The Moho, or Mohorovičić discontinuity, is typically found at a depth of about 5-70 kilometers (3-43 miles) below the Earth's surface. It marks the boundary between the Earth's crust and the underlying mantle.
well that answer will be 6000 km - depths below surface of earth (km)
The average rate of temperature increase below the Earth's surface is about 25 to 30 degrees Celsius per kilometer of depth. This increase is known as the geothermal gradient and varies depending on factors such as location, tectonic activity, and local geology.
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.
Rock can melt from 600- 1200C, depending on the type of rock, but this is assuming 1atm pressure. Under the earth, there are higher pressures, increasing the melting point. So although the rock should have melted by the mantle, which is 500-4000C and at a depth 35-2900km below the surface, it is a silly putty-like plastic solid rather than a liquid. The earth only becomes liquid at a depth of 2900km in the earth's outer core, but that is made of metal, not rock, so essentially, none of it.
At a depth of 5,000 kilometers below the Earth's surface, the pressure is estimated to be around 1.5 million atmospheres (or 150 gigapascals). This immense pressure arises from the weight of the overlying rock and the increasing density of materials as depth increases. However, it's important to note that the Earth's mantle and core are primarily composed of solid and liquid materials that behave differently under such extreme conditions.
On the Earth's surface, the depth is between 8-64 kilometers.
Both temperature and pressure increase with depth.
It's about 3,500 km below the Earth's surface. (For all Earth Science people)
The density of Earth materials generally increases with depth below the surface due to the increasing pressure from the overlying layers. As depth increases, the materials experience more compression, leading to higher densities. The variation in density with depth is important for understanding the structure and composition of the Earth's interior.
between 410 and 660 kilometers below the earth's surface.
As the depth increases, the density increases also.
its hot and the deeper you go the hotter it gets
well that answer will be 6000 km - depths below surface of earth (km)
Rock can start to melt at a depth of around 50-100 kilometers below Earth's surface due to high temperatures and pressure. This process can lead to the formation of magma, which can then rise to the surface and result in volcanic activity.
It increases up to a certain point.
well that answer will be 6000 km - depths below surface of earth (km)
At a depth of 3500 km below the surface, Earth's inferred pressure is estimated to be around 1.3 million times higher than atmospheric pressure at the surface. This extreme pressure is due to the weight of the overlying rock and the compression of material at such depths within the Earth.