The temperature of the Earth's asthenosphere is estimated to range between 1300°C and 1600°C.
130 degrees Celsius is equal to 266 degrees Fahrenheit.
8 degrees Celsius is warmer than 2 degrees Celsius.
The temperature of the asthenosphere ranges from about 1300 to 2400 degrees Fahrenheit (700 to 1300 degrees Celsius). This layer of the Earth's mantle is partially molten, allowing it to flow and contribute to plate tectonics. The actual temperature can vary depending on the depth within the asthenosphere.
20 degrees Celsius is 68 degrees Fahrenheit, and 30 degrees Celsius is 86 degrees Fahrenheit.
704.4 C
2372 degrees F
2000
The temperature of the Earth's asthenosphere is estimated to range between 1300°C and 1600°C.
1300ºC = 2,372ºFTip: Use this formula to convert degrees Celsius (C) to degrees Fahrenheit (F): (C x 1.8) + 32 = F
130 degrees Celsius is equal to 266 degrees Fahrenheit.
Lava - between 700 - 1300 degrees Celsius magma - same as above
We don't know for certain. It's probably around 1300 degrees Celsius.
The temperature of the core of a volcano can reach between 700 to 1300 degrees Celsius (1292 to 2372 degrees Fahrenheit).
No. The lowest temperature , with oxygen closed off and a yellow flame , is about 1000 degrees Celsius. With oxgen feed open temperature of the flame can reach 1300 degrees.
Researching the temperatures of liquid magma has shown that the average temperature ranges are between 700 and 1300 degrees Celsius. On rare occasions the temperature can be as low as 600 or as high as 1600 degrees celsius.
The asthenosphere is located beneath the lithosphere, approximately 80-200 kilometers below the Earth's surface. It has temperatures that range from 1300-2400 degrees Fahrenheit (700-1300 degrees Celsius).