volcanoes
Mountains are formed at the boundary where tectonic plates collide or move apart.
Plates pushed together makes mountains therefore plates pulled apart makes volcanos
Mountain ranges formed by the pushing together of tectonic plates are called fold mountains. Examples include the Himalayas and the Alps, where the collision of plates has caused the Earth's crust to fold and create towering mountain peaks.
At collision, mountains, at separation, long deep holes into the earth.
rift valley Answer 2 Continents are formed when continental plates pull apart.
Regular mountains are typically formed through tectonic plate movements. When two plates collide or move apart, the Earth's crust can be pushed up or folded, creating mountain ranges through processes like folding, faulting, and volcanic activity over millions of years. Erosion also plays a role in shaping the final form of a mountain.
Mountains are created when plates push against each other, some plates pull apart, or rub together instead.
When magma pushes 2 plates apart. :)
The Nile
At divergent boundaries, mid-ocean ridges are formed as tectonic plates pull apart. At converging boundaries, various geologic features are formed such as trenches, mountains, and volcanic arcs, depending on the type of plates involved (oceanic vs. continental).
the rocky mountains are located in North America. A long time ago, there was one big continent on the planet earth and soon enough, it drifted apart into plates. When those plates crashed together, they forced the earth's crust to go up, and over time the plates were pushed together so much, it forced them really high and they formed the Rocky mountains.
Fault block mountains are formed when tectonic plates are pulled apart, creating normal faults that result in blocks of land being uplifted. Rift valleys, on the other hand, are formed when tectonic plates are pulled apart, creating a depression between two parallel fault lines. Fault block mountains are characterized by steep slopes and sharp peaks, while rift valleys are characterized by long, narrow depressions.