2500
2000
90 degrees
700km
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The temperature range of the asthenosphere is between 1500C-1600C.
The asthenosphere is part of the upper mantle. It's upper boundary is approximately 100 km deep and it's base is around 700 km deep.
The sun!
The lithosphere is cold and brittle whereas the asthenosphere is hot and dense.
the Mesosphere
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
Shi, I dk
The temperature range of the asthenosphere is between 1500C-1600C.
The asthenosphere is part of the upper mantle. It's upper boundary is approximately 100 km deep and it's base is around 700 km deep.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
90 degrees
The approximate height of the stratopause is between 50 to 55 km. The temperature is about negative15 degrees Celsius or 5 degrees Fahrenheit.
The sun!
This region is known as the mesosphere. The base of the mesosphere includes the D'' (D double prime) layer which is sometimes considered to be a transition zone between the mantle and the core-mantle boundary zone.
The correlation between cricket chirps and the temperature is very approximate.
The lithosphere is cold and brittle whereas the asthenosphere is hot and dense.
asthenosphere