posted on Mar, 14 2006 @ 09:07 PM
here is a quick link for someone's numbers;
www.madsci.org...
"The mantle extends from the base of the crust to a depth of about 2900 km (1800 mi). Except for the zone known as the asthenosphere, it is solid,
and its density, increasing with depth, ranges from 3.3 to 6 g/cm3. The upper mantle is composed of iron and magnesium silicates. The lower part may
consist of a mixture of oxides of magnesium, silicon, and iron.This layer is made up of mostly 11 elements : oxygen, silicon, aluminum, iron, calcium,
sodium, potassium, magnesium, titanium, hydrogen, and phosphorous. These 11 elements are all mixed up within different compounds in a crystal form, so
that we can call them minerals. For this layer we calculate a value of:
volume = 9.199 x10^20 cubic meters
density ranges from 3.3 g/cm3 (upper mantle) to
6.0 g/cm3 (lower mantle)
mass = 4.278 x10^24 kg = 68.4 % of earth's mass
= 49.5 % of earth's volume"
Magma replenishes itself through subduction, and others in the rock cycle