Plates & Boundaries

Due to the movement of the tectonic plate, the continent of the Earth continually moves. Please check the map below again.

As you can see, there are areas including the continent and some areas under the sea. The type of crust below the continent is called continental crust, the type found under the sea is called oceanic crust. Continental crust is thicker, about 20 to 40 miles (35 to 70 kilometers) thick - usually older than oceanic crust and oceanic crust is only 4 to 6 mile (7 to 10 kilometers) thick. Every section has a name and usually refers to the land, ocean, or region of the earth.

The boundary between two structural plates is called the boundary. All structural plates are constantly moving around the Earth - very slowly, but moving in various directions. Some people are walking toward each other, some are separated, and some are sliding across each other. Because of these differences, the fairing plate boundary is divided into three main types.

The main structural events associated with these plate boundaries are rupture and faulting along the boundary of the tectonic plate, faults and folds along the destructive plate boundary, and transitions along the boundary of the preserved plate. Earthquakes of different sizes are caused by various types of plate motion that cause various imbalances. Typically, moderate earthquakes occur along the boundaries of the structural plate, as the rate of crushing of the crust and the rate of movement of the plate from the mid-oceanic ridge are much slower and the rate of ascent of the lava by the crack flow is also slow . Therefore, shallow earthquakes occur along the structural plate boundary and the mid-ocean ridge.

A plate boundary or plate edge represents a fault zone separating two different plates. Plate boundaries are mainly of three types: convergence, divergence, and conversion or preservation. The boundary of the cover plate represents two mutually moving plates. There are three kinds at the boundary of the convergence board. The destructive Atlantic boundary, the young and less dense oceanic crust are subducting under the old, light continental crust. Secondly, the destructive ocean - the ocean boundary where one oceanic plate submerses under another oceanic plate. These boundaries form an oceanic island arc like the Philippines. Third, the collision boundary between the continental plate and the second continental plate. At the boundary of this plate is a large mountain fold. Himalaya was formed in this way because India fell into Eurasia about 50 million years ago. Removing the board creates different board boundaries