n some areas the mantle can be from 200 to 500 meters
No, mines are not deep enough to reach the Earth's mantle. The Earth's mantle is located about 25 miles beneath the Earth's surface, while most mines only reach depths of a few miles.
Plumes of molten rock originating deep within the mantle are known as mantle plumes. These plumes are believed to be responsible for hotspots and volcanic activity at the Earth's surface.
Of course.
The deep mantle is actually composed of denser materials compared to the outer mantle. These denser materials are mainly made up of silicate minerals rich in iron and magnesium, which contribute to the overall density of the deep mantle. This density variation plays a key role in the movement of material within the Earth's mantle through processes like convection.
Topographic highs in the crust have deep roots that extend into the mantle and provide buoyant support through isostasy. These roots are a result of the difference in density between the crust and underlying mantle, allowing for uplifted regions to be supported by the denser mantle material beneath.
No, mines are not deep enough to reach the Earth's mantle. The Earth's mantle is located about 25 miles beneath the Earth's surface, while most mines only reach depths of a few miles.
No, solid rock located deep in the mantle is not called magma. Magma is molten rock that is found beneath the Earth's surface in the mantle and crust. Solid rock in the mantle is known as the lithosphere.
Plumes of molten rock originating deep within the mantle are known as mantle plumes. These plumes are believed to be responsible for hotspots and volcanic activity at the Earth's surface.
Of course.
2900 km
Conduction. Heat istransferred from the mantle to the crust, melting it to become part of the mantle.
It is not possible to dig deep enough to reach the Earth's mantle because the mantle is located about 1,800 miles below the Earth's surface, much deeper than any human-made hole.
The deep mantle is actually composed of denser materials compared to the outer mantle. These denser materials are mainly made up of silicate minerals rich in iron and magnesium, which contribute to the overall density of the deep mantle. This density variation plays a key role in the movement of material within the Earth's mantle through processes like convection.
rocks
The heat from deep in the earth's mantle.
Topographic highs in the crust have deep roots that extend into the mantle and provide buoyant support through isostasy. These roots are a result of the difference in density between the crust and underlying mantle, allowing for uplifted regions to be supported by the denser mantle material beneath.
In oceanic areas the upper mantle is usually 5-200km thick and on continental areas it is 75-300km deep.