Answer:
The story begins millions of years ago when the Conway Granite was once molten rock that forced its way into older and colder rocks deep below the earth's surface. ... The Conway Granite is one body of igneous rock (bedrock formation) that formed from this magma, underlying much of the White Mountains today.
Explanation:
Answer:Winter
Winter: The northern hemisphere is experiencing winter when the North Pole is tilted away from the sun. You can see this in the picture of the Earth on the right. It is experiencing winter because it doesn't get as many direct sun rays.
Explanation:
Correct Option is D). Burial type/form of metamorphism has a tendency to arise in areas wherein large quantities of sedimentary or volcanic substances gather in a subsiding basin, pushing older rocks similarly into the interior.
Burial metamorphism happens while sediments are buried deeply sufficient that the warmth and strain purpose minerals to start to recrystallize and new minerals to grow, however does now no longer depart the rock with a foliated appearance. As metamorphic strategies go, burial metamorphism takes location at notably low temperatures (up to ~300 °C) and pressures (100s of m depth). To the unaided eye, metamorphic modifications might not be obvious at all.
Regional metamorphism refers to large-scale metamorphism, together with what occurs to continental crust alongside convergent tectonic margins (wherein plates collide). The collisions bring about the formation of lengthy mountain ranges, like the ones alongside the western coast of North America.
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I think the answer is either C or D
Answer: seafloor spreading and subduction magmatism
Explanation: Continental crust are termed as the crust destroyed by plate tectonic process mostly.Continental crust usually lies above sea level and because of this existence of land life to evolve from marine life possible.
Seafloor spreading is a type of process in which tectonic plate of Earth's lithosphere separate from one another. Subduction is also a process related with continental crust that occurs when tectonic plates collide with each other rather than getting apart.
