Rocks are very useful when studying the theory of continental drift. For example, one might find a place in Brazil where the type of rock is the same type of rock in Morocco. Or, you might notice that some geological landforms look like they're shaped in a certain way on the eastern South American coast. You might find the exact opposite shape of rocks or landforms on the western side of Africa. This helps explain that South America was once connected to Africa.
Seafloor spreading provided evidence for continental drift by showing that new oceanic crust is formed at mid-ocean ridges, pushing older crust away. This process helped explain how continents could move and supported the idea of plate tectonics. The pattern of magnetic stripes on the seafloor also matched with predictions based on the movement of continents, further supporting the theory of continental drift.
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.
It supports the theory because it can be found on all of the continents.
The 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.
simple....the answer is mantle.(: Glad to help!
Rocks help support the theory of continental drift through evidence such as similar rock formations and fossils found on different continents, matching up when the continents were once part of the same landmass. Additionally, the alignment of magnetic minerals in rocks provides further evidence of past positions of continents as they moved over the Earth's surface.
It can help show that continental drift happened, if you find the same fossils on different continents. This would mean that the continents had to be close together if the fossils are found on land.
Fossils of the same species can be found on continents that are now today separated by oceans. btw continental drift is a fact.
Seafloor spreading provided evidence for continental drift by showing that new oceanic crust is formed at mid-ocean ridges, pushing older crust away. This process helped explain how continents could move and supported the idea of plate tectonics. The pattern of magnetic stripes on the seafloor also matched with predictions based on the movement of continents, further supporting the theory of continental drift.
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.
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.
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Scientists accepted continental drift after observations of matching geological formations and fossils on different continents, the discovery of mid-ocean ridges and magnetic striping on the ocean floor, and the development of plate tectonics theory to explain these phenomena. This provided a comprehensive explanation for the movement of continents over time.
It supports the theory because it can be found on all of the continents.
Fossils found on separate continents that are now far apart provide evidence for continental drift. Similar fossil species found on continents that were once connected suggest that these landmasses were once united. Additionally, matching rock formations and paleoclimate evidence from fossils support the hypothesis of continental drift.
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.
I’m sorry, but I cannot provide specific answers to a worksheet without knowing its content. However, I can summarize the concept of continental drift if that helps! Continental drift refers to the theory that continents move slowly over time due to tectonic plate movements, influencing geological features and climate over millions of years. If you have specific questions about continental drift, I'd be happy to help!