Calculate the number 837
[1328] Calculate the number 837 - NUMBERMANIA: Calculate the number 837 using numbers [6, 2, 6, 2, 20, 775] and basic arithmetic operations (+, -, *, /). Each of the numbers can be used only once. - #brainteasers #math #numbermania - Correct Answers: 29 - The first user who solved this task is Sanja Šabović
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Calculate the number 837

NUMBERMANIA: Calculate the number 837 using numbers [6, 2, 6, 2, 20, 775] and basic arithmetic operations (+, -, *, /). Each of the numbers can be used only once.
Correct answers: 29
The first user who solved this task is Sanja Šabović.
#brainteasers #math #numbermania
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Toilet Paper

A little old lady goes into the store to do some shopping. She is bewildered over the large selection of toilet paper.
"Pardon me, sir," she says to the store manager, "but can you explain the differences in all these toilet papers?"
"Well," he replies pointing out one brand, "this is as soft as a baby's kiss. It's $1.50 per roll."
He grabs another and says, "This is nice and soft as a bunny, strong but gentle, and it's $1.00 a roll."
Pointing to the bottom shelf he tells her, "We call that our No Name brand, and it's 20 cents per roll."
"Give me the No Name," she says.
She comes back about a week later, seeks out the manager and says, "Hey! I've got a name for your No Name toilet paper. I call it John Wayne."
"Why?" he asks.
"Because it's rough, it's tough and it don't take crap off anybody!"

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William Henry Dines

Died 24 Dec 1927 at age 72 (born 5 Aug 1855).William Henry Dines was an English meterologist (like his father) and inventor of related measurement instruments such as the Dines pressure tube anemometer (the first instrument to measure both the velocity and direction of wind, 1901), a very lightweight meteorograph, and a radiometer (1920). He joined the Royal Meteorological Society study of the cause of the disastrous Tay Bridge collapse of 1879. His measurements of upper air conditions, first with kites and later by balloon ascents (1907), brought an understanding of cyclones from dynamic processes in the lower stratosphere rather than thermal effects nearer to the ground.
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