Tectonic plates, although rigid, also move. And they move in rebound, because of the tremendous heat that comes out of the interior of our planet, which burns at 6.7500º C, almost like the sun. This fiery heat moves the mantle and consequently expands into the lithosphere and Earth's crust.
Recrystallization is when original grain sizes are obliterated so grains become uniform and larger.
The annual temperature range in Vancouver with that at most other locations at a similar latitude have similarities as well as differences.
It is similar due to the presence of same latitude from the sea level means they are presence near the water body but at the same time it has differences due to the presence of different environmental conditions as compared to other regions.
The seasonal migration of pressure and wind systems is responsible for the precipitation in a region so if change occurs in both these factors, it will reduced summer precipitation at Vancouver.
The humid continental climate type rare in the Southern Hemisphere because of the larger ocean area at that latitude and greater maritime moderation. Continental climates are not found in the Southern Hemisphere because of the absence of a continent large enough to generate this effect.
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Answer:
B. intrusion of magma into fractions
Explanation:
A pluton is a type of rock that is formed when magma cools and solidifies underground, they are an intrusive igneous rock (forced into other layers of rock), usually in cracks. The three main types of pluton are bysmalith (cylindrical), lopolith (mushroom-shaped), and laccolith (blister-shaped).
Because magma is under high pressure and takes a long time to cool, it allows time for the formation of large crystals. Therefore, plutonic rocks have coarse-grained crystals that come in many different colors and sizes. A good example is granite.
<em>Considering this information we can conclude that pluton is not manmade rock, they come in different sizes (not only large) so the correct answer is B. intrusion of magma into fractions. </em>
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