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Home » Rocks » Metamorphic Rocks » Slate

Slate


What Is Slate?   What Minerals Are In Slate?   What Is Slate Used For?


What is Slate?



Slate is a fine-grained, foliated metamorphic rock that is created by the alteration of shale or mudstone by low-grade regional metamorphism. It is popular for a wide variety of uses such as roofing, flooring and flagging because of its durability and attractive appearance.


Composition of Slate



Slate is composed mainly of clay minerals or micas depending upon the degree of metamorphism to which it has been subjected. The original clay minerals in shale alter to micas with increasing levels of heat and pressure. Slate can also contain abundant quartz and small amounts of feldspar, calcite, pyrite, hematite and other minerals.


Color of Slate



Most slates are gray in color and range in a continuum of shades from light to dark gray. Slate also occurs in shades of green, red, black, purple and brown. The color of slate is often determined by the amount and type of iron and organic material that are present in the rock.


How Does Slate Form?



The tectonic environment for producing slate is usually a former sedimentary basin that becomes involved in a convergent plate boundary. Shales and mudstones in that basin are compressed by horizontal forces with minor heating. These forces and heat modify the clay minerals in the shale and mudstone. Foliation develops at right angles to the compressive forces of the convergent plate boundary to yield a vertical foliation that usually crosses the bedding planes that existed in the shale.


Uses of the Word "Slate"



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The word "slate" has not been used consistently over time and in some industries. Today most geologists are careful not to use the word "slate" when talking about "shale". However, in the past the word slate was often used freely in reference for shale.

This confusion of terms partially arises from the fact that shale is progressively converted into slate. Imagine driving your car eastwards in Pennsylvania through areas of increasing metamorphism, starting where the rock is definitely "shale" and stopping to examine rock at each outcrop. You will have a difficult time deciding where on that route "shale" has been converted into "slate". It can be difficult to pick up a rock and apply the proper name where the rocks have been lightly metamorphosed.

In the coal mining industry of the Appalachian Basin, the word "slate" is still used by many miners to in reference to the shale that forms the roof and floor of a mine and for fragments of shale that are separated from the coal in preparation plants. Experienced miners train newer miners and archaic language is passed along.

In the 1800's elementary school students used a small piece of slate mounted in a wooden frame for writing practice and arithmetic problems. Writing was done with a small pencil made of slate, soapstone or clay. The slate could be wiped clean with a soft cloth. Small slates were also used in schools and businesses to list daily events, schedules, menus, prices and other notices. Today, over 150 years after writing slates started to disappear from schools the word "slate" is still used in phrases such as "clean slate," "wipe the slate clean," "slated for today," "put it on the slate" and more.


Slaty Cleavage



Foliation in slate is caused by the parallel orientation of platy minerals in the rock such as microscopic grains of clay minerals and mica. These parallel mineral grain alignments give the rock an ability to break smoothly along planes of foliation. People exploit this property of slate to produce thin sheets of slate that are used in construction projects and manufacturing.


Uses of Slate



Most of the slate mined throughout the world is used to produce roofing slates. Slate performs well in this application because it can be cut into thin sheets, absorbs minimal moisture and stands up well in contact with freezing water. A disadvantage is the cost of the slate and its installation in comparison with other roofing materials. As a result, in new construction slate is mainly confined to high end projects and prestige architecture.

Slate is also used for interior flooring, exterior paving, dimension stone and decorative aggregate. Small pieces of slate are also used to make turkey calls. The photos and video on this page document several uses of slate. Historically slate has been used for chalkboards, student writing slates, billiard tables, cemetery markers, whetstones and table tops. Because it is a good electrical insulator it was also used for early electric panels and switch boxes.

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Gabbro
Slate is a fine-grained, foliated metamorphic rock that is created by the alteration of shale or mudstone by low-grade regional metamorphism. The specimen shown above is about two inches (five centimeters) across.




Magnified gabbro
Most of the slate mined throughout the world is used to produce roofing slates. Slate performs well in this application because it can be cut into thin sheets, absorbs minimal moisture and stands up well in contact with freezing water. A disadvantage is the cost of the slate and its installation in comparison with other roofing materials. As a result, in new construction slate is mainly confined to high end projects and prestige architecture. Image © Iain Sarjeant, iStockphoto.


Gabbro chart
Slate is a durable rock that is suitable for use as flooring, stair treads, sidewalk slabs and patio stone. It is also produced in a variety of colors that allow it to be incorporated into a variety of design projects. Shown above are multi-color flooring tiles. Image © Chad Truemper, iStockphoto.


Divergent boundary
Slate is sometimes used as facing stone on building exteriors. Image © John Bloor, iStockphoto.


Black granite
School slate used for writing practice and arithmetic. Students wrote on the slate with a "pencil" made from slate, soapstone or clay. These slates were widely used until the late 1800's when wood-case pencils were easily produced and the price of paper became affordable. Image © Bruce Lonngren, iStockphoto.


More Metamorphic Rocks
  Schist
  Slate
  Soapstone
  Quartzite
  Novaculite
  Gneiss
  Marble
  Amphibolite


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