Mountain ranges form on previously converging boundaries and take a very long time to form into the mountains known today.
volcano occur in hot spot and diverging boundaries and converging boundaries.
mountains
Approximately 90% of earthquakes occur at or near tectonic plate boundaries. These boundaries are where the Earth's plates interact—diverging, converging, or sliding past one another—resulting in significant geological activity. The remaining earthquakes occur within tectonic plates, often referred to as intraplate earthquakes.
Converging Plate Boundaries
Compressional stresses occur at convergent plate boundaries.
Along the tectonic plate boundaries.
Most earthquakes occur on plate boundaries such as Japan and Chile and most volcanoes occur in diverging plate boundaries like Dallol and Iceland and the Pacific Ring of Fire like Ecuador and Indonesia
Where tectonic plates are converging and diverging with each otherThey are mostly found around the Pacific "Ring of Fire", and more generally on any destructive or contstructive plate boundary.Most occur on destructive plate boundaries. The Pacific 'ring of fire' is an example of a long series of destructive plate margins and most volcanoes and earthquakes on Earth are on it.
In plate tectonics, divergent boundaries occur when plates pull apart. On land, divergent boundaries form rifts or valleys. More commonly, divergent boundaries in the ocean occur and cause mid-oceanic ridges. Divergent boundaries can also form volcanoes when the plates separate enough to allow molten lava to seep out, harden, and eventually form islands.
Convergent boundaries are boundaries where tectonic plates are moving together. Since the edges of both can't be in the same place, one plate will be forced under another plate (and the other above). The plate going 'down' will thus go deeper into the earth - allowing deeper earthquakes to occur.
Volcanoes typically occur at two different types of plate boundaries. These two plate boundaries are: the diverging plate boundary where plates separate, and the converging plate boundaries where one plate is beneath another one at subduction zones.
Converging plate boundaries, also known as convergent boundaries, occur where two tectonic plates move toward each other. This interaction can lead to the subduction of one plate beneath another, resulting in geological features such as mountain ranges, deep ocean trenches, and volcanic activity. The intense pressure and friction at these boundaries can also cause earthquakes. Examples include the boundary between the Pacific Plate and the North American Plate.