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The difference between the lithosphere and the asthenosphere is that the asthenosphere is the lower part of the upper mantle it behaves like a plastic but flows much more easily than the rest of the mantle. The lithosphere however, includes the entire crust and the uppermost part of the mantle, it is more rigid and brittle and doesn't flow.
Yes, it is more viscous.
While still solid, the asthenosphere is able to flow. The ability of a solid to flow is called plasticity. See "What's the matter?" for an activity to demonstrate plasticity. Since the asthenosphere is more liquid than the rest of the mantle, the broken lithosphere plates are able to "float" on it.
The lithosphere is the upper portion of the mantle. Its temperature is around 300 to 500 degrees Celsius. The lower portion of the mantle, which is the asthenosphere, has a temperature of around 4500 degrees Celsius.
Pluto has a weaker gravity than Earth. In fact, Pluto has a weaker gravity than Earth's moon.
The asthenosphere is part of the mantle, so the question is misguided. It is less dense than the lower mantle.
The difference between the lithosphere and the asthenosphere is that the asthenosphere is the lower part of the upper mantle it behaves like a plastic but flows much more easily than the rest of the mantle. The lithosphere however, includes the entire crust and the uppermost part of the mantle, it is more rigid and brittle and doesn't flow.
The asthenosphere.
Yes, it is more viscous.
While still solid, the asthenosphere is able to flow. The ability of a solid to flow is called plasticity. See "What's the matter?" for an activity to demonstrate plasticity. Since the asthenosphere is more liquid than the rest of the mantle, the broken lithosphere plates are able to "float" on it.
The tectonic plates (the lithosphere) are made of the crust and upper brittle part of the mantle. They 'float' on the hotter and softer mantle below, which is still a solid, but can flow like plasticine (the asthenosphere)
The lithosphere is on the top of the mantle. :=]
The lower mantle is older and cooler than the upper mantle. Thank you for reading this I'm comment if you like one direction(: hehe
The lithosphere is the upper portion of the mantle. Its temperature is around 300 to 500 degrees Celsius. The lower portion of the mantle, which is the asthenosphere, has a temperature of around 4500 degrees Celsius.
Subducting oceanic crust is more dense and colder than the surrounding hot pliable rock of the asthenosphere.
The asthenosphere is more dense than the lithosphere.
The mantle is more dense than the asthenosphere, lithosphere, and the crust. The inner core and the outer core are more dense, however. The mantle is also a solid. I am learning this in my science class right now! :)