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 Earth's crust varies depending on location and depth. On average, the temperature increases by about 25-30 degrees Fahrenheit per kilometer of depth. At the surface, the average temperature is around 50-70 degrees Fahrenheit, but it can reach much higher temperatures at greater depths.
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 between 8 Fahrenheit and -12 Fahrenheit is -2 Fahrenheit.
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 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 the Earth's crust varies depending on location and depth. On average, the temperature increases by about 25-30 degrees Fahrenheit per kilometer of depth. At the surface, the average temperature is around 50-70 degrees Fahrenheit, but it can reach much higher temperatures at greater depths.
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).
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 between 8 Fahrenheit and -12 Fahrenheit is -2 Fahrenheit.
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.
Temperature Fahrenheit = Temperature Celsius(1.80) + 32 Temperature Fahrenheit = (39.4o Celsius)(1.80) + 32 = 102.9o Fahrenheit ==============
1,600 degrees Fahrenheit...
The temperature scale is Fahrenheit, named for scientist Daniel Gabriel Fahrenheit.
The temperature scale based on the keyword "Fahrenheit" is the Fahrenheit scale.
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 Celsius to Fahrenheit graph shows the relationship between temperature measurements in Celsius and Fahrenheit. It illustrates how the two temperature scales are related and how a temperature in Celsius corresponds to a temperature in Fahrenheit.