The temperature at 3000 km below the surface of the Earth is estimated to be around 6000°C to 7000°C. This temperature is mainly due to the extreme heat generated by the Earth's core.
The ground temperature at 5 feet below the surface is typically more stable and closer to the average annual air temperature of the region.
The ground temperature at 10 feet below the surface is typically around 50-60 degrees Fahrenheit.
The ground temperature at 20 feet below the surface is typically around 50-60 degrees Fahrenheit.
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.
If water vapor condenses on a surface below 0 degrees Celsius, it will freeze and form ice. This occurs because the temperature of the surface is below the freezing point of water, causing the water vapor to change into a solid state.
The ground temperature at 5 feet below the surface is typically more stable and closer to the average annual air temperature of the region.
The ground temperature at 10 feet below the surface is typically around 50-60 degrees Fahrenheit.
The ground temperature at 20 feet below the surface is typically around 50-60 degrees Fahrenheit.
The temperature of the ocean is 39 degrees below the surface.
temperature increases with depth
When a liquid changes to a gas below its surface as well as at the surface, the liquid is at a temperature equal to or greater than its boiling point.
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.
If water vapor condenses on a surface below 0 degrees Celsius, it will freeze and form ice. This occurs because the temperature of the surface is below the freezing point of water, causing the water vapor to change into a solid state.
it increases
Both temperature and pressure increase with depth.
At depths of 50 to 200 km below Earth's surface rocks will melt.
The average ground temperature varies at different depths below the surface. Generally, the temperature increases the deeper you go. This is due to the Earth's internal heat. At a depth of about 10 feet, the ground temperature remains relatively stable, around 50-60 degrees Fahrenheit.