Evidence supporting continental drift includes the distribution of fossils and rock formations that match across continents, the fit of continental coastlines like puzzle pieces, and the alignment of mountain ranges and geological structures across continents. Additionally, the matching of ancient climates and glacial deposits across separate continents supports the theory of continental drift.
The plates have different shapes, and they all fit together like a jigsaw puzzle. They are like puzzle pieces because many years ago, they used to be joined and then they parted. On the other hand, unlike puzzle pieces, some plates are being pushed underneath other plates (usually oceanic under continental), and new crust is being formed at spreading rifts.
The continental Coastlines fit together like puzzle pieces, fossils, and glacier Grover in warm places
Earth's tectonic plates.
Puzzle pieces
pates
pates
The east coast of South America and the west coast of Africa appear to match up like puzzle pieces. This phenomenon is known as the "Atlantic Puzzle" and is evidence of the theory of continental drift.
South America and Africa fit together like puzzle pieces.
The smallest puzzle was 7.75 cm by 5.7cm and had 99 pieces and was considered the hardest puzzle ever with a piece density of 40,000 pieces per meter
Alfred Wegener proposed that Africa and South America looked like they could fit together like puzzle pieces, supporting his theory of continental drift.
Pieces are to a puzzle as notes are to music. Each are essential to completing the whole.
They are like puzzle pieces because many years ago, they used to be joined and then they parted. On the other hand, unlike puzzle pieces, some plates are being pushed underneath other plates (usually oceanic under continental), and new crust is being formed at spreading rifts.
Evidence supporting continental drift includes the distribution of fossils and rock formations that match across continents, the fit of continental coastlines like puzzle pieces, and the alignment of mountain ranges and geological structures across continents. Additionally, the matching of ancient climates and glacial deposits across separate continents supports the theory of continental drift.
The plates have different shapes, and they all fit together like a jigsaw puzzle. They are like puzzle pieces because many years ago, they used to be joined and then they parted. On the other hand, unlike puzzle pieces, some plates are being pushed underneath other plates (usually oceanic under continental), and new crust is being formed at spreading rifts.
the puzzles are done
the puzzles have ended