Usually a dense basaltic magma with low water content.
The three basic kinds of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates come together; and transform boundaries, where plates slide past each other horizontally.
A rift valley is a large depression where tectonic plates are moving apart, creating a gap in the Earth's crust. This forms at divergent boundaries, where plates move away from each other. A mid-ocean ridge is an underwater mountain range formed by the divergence of tectonic plates. They also form at divergent boundaries, specifically at oceanic spreading centers.
At convergent boundaries, where tectonic plates collide, the primary types of magmas formed are andesitic and basaltic magmas. The subduction of an oceanic plate beneath a continental or another oceanic plate leads to the melting of both the subducted slab and the overlying mantle, resulting in magma that is often rich in silica. This process can create stratovolcanoes, which are characterized by explosive eruptions due to the high viscosity of the andesitic magma. Additionally, some basaltic magma can also form from partial melting of the mantle wedge above the subducting slab.
An area where two tectonic plates collide is called a boundary. There are three kinds of boundaries. They are convergent, divergent, and transform boundaries.
Subduction (where one plate is forced beneath another less dense plate - may occur at oceanic-oceanic and oceanic-continental boundaries), obduction (where oceanic plate is forced over a continental plate) and orogenesis where two continental plates collide and mountains are formed (e.g. the Himalayas).
Convergent divergent transform,
The three basic kinds of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates come together; and transform boundaries, where plates slide past each other horizontally.
it can be caused by many things, such as hot spots, convergent plate boundaries, and divergent plate boundaries
There are four transform boundaries divergent boundaries convergent boundaries a fourth boundary where the interactions are not clear and the boundaries are not well defined
Convergent boundaries (plates moving toward each other, also called destructive boundaries), divergent boundaries (plates moving away from each other (sometimes called constructive boundaries), fault lines (sideways movement).
There are three kinds of plate boundaries:spreading boundaries, colliding boundaries, and sliding boundaries. The platea move at amazing show rates, from about 1 to 24 centimeters per year. Thet have been moving for tens of millions of years.
There are three kinds of plate boundaries:spreading boundaries, colliding boundaries, and sliding boundaries. The platea move at amazing show rates, from about 1 to 24 centimeters per year. Thet have been moving for tens of millions of years.
There are three main types of plate boundaries: divergent boundaries (plates move apart), convergent boundaries (plates collide), and transform boundaries (plates slide past each other). These boundaries can create various features such as mountain ranges, volcanoes, and earthquakes.
When plates collide, plate boundaries are formed. There are three kinds. At divergent boundaries, two tectonic plates move away from each other and make earthquakes. At convergent boundaries, two plates come together and make mountain ranges. At transform boundaries, one plate slides under the other.
Shearing stress is one of three kinds of stresses. Compressional and tensional are the others. Shearing stress is associated with transform. The other two kinds of plate boundaries are convergent and divergent.
There are three kinds of plate boundaries:spreading boundaries, colliding boundaries, and sliding boundaries. The platea move at amazing show rates, from about 1 to 24 centimeters per year. Thet have been moving for tens of millions of years.
A rift valley is a large depression where tectonic plates are moving apart, creating a gap in the Earth's crust. This forms at divergent boundaries, where plates move away from each other. A mid-ocean ridge is an underwater mountain range formed by the divergence of tectonic plates. They also form at divergent boundaries, specifically at oceanic spreading centers.