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Alfred Wegener
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...
Alfred Wegener
Alfred Wegener studied astronomy and meteorology--and was even a record-holding balloonist--before he became famous for his theories on how the land and seas on Earth were formed and change. These ideas are continental drift and plate tectonics. Seeing that the continents fit together like a puzzle, Wegener proved the theory that all of Earth's continents were once connected. Although his theories weren't accepted until after his death, scientists use plate tectonics to explain volcanoes and many other changes on Earth.
Alfred Wegener
Many landforms make up Earths surface, including mountains, glaciers, deserts, and even coral reefs. Some scientists specialize in geomorphology, which is the study of landforms. Others who study the land can become mapmakers or geologists. Earth is constantly changing, which means there is always something new to learn. For more information, read Landforms, another book in the Mission: Science series.
The Origin of Continents and Oceans
A source of profound influence and controversy, this landmark 1915 work explains various phenomena of historical geology, geomorphy, paleontology, paleoclimatology, and similar areas in terms of continental drift. 64 illustrations. 1966 edition.
The Origin of Continents and Oceans
Alfred Lothar Wegener (1880-1930) was a German geophysicist and meteorologist. His research focused mainly on meteorology and polar research, however he is most remembered as the originator of the theory of continental drift, i.e. that the continents are slowly drifting around the Earth. His hypothesis was controversial and widely rejected by mainstream geology until the 1950s, when novel discoveries such as palaeomagnetism provided strong support for continental drift, which is the basis for today's model of plate tectonics. Third edition, originally published in 1924.
Alfred Wegener
In this appealing biography, children will read about the fascinating life, theories, and discoveries of Alfred Wegener. From his time in Greenland studying meteorology with hot balloons to his theory of Pangea, readers will be eager to learn more about Wegener's contributions to science and the strides he took towards developing the study of plate tectonics. The easy-to-read text, accessible glossary, helpful index, and intriguing facts work in conjunction with the lively images and captivating lab activity to engage readers from beginning to end!
Ending in Ice
An old truism holds that a scientific discovery has three stages: first, people deny it is true; then they deny it is important; finally, they credit the wrong person. Alfred Wegener's "discovery" of continental drift went through each stage with unusual drama. In 1915, when he published his theory that the world's continents had once come together in a single landmass before splitting apart and drifting to their current positions, the world's geologists denied and scorned it. The scientific establishment's rejection of continental drift and plate tectonic theory is a story told often and well. Yet, there is an untold side to Wegener's life: he and his famous father-in-law, Wladimir Köppen ...
The Mountain Mystery
Fifty years ago, no one could explain mountains. Arguments about their origin were spirited, to say the least. Progressive scientists were ridiculed for their ideas. Most geologists thought the Earth was shrinking. Contracting like a hot ball of iron, shrinking and exposing ridges that became mountains. Others were quite sure the planet was expanding. Growth widened sea basins and raised mountains. There was yet another idea, the theory that the world's crust was broken into big plates that jostled around, drifting until they collided and jarred mountains into existence. That idea was invariably dismissed as pseudo-science. Or "utter damned rot" as one prominent scientist said. But the doubtful theory of plate tectonics prevailed. Mountains, earthquakes, ancient ice ages, even veins of gold and fields of oil are now seen as the offspring of moving tectonic plates. Just half a century ago, most geologists sternly rejected the idea of drifting continents. But a few intrepid champions of plate tectonics dared to differ. The Mountain Mystery tells their story.
