The depth of the crust varies between 10 and 70 km in different areas, depending where you would measure it.
On the Earth's surface, the depth is between 8-64 kilometers.
50km
The temperature range of the Earth's crust varies depending on location and depth, but generally ranges from about 0 to 1,000 degrees Celsius. The temperature increases with depth due to the geothermal gradient, which is the rate at which the Earth's temperature increases with depth below the surface.
The temperature of the Earth's crust varies depending on location and depth. On average, the temperature increases by about 25-30 degrees Fahrenheit per kilometer of depth. At the surface, the average temperature is around 50-70 degrees Fahrenheit, but it can reach much higher temperatures at greater depths.
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.
temperature increases with depth
On the Earth's surface, the depth is between 8-64 kilometers.
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.
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.
Check your thermometer. That's how hot it is on the outer crust where you are. There exists a geothermal gradient where temperature rises with depth from the surface. See the link below.
Skin of an apple
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.
none of your business
The temperature range of the Earth's crust varies depending on location and depth, but generally ranges from about 0 to 1,000 degrees Celsius. The temperature increases with depth due to the geothermal gradient, which is the rate at which the Earth's temperature increases with depth below the surface.