There are three kinds of plate tectonic boundaries: divergent, convergent, and transform plate boundaries.

This figure shows the three main types of plate boundary, divergence, convergence, and transformation. Image provision by US Geological Survey

Chile's triple interchange is the only modern place on the planet. There is a subduction zone at the edge of the continent, and an active central ridge enters. This is a particularly interesting research area, as we can observe the two plate boundaries (divergence and convergence) and their very close processes.

A diverging boundary arises when the two structural plates are separated from each other. Along these boundaries long cracks and lava from the geyser spewed hot water. Frequent earthquakes occur along the rips. Under the crack, magmatic lava rose from the mantle. It penetrates into the gap and clumps into a hard rock, forming a new shell at the torn end of the panel. Magmas from the mantle clump to the basalts at the seafloor, dark and dense rocks. Therefore, at different boundaries, oceanic crust made of basalt is generated.

When two plates are brought together, it is called the convergence boundary. Collision of two collision plates bends the edges of one or both plates into a steep mountain, sometimes bends the other into a deep-sea bottom groove. The chain of volcanoes is usually parallel to the boundary, mountains and grooves. A strong earthquake shook a vast area on both sides of the boundary

If one of the collision plates has an oceanic crust at the top it will be forced to the mantle where it begins to melt. Magma enters another plate, passes through, and solidifies. Magma formed by the melting plate solidifies into granite. Granite is a light-colored, low density rock that forms the continent. Therefore, at the convergence boundary, a continental crust consisting of granite is formed and the oceanic crust is destroyed.

Two plates sliding against each other form the boundary of the transition plate. Natural or artificial structures passing through the transformed boundary are transmitted in the opposite direction offset to the fragments. Rocks lining along the boundary are shattered when the plate is crushed to form a linear fault valley or an undersea canyon. If the plates jump alternately blocking and jumping, the earthquake will ham in a wide boundary area. Contrary to the convergence boundary and the branch boundary, magma was not formed. Therefore, the crust ruptures and ruptures at the edge of deformation, but it will not produce or destroy

There are three types of plate boundary: convergence, divergence, and deformation. According to the "Future Classroom" website, the boundaries converge when the two structural plates meet directly, either squeezed together or squeezed together. A divergent boundary is formed when the two plates are separated. The transition boundary occurs when two plates slide against each other, like the San Andreas fault in California. Volcanoes only occur at the boundary of converging and diverging plates. At the convergence boundary, a plate is pushed under another plate to form a volcano that develops along the ridge and its ridge. When the plate meets, a great force is applied. This creates cracks in the Earth's crust. And it is filled with magma escaping from the mantle and ultimately produces a volcano as described by BBC Bitesize. Conversely, as plates move in opposite directions at different boundaries, the casing bursts and creates gaps.

How do structural plates move relative to each other? Geologists classify different types of structural plate boundaries by moving them relative to each other. There are mainly three types at the plate boundary. Convergence, divergence, and transformation. On different boundaries, the construction plates are far apart from each other. The structural plates move toward one another at the convergence boundary. At the boundary of the deformed plate, the structural plates move relative to each other. Earthquakes can occur at any of these plate boundaries