- contributes to the high thermal energy flow readings near the center of the mid-ocean ridge
1 answer:
Magma contributes to the high thermal energy flow readings near the center of the mid-ocean ridge.
<h3>
What is magma? </h3>
Magma is the molten or semi-molten natural substance that gives rise to all igneous rocks. Magma can be found beneath the Earth's surface, and evidence of magmatism has been identified on other terrestrial planets and natural satellites. Magma adds to the high thermal energy flow readings around the mid-ocean ridge's center. <h3>What is the mid-ocean ridge?</h3>
A mid-ocean ridge is a system of seafloor mountains generated by plate tectonics. It is normally around 2,600 meters deep and rises about 2,000 meters above the deepest part of an ocean basin. This characteristic occurs when seafloor spreading occurs along a divergent plate boundary.
As the definition itself says, magma adds to the high thermal energy flow readings around the mid-ocean ridge's center.
Therefore, magma contributes to the high thermal energy flow readings near the center of the mid-ocean ridge.
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