They are all boundaries between or fractures within the Tectonic Plates forming the Earth's crust.
A convergent boundary is that between two approaching plates; usually an ocean-floor plate being subducted beneath the continental plate as the ocean closes. This is happening now to the Pacific Ocean.
A divergent boundary is the opposite: the fracture of plate into two parts moving away from each other. The break is closed by upwelling magma. E.g. The Mid-Atlantic Ridge - the Atlantic is presently widening away from this subsea mountain-range at a mean rate of about 25mm/yr.
Transform boundaries, or Transform Faults, are shear fractures across the plate at roughly right-angles to the spreading-ridge from which the emanate. They represent the effect of unequal spreading forces. If you look at a relief map of the Atlantic Ocean bed you will see many transform faults to E and W of the Mid-Atlantic Ridge
They are all boundaries between or fractures within the Tectonic Plates forming the Earth's crust.
A convergent boundary is that between two approaching plates; usually an ocean-floor plate being subducted beneath the continental plate as the ocean closes. This is happening now to the Pacific Ocean.
A divergent boundary is the opposite: the fracture of plate into two parts moving away from each other. The break is closed by upwelling magma. E.g. The Mid-Atlantic Ridge - the Atlantic is presently widening away from this subsea mountain-range at a mean rate of about 25mm/yr.
Transform boundaries, or Transform Faults, are shear fractures across the plate at roughly right-angles to the spreading-ridge from which the emanate. They represent the effect of unequal spreading forces. If you look at a relief map of the Atlantic Ocean bed you will see many transform faults to E and W of the Mid-Atlantic Ridge
Rhe tectonic plates are moving in both divergent and transform boundaries
Subduction doesnt occur at divergent boundaries, but rather they are found at convergent boundaries.
.....tectonic plates
Volcanoes are more common along convergent boundaries
There are three main types: Convergent boundaries (where two plates are being pushed together) Divergent boundaries (where two plates are being pulled apart) Transform boundaries (where two plates are sliding past each other).
Rhe tectonic plates are moving in both divergent and transform boundaries
Subduction doesnt occur at divergent boundaries, but rather they are found at convergent boundaries.
Any type of plate boundary can cause an earthquake. That said, areas along convergent, divergent, and transform tectonic plate boundaries are the most likely places for earthquakes to occur.
.....tectonic plates
Volcanoes are more common along convergent boundaries
There are three main types: Convergent boundaries (where two plates are being pushed together) Divergent boundaries (where two plates are being pulled apart) Transform boundaries (where two plates are sliding past each other).
Convergent (or destructive): Where two plates are moving toward each other. Collisions between oceanic plates results in subduction of the more dense plate. Collisions between an oceanic plate and a continental plate may result in the subduction of the oceanic plate because oceanic plates are more dense than continental plates. Collisions between two continental plates results in uplift and mountain formation where neither plate subducts.Divergent (or constructive): Where two plates are moving away from each other. Divergent plate boundaries are the site of new crust formation, particularly at the mid-ocean ridges, where spreading plates are infilled with basaltic magma from the asthenosphere.Transform (or conservative): Where two plates slide (actually 'grind') alongside each other and neither plate subducts. Earthquakes are common at transform faults due to the grinding and snapping movements of the plates as they move.
The things in common is that they form something.
The things in common is that they form something.
Rift Valleys are the most common at oceanic-continental convergent boundaries.
They are common at transform boundaries because strike-slip faults move up and down like transform boundaries.
Composite cone volcanos are the most common.. Shielding and other types are results from a divergent boundary.