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β 11y agoContinental drift :)
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β 11y agoWiki User
β 12y agoThe continental drift
comparative statics is a comparative study of economic conditions at two equilibrium positions under two static conditions at two different points in time. in a comparative static analysis, in fact, we are comparing the equilibrium values of the system corresponding to the two equilibrium positions with one another. this sort of comparative analysis of two equilibrium positions may be described as comparative static analysis.
A physical model is an object that represents whatever you are trying to explain. A mathematical model is an equation that shows something (usually some sort of movement or energy might not be applicable in most situations.)
Explain how to disentangle hair after shampooing and explain the importance of considering the cuticle scales:
Describe is what it is and explain is why it is as it is
What did SpongeBob do wrong in this experiment? Explain
Wegener believed that all continents were once part of a supercontinent called Pangaea, which began breaking apart about 200 million years ago. He proposed the theory of continental drift to explain the movement of the continents over time.
Continental drift is the theory that Earth's continents were once all connected as a single supercontinent called Pangaea and have since drifted apart to their current positions over millions of years. This movement is driven by the slow shifting of tectonic plates that make up Earth's crust.
no.i think it doesnt.
The current shape and position of continents provide evidence for the theory of plate tectonics, which suggests that continents were once part of a supercontinent called Pangaea that has since drifted apart. This movement helps explain the similarities between the geology and fossils of now widely separated continents, as well as the presence of matching coastlines and mountain ranges.
Pangaea was a supercontinent that existed about 335 million years ago. It is believed to have later broken apart into the continents we know today due to the movement of tectonic plates. This theory of continental drift helps explain the similarities in geology and fossil evidence found across different continents.
Wegener named his supercontinent "Pangaea," which means "all lands" in Greek. He proposed the theory of Pangaea to explain how the continents once fit together and have since drifted apart due to plate tectonics.
Alfred Wegener proposed the theory of continental drift in 1912, suggesting that continents were once joined together in a supercontinent called Pangaea and have since drifted apart. This theory laid the foundation for the modern understanding of plate tectonics and the movement of Earth's continents. Despite facing initial skepticism, Wegener's ideas were eventually accepted and revolutionized the field of geology.
it explains y there is volcanoes, earthquakes, and the movement of the continents
The hypothesis is called continental drift, proposed by Alfred Wegener in the early 20th century. It suggests that a supercontinent called Pangaea broke apart over millions of years to form the continents as we know them today. This theory was later developed into the theory of plate tectonics to explain the movement of the Earth's lithosphere.
Wegener proposed the theory of continental drift, suggesting that continents were once connected in a single supercontinent called Pangaea, which later broke apart and drifted to their current positions. He argued that continents moved due to the process of plate tectonics, driven by forces such as mantle convection.
Wegener's theory proposed that continents were once part of a single supercontinent called Pangaea, which slowly drifted apart over time due to the movement of tectonic plates. This movement caused the continents to shift their positions on the Earth's surface, leading to their current configuration. Wegener's theory was later expanded upon and refined into the theory of plate tectonics.
Seafloor spreading is a key component of the theory of continental drift. As new oceanic crust forms at mid-ocean ridges during seafloor spreading, it pushes the existing crust outward on both sides of the ridge. This movement can help explain how continents have shifted positions over time due to the movement of tectonic plates.