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This changes the shapes of continents because different parts of the continents converge and diverge at different rates. So the Northern part of a continent could be spreading apart faster than the southern.
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Due to plate tectonics still moving, it causes the Earth's oceans and continents to continue moving.
Climates can change suddenly for brief periods after a volcanic eruption. In contrast, the movement of continents causes steady climate changes over many millions of years
Continents moving is an example of Earth's slow change.
they can increase or move the size of the continents
This changes the shapes of continents because different parts of the continents converge and diverge at different rates. So the Northern part of a continent could be spreading apart faster than the southern.
Continental rifting will cause plants and animals to evolve due to their changing habitats. Plants and animals that become isolated will begin to diverge and change to fit into their new ecosystems.
Continents have undergone changes such as plate tectonics, leading to their movement across the Earth's surface over millions of years. These movements have resulted in the formation and breakup of supercontinents, the opening and closing of oceans, and the creation of mountain ranges and other geological features. Additionally, factors like climate change and sea level fluctuations have also influenced the shape and position of continents over time.
It has the properties of a chemical change.
The cycle of repeated collisons and rifting caan create old and complicated mountain ranges, such as the Appalachian Mountain
identify the different face change in matter
No, not currently. The continents won't change for hundreds of millions of years as they move extremely slowly.
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The breakup of Pangaea led to the drifting of the continents to their current positions due to tectonic plate movement. This process involved the formation and shifting of ocean basins, creation of mountain ranges, and the development of new geological features. The movement continues today through processes such as seafloor spreading and subduction.
Condensation
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