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.
2900 km
The thickness of the Earth's mantle is about 2900 km and it's upper boundary is about 100km deep. There is a really cool cutaway drawing available by using the Wikipedia link.
The Earth's mantle extends from about 35 kilometers (22 miles) below the Earth's surface to approximately 2,900 kilometers (1,800 miles) deep, reaching the outer core. It makes up about 84% of the Earth's total volume and is primarily composed of silicate minerals rich in iron and magnesium. The mantle is divided into the upper and lower mantle, with the upper mantle being more rigid and the lower mantle being more fluid in nature.
From seismic interpretations of earthquake date. From computer modeling. From the study of meteorites, From geochemistry and form the study of mantle xenoliths.
The Earth is thus a relatively dry planet, and the oceans truly are only skin deep. It is possible that Earth's solid mantle contains a mass of dissolved water.
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.
The Wadati-Benioff zone can extend up to several hundred kilometers deep into the Earth's mantle, reaching depths of 700 kilometers or more. This zone is associated with the subduction of tectonic plates beneath another plate.
Diamonds are formed deep within the earth's mantle, under enormous pressure and extreme, high heat. Then, volcanic pipes erupt the diamonds to the earth's surface.
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.
The three main spheres in the Earth's mantle are the upper mantle, the transition zone, and the lower mantle. The upper mantle extends from the Moho (the boundary between the crust and the mantle) to about 410 kilometers deep, while the transition zone lies between 410 and 660 kilometers. The lower mantle extends from 660 kilometers to the outer core, reaching depths of around 2,900 kilometers. Each of these layers has distinct physical and chemical properties that influence geological processes.
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.
Lava is molten rock. The rock deep inside the earths mantle is always molten, and when it occasionally breaks through to the surface, the opening is called a volcano, and the liquid rock spilling out of the top is lava.