Calculate the number 5006
[351] Calculate the number 5006 - NUMBERMANIA: Calculate the number 5006 using numbers [4, 9, 6, 5, 31, 486] 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 5006

NUMBERMANIA: Calculate the number 5006 using numbers [4, 9, 6, 5, 31, 486] 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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A sweet little boy surprised h...

A sweet little boy surprised his grandmother one morning and brought her a cup of coffee. He made it himself and he was so proud. Anxiously, he waited to hear the verdict. The grandmother in all her life had never had such a bad cup of coffee. As she forced down the last sip, his grandmother noticed three of those little green army guys were in the bottom of the cup.

She asked, "Honey, why would three of your little army men be in the bottom of my cup?"

Her grandson replied, "You know grandma, it's like on TV. 'The best part of waking up is soldiers in your cup'."

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Tuzo Wilson

Born 24 Oct 1908; died 15 Apr 1993 at age 84. John Tuzo Wilson was a Canadian geologist and geophysicistwho determinedthe underlying structure of faults, continents across the globe. From the early 1960s, Wilson revolutionized the emerging field of plate tectonics. He coined the word“plate” for the rigid subdivisions of the Earth's crust of both land and ocean beds. By 1963, he identified some of the earliest evidence supporting the sea-floor spreading hypothesis of Harry H. Hess. Wilson showed the relationship that islands were older for those further away from mid-ocean ridge. One of his important new ideas (1965) was for transform faults, where plate boundaries meet in a series of of offsets, and the plates slide alongside past each other without any creation or destruction of the crust. It is a conservative plate boundary beecause neither plate slides under the other.«
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