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
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 = (- 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 temperture of earths crust is -70 to +750
1 because the crust is not that big
39.4 degrees Celsius is equivalent to 102.9 degrees Fahrenheit.
To convert -1.69 degrees Celsius to Fahrenheit, use the formula: F = (C * 9/5) + 32 Where C is the temperature in Celsius and F is the temperature in Fahrenheit. Plugging in -1.69 for C, we get -1.69 * 9/5 + 32 = 28.502 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.
Celsius and Fahrenheit are two common temperature scales used to measure temperature. In Celsius, water freezes at 0 degrees and boils at 100 degrees, while in Fahrenheit, water freezes at 32 degrees and boils at 212 degrees.
0.6 degrees Celsius is equal to 33.08 degrees Fahrenheit.
The core's temperature is approximately 1500C and in Fahrenheit its 45699F