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The fact that similar fossils are found on both sides of the ocean is evidence of past land connections between continents, such as Pangaea. This supports the theory of continental drift, where continents were once joined together and have since drifted apart.
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The theory of plate tectonics provides evidence that continents have moved over time. This evidence includes matching geological features between continents that were once part of the same landmass, like the coastlines of Africa and South America. Additionally, the distribution of fossils and the alignment of mountain ranges suggest that continents were once connected and have since drifted apart.
Pangaea began to break apart around 200 million years ago during the Early Jurassic period. This process of continental drift continued over millions of years to form the continents as we know them today.
The breakup of Pangaea occurred due to the movement of tectonic plates. Over millions of years, the immense forces of plate tectonics caused Pangaea to gradually break apart into separate continents that drifted away from each other. This process resulted in the formation of the continents as we know them today.
The word Pangaea means entire Earth. Pangaea is the name for the supercontinent that existed about 200 million years ago. The continents broke apart and drifted into the current positions we know today.
Pangaea was a supercontinent that existed about 335 million years ago. Over time, tectonic plate movements caused Pangaea to break apart, leading to the formation of the continents that we know today. This process is known as continental drift.
Pangaea, the supercontinent that existed around 335 million years ago, has since split apart into the continents we know today. Its landmasses have shifted and drifted due to plate tectonics, and the remnants of Pangaea can be found distributed across the globe in the form of the current continents.
a single landmass or supercontinent
The single continent that split into two continents called Gondwana and Laurasia is Pangaea. Pangaea was a supercontinent that existed about 335-175 million years ago, before eventually breaking apart into these two landmasses which later drifted to form the continents we know today.
The super-continent proposed by the theory of continental drift is called Pangaea. It is believed to have existed about 300 million years ago and subsequently broke apart to form the continents as we know them today.
Before the continents broke apart, they were part of a supercontinent known as Pangaea. Pangaea existed during the late Paleozoic and early Mesozoic eras, around 335 to 175 million years ago. Over millions of years, tectonic plate movements caused Pangaea to gradually split into the continents we know today. As these landmasses drifted apart, they formed separate continents, leading to the present-day configuration of Earth's landmasses.