AThe Crust
BThe Upper Mantle
CThe Core
DThe Lower Mantle
Answer:
B. The Upper Mantle
Read Explanation:
Earth's Interior Layers
The Asthenosphere: It is a highly viscous, mechanically weak, and ductile region of the Earth's upper mantle. It lies just below the lithosphere.
Depth and Location: It typically begins at a depth of about 80 to 100 km and extends to approximately 700 km below the Earth's surface.
Physical Properties: The material here is in a semi-molten state due to high temperatures and pressures, which allows it to behave plastically. It is the zone where convection currents occur.
Geological Significance: The movement of tectonic plates, which make up the rigid Lithosphere, is facilitated by the plastic, flowing nature of the asthenosphere beneath them.
Key Comparisons:
Lithosphere: The rigid, outermost shell of the Earth, consisting of the crust and the uppermost part of the mantle.
Asthenosphere: The ductile, flowing layer immediately beneath the lithosphere.
Mesosphere: The section of the mantle below the asthenosphere, extending to the core-mantle boundary (the Gutenberg discontinuity).
Scientific Terminology: The term astheno comes from the Greek word meaning 'without strength', reflecting its ability to deform rather than fracture under stress.
