plate tectonics and Pangaea you get evidence from ancient climate zones,land features,and fossils! hope this helped! all credit goes to California Earth Science textbook for 6th graders.
Geologic Evidence For Continental Drift
Rocks in India, southern Africa, and Brazil contain deep scratches and scars that were formed by glaciers. But how could glaciers exist in places with such warm climates? The climates of these areas must have been much colder at one time. Scientists now know that these areas were part of a single land mass, or continent. It was located near the South Pole about 280 million years ago.
-7th grade life science
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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.
One type of evidence for continental drift is fossil evidence, such as plant and animal fossils that are found on separate continents but are closely related. Another type is geological evidence, including the matching of rock formations and mountain ranges on different continents, as well as the distribution of earthquakes and volcanoes along continental boundaries.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
Fossil evidence of the same species found on different continents and rock formations that match up across different continents are two pieces of evidence for continental drift. These support the theory that continents were once connected and have since moved apart.
In addition to matching coastlines, Wegener used similarities in rock formations and mountain ranges across different continents as evidence for his theory of continental drift. He also noted similarities in the distribution of fossils on separate continents, suggesting that the same species were once connected when the continents were joined.
Fossil evidence of plants and animals that were once distributed across continents and matching geological formations such as mountain ranges or rock layers on different continents provide clues supporting the continental drift hypothesis. Additionally, evidence of past climates, such as ancient glacial deposits in regions that are now far from the poles, further support the idea of continental drift.
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.
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One type of evidence for continental drift is fossil evidence, such as plant and animal fossils that are found on separate continents but are closely related. Another type is geological evidence, including the matching of rock formations and mountain ranges on different continents, as well as the distribution of earthquakes and volcanoes along continental boundaries.
The continents of Africa and South America are often used as evidence for the continental puzzle due to their matching coastlines and geological features, suggesting they were once connected. This supports the theory of continental drift and plate tectonics.
Two forms of evidence used to support the continental drift theory are the fit of the continents (jigsaw-like arrangement of continents' coastlines) and matching geological formations (similar rock types, structures, and mountain ranges on different continents). Additionally, paleontological evidence, such as similar fossil records found across separate continents, also supports the theory.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
Fossil of an ocean fish found on two different continents would not be good evidence of continental drift because Fossils of land animals are a better piece of evidence of continental drift than fish.
Fossil evidence of the same species found on different continents and rock formations that match up across different continents are two pieces of evidence for continental drift. These support the theory that continents were once connected and have since moved apart.
In addition to matching coastlines, Wegener used similarities in rock formations and mountain ranges across different continents as evidence for his theory of continental drift. He also noted similarities in the distribution of fossils on separate continents, suggesting that the same species were once connected when the continents were joined.
Continental drift is the drift of continents. The earth consists of large plates floating on a ball of molten rock. Such a plate is called a tectonic plate, and since they float, they can float a way. This is called continental drift. Continental drift is one of the main causes of earthquakes. Earthquakes especially happen when two continental plates are shifting next to each other.
its not the answer i got from my text book so dont listen 2 tht person............................