There are three kinds of plate tectonic boundaries<span>: </span>divergent<span>, convergent, and transform </span>plate boundaries<span>. So your answer is false !</span>
It should be noted that the three types of rocks are igneous, sedimentary, and the metamorphic rock.
<h3>Types of rocks.</h3>
Your information is incomplete. Therefore, an overview will be given. It should be noted that rocks are a solid mass of geological material.
There are three main types of rocks and they are igneous, sedimentary, and the metamorphic rock.
Learn more about rocks on:
brainly.com/question/13291293
S.P.R.I.T.E
Social Globalization
Political Globalization
Religious Globalization
Intellectual Globalization
Technological Globalization
Economic Globalization
Explanation:
are tectonic earthquake in one that occurs when the earth crust death due to geological forces on Rock and adjoining place that cause physical and chemical changes volcanic earthquake is any earthquake that results from tectonic forces which occurs in conjunction with volcanic activity .
Answer:
Partial melting occurs when only a portion of solid is melted. It is thus enriched in the chemical components of minerals with lower melting temperatures and the remaining unmelted portion of the rock is composed of minerals with highest melting temperatures. Partial melting preferentially enriches melts with incompatible elements.
Partially melted rock do not usually experience complete melting inside the Earth, due to their different chemical composition and their melting points.
It is thought that partial-melting processes play a major role in generating more-defined liquids from less-evolved ones, so that many basalts may be the result of partial melting in the upper mantle, and many granites may have derived partly or completely from the partial melting of continental crust (anatexis).With increasing temperature and pressure, the subducted oceanic crust (of basic composition) first undergoes metamorphism and then begins to melt or release watery fluids; this material rises into the overlying mantle, which may also begin to melt, giving rise to intermediate magma.