The soft, weak layer of rock below the lithosphere is called the asthenosphere. It is semi-molten and behaves plastically, allowing the tectonic plates of the lithosphere to move and slide on top of it.
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.
If there were such a thing it would not be soft, it would be liquid, and would be called magma. There really is no completely molten layer of Earth except for the outer core which is composed primarily of liquid iron along with some nickel and other trace elements.
The plastic-like part of the mantle is known as the asthenosphere. It is a semi-fluid layer located beneath the lithosphere, composed of partially molten rock material that allows for the movement of tectonic plates.
No layer is truly made of liquid rock. The mantle is sometimes, inaccurately, said to be liquid rock when it is in fact solid, albeit relatively soft. The outer core is liquid, but it consists of liquid metal, not rock.
The layer of rock that is somewhat soft and less rigid is typically the sedimentary layer, particularly those that contain materials like clay or silt. These rocks can be more easily eroded and deformed compared to harder igneous or metamorphic rocks. Additionally, the presence of water can further soften these sedimentary layers, making them susceptible to changes.
The relatively soft, weak layer of rock below the lithosphere is called the asthenosphere. It is partially molten and allows the lithospheric plates to move on top of it. The asthenosphere plays a key role in the process of plate tectonics.
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.
The soft layer of rock in the mantle is called the asthenosphere. It is located beneath the lithosphere and consists of partially molten rock that allows for the movement of tectonic plates.
The soft layer of rock in the mantle is called the asthenosphere. It is partially molten and enables the movement of tectonic plates. This layer lies beneath the lithosphere and contributes to the process of plate tectonics.
asthenosphere
asthenosphere
If there were such a thing it would not be soft, it would be liquid, and would be called magma. There really is no completely molten layer of Earth except for the outer core which is composed primarily of liquid iron along with some nickel and other trace elements.
The soft layer of rock in the Earth's mantle is called the asthenoshere. The asthenoshere is a solid but able to flow slowly.
It Is Known As The Asthenoshere
The soft layer of the mantle on which the lithosphere floats is called the asthenosphere. It is a partially molten layer that allows for the movement of tectonic plates due to its weak and ductile properties. The lithosphere, which is the rigid outer layer of the Earth, sits on top of the asthenosphere and moves due to the convection currents in the mantle beneath it.
The flowing water falls on the soft rock below, it wears it away and hard rock from the top of the water fall falls on the soft rock, as the hard rock falls from the top, it leaves a dent and the water wears this away, then pushing the waterfall back, wooop woopA waterfall is formed when there is a layer of hard rock and a layer of soft rock. The soft rock is eroded away first, so that the harder rock just hangs over, creating a waterfall.
The flowing water falls on the soft rock below, it wears it away and hard rock from the top of the water fall falls on the soft rock, as the hard rock falls from the top, it leaves a dent and the water wears this away, then pushing the waterfall back, wooop woopA waterfall is formed when there is a layer of hard rock and a layer of soft rock. The soft rock is eroded away first, so that the harder rock just hangs over, creating a waterfall.