These are plate boundary where there is relatively little or no creation of new crust or destruction of old crust. At the conservative plate boundary, tectonic plate move side by side horizontally sliding pass one another and berely interacting but only leading to the formation of a kind of line in-between called tranform fault or transform fault line. So it just seem as if the lithosphere in such boundary is conserved and preserved.
The four main types of plate tectonics are divergent boundaries, where plates move away from each other; convergent boundaries, where plates collide; transform boundaries, where plates slide past each other horizontally; and subduction zones, where one plate is forced beneath another.
The three types of plate margins are convergent boundaries, where plates move toward each other; divergent boundaries, where plates move apart from each other; and transform boundaries, where plates slide past each other horizontally.
The older denser plate sinks under a deep ocean trench into the mantle. Some rock above the subducting plate melts and forms magma. Since the magma is less dense than the surrounding rock, it rises toward the surface. Eventually, the magma breaks through the ocean floor, making a volcanoe.
It's Constructive plate boundary which is often found near north & south america... The other r destructive & conservative.. BUT THE ANS IZZZ CONSTRUCTIVE,,,,
tectonic boundaries where plates interact, such as divergent boundaries where plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past each other. These interactions create earthquakes, volcanic activity, mountain ranges, and oceanic trenches, providing evidence for plate movement. Seafloor spreading and paleomagnetism also support the theory of plate tectonics.
a plate boundary there are constructive plate boundaries, destructive plate boundaries, conservative plate boundaries and collision plate boundaries
luke worth
YES!
they are mainly conservative plate boundaries but can be all but constructive plate boundarys by callum 11
No, the L'Aquila earthquake was not caused by a conservative plate boundary. It was associated with the movement along a normal fault within the Eurasian Plate. Normal faulting occurs at divergent plate boundaries, where plates move away from each other, rather than at conservative plate boundaries where plates slide past each other horizontally.
Earthquakes occur at conservative plate boundaries because plates are grinding past each other, causing friction to build up. When the stress from built-up friction is released, it sends seismic waves through the Earth's crust, resulting in an earthquake. These boundaries are also known as transform boundaries.
New crust is not formed at conservative plate boundaries. Instead, these boundaries involve plates sliding past each other horizontally without any creation or destruction of crust. This movement can cause earthquakes as the plates interact.
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
Transform boundaries, also known as conservative boundaries, are locations where two tectonic plates slide past each other horizontally. These boundaries are characterized by lateral movement, where the plates grind against each other, causing earthquakes due to friction. An example of a transform boundary is the San Andreas Fault in California, where the Pacific Plate and the North American Plate are sliding past each other.
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
Slip slide Reverse thrust Normal I think that's right. School sucks.The 3 types of tectonic plate boundaries are: constructive boundary, destructive boundary and conservative boundary.
The four main types of plate tectonics are divergent boundaries, where plates move away from each other; convergent boundaries, where plates collide; transform boundaries, where plates slide past each other horizontally; and subduction zones, where one plate is forced beneath another.