-150 Celsius = -238 Fahrenheit
the melting point of ice is not dependent on its mass, it has a fixed melting point, hundred degree Celsius. The melting point of water (ice) should be zero degrees Celsius or any thing higher, Yes ice would melt a one hundred degrees Celsius but it would also boil at that temperature.
Water freezes at 0 degrees Celsius and boils at 100 degrees Celsius.
The freezing point of water is 0 degrees Celsius and the boiling point is 100 degrees Celsius.
Comets range in temperature from about minus 200 degrees Celsius (minus 328 degrees Fahrenheit) in the outer solar system to a few hundred degrees Celsius (up to around 500 degrees Fahrenheit) when passing close to the Sun.
False. The inner core of the Earth is actually much hotter, with temperatures estimated to reach around 9,932 degrees Fahrenheit (5,500 degrees Celsius). This extreme heat is primarily due to the pressure and radioactive decay occurring within the Earth's core.
One hundred and fifty degrees Fahrenheit is equal to 65.6 degrees Celsius.
60 degrees Celsius.
122 degrees Fahrenheit is 50 degrees Celsius.
100 degrees Fahrenheit = 37.78 degrees Celsius
To convert Celsius to Kelvin, add 273.15, so -100C = 173.15K. To convert Celsius to Fahrenheit, multiply by five-ninths and add 32, so the answer is -148.
140oF = 60oC.
A+ . . . . 127k
One-hundred degrees celsius
0 degrees Celsius is a temperature.0 Celsius = 32 Fahrenheit = 273.15 CalvinOn the centigrade scale the temperature at which water freezes at normal pressure. One hundred on the scale is the boiling point of water.
The average body temperature for a bird is one hundred and five degrees Fahrenheit, or forty point five degrees Celsius. As with all creatures, body temperatures fluctuate with age, stress, and surrounding environments.
Conversion formula: [°C] = ([°F] - 32) * 5 / 9 = (100 - 32) * 5 / 9 = 37.78 °C
No, the inner core of the Earth is estimated to be much hotter, reaching temperatures of around 5700 degrees Celsius (10,000 degrees Fahrenheit). This extreme heat is a result of the immense pressure at the Earth's core.