Wiki User
∙ 14y agoAway 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.
Wiki User
∙ 14y ago7389 ------ 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
with the help of pyrometer
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.
well that answer will be 6000 km - depths below surface of earth (km)
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.
1000 atmospheres is equivalent to approximately 15,000 feet of depth in water.
6.4˚C per 1000 m elevation gain or 3.5˚F for 1000 ft elevation gain
1000 of barnds
1000 feet
In the troposphere, the temperature generally decreases with increasing altitude due to lower air pressure. In the stratosphere, the temperature remains relatively constant then begins to increase due to the absorption of solar radiation by ozone. In the mesosphere and thermosphere, the temperature decreases again as altitude increases due to a decrease in the density of air molecules.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
The temperature of the lithosphere varies depending on depth, location, and geologic activity. Generally, temperatures can range from around 200°C to over 1000°C in the upper mantle. The outermost layer, the crust, has a temperature that ranges from around 200°C to 500°C.
C can be calculated by adding your cash flow from investing actives and financing activities this can be found in the statement of cash flows. From FCF = NOPAT + Depr change in non cash working capital C
The Fahrenheit temperature of 1000 Kelvin is 1340 degrees Fahrenheit.