87 °c = 188.6 °f
[°c] × 9⁄5 + 32 = [°f]
870 degrees Celsius is equal to 1598 degrees Fahrenheit. This can be calculated using the formula °F = (°C × 9/5) + 32.
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.
The temperature of the Inner Core of the earth is about 5700 deg C. The outer core, and the mantle both have a similar temperature. This is about the same as the surface of the sun. That is why very hot lava is yellow - that indicates its temperature.
The temperature of the Earth's mantle can vary but generally ranges between 500 to 900 degrees Celsius near the top (upper mantle) to over 4,000 degrees Celsius near the bottom (lower mantle). This heat comes from the Earth's interior and drives processes like mantle convection and plate tectonics.
Earth's mantle reaches temperatures of about 3700°C.
870 degrees Fahrenheit = 465.5 degrees Celsius.
870 degrees Fahrenheit = 465.56 degrees Celsius
870ºC = 1,598ºF
870 degrees Celsius is equal to 1598 degrees Fahrenheit. This can be calculated using the formula °F = (°C × 9/5) + 32.
The burning temperature of a candle flame is typically between 1400-1600 degrees Fahrenheit (760-870 degrees Celsius). The temperature varies depending on the type of wax and additives in the candle.
The temperature for the asthenosphere ranges from around 1300 to 1600 degrees Fahrenheit (700 to 870 degrees Celsius). These elevated temperatures are due to the combination of geothermal heat and the residual heat from the Earth's formation.
oF = oC x 9/5 + 32 870oC x 9/5 + 32 = 1598oF
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.
The temperature of the Inner Core of the earth is about 5700 deg C. The outer core, and the mantle both have a similar temperature. This is about the same as the surface of the sun. That is why very hot lava is yellow - that indicates its temperature.
Venus is the hottest planet, with temperatures of 600oC.
The hottest temperature on Venus is around 900 degrees Fahrenheit, while the coldest temperature is around 870 degrees Fahrenheit. Venus has an extremely hot and uniform surface temperature due to its thick atmosphere that traps heat.
The smelting temperature of gold ore typically ranges between 1,600 to 2,000 degrees Fahrenheit (870 to 1,100 degrees Celsius). This high temperature is required to melt and separate the gold from other minerals in the ore during the smelting process.