The asthenosphere is a hot, semi-fluid layer in the upper mantle beneath the lithosphere. It is ductile and allows tectonic plates to move by flowing slowly. It has partially melted rock, causing seismic waves to slow down, and plays a key role in plate tectonics and mantle convection.
Answer:Location:The asthenosphere is found beneath the lithosphere, roughly 100 to 350 kilometers below the Earth's surface.Physical State:It is semi-solid or partially molten. The rocks here are not completely liquid but are soft and can flow slowly.Temperature and Pressure:The temperature is very high (about 1,300°C to 2,000°C), causing rocks to be close to their melting point. The pressure is also very high due to the depth.Plasticity:The asthenosphere is plastic, meaning it can bend, flow, and deform without breaking. This allows the tectonic plates above it (the lithosphere) to move.Role in Plate Tectonics:The movement of the asthenosphere is what drives the movement of tectonic plates, causing earthquakes, volcanic activity, and the formation of mountains.Composition:It is mainly composed of peridotite, a type of ultramafic rock rich in iron and magnesium.Convection Currents:The heat from the Earth's interior causes convection currents in the asthenosphere, which help move the lithospheric plates.Summary:The asthenosphere is a hot, semi-fluid layer of the Earth beneath the lithosphere, characterized by its ability to flow and its role in plate tectonics.