ALithosphere
BMantle
CAsthenosphere
DBarysphere
Answer:
C. Asthenosphere
Read Explanation:
Correct Answer: Option C (Asthenosphere)
The asthenosphere is the primary source of magma that causes volcanic eruptions. Located in the upper mantle beneath the lithosphere, the asthenosphere is a semi-molten layer of rock that exists at depths of approximately 80-200 kilometers below the Earth's surface.
The asthenosphere has several key characteristics that make it the source of magma:
1. Temperature and Pressure: The asthenosphere experiences high temperatures (around 1300-1600°C) and moderate pressure conditions that keep the rock in a partially molten state.
2. Partial Melting: Due to the specific temperature-pressure conditions, rocks in the asthenosphere undergo partial melting, creating pockets of molten rock (magma).
3. Convection Currents: The asthenosphere experiences convection currents that help transport the molten material upward toward the Earth's surface.
4. Tectonic Activity: At plate boundaries, the asthenosphere's magma can rise through cracks and weaknesses in the overlying lithosphere, eventually reaching the surface as volcanic eruptions.
While the lithosphere is the outermost solid layer, the mantle (including the asthenosphere) is the deeper layer, and the barysphere refers to the Earth's core - it is specifically the asthenosphere within the upper mantle that provides the ideal conditions for magma generation and volcanic activity.