The crust thins and thickens over the surface of the earth. At a mid-ocean ridge spreading center, the mantle is essentially at the surface. Under neath the Himalayan mountains it is well over 40km.
The Earth's mantle extends from the base of the crust down to a depth of about 2,900 kilometers (1,800 miles) at the boundary with the outer core. This region is divided into the upper mantle and lower mantle based on differences in composition and behavior.
The upper mantle of Earth begins just beneath the crust, which ranges in thickness from about 5-70 km (3-44 miles) depending on the location. The upper mantle extends to a depth of about 670 km (416 miles) beneath the Earth's surface, marking the boundary with the lower mantle.
The mantle, by far, is the thickest layer of the Earth.
The core is the hottest part of the Earth, with temperatures reaching up to 5,700°C (10,000°F). The mantle is cooler than the core but hotter than the crust, with temperatures that range from about 500°C (932°F) to 900°C (1,652°F). The Earth's crust has the lowest temperatures of the three layers.
This is called a destructive plate boundary. It occurs due to the fact that the oceanic crust is far denser than the continental crust. As a result it subducts into the mantle and is incenerated. Hope it helped:)
You're standing on it. The lithosphere is the crust and upper mantle of the earth.
Not even close. It goes down less than two kilometers into the continental crust, over thirty kilometers away from the upper reaches of the mantle. The bottom of the ocean is far closer to the mantle.
The Earth's mantle extends from the base of the crust down to a depth of about 2,900 kilometers (1,800 miles) at the boundary with the outer core. This region is divided into the upper mantle and lower mantle based on differences in composition and behavior.
The mantle is located directly beneath the Earth's crust and is approximately 1,800 miles (2,900 kilometers) thick. The boundary between the crust and the mantle is known as the Mohorovičić discontinuity or Moho.
The upper mantle of Earth begins just beneath the crust, which ranges in thickness from about 5-70 km (3-44 miles) depending on the location. The upper mantle extends to a depth of about 670 km (416 miles) beneath the Earth's surface, marking the boundary with the lower mantle.
The lithosphere is part of the Earth's crust and uppermost mantle; it includes the crust itself. So, the distance to the lithosphere is essentially the same as the thickness of the crust, which varies from about 5 to 75 kilometers (3 to 46 miles) beneath the oceans and continents.
The Earth's mantle is composed of solid rock that is denser than the crust above it. As a result, the mantle does not float on the Earth's surface, but rather acts as a semi-rigid layer that lies beneath the crust and above the core.
In my 7th grade science class, so far I know that the first layer is the Crust, the second is the Lithosphere, the third is the Asthenosphere, the fourth is The Upper Mentle Region, the fifth is The Lower Mantle Region, this next layer is not considered a layer but it is called the Metal Oxide Belt\Region, the sixth is the Outer Core, and the seventh is the Inner Core.
The mantle, by far, is the thickest layer of the Earth.
The upper mantel is the part of the mantel nearest to the Earth's surface. It is a little cooler than the lower mantel therefore more viscous, or pasty, than the lower mantel. Temperatures range between 932 °F-1,652 °F. at the upper boundary with the crust to over 7,200 °F at the boundary with the core. Although the higher temperatures far exceed the melting points of the mantle rocks at the surface (about 1200 °C for representative periditute), the mantle is almost exclusively solid. The enormous lithostatic pressure exerted on the mantle prevents "melting," because the temperature at which melting begins (the solidus) increases with pressure.
It is 500 to 900 Celsius at the upper boundary and 4000 Celsius at the boundary near the outer core. A2. The values range between 500 deg C at the crust boundary, to over 4 000 deg C at the outer Core boundary.A1. between 100 to 1600 Celsius. The Mantle temperature varies to about 1600-4000 degrees.The average temperature of the mantle is is 5400 ºF (3000ºC).
The mantle is the largest zone of interior of the Earth by volume. It makes up about 84% of Earth's volume and extends from the base of the crust to the outer core.