Yes, fossil evidence supports the theory of plate tectonics by showing how identical plant and animal species are found on continents that are now separated by oceans, indicating that those landmasses were once connected and have since drifted apart. Fossils of ancient marine animals found on mountaintops provide further evidence of past tectonic movements.
Continental drift, sea floor spreading, glacial striation, jigsaw fit of the continents, geological matches on different contintents (such as type of rock or fossil found) ,earthquakes, and volcanoes led to the theory of plate tectonics.
Alfred Wegener proposed the theory of continental drift, not a shrinking Earth theory. He used evidence such as the fit of the continents, matching rock formations, and fossil distribution to support his idea that the continents had once been part of a single landmass called Pangaea. Wegener's theory eventually led to the development of the theory of plate tectonics.
The theory that states that plates move around on the asthenosphere is called plate tectonics. This theory explains the movement of the Earth's lithosphere into different plates and their interactions at plate boundaries due to the convective currents in the asthenosphere beneath them.
Plate tectonics is the combination of the seafloor spreading and continental drift. When Alfred Wegner described this process it was rejected due to lack of evidence. Since, we have discovered new evidence and proven his theory true.
plate tectonics=D
Plate tectonics led to the theory of Pangaea.
Fossil evidence, particularly fossils of the same species found on different continents, provided initial support for the hypothesis of continental drift. Further evidence from the mapping of the seafloor, such as mid-ocean ridges and magnetic striping, led to the development of the theory of plate tectonics.
Creationist theory and plate tectonics do not disagree in any way.
The theory of plate tectonics has succumbed to the newer theory of continental drift. Scientists believe this theory today due to three main factors. First, the continents appear to fit together. When the continental shelves, as opposed to just the continents, are placed together, the fit appears uncanny. Second, the distribution of fossils is consistent with continental drift. Lastly, glacial deposits once covered parts of the earth that are currently tropical.ANSWER: The plate tectonics theory is relatively new and formulated only in the 1960s. The evidence listed above in the first answer can only support the continental drift theory which was developed by Alfred Wegener in 1912. Evidence that can support the plate tectonics theory are the age, depth of oceanic sediments, volcanic activity, geothermal gradient, gravity anomalies, paleomagnetism and seismologic evidence. If you are answering an exam question on evidence supporting plate tectonics, evidence supporting continental drift theory should only come later in your answer and should not be given too much emphasis, for the plate tectonics theory involves more than just the continental crust drifting around and cannot support the main hypotheses of the plate tectonics theory.
Plate tectonics
A theory that says the lithosphere is divided into plates that move around on top of the asthenosphere is called '' plate tectonics''
Plate tectonics
yes it represets plate tectonics
Continental drift, sea floor spreading, glacial striation, jigsaw fit of the continents, geological matches on different contintents (such as type of rock or fossil found) ,earthquakes, and volcanoes led to the theory of plate tectonics.
plate tectonics, which explains the movement of Earth's outer shell. Fossil remains on separate continents that were once part of the same landmass suggest that continents were once connected and have since drifted apart. The shape of continents also fits together like a puzzle, supporting the idea of continental drift and plate tectonics.
The theory of plate tectonics explains large scale motion of the earth's lithosphere.
The theory of plate tectonics explains large scale motion of the earth's lithosphere.