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
that the continents were once all connected as one supercontinent, called Pangaea, which broke apart and drifted to their current positions over millions of years. This theory eventually led to the development of the theory of plate tectonics to explain the movement of Earth's large landmasses.
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.
Fossils found on different continents with similar characteristics suggest that these landmasses were once connected millions of years ago. As continents drift apart, similar fossils can only be explained by the movement of landmasses over time, supporting the theory of continental drift. This provides evidence that different continents were once part of a single supercontinent, such as Pangaea.
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.
Climate clues such as glacial deposits and ancient sea level changes can help support the theory of continental drift by showing how certain landmasses were once connected and located in different positions on Earth. By looking at these climate indicators, scientists can reconstruct past climates and the movement of continents over millions of years. This evidence helps explain how continents have shifted and drifted to their current positions.
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.
it explains y there is volcanoes, earthquakes, and the movement of the continents
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.
Seafloor spreading provides evidence for the theory of continental drift by showing that new oceanic crust is continuously formed at mid-ocean ridges and spreads outward, pushing the continents away from each other. This process accounts for the movement of the continents over time and helps explain how separate landmasses once formed a single supercontinent called Pangaea.