convering divevering sliding
Mountains, volcanoes, rift valleys. Commonly associated with eartquakes. The landform depends on the type of boundary: converging, diverging, transform.
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.
along tectonic plate boundaries
Earthquake foci can be used to mark the earths plate boundaries . The movement along the plate boundary causes the earthquake. Knowing where the foci is can help predict future earthquakes in that scientists can monitor the area for shifts in the plates.
The regions that are located along the tectonic plate boundaries, such as the pacific ring of fire, are most prone to earthquakes due to the movement and interaction of the earth's crustal plate.
they are formed along the crustal movements of the earth.
Mountains, volcanoes, rift valleys. Commonly associated with eartquakes. The landform depends on the type of boundary: converging, diverging, transform.
Because they are generate and evolve from regions within the earth of crustal disturbance and lithospheric instability.
convergent boundaries, divergent boundaries, transform boundaries and plate boundaries
convergent boundaries, divergent boundaries, transform boundaries and plate boundaries
The movement along plate boundaries would cause an earth quake, a tsanami, or either the building of a mountain.
They are geologic features because when the crustal plates move its makes cracks on earth the the mountains are one because everytime the crustal plates move it breaks the earths surface and the dirt and rocks start gathering together
along tectonic plate boundaries.
along plate boundaries
The correct spelling is "asthenosphere" -- the ductile upper layer of the Earth's mantle over which the crustal features or lithosphere moves.
penis.
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.