Explanation: The oceanic crust of earth is different from the continental part of the earth’s crust. It is much thinner which is about 5 km to 80 km in thickness. It is described as having much similarities with the mantle of the earth which is also very varying in thickness.

Which objects can an S wave travel through? Secondary waves, which are called S waves, usually travel through solids such as the crust, granite and soil. You just studied 16 terms!

Terms in this set (5) – S waves travel through solids, liquids, and gasses.

Which statement describes how the mantle is similar to Earth’s oceanic crust? It is composed mostly of basalt. It consists primarily of molten rock. It has varying degrees of thickness.

mantle

Answer. Earth’s Core 1,000 Degrees Hotter Than Expected. The difference in temperature matters, because this explains how the Earth generates its magnetic field. The Earth has a solidinner core surrounded by a liquid outer core, which, in turn, has the solid, but flowing, mantle above it.

The correct answer is the crust. The crust is present above the mantle and is the hard outer shell of the Earth.

The answer is soil.

Answer : The best pressure is 110 GPa of the lower mantle.

Of the mentioned layers, the lithosphere is the outermost layer of the Earth, that is, of 100 kilometers in thickness, and it exhibits the pressure in the range of 75 GPa to 110 GPa, that is, up to 109 GPa.

The difference between the lower mantle and the oceanic crust is first their respective locations, pressure and temperature– the pressure and temperature increases with depth in the earth this the mantle is more hot and under great pressure than the crust.

110 GPa

Answer. Geologists have used two main types of evidence to learn about Earth’s interior: direct evidence from rock samples and indirect evidence from seismic waves. The geologists are observing rock on Earth’s surface.

crust

How is Item A different from Item B? The crust in Item A is found partially below sea level as compared to the crust in Item B. The continental crust is the coolest region.

How is Item A different from Item B? The crust in Item A is found partially below sea level as compared to the crust in Item B.

outer core

Hot material near the core is less dense and rises, when it cools, it becomes more dense and sinks. Explanation: This best explains how heat plays a role in the movement of materials within Earth’s interior because it’s how convection works.

Which best explains how heat plays a role in the movement of materials within Earth’s interior? Hot material near the core is less dense and rises, and when it cools, it becomes more dense and sinks.

The three main layers of Earth are : the crust, the mantle, and the core. These layers vary greatly in size, composition, temperature and pressure.

Explanation: Geologist obtain direct information about the interior of the earth by carrying out core rock sampling. The rocks contained in the core used gives a better view as to the nature of the rock found at a particular depth in the earth.

Because you can’t go inside earth because it is too hot. You have to use your evidence from rock samples and seismic waves. Geologists have used two main types of evidence to learn about Earth’s interior: direct evidence from rock samples and indirect evidence from seismic waves.

The crust is thickest under high mountains and thinnest beneath the ocean.

When you slice an apple, you find different layers. A small core is in the center. A thick layer is in the middle. A thin skin is all around the outside.

Temperature of the lithosphere can range from a crustal temperature of zero degrees Celsius (32 degrees Fahrenheit) to an upper mantle temperature of 500 degrees Celsius (932 degrees Fahrenheit).