You can feel it, but you can't...
[2862] You can feel it, but you can't... - You can feel it, but you can't touch it. You can hear it, but you can't see it. What is it? - #brainteasers #riddles - Correct Answers: 199 - The first user who solved this task is On On Lunarbasil
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You can feel it, but you can't...

You can feel it, but you can't touch it. You can hear it, but you can't see it. What is it?
Correct answers: 199
The first user who solved this task is On On Lunarbasil.
#brainteasers #riddles
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Retaking exam

Four college students missed an important exam, choosing to party instead. They go together to their professor the next day, and said, "We're sorry we missed the exam. We had a flat tire on the way to class. Is there any way we could possibly take a re-test?"

"Sure," replied the professor. "Come on in tomorrow, and you can all take a retest. But remember, it's a pass or fail."

The four students arrived the next day to take the retest, and all of them sat down in their seats. Before handing them their exams, their professor told them, "I've got good news and bad news. The good part is, there's only one question on the test. The bad news is, if any of you fail, you all fail the test."

The students sat there, a bit worried from this professor's strange introduction to the exam. Then the professor handed out the four exams, and each student stared down at their papers, which contained just one simple question:

"Which tire was it?"

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John Fillmore Hayford

Born 19 May 1868; died 10 Mar 1925 at age 56.American civil engineer and geodesist who established the modern science of geodesy, and made a precise determination of the ellipsoidal shape and size of the earth (1909). The International Union of Geodesy and Geophysics adopted Hayford's calculations in 1924. This International ellipsoid has a flattening of exactly 1 part in 297. The Earth's equatorial radius is 6,378,388 m. The radius along the polar axis is then 1/297 less than that or 6,356,912 m. (Surprisingly, the U.S. did not adopt this datum.) Hayford's theory of isostasy gave that the pressure exerted by the earth's crust is approximately the same over the entire globe, regardless of the nature of the surface (for example, lowlands or mountains). With modification, this theory is now used to explain phenomena within the crust. At the time of his death he was investigating the problems connected with evaporation and the water level of the Great Lakes.
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