MAGIC SQUARE: Calculate A*B-C
[6640] MAGIC SQUARE: Calculate A*B-C - The aim is to place the some numbers from the list (17, 18, 21, 31, 32, 35, 41, 42, 43, 45, 84, 87, 89) into the empty squares and squares marked with A, B an C. Sum of each row and column should be equal. All the numbers of the magic square must be different. Find values for A, B, and C. Solution is A*B-C. - #brainteasers #math #magicsquare - Correct Answers: 12 - The first user who solved this task is Nílton Corrêa de Sousa
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MAGIC SQUARE: Calculate A*B-C

The aim is to place the some numbers from the list (17, 18, 21, 31, 32, 35, 41, 42, 43, 45, 84, 87, 89) into the empty squares and squares marked with A, B an C. Sum of each row and column should be equal. All the numbers of the magic square must be different. Find values for A, B, and C. Solution is A*B-C.
Correct answers: 12
The first user who solved this task is Nílton Corrêa de Sousa.
#brainteasers #math #magicsquare
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Fear of alligators

While sports fishing off the Florida coast, a tourist capsized his boat. He could swim, but his fear of alligators kept him clinging to the overturned craft. Spotting and old beachcomber standing on the shore, the tourist shouted,"Are there any gators around here?!"

"Naw," the man hollered back, "they ain't been around for years!"

"Feeling safe, the tourist started swimming leisurely toward the shore.

About halfway there he asked the guy,"How'd you get rid of the gators?"

"We didn't do nothin'," the beachcomber said.

"The sharks got 'em."

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Joseph Paxson Iddings

Born 21 Jan 1857; died 8 Sep 1920 at age 63.American geologist who advanced understanding in the field of petrology - the study of the origin, composition, structure, and alteration of rocks. Around 1880, he was one of the first in the U.S. to study thin rock sections with a microscope. He explored and mapped the geology of Yellowstone National Park during seven field seasons (1883-1890). From this study he introduced original ideas concerning the range of crystal line textures and mineral composition of granular igneous rocks. He proposed that physical and chemical conditions causing differences in the formationof neighbouring igneous rock from the same igneous magma. Further, he rejected the prevailing view that granular rocks were only formed in large masses at depth.«
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