At first, Alfred Wegener studied mathematics and astronomy in the city of Berlin and Heidelberg. However, Alfred Wegener was soon drawn into meteorology, and geophysics. Alfred Wegener and his brother, Kurt Wegener, both enjoyed hiking, mountain climbing, kiting, ballooning and sailing. Furthermore, Alfred Wegener went to a lot of expeditions and continued his career as a famous meteorologist and geophysicist. Alfred Wegener even came up with the Continental Drift theory.
In 1905 Alfred went to work with his older brother at the Aeronautischen Observatorium Lindenberg in Beeskow. The two brothers would be the first ones to pioneer the use of weather balloons to investigate air masses. Alfred Wegener was a meteorologist and explorer who was a pioneer in the studies of not only meteorology, astronomy, and polar exploration, but he also came up with the concept of the Continental Drift Theory. During his lifetime, Alfred was probably known best for his studies in meteorology and his explorations in Greenland. He participated in four separate Greenland expeditions where he and the team that he was with were charged with the duty of studying the last unknown portion of the Greenland coastal area.
After Char-les had graduated from Cambridge he was taken aboard the English survey ship HMS Beagle, largely on Henslow’s recommendation, as an unpaid naturalist on a scientific expedition around the world. Now Charles Darwin was around the age twenty-two while he was on the HMS Beagle. Darwin’s job as a naturalist aboard the Beagle gave him the opportu-nity to observe the various geological formations found on different continents and islands along the way, as well as a huge variety of fossils and organisms. In his geo-logical observations he was amazed mostly with the effect that natural forces had on shaping the earth’s surface. During this time, most geologists stuck to the so-called catastrophes theory that the earth had experienced a succession of creations of animal and plant life, and that each creation had been destroyed by a sudden catastrophe, such as an upheaval of the earth’s surface.
The first project Barbeau researched was the native peoples of eastern Canada. Throughout time, this research expanded and included all of the native peoples of Canada. In 1910 he won a Rhodes scholarship and Oxford University awarded him the B.Sc degree and diploma in anthropology for his thesis ‘The totemic Systems of the North Western tribes of North American’. When he returned to Canada he was chosen as an anthropologist to the National Museum of Canada then The Museum Branch of the Geological Survey of Canada in 1911 where he continued to work until his retirement in 1949. Furthermore, in 1911 he began recording on Edison wax cylinders on a Huron Indian reserve near Quebec.
It was not until long after Wegener’s death that proof was obtained and his theory verified. The Life of Alfred Wegener Alfred was born in Germany in 1880 and led a very busy life. He received a PhD in astronomy but quickly moved on to meteorology. He and his brother experimented with kites and balloons. They set a record flying a balloon during his first expedition to Greenland in 1906 (PBS, 1998, para.
His father was secretary to the head of the government. After Felix Klein graduated from the gymnasium in Düsseldorf, he went to the University of Bonn and studied math and physics from 1865-1866. Before Felix Klein had studied non-Euclidean geometry, he first wanted to be a physicist. While still at the University of Bonn he was appointed to lab assistant to Julius Plücker (Felix Klein German Mathematician). Felix Klein got his doctorate, which was supervised by Plücker.
After this he married Jane Mary Cox on September 1, 1945. Working as a police reporter, he studied Anthropology at the University of Chicago, but his thesis was rejected. In 1947, his son Mark was born, later, in 1949 his daughter Edith. He then became a publicist for General Electric in Schenectady, New York, but in 1950 he quit GE, and moved to Cape Cod to write. He published Player Piano in 1952.
This field of study is called paleontology. Mr. Gould graduated from Antioch University in Ohio “in 1963 with a degree in geology and philosophy” (Theory, 2009). While at Antioch, Stephen interned on a sea expedition with Woods Hole Oceanographic Institute. In Bermuda he collected tons of snail fossils and brought them back to Antioch to study them. Gould continued his studies at Columbia University where he received his doctorate degree in paleontology.
In 1912, however, the German meteorologist Alfred Wegener investigated the fit of the Atlantic coasts more carefully than had his predecessors and grouped all the continents together into one great land mass, which he called Pangaea. He supposed that the mass began to break apart about 200 million years ago. He also showed that some geological features on the opposite coasts could have fitted together, and that there were many striking similarities between the fossil plants and reptiles on the opposite coasts, particularly the coasts of Africa and South America. If the continents were pushed together, the geological, fossil, and other lines of evidence would join together accurately in the way that lines of print on a torn newspaper would join when the paper was reassembled. Wegener also pointed out that ancient climatic zones seemed to have lain in different places from the present zones.
It is what makes science reliable as this approach provides a scientific explanation, hence distinguishing it from the ordinary subjective approaches (Understanding Science n. d.). The scientific method can transform a belief or superstition to a scientific opinion. For example, the Continental Drift hypothesis, with a few alterations, is now in the name of Plate Tectonics. The Continental Drift Hypothesis began to arise in the early 19th Century after geologists noticed similarities in the earth rock formation. Continents were also a geographical match; fitting together like a jigsaw puzzle.