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∙ 12y agoThe best places to look for evidence of continental drift are paleontological evidence, such as similar fossils found on different continents that were once connected, and geological evidence, such as matching rock formations and mountain ranges on different continents. These can help support the theory of continental drift proposed by Alfred Wegener in the early 20th century.
continental drift
One reason people didn't believe Alfred Wegener's theory of continental drift was because he couldn't provide a plausible mechanism for how the continents moved. Additionally, Wegener's evidence was mostly based on geological and paleontological similarities between continents, which was not considered sufficient proof at the time. The scientific community also generally resisted accepting radical new ideas, and many scientists were reluctant to challenge the prevailing belief in static continents.
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 evidence isfossil evidence - identical fossils in different continentrock type and structural similarities - found similar rocks on continents on opposite sidesstudy of climate - the heat of the sunfrom a book thanks
Alfred Wegener is best known for developing the theory of continental drift, proposing that the continents were once joined together in a single supercontinent called Pangaea. He also made contributions to meteorology and polar research, and participated in several expeditions to Greenland. Wegener's work laid the foundation for the modern theory of plate tectonics.
Continental Drift.
continental drift
Alfred Wegener's evidence for continental drift included the jigsaw-like fit of continents, similarities in rock formations and fossils across continents, and matching mountain ranges. Additionally, he observed similar ancient climates found on continents that are now separated by oceans.
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."
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