Every School Used To Have It --Chalk : What Is It Made Of? Coccolithophores! | Educational technology , Erate, Broadband and Connectivity | Scoop.it

When a school teacher writes her name on a blackboard on the first day of class, what she's really doing is crushing the skeletons of terribly ancient earthlings into a form that spells out the name "Mrs. ...".


A piece of chalk, when you think about too much, is a miracle. What is it, exactly? Well, if you look under a microscope, as British naturalist Thomas Huxley did in the 1860s, what you see is this (see figure). Chalk is composed of extremely small white globules. They look, up close, like snowballs made from brittle paper plates. Those plates, it turns out, are part of ancient skeletons that once belonged to roundish little critters that lived and floated in the sea, captured a little sunshine and carbon, then died and sank to the bottom. There still are trillions of them floating about in the oceans today, sucking up carbon dioxide, pocketing the carbon. Over the millennia, so many have died and plopped on top of each other, the weight of them and the water above has pressed them into a white blanket of rock, entirely composed of teeny skeletons. Scientists call these ancient plates "coccoliths." Technically, they are single-celled phytoplankton algae.


Chalk doesn't proclaim itself. It is usually out of view, buried in the ground below. Every so often, when a highway is being carved through a mountain, or when the sea and wind erode the side of a hill, that's when the green cover comes off, then you can see it. The White Cliffs of Dover are all chalk, piled hundreds of feet high.


In 1853, when the transatlantic cable was being laid, engineers would occasionally yank thick loops of wire up 10,000 feet from the ocean bottom, and every time, they found the same coating of white muck: chalk again. It turns out, writes biologist Bernd Heinrich, "the Atlantic mud, which stretches over a huge plain thousands of square miles, is raw chalk."

“A great chapter of the history of the world is written in chalk.


Since then geologists have found a chalk layer stretching 3,000 miles across Europe into Asia. It's under France, Germany, Russia, Egypt, Syria. How did it get there?


That, said Thomas Huxley (who first saw those teeny skeletons under his microscope) is one of the "most startling conclusions of physical science." In 1868, he gave a lecture to the "working men of Norwich" where he declared that "a great chapter of the history of the world is written in chalk."



Via Dr. Stefan Gruenwald, Ron Peters