Away from tectonic plate boundaries, it is 25-30°C per km of depth in most of the world
therefore it is somewhere between 75 and 90°C at that depth
thanks to Wikipedia for that one.
At a depth of about 1000 kilometers, the temperature of the Earth's interior can reach approximately 1300 to 1500 degrees Celsius (about 2372 to 2732 degrees Fahrenheit). This temperature is primarily due to the immense pressure and the heat generated from the decay of radioactive isotopes within the Earth's mantle and core. The exact temperature can vary based on specific geological conditions and the composition of the surrounding materials.
7389 ------ 1000 or 7389/1000 or 7 & 389/1000
1 meter is 1000 milimeters to change from mm to m, you divide mm by 1000 to change from m to mm, you times m by 1000, as you get 1000mm for every 1m
37.069 = 37 + 0.069 = 37 +69/1000 37000/1000 + 69/1000 = 37069/1000
86.007 = 86 and 7/1000 = 86007/1000
The average temperature gradient in the Earth's crust is approximately 25-30 degrees Celsius per kilometer of depth. Therefore, the total temperature change between 1000 m and 4000 m in depth would be around 75-120 degrees Celsius.
The temperature typically decreases by about 3.5F per 1000 feet increase in elevation.
The rate of temperature change per 1000 feet in the atmosphere is called the lapse rate. On average, the lapse rate is about 3.5F per 1000 feet of elevation.
well that answer will be 6000 km - depths below surface of earth (km)
The temperature at a depth of 1000 km inside the Earth can reach around 1000 to 2000 degrees Celsius. This heat is primarily generated by the radioactive decay of elements in the Earth's mantle and core.
At a depth of about 1000 kilometers, the temperature of the Earth's interior can reach approximately 1300 to 1500 degrees Celsius (about 2372 to 2732 degrees Fahrenheit). This temperature is primarily due to the immense pressure and the heat generated from the decay of radioactive isotopes within the Earth's mantle and core. The exact temperature can vary based on specific geological conditions and the composition of the surrounding materials.
As altitude increases by 1000 feet, the temperature typically decreases by about 3.5F. This change in temperature can impact weather patterns by influencing air pressure, wind patterns, and the formation of clouds and precipitation.
At a depth of 1000 km below the surface, the temperature of the Earth's interior is estimated to be around 1200-1400 degrees Celsius. This heat is generated by the Earth's core and is a result of radioactive decay and residual heat from the planet's formation.
1,000atm is about 33,900 feet of water depth.
6.4˚C per 1000 m elevation gain or 3.5˚F for 1000 ft elevation gain
1000 of barnds
1000 feet