100km
50km
The inferred pressure at a depth of 3500 km below the Earth's surface is estimated to be around 1.3 million times atmospheric pressure at sea level. At such depths, the immense weight of the overlying rock layers causes this high pressure.
The temperature at 3.4 km below the Earth's surface generally increases with depth due to geothermal heating. On average, the geothermal gradient is about 25-30 degrees Celsius per kilometer, so at 3.4 km below the surface, the temperature could be around 85-102 degrees Celsius.
Well I'm not to sure about that, but 70% of the earth is water!And only 3% of all the water is fresh
For the most part, yes. (There are exceptions, of course.)
temperature increases with depth
50km
it increases
As the depth increases, the density increases also.
At depths of 50 to 200 km below Earth's surface rocks will melt.
none of your business
Geothermal gradient refers to the increase in temperature with depth below the Earth's surface. On average, the geothermal gradient is about 25-30°C per kilometer. This gradient varies depending on factors like location and geologic conditions.
The inferred pressure at a depth of 3500 km below the Earth's surface is estimated to be around 1.3 million times atmospheric pressure at sea level. At such depths, the immense weight of the overlying rock layers causes this high pressure.
Yes it is.
The temperature at 3.4 km below the Earth's surface generally increases with depth due to geothermal heating. On average, the geothermal gradient is about 25-30 degrees Celsius per kilometer, so at 3.4 km below the surface, the temperature could be around 85-102 degrees Celsius.
At a depth of 500 m below the surface, the pressure would be approximately 5 atmospheres (1 atm for every 10 m of depth).
Well I'm not to sure about that, but 70% of the earth is water!And only 3% of all the water is fresh