
The very strong foliation is called “slaty cleavage”. It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly “cut” by striking parallel to the foliation, with a specialized tool in the quarry, many slates will form smooth flat sheets of stone which have long been used for roofing and floor tiles and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for example, slate from North Wales can be found in many shades of grey, from pale to dark, and may also be purple, green or cyan. Slate is not to be confused with shale, from which it may be formed, or schist. Ninety percent of Europe’s natural slate used for roofing originate from Spain.

The History of Writing Slate: The exact origins of the writing slate remain unclear, but references to its use can be found as far back as the fourteenth century and evidence suggests that it was used on occasion through the sixteenth and seventeenth centuries as well. The central time period for the writing slate, however, “appears to begin in the later eighteenth century, when developments in sea and land transport permitted the gradual expansion of slate quarrying in Wales and the growth of a substantial slate workshop industry.” By the nineteenth century, writing slates were used around the world in nearly every school and were a central part of the overall slate industry. At the dawn of the twentieth century, writing slates were still the primary tool in the classroom for students and it was not until the 1930s (or later) that writing slates started being replaced by more modern methods. However, writing slates did not become obsolete. They are still made today, though in small quantities.
source: http://en.wikipedia.org/wiki/Slate

