The chain in The Mid-Atlantic ridge is part of the longest mountain chain in the world. Which new oceanic lithosphere is created as older materials are pulled away.
i dont exactally know but it would the closest answer i could find is,scientists surmised that instead of continents drifting, they actually rode on top of moving ocean floor peices.
Climate, and landforms
the continents fit together like a puzzle
the age of the rocks in the sea floor is all the same
he used fossils, glacial indentations, and different types of rock.
The pieces of evidence Alfred Wegener used to support his theory about continental drift were; Puzzle Fit, Fossil evidence from animals that were once on the same continent, geologic evidence like mountain chains that were connected and now split apart, and ice sheets. Thank you for reading this article and I hoped it answered your question!
Climate fossil and fossil climate
the continents fit together like a puzzle
the age of the rocks in the sea floor is all the same
he used fossils, glacial indentations, and different types of rock.
The pieces of evidence Alfred Wegener used to support his theory about continental drift were; Puzzle Fit, Fossil evidence from animals that were once on the same continent, geologic evidence like mountain chains that were connected and now split apart, and ice sheets. Thank you for reading this article and I hoped it answered your question!
Climate, and landforms
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.
it is the process of you finding it yourself!!!
Climate fossil and fossil climate
The 100% correct answer is A similar fossil was found in Africa, South America, Australia, India, and Antarctica.
He used evidence from landform, climate, and fossils to support his theory of the continental drift.
Its fossils are found in many different places like South America and Africa which support the theory of continental drift.
explain how fossils support the theory of continental movement