How do I identify Slate?

Slate can be identified by its hardness of 2.5 - 4 on the Mohs scale, Gray to black color. Look for these key characteristics when examining specimens.

Slate typically appears in Gray to black, sometimes green, yellow, brown, red. Color can vary depending on impurities and formation conditions.

Slate has a hardness of 2.5 - 4 on the Mohs scale. This makes it a soft mineral that can be scratched easily.

Slate

A variety of Metamorphic

Common

What is Slate?

Slate is a fine-grained, metamorphic rock that is created when shale or mudstone is altered by the heat and pressure of metamorphic action. Most slate is gray in color. Its durability and physical appeal make it a popular material for roofing and flooring. It is also used to build school blackboards and even pool tables.

Etymology & Origins

Before the mid-19th century, the terms slate, shale and schist were not sharply distinguished. In the context of underground coal mining in the United States, the term slate was commonly used to refer to shale well into the 20th century. For example, roof slate referred to shale above a coal seam, and draw slate referred to shale that fell from the mine roof as the coal was removed.

Uses & Applications

Slate has been used for centuries in construction, particularly as roofing tiles due to the flat nature of its fracture pattern and its durability. Slate has also been used in the creation of chalkboards, and it is an excellent insulator, making a popular material for electric panels. Smaller pieces can be used to make turkey calls.

Slate Market Value Calculator

Estimate the market value of Slate using size, quality, and finish. This preview calculator is for quick context and is not a formal appraisal.

Slate Localities Map

See where Slate is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

Map preview

North ZoneCentral RidgeSouth Basin

Key Characteristics

Characteristics of Slate

Because slate was formed in low heat and pressure, compared to a number of other metamorphic rocks, some fossils can be found in slate; sometimes even microscopic remains of delicate organisms can be found in slate.

Composition of Slate

Slate is mainly composed of the minerals quartz and muscovite or illite, often along with biotite, chlorite, hematite, and pyrite and, less frequently apatite, graphite, kaolinite, magnetite, tourmaline, or zircon as well as feldspar. Occasionally, as in the purple slates of North Wales, ferrous reduction spheres form around iron nuclei, leaving a light green spotted texture. These spheres are sometimes deformed by a subsequent applied stress field to ovoids, which appear as ellipses when viewed on a cleavage plane of the specimen.