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The evidence supporting continental drift emerged in the early to mid-20th century, with key contributions from scientists like Alfred Wegener and Arthur Holmes. By the 1960s, advancements in technology, such as ocean floor mapping and paleomagnetism, provided further support for the theory.
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What is the evidence supporting the hypothesis of continental dift?
Evidence supporting the hypothesis of continental drift includes the fit of continental coastlines, matching rock formations and fossils across continents, and the alignment of mountain ranges. Additionally, the distribution of ancient glacial deposits and paleoclimate data further support the idea that continents were once connected.
Which of the following is not evidence supporting the theory of continental drift?
The presence of similar rock formations on different continents is not evidence supporting the theory of continental drift. This is because the theory of continental drift proposes that the continents were once one supercontinent and have since drifted apart, so the similarity in rock formations actually supports this theory.
What are two types of climate clues that support the continental drift hypotheis?
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.
What paleoclimatic evidence supports continental drift?
Paleoclimatic evidence supporting continental drift includes the matching of certain rock formations, geological structures, and fossil distribution on continents now separated by vast oceans. For example, the presence of glacial deposits and coal seams that match across continents provides evidence that these landmasses were once connected. Additionally, the alignment of ancient climatic belts and the distribution of certain plant and animal species further support the theory of continental drift.
What was the weakness of wegeners proposal of continental drift?
One weakness of Wegener's proposal of continental drift was the lack of a mechanism to explain how continents could move. Additionally, Wegener's theory was not widely accepted at the time due to insufficient supporting evidence and the reluctance of the scientific community to accept such a radical idea.
Are fossils evidence of continental drift?
Yes, fossils are evidence of continental drift because similar fossils have been found on different continents that are now far apart. This suggests that these continents were once connected, supporting the theory of continental drift.
Wegeners hypothesis of continental drift was finally confirmed by?
evidence supporting the idea of sea-floor spreading.
What does provide evidence for continental drift?
Is there a list? Continental drift is real, so religious fanatics don't provide evidence for continental drift.
Why is the platypus good evidence for continental drift?
It is good evidence of continental drift as fossils of previous duck billed platypuses were found in America and Alaska, which Australia was once connected to. This means the platypuses once lived there hence evidence of continental drift.
What is the evidence supporting the hypothesis of continental dift?
Evidence supporting the hypothesis of continental drift includes the fit of continental coastlines, matching rock formations and fossils across continents, and the alignment of mountain ranges. Additionally, the distribution of ancient glacial deposits and paleoclimate data further support the idea that continents were once connected.
Which of the following is not evidence supporting the theory of continental drift?
The presence of similar rock formations on different continents is not evidence supporting the theory of continental drift. This is because the theory of continental drift proposes that the continents were once one supercontinent and have since drifted apart, so the similarity in rock formations actually supports this theory.
What is the weakness in Wegener's continental drift hypothesis?
A weakness in Wegener's continental drift hypothesis was the lack of a mechanism explaining how the continents moved. Additionally, he was unable to provide evidence supporting the force that would be strong enough to move continents across the Earth's surface. Lastly, Wegener's theory faced skepticism from the scientific community at the time due to a lack of detailed data and observations supporting his idea of continental drift.
What was a plant used for evidence for continental drift?
their roots
What are two types of climate clues that support the continental drift hypotheis?
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.
Why is the continental drift theory a theory and not a scientific law?
The Continental Drift theory is a theory because there is no evidence to support it. Alfred Wegener developed the Continental Drift theory in the 1800's.
Did wegener use paleomagnetism?
No, Alfred Wegener did not use paleomagnetism in his theory of continental drift. Wegener's theory was based on evidence from fossil records, geological formations, and similarities in rock types and mountain ranges on different continents. Paleomagnetism became a significant piece of evidence supporting continental drift theory after Wegener's time.
What paleoclimatic evidence supports continental drift?
Paleoclimatic evidence supporting continental drift includes the matching of certain rock formations, geological structures, and fossil distribution on continents now separated by vast oceans. For example, the presence of glacial deposits and coal seams that match across continents provides evidence that these landmasses were once connected. Additionally, the alignment of ancient climatic belts and the distribution of certain plant and animal species further support the theory of continental drift.
