Alfred Wegener and the Continental Drift

In 1912, he first introduced the theory of continental movement at a meeting in Germany. He speculated that the mainland had been away from each other for a while and denied that there was already a crossover connecting the mainland. In the same year, he married a meteorologist's daughter and returned to another exploration to Greenland. During the First World War, he continued to serve in the army. The concept of continental migration has never disappeared, but he did not release his theory until 1915.

Only in the early 1950's the continental drift theory controversial by Alfred Wegner was taken seriously by leading geologists and other scientists along with the arrival of new paleomagnetic studies and was finally accepted by mainstream science It was. Theory of plate theory in the 1960's

The theory of continental drift is most relevant to scientist Alfred Wegner. In the beginning of the 20th century, Wegner published a thesis explaining his theory that the land of the mainland "drifts" the earth and sometimes plows each other in the sea. He called the movement a drift of the continent. Wegener is astronomer who uses biology, botany and geology to explain the drift of Pangea and the continent. For example, ancient reptile dragon fossils were found only in South America and South America. Only one meter (3.3 feet) of freshwater reptiles, mesosaurus can not swim the Atlantic Ocean. The presence of the midbrain dragon means a single habitat with many lakes and rivers.

Continental drift is a theory that explains how the continent shifts its position on the surface of the earth. Geophysicist and meteorologist Alfred Wegener suggested in 1912 why drift of the continent explains why similar animal and plant fossils and similar rocks were found on different continents. Wegener believes that all continents have united with "Urkontinent", then broke up and moved to the current position. However, geologists criticized the theory of continental drifting of Wegner after announcing detailed information in the book entitled "The Origin of the Continent and the Sea" published in 1915. Part of the objection is because Wegner does not have a good model to explain how the continent splits.

Alfred Wegner proposed the idea of ​​continental drift theory - movement of the continent of the earth. Despite evidence of persuasive fossils and rocks from 1912 to 1929, most other scientists denied this evidence. Only in the 1960's the drift of the continent became part of the mainstream science. I started college in Berlin in 1899 and received various science courses when I was 18 years old. He specializes in astronomy, meteorology and physics. In 1902 he got a doctorate in astronomy. He spent one year in Berlin's famous Uranus Observatory.