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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.
The sum of the interior and exterior angles at the same vertex is always 180 degrees or 1 straight angle. So, if there are 1000 st angles, then there must be 1000 vertices and so 1000 sides.
It is: 998*180 = 179640 degrees
with the help of pyrometer
you need three measurements...the height,width an depth of the pool..volume in litres = height (cm)x width(cm)x depth(cm) /1000
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.
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 asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
The Earth's mantle is the thickest part of the interior, about 2900 km thick, and has a temperature of about 1000 degrees C. This makes it elastic : it can be pushed down by the weight of the crust, and return to its original position when the load decreases. This has occurred when large ice caps (such as Greenland and Antarctica) add to the weight of the crust.
1000 atmospheres is equivalent to approximately 15,000 feet of depth in water.
The temperature of lithospheric plates varies depending on their depth within the Earth's crust. Generally, the temperature increases with depth due to the geothermal gradient. At the surface, temperatures can range from around 0°C to over 1000°C at greater depths.
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.
Magma rises towards the Earth's surface because it is less dense than the solid rock surrounding it. This buoyancy is driven by heat from the Earth's interior, causing the magma to move upwards through cracks and fissures in the crust. Upon reaching the surface, it may erupt as lava or solidify underground to form intrusive igneous rocks.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
1000 of barnds
1000 feet