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 temperture of earths crust is -70 to +750
1 because the crust is not that big
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (- 0.5o C)(1.80) + 32 = 31o Fahrenheit ===========
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (37.8 degrees Celsius) * (1.80) + 32 Temperature Fahrenheit = 100.04 degrees -------------------------------------------------------
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 temperture of earths crust is -70 to +750
1 because the crust is not that big
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (39.4o Celsius)(1.80) + 32 = 102.9o Fahrenheit ==============
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (- 1.69)(1.80) + 32 = 29 degrees Fahrenheit --------------------------------
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (- 0.5o C)(1.80) + 32 = 31o 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!
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (37.8 degrees Celsius) * (1.80) + 32 Temperature Fahrenheit = 100.04 degrees -------------------------------------------------------
The temperature scale is Fahrenheit, named for scientist Daniel Gabriel Fahrenheit.
temperature scalesBoth Celsius and Fahrenheit are forms of measuring the temperature.
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (0.6 Celsius )(1.80) + 32 = 33.1 degrees Fahrenheit -----------------------------------
The core's temperature is approximately 1500C and in Fahrenheit its 45699F