The asthenosphere is the highly viscous, mechanically weak and ductilely
deforming region of ... The thickness of the asthenosphere depends mainly on
the temperature. In some regions the asthenosphe...
Asthenosphere). The temperature of the lithosphere and asthenosphere is 300 to
500 degrees celsius. The mantles temperature 4500 degrees celsius and ...
The temperature of the asthenosphere begins at a little over 1600 degrees
Fahrenheit but does not rise above 6700 degrees F. It lies beneath the
lithosphere or ...
Dec 23, 2011 ... The asthenosphere is composed of matter in the molten or semi-molten state. Its
temperature is normally between 1,400 degree Celsius to ...
Mechanical properties - 'lithosphere' and 'asthenosphere' ... The rocks remain
solid at depth despite their temperature because of the extreme pressures acting
May 21, 2008 ... The asthenosphere is solid even though it is at very hot temperatures of about
1600 C due to the high pressures from above. However, at this ...
Another indicator of heat flow is the increase in temperature with depth inside
deep ... This zone, where rock is soft enough to flow, is called the asthenosphere.
Surrounding the inner core is a zone where temperature and pressure are so ...
in the mesosphere, rocks in the asthenosphere are weak and easily deformed, ...
The inner core may have a temperature up to about 13,000°F (7,200°C ... The
asthenosphere is a part of the upper mantle that exhibits plastic properties.
The difference between asthenosphere and lithosphere is how the materials in ...
manner (bending or breaking) or a plastic manner (flowing) is temperature.