Magma contributes to the high thermal energy flow readings near the center of the mid-ocean ridge.
What is magma?
- 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.
What is the mid-ocean ridge?
- 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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