mantle
The layer directly below the lithosphere is the asthenosphere. The asthenosphere is partially molten and allows for the movement of tectonic plates above it.
The layer directly under the Lithosphere is the Asthenosphere. The Asthenosphere is a semi-fluid layer of the Earth's mantle that allows for the movement of the tectonic plates above it. It is hotter and more ductile compared to the rigid Lithosphere.
Oceans are primarily found on the Earth's surface, which is part of the outermost layer known as the lithosphere. Beneath the lithosphere lies the asthenosphere, but the oceans themselves rest directly on the lithosphere. The water in the oceans also interacts with the atmosphere above and the hydrosphere, which encompasses all water on Earth.
The layer directly above the asthenosphere is the lithosphere.
The Earth layer known as the lithosphere consists of the crust and uppermost mantle. There is no solid layer above the lithosphere.
The Earth layer known as the lithosphere consists of the crust and uppermost mantle. There is no solid layer above the lithosphere.
Asthenosphere is directly before the lithosphere.
lithosphere
The asthenosphere.
The Earth's lithosphere, which includes the rigid outer layer of the Earth's surface where seismic waves travel through, is located directly above the source of vibration.
The Gutenberg discontinuity is found directly above the outer core.
The asthenosphere.