To convert Fahrenheit to Celsius, you can use the formula: °C = (°F - 32) / 1.8 Substitute 4000 for °F: °C = (4000 - 32) / 1.8 The result is 2204.44 degrees Celsius.
The answer is 3726.85 C (approx.). The Kelvin scale starts at absolute zero and is used in scientific laboratories. Celsius is for general use and set 0 and 100 as melting and boiling point of water respectively. To convert from K to C, subtract 273.15 from K.
The average temperature gradient in the Earth's crust is approximately 25-30 degrees Celsius per kilometer of depth. Therefore, the total temperature change between 1000 m and 4000 m in depth would be around 75-120 degrees Celsius.
The Earth's mantle can range from about 500 to 900 degrees Celsius at its upper boundary near the crust to over 4000 degrees Celsius at its lower boundary near the outer core.
8 degrees Celsius is warmer than 2 degrees Celsius.
4000 degrees Celsius=7232 degrees Fahrenheit.
4000 degrees Celsius is equal to 7232 degrees Fahrenheit.
4000 degrees Celsius is equivalent to 7232 degrees Fahrenheit.
4000 degrees Celsius is equivalent to 7232 degrees Fahrenheit.
To convert Fahrenheit to Celsius, you can use the formula: °C = (°F - 32) / 1.8 Substitute 4000 for °F: °C = (4000 - 32) / 1.8 The result is 2204.44 degrees Celsius.
About 4000 degrees Celsius
Sunspots are typically between 3000-4000 degrees Celsius. This is, relatively speaking, cool compared to the normal photosphere temperature of about 5500 degrees Celsius.
F = 9C ÷ 5 + 32°, where F is the temperature in degrees Fahrenheit and C is the temperature in degrees Celsius. 9 x 1600° ÷ 5 + 32° = 14400° ÷ 5 + 32° = 2880° + 32 ° = 2912° 9 x 4000° ÷ 5 + 32° = 36000° ÷ 5 + 32° = 7200° + 32° = 7232° So 1600 to 4000 degrees Celsius is roughly 2900 to 7200 degrees Fahrenheit.
The answer is 3726.85 C (approx.). The Kelvin scale starts at absolute zero and is used in scientific laboratories. Celsius is for general use and set 0 and 100 as melting and boiling point of water respectively. To convert from K to C, subtract 273.15 from K.
The average temperature gradient in the Earth's crust is approximately 25-30 degrees Celsius per kilometer of depth. Therefore, the total temperature change between 1000 m and 4000 m in depth would be around 75-120 degrees Celsius.
The core of the sun is about 15 million degrees Celsius, while the surface temperature is around 5,500 degrees Celsius.
The Earth's mantle can range from about 500 to 900 degrees Celsius at its upper boundary near the crust to over 4000 degrees Celsius at its lower boundary near the outer core.