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 approximately 1,000 kilometers, the temperature of the Earth's interior can reach around 1,000 to 1,500 degrees Celsius (1,832 to 2,732 degrees Fahrenheit). This temperature is influenced by the geothermal gradient, which varies depending on location and geological conditions. As depth increases, both pressure and temperature rise, contributing to the extreme conditions found in the Earth's mantle.
At a depth of approximately 1,000 kilometers, the temperature of the Earth's interior can reach around 3,000 to 4,000 degrees Celsius (5,432 to 7,232 degrees Fahrenheit). This high temperature is primarily due to the heat generated by the decay of radioactive isotopes, as well as the residual heat from the planet's formation. The extreme pressure at this depth further influences the thermal conditions, contributing to the Earth's dynamic geophysical processes.
The crust is the cool part of the Earth. It is the surface we live on. It should be at a comfortable temperature until it reaches down to the mantle, the next layer. That area will be hotter. Then at the center, is the core. That is the hot part of the Earth's interior. It is about 3500° C. Estimates vary from 2000 to 7000, but it is HOT!About 447 in Fahrenheit
Magma is a complex high-temperature fluid substance. Temperatures of most magmas are in the range 700 °C to 1300 °C (or 1300 °F to 2400 °F), but very rare carbonatite melts may be as cool as 600 °C, and komatiite melts may have been as hot as 1600 °C. Most are silicate mixturess.
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 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.
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.
1,000atm is about 33,900 feet of water depth.
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.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
Magma rises from the asthenosphere to the surface of the Earth. After it reaches temperature upward to 1000 degrees Fahrenheit, the magma starts to rise. Gases also aid in pushing the magma toward the surface, along with the tremendous pressure from the depth at which it originates.
1000 feet