4152 kg/m3
The earths mantle has a density of about 3.3 g/cubic cm.
To tell you the truth I only know that the mantle is less dense than the inner core.
It is not as low dense as the crust or the outer core but it is basiclly the second most dense out of them.
Do you get it kind of what I'm saying?
Upper mantle, depth 35-60 Km, density 3.4-4.4g/cm3.
Mantle, depth 35-2890 Km, density 3.4-5.6g/cm3.
The mantle is less dense than the earth's core, but more dense than the eath's crust.
4152 kg/m3
The earths mantle has a density of about 3.3 g/cubic cm.
the density of the lower mantle is approximately 2587 km.
its 3.5 but yes it is about 3.3
3.5
the density is greater at the middle of the mantle
False. Density increases with increasing depth.
3.3 g/cm3
The mantle is less dense than the core but more dense than the crust.
Mineralogy, pressure, temperature, and density differences exist among the 'layers' of the mantle.
the density is greater at the middle of the mantle
the density of the lower mantle is 3.4-4.3g/cm
by density change
why do scientists believe explains the increased density of material deeper into the mantle
False. Density increases with increasing depth.
How do changes in heat energy affect the density of earths mantle material
The moon's average density is about the same as the density of mantle of the Earth.
3.3 g/cm3
The crust
Earth.
The mantle is less dense than the core but more dense than the crust.
The increased amount of iron deeper into the mantle explains it.