- What evidence supports the theories of continental drift and plate tectonics?
- What are 4 pieces of evidence for plate tectonics?
- What drives plate tectonics?
- What is the difference between plate tectonics and continental drift theory?
- What is the best piece of evidence for plate tectonics?
- What are 5 pieces of evidence that support continental drift?
- What is the evidence for Pangea?
- What evidence supports the theory of plate tectonics quizlet?
- What are three lines of evidence that are used to support continental drift and the theory of plate tectonics?
- What are the 3 theories of plate tectonics?
- What evidence supports Alfred’s theory?
What evidence supports the theories of continental drift and plate tectonics?
Fossil Evidence One type of evidence that strongly supported the Theory of Continental Drift is the fossil record.
Fossils of similar types of plants and animals in rocks of a similar age have been found on the shores of different continents, suggesting that the continents were once joined..
What are 4 pieces of evidence for plate tectonics?
There is variety of evidence that supports the claims that plate tectonics accounts for (1) the distribution of fossils on different continents, (2) the occurrence of earthquakes, and (3) continental and ocean floor features including mountains, volcanoes, faults, and trenches.
What drives plate tectonics?
Heat and gravity are fundamental to the process The energy source for plate tectonics is Earth’s internal heat while the forces moving the plates are the “ridge push” and “slab pull” gravity forces.
What is the difference between plate tectonics and continental drift theory?
The difference between continental drift and plate tectonics is that the theory of continental drift states that the world was made up of a single continent. The theory of plate-tectonics, on the other hand, states that earth’s surface is broken into numbers of shifting plates or slabs.
What is the best piece of evidence for plate tectonics?
Modern continents hold clues to their distant past. Evidence from fossils, glaciers, and complementary coastlines helps reveal how the plates once fit together. Fossils tell us when and where plants and animals once existed.
What are 5 pieces of evidence that support continental drift?
In the early part of the 20th century, scientists began to put together evidence that the continents could move around on Earth’s surface. The evidence for continental drift included the fit of the continents; the distribution of ancient fossils, rocks, and mountain ranges; and the locations of ancient climatic zones.
What is the evidence for Pangea?
Evidence of existence Fossil evidence for Pangaea includes the presence of similar and identical species on continents that are now great distances apart.
What evidence supports the theory of plate tectonics quizlet?
Rock and fossils found in South America match those found in Africa, although there is an ocean in between. This also indicates that the two continents were once joined. Other evidence of plate tectonics include Seafloor spreading, which involves the creation of new crust at divergent plate boundaries.
What are three lines of evidence that are used to support continental drift and the theory of plate tectonics?
Alfred Wegener, in the first three decades of this century, and DuToit in the 1920s and 1930s gathered evidence that the continents had moved. They based their idea of continental drift on several lines of evidence: fit of the continents, paleoclimate indicators, truncated geologic features, and fossils.
What are the 3 theories of plate tectonics?
Plates interact at three types of plate boundaries: divergent, convergent and transform. Most of the Earth’s geologic activity takes place at plate boundaries. At a divergent boundary, volcanic activity produces a mid ocean ridge and small earthquakes.
What evidence supports Alfred’s theory?
He presented his Continental Drift hypothesis on 6 January 1912. He analyzed both sides of the Atlantic Ocean for rock type, geological structures and fossils. He noticed that there was a significant similarity between matching sides of the continents, especially in fossil plants.