The upper mantle is divided into two main sections: the lithosphere and the asthenosphere. The lithosphere is rigid and includes the crust, while the asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur.
Large sections of Earth's crust and upper mantle are called tectonic plates. These plates are responsible for the movement and interactions that shape the Earth's surface, including the formation of mountains, earthquakes, and volcanoes.
The Earth's mantle is typically divided into two main sections: the upper mantle and the lower mantle. The upper mantle lies beneath the Earth's crust and extends down to a depth of about 410 kilometers, while the lower mantle extends from about 410 to 2,890 kilometers below the Earth's surface.
The mantle is divided into the upper mantle, transition zone, and lower mantle. The upper mantle is beneath the lithosphere, the transition zone lies between the upper and lower mantle, and the lower mantle extends to the outer core.
The lower part of the mantle is called the "lower mantle" or "mesosphere", while the upper part of the mantle is referred to as the "upper mantle" or "asthenosphere".
The lithosphere is the crust Moho and upper mantle. It floats on a plasticity zone called the asthenosphere.
Large sections of Earth's crust and upper mantle are called tectonic plates. These plates are responsible for the movement and interactions that shape the Earth's surface, including the formation of mountains, earthquakes, and volcanoes.
The Earth's mantle is typically divided into two main sections: the upper mantle and the lower mantle. The upper mantle lies beneath the Earth's crust and extends down to a depth of about 410 kilometers, while the lower mantle extends from about 410 to 2,890 kilometers below the Earth's surface.
lithosphere
The lithosphere is made up of the "upper mantle" and earth's crust.The lithosphere is broken into separate sections called plate tectonics or tectonic plates.
The mantle is divided into the upper mantle, transition zone, and lower mantle. The upper mantle is beneath the lithosphere, the transition zone lies between the upper and lower mantle, and the lower mantle extends to the outer core.
The Theory of Plate-techtonics
Earth's crust and upper mantle are broken into sections called tectonic plates. These plates float on the semi-fluid asthenosphere below them and interact with each other at plate boundaries, leading to geological processes like earthquakes and volcanic activity.
That would be the lithosphere. This is broken into sections known as lithospheric (or tectonic) plates.
Earths lithosphere is made up of upper mantle. The earths lithosphere is broken into separate sections and it is called as tectonic plates or plate tectonics.
They are called plates!
The upper mantle is made of something called peridodite.
The upper mantle is made of something called peridodite.