Calculate the number 770
[6959] Calculate the number 770 - NUMBERMANIA: Calculate the number 770 using numbers [7, 1, 6, 2, 95, 397] and basic arithmetic operations (+, -, *, /). Each of the numbers can be used only once. - #brainteasers #math #numbermania - Correct Answers: 9 - The first user who solved this task is Nasrin 24 T
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Calculate the number 770

NUMBERMANIA: Calculate the number 770 using numbers [7, 1, 6, 2, 95, 397] and basic arithmetic operations (+, -, *, /). Each of the numbers can be used only once.
Correct answers: 9
The first user who solved this task is Nasrin 24 T.
#brainteasers #math #numbermania
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Fast Promotions

The boss called one of his employees into the office. “Rob,” he said, “you've been with the company for a year. You started off in the post
room, one week later you were promoted to a sales position, and one month after that you were promoted to district manager of the sales
department. Just four short months later, you were promoted to vice-chairman.”

“Now it's time for me to retire, and I want you to take over the company. What do you say to that?”

“Thanks,” said the employee.

“Thanks?” the boss replied. “Is that all you can say?”

“I suppose not,” the employee said. “Thanks, Dad.”

“I suppose not,” the employee said. “Thanks, Dad.”

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Oldest fossils

In 1977, American paleontologist Elso S. Barghoorn of Harvard announced the discovery of Pre-Cambian spherical one-celled algae microfossils (named Eobacterium) 3.4 billion years old, earth's earliest life forms. Barghoorn, with J. William Schopf, studied the ancient chert (a flintlike or quartz-like rock) of the Fig Tree formation in Transvaal, South Africa. Rubidium and strontium ratios in the chert are used to establish the age of the rock, and the fossils contained in it. The fossils are a kind of Prokaryotes, organisms with simple cell wall containing organic chemicals, and examples of cell division are visibile in the remains. A huge number of varieties exist today. They all produce oxygen; and, in the Precambrian period, began to change the earth's primoidal reducing atmosphere to the oxygenated one we have today.
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