It runs and runs but can nev...
[3548] It runs and runs but can nev... - It runs and runs but can never flee. It is often watched, yet never sees. When long it brings boredom, When short it brings fear. What is it? - #brainteasers #riddles - Correct Answers: 68 - The first user who solved this task is Linda Tate Young
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It runs and runs but can nev...

It runs and runs but can never flee. It is often watched, yet never sees. When long it brings boredom, When short it brings fear. What is it?
Correct answers: 68
The first user who solved this task is Linda Tate Young.
#brainteasers #riddles
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A trucker came into a truck st...

A trucker came into a truck stop cafe and placed his order. He said, "I want three flat tires, a pair of headlights and a pair of running boards."
The brand new blonde waitress, not wanting to appear stupid, went to the kitchen and said to the cook, "This guy out there just ordered three flat tires, a pair of headlights and a pair of running Boards. What does he think this place is, an auto parts store?"
"No," the cook said, "Three flat tires mean three pancakes, a pair of headlights is two eggs sunny side up, and running boards are 2 slices of crisp bacon."
"Oh, OK!" said the blonde. She thought about it for a moment and then spooned up a bowl of beans and gave it to the customer.
The trucker asked, "What are the beans for, Blondie?"
She replied, "I thought while you were waiting for the flat tires, headlights and running boards, you might as well gas up!"
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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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