The upper mantle extends from the base of the Earth's crust down to a depth of about 410 kilometers (approximately 255 miles). It lies above the transition zone, which separates the upper mantle from the lower mantle. The upper mantle is primarily composed of silicate minerals and is involved in tectonic processes, including plate tectonics and mantle convection.
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The mantle is composed of two main sublayers: the upper mantle and the lower mantle. The upper mantle lies beneath the Earth's crust and extends to a depth of about 670 km. Below the upper mantle lies the lower mantle, which extends from approximately 670 km to 2,900 km below the Earth's surface.
somewhere between 1000 to 4000 degrees Celsius.
The temperature of the upper mantle ranges from around 500 to 900 degrees Celsius. However, this can vary depending on the depth and location within the mantle.
The depth below the Earth's surface of the lithosphere varies depending on location, but on average it extends to about 100 kilometers (62 miles) deep. This layer includes the crust and upper part of the mantle and is characterized by its rigidity and brittle behavior.
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The mantle is divided into the upper mantle and the lower mantle. The upper mantle lies directly beneath the Earth's crust and extends to a depth of about 410 miles. The lower mantle extends from the bottom of the upper mantle to a depth of about 1,800 miles.
The two main parts of the Earth's mantle are the upper mantle and the lower mantle. The upper mantle sits below the Earth's crust and extends to a depth of about 410 miles, while the lower mantle extends from about 410 miles to 1,800 miles depth.
The mantle is typically divided into two parts: the upper mantle and the lower mantle. The upper mantle sits beneath the Earth's crust and extends to a depth of about 410 kilometers, while the lower mantle extends from 410 to 2,890 kilometers below the Earth's surface.
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 composed of two main sublayers: the upper mantle and the lower mantle. The upper mantle lies beneath the Earth's crust and extends to a depth of about 670 km. Below the upper mantle lies the lower mantle, which extends from approximately 670 km to 2,900 km below the Earth's surface.
410km
The main difference between the upper and lower mantle is their depth within the Earth. The upper mantle is located closer to the Earth's surface, extending from the crust to a depth of about 410-660 km, while the lower mantle lies beneath the upper mantle, extending from around 660-2,891 km deep. Additionally, the upper mantle is more rigid and composed of mainly solid rock, while the lower mantle experiences higher pressures and temperatures, leading to more plastic behavior.
The average temperature is 5400 ºF (3000ºC),
The upper mantle is a solid layer of rock located beneath the Earth's crust. It is part of the Earth's mantle and extends from the base of the crust to a depth of about 660 kilometers. The upper mantle is mostly composed of peridotite, a dense rock made up of minerals like olivine and pyroxene.
The upper part of the mantle is also called the asthenosphere. This layer is partially molten and lies just beneath the lithosphere.