continental drift
His evidence was good. i.e. continental fit across the Atlantic Multiple species matches (best of which where shallow water or terrestrial where it was infeasible for them to cross such a large water mass) Mountain ranges fitted together both sides of the Atlantic
Alfred Wegener did not specifically study the attic atmosphere; rather, he is best known for his theory of continental drift, which he proposed in the early 20th century. His work focused on the movement of continents and the evidence supporting this idea, such as fossil correlations and geological formations across continents. Wegener's research included meteorological studies, but his primary contributions were in geology and paleontology, not atmospheric studies.
Alfred Wegener, a German meteorologist, proposed the theory of continental drift in the early 20th century. He suggested that the continents were once part of a single supercontinent called Pangaea that broke apart and drifted to their current positions. Although his ideas were initially met with skepticism, they formed the foundation for the modern theory of plate tectonics.
The German geophysicist who initiated the study of tectonic plates is Alfred Wegener. He is best known for proposing the theory of continental drift in the early 20th century, which laid the groundwork for the later development of plate tectonics. Wegener's ideas were initially met with skepticism, but they eventually gained acceptance as more evidence accumulated, leading to a better understanding of Earth's geological processes.
Continental Drift.
continental drift
i.e. continental fit across the Atlantic Multiple species matches (best of which where shallow water or terrestrial where it was infeasible for them to cross such a large water mass) Mountain ranges fitted together both sides of the Atlantic
The coastlines of South America and Africa seem to fit together the best because of their similar shapes and continental shelf structures. This is a key piece of evidence supporting the theory of continental drift.
The moon's lack of continental drift suggests that it does not have the same geological processes as Earth, such as tectonic plate movement. The absence of continental drift on the moon could be due to its smaller size and lack of a liquid outer core, which are key factors in driving plate tectonics on Earth.
Continental drift is what happens when the Earth's plates shift either towards or away from the other plates. Earthquakes occur when two of the plates bump into each other. It happens when the magma from within the Earth rises up and pushes the plates, due high pressure they pose. That's the best I can do.
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South America and Africa are often considered to fit together well due to their similar shapes along the Atlantic Ocean coastlines. This observation was one of the key pieces of evidence used to support the theory of plate tectonics and the concept of continental drift.
Africa and South America have the best fit when Pangaea is reassembled due to the matching of their coastlines and geological features, including rock formations and fossils found on both continents. This fit was a key piece of evidence used to support the theory of continental drift proposed by Alfred Wegener.
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Continental Drift is the name of a theory, developed by German meteorologist and geologist Alfred Wegener (1880-1930), asserting that parts of the earth's crust are slowly drifting on top of a liquid core. Wegener hypothesized that 200 million years ago, the earth was comprised of one great supercontinent, containing all of earth's land masses. He called the supercontinent "Pangaea," which means "all the land" in Greek. According to Wegener, Pangaea broke apart during the period bounded by the Jurassic and Cretaceous periods, to the point where the super land mass was finally separated into the distinct land masses we now recognize as modern-day continents. Wegener's theory of continental drift is published in his 1915 work entitled, "On the Origin of the Continents and Oceans."