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.
The deeper portions of it are quite hot. However, the lithosphere includes the crust, which extends to the surface, which is not necessarily hot.
hot
The lithosphere is cold and brittle whereas the asthenosphere is hot and dense.
New lithosphere is commonly formed at mid-ocean ridges, hot spots, and where there are active volcanoes.
both the lithosphere and the asthenosphere have hot matierial
A Hot spot is stationary in time and burns though the solid lithosphere creating an island through volcanic eruptions. The lithosphere is separated into plates that move around so if a hot spot occurs under an oceanic plate it forms a island and as the plate moves (and the hot spot does not) it forms a chain of islands (as the plate moves over the hot spot). This is how the Hawaiian chain is formed.
hot
The same about the lithosphere and the core is they both are hot :-(
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.
The lithosphere is cold and brittle whereas the asthenosphere is hot and dense.
New lithosphere is commonly formed at mid-ocean ridges, hot spots, and where there are active volcanoes.
hot spring
I think you mean Lithosphere. the lithosphere is the top solid crust portion of planet Earth. it consists of the Ocean floor and Continents. Below the lithosphere is the aesthenosphere. Which begins to get very hot.
Often, volcanoes.
it is under the lithosphere and is semi hot liquid
the hot magma moves around and they move.
both the lithosphere and the asthenosphere have hot matierial
The rock of the mantle is hot enough that it would melt at surface pressure. The weight of the lithosphere creates such great pressure on the mantle that it remains solid.