The density of the Earth's asthenosphere is 4 gm/cm^3.
the density of the asthenosphere is 4gm/cm^3
The density of the Earth's asthenosphere is 4 gm/cm^3.
The viscosity of the mantle is estimated to be about 10^21 poise (10^19 Pascal seconds).
The rock in a rising convection current is hotter and more buoyant than the surrounding rock, causing it to rise.
It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
It is called the asthenosphere.
The density of the Earth's asthenosphere is 4 gm/cm^3.
Density and tempurature.
thermal energy !
The viscosity of the mantle is estimated to be about 10^21 poise (10^19 Pascal seconds).
density
Isostasy is the balance and buoyancy of the Earth's crust floating on the asthenosphere, the top layer of the mantle. The asthenosphere, like Silly Putty, adjusts to the different densities and thicknesses of the crust. For instance, glaciers add weight (density, really) to the surface of the Earth. The added density depresses the flexible crust down into the asthenosphere, which, in turn, responds by slowly flowing away from the added burden. As the glaciers melt, the crust under them rebounds (rises), and the asthenosphere flows back, returning to its normal level.
Because of something called Isostacy-the gravitational equilibrium between lithosphere and asthenosphere, such that plates "float" at an elevation that dependes on the thickness and density. EX. Think floating ice cubes
It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
Asthenosphere
The rock in a rising convection current is hotter and more buoyant than the surrounding rock, causing it to rise.
It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
It is called the asthenosphere.