The temperature in Earth's mantle ranges from about 870 to 2200 degrees Fahrenheit (470 to 1200 degrees Celsius) at the upper boundary with the crust and increases with depth. Towards the core-mantle boundary, temperatures can reach up to 7250 degrees Fahrenheit (4000 degrees Celsius).
The burning point of paper is around 450-470 degrees Celsius, which is equivalent to 723-743 Kelvin. At this temperature, the cellulose fibers in the paper begin to break down and undergo combustion.
Mosses first appeared around 470 million years ago during the Ordovician period. They were some of the earliest plants to colonize land.
The annual rainfall in Greenland varies from less than 50 millimetres (2 inches) in Peary Land in the north to over 1,000 millimetres in the south around Torgilsbu.In the latter region the total annual precipitation (rain and snow) can be as high as 2,500 millimetres (100 inches) including over 12 metres (470 inches) of snow. This is due to the extremely unsettled conditions produced by the Icelandic Low which drives moist air from the Atlantic onto southeastern Greenland. A result of this gradient is that on the Greenland Ice Sheet flow is frequently poleward rather than equatorward, since most accumulation is int eh southern part of the island.
To make a 500 ml solution of 3% H2O2 from a 50% solution, you would need to dilute the 50% solution with water. You would add 325 ml of water to 175 ml of the 50% H2O2 solution to achieve a final volume of 500 ml with a concentration of 3% H2O2.
880 degrees Fahrenheit
To convert Fahrenheit to Celsius, you can use the formula: Celsius = (Fahrenheit - 32) x 5/9. Plugging in the value of 470 Fahrenheit, the conversion would be: (470 - 32) x 5/9 ≈ 243.33 degrees Celsius.
Lead is a metal that is solid at 470 degrees Celsius. It has a melting point of 327.5 degrees Celsius, so it would be in its solid state at 470 degrees Celsius.
Paper typically burns at temperatures between 440 to 470 degrees Celsius (824 to 878 degrees Fahrenheit). However, this can vary depending on factors such as the type of paper and the presence of other materials.
293 K is approximately 20°C, and 470 K is approximately 197°C.
The temperature in Earth's mantle ranges from about 870 to 2200 degrees Fahrenheit (470 to 1200 degrees Celsius) at the upper boundary with the crust and increases with depth. Towards the core-mantle boundary, temperatures can reach up to 7250 degrees Fahrenheit (4000 degrees Celsius).
The average temperatures range from 470 deg Celsius on Venus to -200 deg C on Neptune.
Venus has a surface temperature of around 470 degrees Celsius, making it the hottest planet in our solar system due to its thick atmosphere that traps heat. The extreme temperatures on Venus are hot enough to melt lead.
First off, you need to know the conversion to inches: 1 inch = 2.54cmNext, you need to convert 470 mm to cm:470 mm = 470 * (10-3)mcm is equal to 10-2 m so you need to divide 470 by 10 = 47cmNow to convert to inches:47cm * (1inch/2.54cm) = 18.5 inchesDirect Conversion Formula 470 mm*1 in25.4 mm=18.50393701 in
It is 470.
81% of 470= 81% * 470= 0.81 * 470= 380.7
30% of 470= 30% * 470= 0.3 * 470= 141