They would differ in temperature, mineralogy, density, and pressure.
Temperature Density and Pressure
Working outwards from the centre: The Earth is believed to be formed of an inner core, outer core, inner mantle, outer mantle, and the crust. The mantle is two thousand miles thick and makes up more than three-quarters of the Earth's volume.
The stiffer mantle or lower mantle is one of the three layers of the earth's interior. It is a solid, rocky shell that extends to a depth of 2890 km.
The three principle divisions of the solid Earth based on compositional differences are the core, the mantle, and the crust.
The density of Earth's mantle varies depending on its depth. The part right below the crust has a density of about 3.4 grams per cubic centimeter while the lowest part of the mantle is 5.6 grams per cubic centimeter.
Temperature Density and Pressure
Working outwards from the centre: The Earth is believed to be formed of an inner core, outer core, inner mantle, outer mantle, and the crust. The mantle is two thousand miles thick and makes up more than three-quarters of the Earth's volume.
Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
The stiffer mantle or lower mantle is one of the three layers of the earth's interior. It is a solid, rocky shell that extends to a depth of 2890 km.
The three principle divisions of the solid Earth based on compositional differences are the core, the mantle, and the crust.
The 3 main layers of earth (crust, mantle, core) are divided into crust, upper mantle, lower mantle, outer core, and inner core.
1.CORE The very heart of the moon. 2.LOWER MANTLE The asthenosphere, from where the majority of moonquakes emanate. 3. UPPER MANTLE The lithosphere which is the most rigid part of the mantle
Three main differences between plastic things and iron include:each are composed of different materialsiron is only flexible when under high temperaturesplastic melts at much lower temperature than iron melts
Technically, the most interior is the inner core, then the outer core, then the lower mantle
1.CORE The very heart of the moon. 2.LOWER MANTLE The asthenosphere, from where the majority of moonquakes emanate. 3. UPPER MANTLE The lithosphere which is the most rigid part of the mantle. 4.CRUST The anorthosite crust is the external envelope of the moon. 5.BASALTS OF THE MARIA Local covering of the moon. The three layers of the Moon: Crust, Mantle, and the Core.
The three parts that make up the Earths mantle are the crust, core, and mantle.
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