Water can be stored above the lithosphere in various places, such as in lakes, rivers, and glaciers on the Earth's surface. Additionally, water can also be stored in the atmosphere as clouds and in the polar ice caps.
Below the lithosphere is the asthenosphere, a semi-solid layer of the upper mantle. This layer is partially molten, allowing for the movement of tectonic plates above it. The asthenosphere is hotter and more ductile compared to the rigid lithosphere above.
The lithosphere is basically the part of Earth that we stand on. It consists of the crust and the uppermost part of the mantle. Under the lithosphere is the mantle, then the outher and inner core. Over it? Technically, just the crust. Then...us.
The crust and the upper mantle are a geological part of the earth called the lithosphere. There are 2 parts of the lithosphere: the oceanic lithosphere, which is made up of land underneath water, and the continental lithosphere, which is the the part made of just land. The lithosphere lies on top of the asthenosphere. The lithosphere is made up of tectonic plates, which are pieces of land floating on the lithosphere.
The lower boundary of the asthenosphere is not well defined. It lies below the lithosphere and above the lower mantle and outer core. It usually lies at depths of 80-200 km but can range as deep as 700 km.
The crust and uppermost hard rocky mantle, together, is known as the lithosphere, which is above the plastic-like upper mantle area known as the asthenosphere.
Water is stored above the surface in bodies of water such as lakes, rivers, and ponds. Below the surface, water is stored in groundwater aquifers, which are underground layers of rock or sediment that hold water.
The Earth layer known as the lithosphere consists of the crust and uppermost mantle. There is no solid layer above the lithosphere.
The top part of the mantle and the crust above it form into lithosphere.
The Earth layer known as the lithosphere consists of the crust and uppermost mantle. There is no solid layer above the lithosphere.
is inaccessible to plant life
lithosphere
The lithosphere. "Lith" is the root word for rock.
Below the lithosphere is the asthenosphere, a semi-solid layer of the upper mantle. This layer is partially molten, allowing for the movement of tectonic plates above it. The asthenosphere is hotter and more ductile compared to the rigid lithosphere above.
mantle
The lithosphere is basically the part of Earth that we stand on. It consists of the crust and the uppermost part of the mantle. Under the lithosphere is the mantle, then the outher and inner core. Over it? Technically, just the crust. Then...us.
lithosphere Islands and continents are usually found in areas that have been surrounded by a large mass of water.
Igneous Rocks