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
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.
The Earth's mantle has a temperature range of about 500 to 900 degrees Celsius (932 to 1652 degrees Fahrenheit) near the upper boundary with the crust, and can reach temperatures of up to 3700 degrees Celsius (6692 degrees Fahrenheit) near the core-mantle boundary.
The Earth's crust has variable temperatures, ranging from about 60 degrees Fahrenheit at the surface to over 1,600 degrees Fahrenheit at certain depths in the upper mantle.
The temperature is the lowest in the mesosphere, the layer of the Earth's atmosphere that lies above the stratosphere. In the mesosphere, temperatures can drop to as low as -90 degrees Celsius or -130 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 sun's crust is around 6,000 degrees Celsius (10,832 degrees Fahrenheit). It is the coolest layer of the sun's atmosphere.
Mars does not have a molten core like Earth, so its crust doesn't reach high temperatures like terrestrial crust. The average temperature of Mars' crust is estimated to be around -80 degrees Celsius (-112 degrees Fahrenheit).
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.
The Earth's mantle has a temperature range of about 500 to 900 degrees Celsius (932 to 1652 degrees Fahrenheit) near the upper boundary with the crust, and can reach temperatures of up to 3700 degrees Celsius (6692 degrees Fahrenheit) near the core-mantle boundary.
The Earth's crust has variable temperatures, ranging from about 60 degrees Fahrenheit at the surface to over 1,600 degrees Fahrenheit at certain depths in the upper mantle.
1,600 degrees Fahrenheit...
The temperature is the lowest in the mesosphere, the layer of the Earth's atmosphere that lies above the stratosphere. In the mesosphere, temperatures can drop to as low as -90 degrees Celsius or -130 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 layers of the Earth in order from lowest temperature to highest are the inner core, outer core, mantle, and crust. The inner core is the hottest layer, with temperatures reaching up to 9,000 degrees Fahrenheit, while the crust is the coolest layer, with temperatures varying between 32 and 212 degrees Fahrenheit.
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)
Molten rock, or magma, typically has a temperature ranging from 1300 to 2400 degrees Fahrenheit (700 to 1300 degrees Celsius). The exact temperature can vary depending on the composition of the rock and where it is located within the Earth's crust.