He said that it was due to plate tectonics, a theory which he is famous for. Two plates, either continental-continental, oceanic-continental or oceanic-oceanic collide at plate boundaries, causing an uplift of land. The oceanic plate or the denser plate will subduct. These uplifts will result in the formation of mountains, mountain ranges, volcanoes and islands.
Alfred Wegener had discovered pangaea in the year of 1912.
Alfred Wegener used evidence such as the fit of the continents, matching geological formations across continents, identical fossil species found on different continents, and similarities in rock types and mountain ranges as support for his theory of continental drift.
Alfred Wegener found several lines of evidence to support the theory of Pangaea, including the fit of the continents, similar rock formations and mountain ranges across continents, matching fossil remains on different continents, and similar climates and glacial deposits in areas that are now far apart.
Alfred Wegener used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similar rock formations and mountain ranges across continents, and the distribution of plants and animals. He also looked at evidence from fossils and ancient climate data to support his hypothesis.
Alfred Wegener's full name is "Alfred Lothar Wegener", and he is a German scientist who came up with the theory of Continental Drift.
Alfred Wegener had discovered pangaea in the year of 1912.
Alfred Wegener used evidence such as the fit of the continents, matching geological formations across continents, identical fossil species found on different continents, and similarities in rock types and mountain ranges as support for his theory of continental drift.
No, Alfred Wegener did not use paleomagnetism in his theory of continental drift. Wegener's theory was based on evidence from fossil records, geological formations, and similarities in rock types and mountain ranges on different continents. Paleomagnetism became a significant piece of evidence supporting continental drift theory after Wegener's time.
Alfred Wegener found several lines of evidence to support the theory of Pangaea, including the fit of the continents, similar rock formations and mountain ranges across continents, matching fossil remains on different continents, and similar climates and glacial deposits in areas that are now far apart.
Alfred thought that mountain were formed by two continents smashing together with such force that the land was forced up.
Alfred Wegener
Alfred Wegener used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similar rock formations and mountain ranges across continents, and the distribution of plants and animals. He also looked at evidence from fossils and ancient climate data to support his hypothesis.
Alfred Wegener's full name is "Alfred Lothar Wegener", and he is a German scientist who came up with the theory of Continental Drift.
The concept of Pangaea, the ancient supercontinent, was proposed by Alfred Wegener in 1912 based on evidence from the fit of continents, fossil similarities, and rock formations. He suggested that the continents were once connected and have since drifted apart.
Alfred Wegener's father, Richard Wegener, passed away when Alfred was just six years old. His mother, Anna Wegener, raised Alfred and his siblings as a widow.
The father of Alfred Wegener was Richard (Wegener), a cleric, and his mother was named Anna, natural from Braddenburg. Alfred has a brother, Kurt Wegener (1878-1964)which was a pioneers in the use of balloons in climatology (At least once, Kurt went to Greenland with Alfred). Alfred Wegener's wife was Else Koppe.
Alfred Wegener came up with the idea of Pangaea by observing the fit of South America and Africa's coastlines, as well as similarities in rock formations and fossils on different continents. He proposed the theory of continental drift to explain how the Earth's landmasses were once joined together in a supercontinent called Pangaea before drifting apart over time.