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swagg
The earth's crust floats on the mantle. The movement is very slowly. Despite this slowness, over millions of years, this movement has created many of our Earth's landforms. Landforms are created because the plates are moving in different directions. When plates are moving away from each other they form divergent boundaries. Plates that are moving towards one another from convergent boundaries. At some places where plates come together, they crumple and lift to form mountains. Other converging plates form subduction zones . An ocean trench marks the region where a denser plate is forced under ( subducts) a less dense plate . Plates also move in sliding motion past one another to form transform fault boundaries. The motion at these boundaries is more like a grinding and scraping with sudden jolts due to the building up of pressure.
cracked flat lands
Paracelsus
Lifeforms.
Convection currents beneath the tectonic plates of the crustal surface of the earth provide heat from the core in circular motions, and make plate boundaries move together from compressional forces at convergent boundaries, apart from tensional forces at divergent boundaries, and side by side from shear force at transform boundaries.
it makes a disaster
swagg
The earth's crust floats on the mantle. The movement is very slowly. Despite this slowness, over millions of years, this movement has created many of our Earth's landforms. Landforms are created because the plates are moving in different directions. When plates are moving away from each other they form divergent boundaries. Plates that are moving towards one another from convergent boundaries. At some places where plates come together, they crumple and lift to form mountains. Other converging plates form subduction zones . An ocean trench marks the region where a denser plate is forced under ( subducts) a less dense plate . Plates also move in sliding motion past one another to form transform fault boundaries. The motion at these boundaries is more like a grinding and scraping with sudden jolts due to the building up of pressure.
The earth's crust floats on the mantle. The movement is very slowly. Despite this slowness, over millions of years, this movement has created many of our Earth's landforms. Landforms are created because the plates are moving in different directions. When plates are moving away from each other they form divergent boundaries. Plates that are moving towards one another from convergent boundaries. At some places where plates come together, they crumple and lift to form mountains. Other converging plates form subduction zones . An ocean trench marks the region where a denser plate is forced under ( subducts) a less dense plate . Plates also move in sliding motion past one another to form transform fault boundaries. The motion at these boundaries is more like a grinding and scraping with sudden jolts due to the building up of pressure.
Glaciation
cracked flat lands
The boundaries of history of eras are marked by great worldwide changes in continental coastline
They can change coastines by a few miles.
Are you thinking of "plate tectonics"? This process changes landforms, but doesn't create them. The only process that creates land is volcanic outflow.
It changes by force rubbing up against items creating friction, causing erosion, which can change landforms.
Landforms change.