Alfred Wegener studied plate tectonics during the early 20th century, particularly in the 1910s and 1920s. His theory of continental drift laid the foundation for the modern understanding of plate tectonics.
Other evidence to support Alfred Wegener's theory of continental drift includes matching geological formations and rock types on different continents, similar fossil collections on continents that are now separated by oceans, and the fit of the continents' coastlines like pieces of a jigsaw puzzle. Additionally, the discovery of mid-ocean ridges and the study of paleomagnetism has further bolstered the theory.
Alfred Wegener was a German meteorologist and geophysicist. He proposed the theory of continental drift in 1912, suggesting that the continents were once joined together in a supercontinent called Pangaea. Wegener's theory was met with skepticism initially, but eventually led to the development of the theory of plate tectonics. He participated in several expeditions to Greenland to study polar air circulation and climate. Wegener died in 1930 during a Greenland expedition. He published his ideas in the book "The Origin of Continents and Oceans" in 1915. Wegener was not formally trained as a geologist. He was inspired by the matching coastlines of South America and Africa to propose his theory. Wegener's theory faced criticism due to lack of a plausible mechanism for continental drift. He made important contributions to our understanding of Earth's history and the processes that shape its surface.
Alfred Wegener's theory of continental drift laid the groundwork for the modern understanding of plate tectonics, fundamentally transforming geology and earth sciences. His ideas prompted further research into the movement of Earth's plates, leading to discoveries about seismic activity, mountain formation, and oceanic trenches. Today, Wegener's work influences a wide range of scientific fields, including climate science and paleontology, as it provides context for understanding the historical distribution of species and climate patterns. His emphasis on interdisciplinary approaches continues to inspire scientists to explore complex Earth systems and their interactions.
Six months later on May 12, 1931, Wegener's body was found in Greenland, halfway between Eismitte and West camp, buried with great care. A pair of skis marked the grave site. At 50 years of age and a heavy smoker, Wegener's suspected cause of death was heart failure through overexertion. His body was reburied in the same spot by the team that found the burial site and marked with a large cross. After burying Wegener, Villumsen departed for the West camp, but was never seen again. It is estimated that the 23-year-old's body now lies buried under more than 100 metres (330 ft) of accumulated ice and snow.
Greenland
he wanted to study science because his dad liked science
Alfred Wegener studied plate tectonics during the early 20th century, particularly in the 1910s and 1920s. His theory of continental drift laid the foundation for the modern understanding of plate tectonics.
he studied physics, astronomy and meteorology at theFriedrich Wilhelms University (today Humboldt University), Berlin. In 1905, he earned his Ph.D. in astronomy
There are some strange noises coming from the attic.
Other evidence to support Alfred Wegener's theory of continental drift includes matching geological formations and rock types on different continents, similar fossil collections on continents that are now separated by oceans, and the fit of the continents' coastlines like pieces of a jigsaw puzzle. Additionally, the discovery of mid-ocean ridges and the study of paleomagnetism has further bolstered the theory.
Alfred Wegener was a German meteorologist and geophysicist. He proposed the theory of continental drift in 1912, suggesting that the continents were once joined together in a supercontinent called Pangaea. Wegener's theory was met with skepticism initially, but eventually led to the development of the theory of plate tectonics. He participated in several expeditions to Greenland to study polar air circulation and climate. Wegener died in 1930 during a Greenland expedition. He published his ideas in the book "The Origin of Continents and Oceans" in 1915. Wegener was not formally trained as a geologist. He was inspired by the matching coastlines of South America and Africa to propose his theory. Wegener's theory faced criticism due to lack of a plausible mechanism for continental drift. He made important contributions to our understanding of Earth's history and the processes that shape its surface.
Because he discovered that similar fossils were being found in different countries, were some of those plants and animals couldn't grow or live there for creating the theory Pangaea.For example,Wegener found a fossil of a plant in South America which made perfect sense for it to grow in but, what wasn't logical was that he found the exact same fossil in Iceland were temperatures are to cold for vegetation.
Alfred o Coffin studied bioligical sciences
Alfred studied in South-East Asia and Africa
Alfred Wegener's theory of continental drift laid the groundwork for the modern understanding of plate tectonics, fundamentally transforming geology and earth sciences. His ideas prompted further research into the movement of Earth's plates, leading to discoveries about seismic activity, mountain formation, and oceanic trenches. Today, Wegener's work influences a wide range of scientific fields, including climate science and paleontology, as it provides context for understanding the historical distribution of species and climate patterns. His emphasis on interdisciplinary approaches continues to inspire scientists to explore complex Earth systems and their interactions.
Alfred Wegener attended school at the Köllnische Gymnasium on Wallstrasse in Berlin (a fact which is memorialized on a plaque on this protected building, now a school of music), graduating as the best in his class. Afterward he studied Physics, meteorology and Astronomy in Berlin, Heidelberg and Innsbruck. From 1902 to 1903 during his studies he was an assistant at the Urania astronomical observatory. He obtained a doctorate in astronomy in 1905 based on a dissertation written under the supervision of Julius Bauschinger at Friedrich Wilhelms University (today Humboldt University), Berlin.