Asthenosphere.
The upper mantle is divided into two main sections: the lithosphere and the asthenosphere. The lithosphere is rigid and includes the crust, while the asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur.
Both the asthenosphere and lithosphere are part of Earth's upper mantle. The asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur, while the lithosphere includes the rigid outer layer of the Earth that consists of the crust and the uppermost part of the mantle.
The lithosphere is generally thought of as the crust and outer mantle of the earth. They're solid, and there are no convection currents in solids as we normally think of them. As we move inward toward the core of the earth, we begin to encounter molten rock (magma), and convection currents exist in this superheated fluid.
Most convection currents that cause seafloor spreading are thought to be located in the asthenosphere, which is a semi-fluid layer of the Earth's upper mantle beneath the lithosphere. The movement of these convection currents is believed to drive the motion of tectonic plates.
mesosphere, asthenosphere, ionosphere
it "surfs" on top of the asthenosphere's convection currents. we walk on it (it's the crust and the brittle portion of the upper mantle)
The upper mantle is divided into two main sections: the lithosphere and the asthenosphere. The lithosphere is rigid and includes the crust, while the asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur.
Both the asthenosphere and lithosphere are part of Earth's upper mantle. The asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur, while the lithosphere includes the rigid outer layer of the Earth that consists of the crust and the uppermost part of the mantle.
The lithosphere is generally thought of as the crust and outer mantle of the earth. They're solid, and there are no convection currents in solids as we normally think of them. As we move inward toward the core of the earth, we begin to encounter molten rock (magma), and convection currents exist in this superheated fluid.
The convection currents running through the asthenosphere are widely believed to be the source of movement of the tectonic plates.
The softer layer below the lithosphere is the asthenosphere. The asthenosphere begins at a depth of approximately 150 km. It has convection currents that arise from the heating and subsequent rising of material from the lower asthenosphere. These convection currents drive the movement of lithospheric plates at the surface, and are the cause of tectonic activity.
Convection currents are circular movements of fluid driven by temperature differences. In Earth's mantle, convection currents occur in the asthenosphere, which is the semi-solid layer beneath the lithosphere. These currents play a significant role in plate tectonics and the movement of Earth's crustal plates.
Most convection currents that cause seafloor spreading are thought to be located in the asthenosphere, which is a semi-fluid layer of the Earth's upper mantle beneath the lithosphere. The movement of these convection currents is believed to drive the motion of tectonic plates.
The asthenosphere is partially molten and has a lower viscosity compared to the lithosphere above it. This low viscosity allows the lithosphere plates to move and glide over the asthenosphere. The plasticity of the asthenosphere enables convection currents to occur, which in turn can drive the movement of the lithosphere plates.
mesosphere, asthenosphere, ionosphere
The rigid zone above the asthenosphere that includes the crust and upper mantle is called the lithosphere. This layer is divided into tectonic plates that float on the semi-fluid asthenosphere and move due to the convection currents beneath them.
The convection currents that drive tectonic plate motion are found in the asthenosphere, which is the semi-fluid layer of the earth located beneath the lithosphere. These currents are created by the heat from the Earth's core, causing the asthenosphere to flow and move the tectonic plates above it.