the temperture of earths crust is -70 to +750
The temperature of Earth's crust can range from -70 degrees Fahrenheit to +750 degrees Fahrenheit depending on location and depth. Higher temperatures would be recorded in regions of crustal melting from magmatic intrusions. Technically, regions heated by magmatic intrusions are still crustal rock, and could reach well over 1,000 degrees Fahrenheit
The temperature of Earth's crust can range from -70 degrees Fahrenheit to +750 degrees Fahrenheit depending on location and depth. Higher temperatures would be recorded in regions of crustal melting from magmatic intrusions. Technically, regions heated by magmatic intrusions are still crustal rock, and could reach well over 1,000 degrees Fahrenheit. The temperature of the crust increases with depth, reaching values typically in the range from about 500 °C (900 °F) to 1,000 °C (1,800 °F) at the boundary with the underlying mantle. It's over 5000c and that's super hot! So hot it could melt rock!
There is a great range of temperatures on Earth. These temperatures range from far be low zero to more than 100 degrees Fahrenheit just on Earth's crust.
It depends on which point of continental crust, but a rough guess based on an average 1 degree F thermal increase for every 100 feet below the surface, with a surface temperature of 55 degrees F, converted to a kilometer depth of 2.5, gives an answer of 137 degrees F.
30 degrees Celsius
The temperature of Earth's crust can range from -70 degrees Fahrenheit to +750 degrees Fahrenheit depending on location and depth. Higher temperatures would be recorded in regions of crustal melting from magmatic intrusions. Technically, regions heated by magmatic intrusions are still crustal rock, and could reach well over 1,000 degrees Fahrenheit
1,600 degrees Fahrenheit...
The temperature of Earth's crust can range from -70 degrees Fahrenheit to +750 degrees Fahrenheit depending on location and depth. Higher temperatures would be recorded in regions of crustal melting from magmatic intrusions. Technically, regions heated by magmatic intrusions are still crustal rock, and could reach well over 1,000 degrees Fahrenheit. The temperature of the crust increases with depth, reaching values typically in the range from about 500 °C (900 °F) to 1,000 °C (1,800 °F) at the boundary with the underlying mantle. It's over 5000c and that's super hot! So hot it could melt rock!
The temperature of the Sun's core is estimated to be about ~15.7×106 Kelvin (16 million degrees Centigrade or 28 million degrees Fahrenheit)
990 degrees F it is 300 degrees
990 degrees F it is 300 degrees
There is a great range of temperatures on Earth. These temperatures range from far be low zero to more than 100 degrees Fahrenheit just on Earth's crust.
Bake an empty pie at 425 degrees Fahrenheit for 15 minutes. Pies that have a lot of filling may take a short time at a high temperature, then reduce the temperature to make the fruit cook. For apple pie, turn it down to 350 degrees after the 15 minutes and cook for 45 minutes.
The sun does not have an outer crust as it is not solid. The "surface" of the sun, called the photosphere, is about 10,000 degrees Fahrenheit.
Pizza. It makes the crust very crisp.
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
It depends on which point of continental crust, but a rough guess based on an average 1 degree F thermal increase for every 100 feet below the surface, with a surface temperature of 55 degrees F, converted to a kilometer depth of 2.5, gives an answer of 137 degrees F.