alfred wegener hypothesis

The theory of continental drift was proposed at the beginning of the last century by German scientist Alfred Wegener. On the following pages you will find out, among other things, how Alfred Wegener arrived at his theory back then and what young geologists today can learn from him.

Alfred Wegener (1880-1930) earned a PhD in astronomy at the University of Berlin in 1904, but he had always been interested in geophysics and meteorology and spent most of … Alfred Wegener died in 1930. The theory of the drift of Wegener's continents has become generally accepted and is still being studied. 1924-1930 (Public domain, via Wikimedia Commons). His knack for questioning accepted ideas started in 1910 when he disagreed with the explanation that the Bering Land Bridge was formed by isostasy and that similar land bridges once connected the continents [ … That was the day 31-year-old meteorologist Alfred Wegener gave his talk on the formation of the oceans and continents and in the process shook the foundations of accepted doctrine. He is most notable for his theory of continental drift, which he proposed in December 1912.

Figure 4.1.1 Prof. Dr. Alfred Wegener, ca. Wegener hypothesis definition is - a hypothesis in geology : the existing continents were originally one land area of which portions have separated and since Carboniferous time have slowly drifted apart moving on a plastic substratum. Alfred Wegener. After 30 years, it was possible to find the cause of the movement of the continents, based on the movement along the mantle. Alfred Wegener (1880-1930) was a German scientist who specialized in meteorology and climatology. Alfred Lothar Wegener (1 November 1880 – 13 November 1930) was a German scientist and meteorologist. This was the idea that the continents were slowly drifting around the Earth.He also had ideas about why the continents drift, which other scientists thought were impossible. Alfred Wegener, in full Alfred Lothar Wegener, (born November 1, 1880, Berlin, Germany—died November 1930, Greenland), German meteorologist and geophysicist who formulated the first complete statement of the continental drift hypothesis.