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Slate (metamorphic rock)

Fine-grained metamorphic rock produced from shale under low-grade metamorphism; notable for slaty cleavage and widespread use in roofing, flooring, tablets and decorative stone.

Overview

Slate is a fine-grained, foliated metamorphic rock derived from clay-rich sediments such as shale. Its most distinctive property is slaty cleavage: the rock splits easily into thin, even sheets. This behavior results from the alignment of microscopic platy minerals during low-grade regional metamorphism and compressive tectonic forces.

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Formation and characteristics

Slate forms when shale or other mudstone is subjected to increased pressure and modest temperatures, causing recrystallization of clay minerals into tiny mica and chlorite flakes. These aligned minerals give slate a planar fabric that is different from the original bedding. Typical colors include various grays, greens, purples and blacks depending on mineral content and trace elements. Slate is generally hard, durable, and impermeable, but it is brittle and can break along its cleavage planes.

Uses and cultural importance

  • Roofing and wall tiles: prized for its weather resistance and the ability to be split into thin, flat sheets.
  • Flooring, countertops and facing stone where a natural, durable surface is desired.
  • Historical uses: writing slates and blackboards, billiard table beds and gravestones.
  • Decorative and architectural elements: trim, pool tables, and landscaping stone.

Slate is part of a metamorphic continuum. With slightly more metamorphism a slate becomes phyllite, which shows a silky sheen; further metamorphism produces schist with visible mineral grains and then gneiss. While slate and schist may appear similar, slate is much finer-grained and splits into thinner, more regular sheets. See metamorphic rock, shale and clay for background on parent materials and processes.

Identification and care

Field identification relies on slaty cleavage, lack of large visible crystals, and the ability to split into thin plates. Slate is long-lasting outdoors but may require proper underlayment and support when used as roofing or flooring because of its brittleness. For further comparisons and geological context consult sources on schist and regional quarrying histories at local geology references.

Clay slate as building stone (roof and facade slate)

Dark clay slate is traditionally used to cover roofs and to clad gables and facades. On the Moselle, in the Hunsrück and in the Eifel, the building of houses with hewn, compact quarry stones made of slate was and is now also common again.

From the Middle Ages until the middle of the 20th century, slates and styluses were made from clay slate. Until the introduction of large-scale industrial paper production and the concomitant fall in the price of writing paper, slates and styluses were a widely used writing material for everyday use, indispensable in trade, in private households, but especially in the elementary school education sector, which had been increasing since the 17th century. From the end of the 19th century until the cessation of industrial stylus slate production in the 1960s, the Thuringian town of Steinach held the world monopoly.

Mining technology

Today's mining is determined by the use of modern equipment and machinery. The fully mechanized, sawing extraction not only facilitates the work of the miners, but also contributes to a careful handling of the valuable rock.

The mineable slate is sawn into grids with a diamond saw along the geological conditions. Block by block, the slate is then released from the mountain. Wheel loaders are used to load the slate underground. The slate is then transported on trolleys by the mine railway to the winding shaft and from there to the production halls above ground. Here the slate blocks are sawn, split and trimmed.

In the surface production, a diamond saw initially takes over the first processing. It ensures that the blocks of different sizes can be used for the production of the capstones largely "cut-free".

Despite all the mechanisation, the shaping operations, splitting and trimming, are still carried out by hand. In the process, the blocks are divided into slabs about 5 millimeters thick.

In the Wadrill roofing slate mine in the Saarland, which was operated until 1953, the slate blocks had to be extracted by steep to vertical bedding (60°-90°) in ridge butt mining. In the mining chambers, the slate blocks were wedged from the bottom to the top by notches or extracted by a gentle, pushing extraction shot with black powder. Extractable blocks were still created underground by splitting parallel to the schistosity (ripping) or splitting perpendicular to the schistosity (heading).

Slate from Germany

In the interest of orderly competition that is transparent to roofers, architects, traders and builders alike, slate quarries with reasonably comparable characteristics from one region have been grouped together under one name.

As with the well-known vineyard sites, the designation of origin thus became a property and quality indication at the same time. The designations and assignments of the pits were determined after long negotiations between the Reichsdachdeckerhandwerk and the German slate industry in the early 1920s. The result was published in the official part of the magazine "Das Deutsche Dachdeckerhandwerk" of August 7, 1932. The specifications were confirmed again in 1953 and 1967 and are still used by the slate companies today: Mosel slate, Thuringian slate, Hunsrück slate and Sauerland slate.

Accordingly, only the slate from the districts of Mayen, Polch, Müllenbach, Trier and the surrounding area may call itself Moselschiefer. Today, only the Katzenberg and Margareta mines in Mayen still bear the name Moselschiefer. The name comes from the historical transport route of this slate across the Moselle to the Lower Rhine and the Benelux countries. For the districts of Altlay, Bundenbach, Kirn, Gemünden and Herrstein as well as their surroundings, the name Hunsrück slate applies. The extraction sites in Fredeburg, Brilon, Nuttlar, etc. fall under the generic term Schiefer aus Westfalen und Waldeck (slate from Westphalia and Waldeck), but are also simply called Sauerländer Schiefer (slate from the Sauerland), although, as in other regions, there can be significant differences in properties within this designation.

The following are still in production today

  • in the Hochsauerland in the area around Bad Fredeburg a compound mine with the mines Bierkeller, Gomer, Magog with a 150-year tradition,
  • in the Hunsrück region, the Altlay slate mine (with underground extraction at a depth of about 120 metres below centuries-old quarries). For 2020, the operator of the Altlay mine announced the start of open-pit slate mining in "new, untouched slate deposit[s]".
  • in Bavaria near (municipality of Geroldsgrün) (after a 500-metre-long winding tunnel) the Lotharheiler slate.

Moselle slate mining around Mayen was traditionally the most productive German site, accounting for over half of Germany's production. However, the largest known roofing slate deposit is located in the area around Bad Fredeburg.

Until 2008, slate was also mined in Thuringia, where a mine in Unterloquitz and an open-cast mine near Schmiedebach were in operation. From the Middle Ages until partly into the second half of the 20th century, the so-called Wissenbach slates were mined as roofing slate in mines and quarries in the Harz region, especially south of Goslar, including the Glockenberg mine. In Kaub on the Middle Rhine, roofing slate of the highest quality was extracted for centuries until 1972. Today, the surface installations of the Wilhelm-Erbstollen mine still bear witness to the former importance of slate mining for the entire region.

Other mining countries

Shale is found in many countries of the world: also outside Europe in North America, South America, South Africa, Japan, China, Russia (Siberia) and India. In Europe, slate deposits are found in Slovenia, Croatia, Greece, Italy, the Czech Republic, Poland, Hungary, Norway, Sweden, Switzerland, Portugal, Spain, France, Belgium, Luxembourg, Great Britain and Ireland.

In terms of volume, significant production is found in Spain, France, Great Britain, Germany and Portugal, in that order. The largest consumer country, however, is by far France. This traditional "slate country" has a formerly important national production (Ardoisières d'Angers), but is also the largest consumer of Spanish slate. Traditional "slate countries" in the sense of use are also Germany, Benelux and Great Britain.

Museums

Germany

Slate museums include:

  • Eifel: German slate mine. It is located at a depth of 16 meters under the Genovevaburg in the town of Mayen.
  • Wittgensteiner Land: Slate mine Bad Berleburg-Raumland Slate mine Raumland
  • Hochsauerland:
    • Slate mining and local history museum Holthausen
    • Slate mining museum Nuttlar
  • Thuringian Slate Mountains: Thuringian-Franconian Slate Road: Along this approximately 100 km long themed road, you can find
    • Slate Museum Ludwigsstadt
    • German Slate Museum, Steinach
    • Slate Park Lehesten, Lehesten
    • Lotharheil slate works, Geroldsgrün
    • Morassina show mine, Schmiedefeld
  • Fell visitor mine, Hunsrück

Abroad

  • Welsh Slate Museum (about the slate industry in Wales)
  • Musée de l'Ardoise in 49800 Trélazé (Maine-et-Loire department, Pays de la Loire region)
  • Musée de l'Ardoise in Haut-Martelange / Uewermaarteleng Slate Museum L-8823, Luxembourg
  • Belgium: 6880 Bertrix

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Slate-clad cottage in the Thuringian Slate Mountains

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Boppard am Rhein: older house (natural slate)

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Slate-roofed houses in Goslar

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Church and houses in Wurzbach covered and clad with slate

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Slate retaining walls in the Hamburg Botanical Garden

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Slate with sponge and rag

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A house number made of slate

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Brilon partial view of a slate roof

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Leonaert Bramer: MORS THRIUMPHANS (painting, oil on slate)

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