The mechanical layer that sits on top of the physical layer in the OSI model is the data link layer. This layer is responsible for node-to-node data transfer and error detection and correction, ensuring reliable communication between devices on the same network. It encapsulates the raw bitstream from the physical layer into frames, adding necessary addressing and control information.
The lithosphere sits on top of the asthenosphere.
The mechanical layer that sits on top of the asthenosphere is the lithosphere. The lithosphere includes the Earth's crust and the uppermost portion of the mantle, which are rigid and behave as a solid layer. This layer is divided into tectonic plates that float on the more ductile asthenosphere beneath.
The mechanical layer that sits on top of the asthenosphere is the lithosphere. The lithosphere comprises the Earth's crust and the uppermost part of the mantle, and it is rigid and relatively cool compared to the underlying, more ductile asthenosphere. This layer is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.
The mechanical layer that sits on top of the asthenosphere is the lithosphere. The lithosphere includes the Earth's crust and the uppermost part of the mantle, characterized by its rigidity and ability to support tectonic plates. It is generally cooler and more brittle compared to the underlying, more ductile asthenosphere.
The Earth's crust is part of the lithosphere, which includes the crust and upper mantle. The lithosphere is a rigid layer that sits on top of the asthenosphere, a partially molten layer beneath it.
The lithosphere sits on top of the asthenosphere.
The mechanical layer that sits on top of the asthenosphere is the lithosphere. The lithosphere includes the Earth's crust and the uppermost portion of the mantle, which are rigid and behave as a solid layer. This layer is divided into tectonic plates that float on the more ductile asthenosphere beneath.
The mechanical layer that sits on top of the asthenosphere is the lithosphere. The lithosphere comprises the Earth's crust and the uppermost part of the mantle, and it is rigid and relatively cool compared to the underlying, more ductile asthenosphere. This layer is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.
The mechanical layer that sits on top of the asthenosphere is the lithosphere. The lithosphere includes the Earth's crust and the uppermost part of the mantle, characterized by its rigidity and ability to support tectonic plates. It is generally cooler and more brittle compared to the underlying, more ductile asthenosphere.
The layer that sits on top of the asthenosphere is the lithosphere. The lithosphere includes the rigid outer layer of the Earth, encompassing the crust and the uppermost part of the mantle. It is characterized by its solid and brittle nature, contrasting with the semi-fluid behavior of the underlying asthenosphere.
The Cornea, which is a clear layer that sits on top of the eyeball.
The Cornea, which is a clear layer that sits on top of the eyeball.
The lithosphere.
It is called ozone layer. It sits in the stratosphere.
The mechanical layer above the core is the mantle. It is a thick layer of rock that sits between the core and the Earth's crust. The mantle is responsible for convection currents that drive plate tectonics and other geological processes.
Soil scientists divide soil into horizons based on depth and soil make up. The O horizon, the very top layer right under the grass, is where the top soil is. This is the soil that is critical to human life.
The mechanical layer below the lithosphere is the asthenosphere. This layer is partially molten and allows the lithosphere to move and float on top of it. The asthenosphere plays a crucial role in plate tectonics by facilitating the movement of tectonic plates.