Want this question answered?
well that answer will be 6000 km - depths below surface of earth (km)
The deepest scientist have been able to study earths interior depth is 12,262 meters
The Gutenberg Discontinuity is the mantle/core boundary within Earth's interior where there is an abrupt change in the seismic waves (generated by earthquakes or explosions) that travel through Earth. It is at a depth of about 1,800 mi (2,900 km) below the surface.
They are all inside earth's mantle and interior.
the three ways in which we know about the interior of the earth are:volcanoesearthquake waves-under the earthdrilling
Increases with depth
Temperature
well that answer will be 6000 km - depths below surface of earth (km)
well that answer will be 6000 km - depths below surface of earth (km)
well that answer will be 6000 km - depths below surface of earth (km)
Geothermal gradient is the rate of increasing temperature with respect to an increasing depth in the Earth's interior. It is approximately 25 degrees Celsius per kilometer of depth.
The geothermal gradient is the rate at which the Earth's temperature increases with depth, indicating heat flowing from the Earth's warm interior to its cooler surface. Away from tectonic plate boundaries, it is 25-30°C per km of depth in most of the world.
5000*C and 1.5 million atmospheres
The earth's interior is called the core.
Lol, do his homework urself. anywayz its pressure and temperature
The stiffer mantle or lower mantle is one of the three layers of the earth's interior. It is a solid, rocky shell that extends to a depth of 2890 km.
The deepest scientist have been able to study earths interior depth is 12,262 meters