its between 9.9- 12.2 g/cm3
The average density of the Earth's outer core is estimated to be around 10-12 grams per cubic centimeter. This high density is mainly due to the presence of iron and nickel in the outer core, which are heavy elements.
9.9-12.2
9.9-12.2
The density of the outer core ranges from about 9 to 12 grams per cubic centimeter. This variation is due to differences in temperature and pressure within the outer core. The outer core is composed mainly of iron and nickel, which are both dense materials.
The layers of the Earth in order of density from least to greatest are: crust, mantle, outer core, and inner core. The inner core is the most dense layer as it is composed primarily of nickel and iron.
about 2,300 km
The layers of the Earth in order of increasing density are the crust, the mantle, the outer core, and the inner core. The inner core is the most dense layer due to the high pressure at its center.
The density of the outer core is calculated to be 10 g/cm3 and a volume of 1.719 *10 to the 20 cubic meters.
When a P-wave reaches the outer core, it undergoes refraction due to the change in density of the material. This causes the wave to slow down and bend as it travels through the outer core.
The outer core of the Earth, which consists of liquid iron and nickel, represents a dramatic decrease in material density compared to the solid inner core. This decrease in density is due to the transition from solid to liquid material, resulting in a noticeable reduction in density within the outer core.
The Earth's core has the greatest density. The inner core, composed mainly of solid iron and nickel, is even denser than the outer core, making it the densest part of the Earth.
about 2,300 km