Calculate the number 8843
[7200] Calculate the number 8843 - NUMBERMANIA: Calculate the number 8843 using numbers [2, 9, 1, 5, 22, 794] and basic arithmetic operations (+, -, *, /). Each of the numbers can be used only once. - #brainteasers #math #numbermania - Correct Answers: 3
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Calculate the number 8843

NUMBERMANIA: Calculate the number 8843 using numbers [2, 9, 1, 5, 22, 794] and basic arithmetic operations (+, -, *, /). Each of the numbers can be used only once.
Correct answers: 3
#brainteasers #math #numbermania
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Fish Jokes 05

What kind of money do fishermen make?

Net profits!

What do you get if you cross a salmon, a bird's leg and a hand?

Birdsthigh fish fingers!

What kind of noise annoys an oyster?

A noisy noise annoys an oyster! (Try saying that fast!)
What kind of fish goes well with ice-cream?

Jellyfish!

What did the boy fish say to his girlfriend?

'Your plaice or mine'!

Where does seaweed look for a job?

In the 'Kelp-wanted' adds!

Why is a fish easy to weigh?

Because it has its own scales!

Why are fish boots the warmest ones to wear?

Because they have electric 'eels!

Why are dolphins cleverer than humans?

Within 3 hours they can train a man to stand at the side of a pool and feed them fish!

To whom do fish go to borrow money?

The loan shark!

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Oliver Heaviside

Born 18 May 1850; died 3 Feb 1925 at age 74. English physicist and electrical engineer who predicted the existence of the ionosphere. In 1870, he became a telegrapher, but increasing deafness forced him to retire in 1874. He then devoted himself to investigations of electricity. In 1902, Heaviside and Arthur Kennelly predicted that there should be an ionised layer in the upper atmosphere that would reflect radio waves. They pointed out that it would be useful for long distance communication, allowing radio signals to travel to distant parts of the earth by bouncing off the underside of this layer. The existence of the layer, now known as the Heaviside layer or the ionosphere, was demonstrated in the 1920s, when radio pulses were transmitted vertically upward and the returning pulses from the reflecting layer were received.
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