient and modern sedimentary sulfide systems - Comprehensive, integrating chemistry, microbiology, geology and environmental science - All key references are included and discussed
A masterful biography of Alfred Wegener (1880–1930), the German scientist who discovered continental drift. Winner of the CHOICE Outstanding Academic Title of the Choice ACRL Alfred Wegener aimed to create a revolution in science which would rank with those of Nicolaus Copernicus and Charles Darwin. After completing his doctoral studies in astronomy at the University of Berlin, Wegener found himself drawn not to observatory science but to rugged fieldwork, which allowed him to cross into a variety of disciplines. The author of the theory of continental drift—the direct ancestor of the modern theory of plate tectonics and one of the key scientific concepts of the past century—Wegener al...
The shifting continents of the Earth are heading for inevitable collision: 250 million years from now, all the land masses on this planet will come together in a single, gigantic supercontinent which no human is ever likely to see. That future supercontinent will not be the first to form on Earth, nor will it be the last. Each cycle lasts half a billion years, making it the grandest of all the patterns in nature. It is scarcely a century since science first understood how Pangaea, the supercontinent which gave birth to dinosaurs, split apart, but scientists can now look back three-quarters of a billion years into the Earth's almost indecipherable past to reconstruct Pangaea's predecessor, an...
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1919/28 cumulation includes material previously issued in the 1919/20-1935/36 issues and also material not published separately for 1927/28. 1929/39 cumulation includes material previously issued in the 1929/30-1935/36 issues and also material for 1937-39 not published separately.
Over the course of the twentieth century, scientists came to accept four counterintuitive yet fundamental facts about the Earth: deep time, continental drift, meteorite impact, and global warming. When first suggested, each proposition violated scientific orthodoxy and was quickly denounced as scientific—and sometimes religious—heresy. Nevertheless, after decades of rejection, scientists came to accept each theory. The stories behind these four discoveries reflect more than the fascinating push and pull of scientific work. They reveal the provocative nature of science and how it raises profound and sometimes uncomfortable truths as it advances. For example, counter to common sense, the E...