Chess Knight Move
[4472] Chess Knight Move - Find the country and its capital city, using the move of a chess knight. First letter is C. Length of words in solution: 8,6. - #brainteasers #wordpuzzles #chessknightmove - Correct Answers: 45 - The first user who solved this task is Manguexa Wagle
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Chess Knight Move

Find the country and its capital city, using the move of a chess knight. First letter is C. Length of words in solution: 8,6.
Correct answers: 45
The first user who solved this task is Manguexa Wagle.
#brainteasers #wordpuzzles #chessknightmove
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There was an elderly widow who...

There was an elderly widow who lived in a large mansion. She was feeling generous when it came to Thanksgiving, so she called up the local military base, and asked to speak with the lieutenant.
"Please send up four nice young men to eat dinner here on Thanksgiving, but please, don't send any Jews. Please, no Jews."
The lieutenant replied, "No problem ma'am, and I am sure I speak for the army when I say we all appreciate your kindness."
Well, Thanksgiving rolled around, and the widow went to answer the door when it rang. She was surprised to see four black recruits. "But... But... There must be some mistake," she stammered.
One of them replied, "No ma'am, Lieutenant Goldstein doesn't make mistakes."
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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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