This is known as the Asthenospehere.
The crust is the outermost layer of the Earth's surface, while the lithosphere includes the crust as well as the uppermost part of the mantle. In this context, the crust is part of the lithosphere. The lithosphere is composed of the crust and the rigid upper portion of the mantle and is divided into several tectonic plates.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
The name given to a portion of the Earth's surface is known as a region or area. Regions can be defined by physical characteristics, such as climate or landforms, or by human characteristics, such as culture or economic activities.
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
Magma is the name given to molten underground rock. It can be found beneath the Earth's surface in the mantle and can eventually rise to the surface through volcanic activity.
The crust is the outermost layer of the Earth's surface, while the lithosphere includes the crust as well as the uppermost part of the mantle. In this context, the crust is part of the lithosphere. The lithosphere is composed of the crust and the rigid upper portion of the mantle and is divided into several tectonic plates.
FalseThe Mantle is the Earth's 2nd layer. It goes in the order of the Crust, the Mantle, the Outer Core and then the Inner Core.If you follow this answer, you will get it wrong on Are You Smarter Than A Fifth Grader. The Answer given is Mantle.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
The boundary between the crust and the mantle is called the Mohorovicic discontinuity. It is also called simply the Moho and it is the abrupt divide between faster and slower speeds where the mantle starts.
Since the Earth is a Spheroid shape, (not a true sphere) 50% of its surface is illuminated by the Sun, at any given moment.
The earth's crust lower mantle is made up of silicate perovskites and ferropericlase. While the silicate perovskites are the names given to calcium silicates and magnesium iron, ferropericlase is an oxide of magnesium/iron. The lower mantle is at a depth that ranges from 650 kilometers to 2,890 kilometers.
The name given to a portion of the Earth's surface is known as a region or area. Regions can be defined by physical characteristics, such as climate or landforms, or by human characteristics, such as culture or economic activities.
The crust and the upper part of the mantle are the solid part of the Earth called the lithosphere.
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
The area of Earth that forms the land is called the lithosphere. It includes the outermost layer of the Earth, which consists of the crust and the upper part of the mantle.
No, the mantle of the earth is not liquid. It is fairly solid, but the lower parts nearer the core are extremely hot and are plastic. The mantle is under tremendous pressure, and this pressure prevents rock from melting, even at the elevated temperatures there. Use the link below for more information.
The idea that the earth's crust is broken into plates that move on top of the mantle is known as the theory of plate tectonics.Magma is the name given to molten rock below the Earth's surface.