Just go outside and put your feet on the ground, that is an example of our lithosphere.
The ground you are standing on, i.e. the surface of a planet.
The word Lithosphere means ball of stone
Hydrosphere erodes a part of lithosphere and at the same time the atmosphere is constantly incorporating a part of hydrosphere via evaporation and dumping some of it in lithosphere. From the lithosphere, it is transported back to the hydrosphere and the cycle continues.
Oceans: Oceans are not made up of solid lithosphere, but rather liquids and gases. Volcanoes: Volcanoes are composed of molten rock, which is not part of the lithosphere. Soil: Soil is composed of organic matter and weathered rocks, and is not part of the lithosphere. Atmosphere: The atmosphere is composed of gases and does not form part of the lithosphere. Subduction Zones: Subduction Zones are areas of Earth's crust where one plate slides beneath another, and are not part of the lithosphere.
hot spring
Just go outside and put your feet on the ground, that is an example of our lithosphere.
The word Lithosphere means ball of stone
The ground you are standing on, i.e. the surface of a planet.
So the lithosphere is the crust that we live on, and the hydrospehere is the layer of water/oceans etc. So if the lithospehere cracks, it sends magma up, into the hydrosphere. Also, search subduction zones. Hope this helps!
lithosphere itself tells us that light the land do not make it barren
turd
Lithosphere, Hydrosphere, Atmosphere, Biosphere
The lithosphere is extremely hot. The temperature of the lithosphere can reach around 600 degrees Celsius. Although this is the case in a general sense, some scientists argue that temperatures can reach up to 1200 degrees Celsius within the lithosphere.
because stuff goes and hits some other stuff and.........BOOM..... oceanic lithosphere
Hydrosphere erodes a part of lithosphere and at the same time the atmosphere is constantly incorporating a part of hydrosphere via evaporation and dumping some of it in lithosphere. From the lithosphere, it is transported back to the hydrosphere and the cycle continues.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.