To determine the best inferred density of Earth from the upper mantle to the lower mantle, one would typically look for a graph that displays density values increasing with depth. This trend is due to the increasing pressure and temperature conditions as you move deeper into the Earth. A graph that shows a smooth, continuous increase in density, consistent with geophysical models, would be most indicative of the mantle's density profile. Look for key markers indicating the transition zones between the upper and lower mantle, where density changes more significantly.
The graph that best shows the inferred density of Earth from the upper mantle to the lower mantle typically demonstrates a gradual increase in density with depth. This trend reflects the increasing pressure and temperature conditions as you move deeper into the Earth, leading to denser materials forming in the lower mantle. A line graph or a bar graph that illustrates this increase clearly, with depth on the x-axis and density on the y-axis, would effectively represent this relationship.
The moon's average density is about the same as the density of mantle of the Earth.
thez nuts
The temperature in Earth's plastic mantle, which is part of the upper mantle, is typically inferred to range from about 500 to 900 degrees Celsius (932 to 1,652 degrees Fahrenheit) near the lithosphere-asthenosphere boundary. As you go deeper into the mantle, temperatures can increase significantly, reaching up to 3,000 degrees Celsius (5,432 degrees Fahrenheit) near the core-mantle boundary. These temperatures are crucial for the ductility of the mantle material, allowing for the slow convection processes that drive plate tectonics.
To determine the best inferred density of Earth from the upper mantle to the lower mantle, one would typically look for a graph that displays density values increasing with depth. This trend is due to the increasing pressure and temperature conditions as you move deeper into the Earth. A graph that shows a smooth, continuous increase in density, consistent with geophysical models, would be most indicative of the mantle's density profile. Look for key markers indicating the transition zones between the upper and lower mantle, where density changes more significantly.
The graph that best shows the inferred density of Earth from the upper mantle to the lower mantle typically demonstrates a gradual increase in density with depth. This trend reflects the increasing pressure and temperature conditions as you move deeper into the Earth, leading to denser materials forming in the lower mantle. A line graph or a bar graph that illustrates this increase clearly, with depth on the x-axis and density on the y-axis, would effectively represent this relationship.
The moon's average density is about the same as the density of mantle of the Earth.
The Earth's mantle is below the crust. The layers of the Earth form concentric spheres. Below the mantle is the core.
2000 celcius
thez nuts
Mantle Is The Below Layer Of The Crust In Earth.
mantle
The density of Earth's mantle is lower than the density of Earth's core. The mantle is composed of solid rock while the core is made of mostly iron and nickel, which are denser materials. This difference in density contributes to the layering of the Earth's structure.
The Earth's mantle
The mean density of the Moon is around 3.34 g/cm³, which is similar to the densities of mantle rocks found on Earth. The Moon's composition is primarily made up of silicate rocks similar to those found in the Earth's mantle, which contributes to its comparable density.
the mantle