The earth’s inner core is a solid ball of iron, nickel and other metals, while the outer core is liquid metal composed of iron and nickel as well. The temperature of the inner core is estimated to be about 5,400 degrees C or 9,800 degrees F, far beyond iron’s melting point.
71 million years ago. Hope it helps :)
Answer:
As the temperature nears the dew point, the evaporation rate and condensation rate become increasingly similar, and relative humidity increases. On the other hand, if the difference between temperature and dew point grows, relative humidity decreases.
Explanation:
I can assume and hope since there's no answer choice below the question, that it's a free choice question. Hope this helps! Don't forget to make me Brainliest ;]
A.GOD is the answer your searching for
