Slate

Last updated

Slate
Metamorphic rock
Slate (Knife Lake Formation, metamorphism at 2.7 Ga, Neoarchean; Rt. 135 roadcut, Gilbert, Minnesota, USA) 3 (23140002749).jpg
Slate at Knife Lake Formation
Composition
Primary quartz, muscovite/illite
Secondary biotite, chlorite, hematite, pyrite Specific gravity: 2.7 – 2.8,2.9

Slate is a fine-grained, foliated, homogeneous, metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade, regional metamorphism. It is the finest-grained foliated metamorphic rock. [1] Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. [1]

Contents

The foliation in slate, called "slaty cleavage", [1] is caused by strong compression in which fine-grained clay forms flakes to regrow in planes perpendicular to the compression. [1] When expertly "cut" by striking parallel to the foliation with a specialized tool in the quarry, many slates display a property called fissility, forming smooth, flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. [1] 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.

The word "slate" is also used for certain types of object made from slate rock. It may mean a single roofing tile made of slate, or a writing slate, which was traditionally a small, smooth piece of the rock, often framed in wood, used with chalk as a notepad or notice board, and especially for recording charges in pubs and inns. The phrases "clean slate" and "blank slate" come from this usage.

Description

Slate with pyrite Slate with pyrite.JPG
Slate with pyrite

Slate is a fine-grained, metamorphic rock that shows no obvious compositional layering but can easily be split into thin slabs and plates. [2] [3] It is usually formed by low-grade regional metamorphism of mudrock. [4] [5] This mild degree of metamorphism produces a rock in which the individual mineral crystals remain microscopic in size, [5] producing a characteristic slaty cleavage in which fresh cleavage surfaces appear dull. This is in contrast to the silky cleaved surfaces of phyllite, which is the next-higher grade of metamorphic rock derived from mudstone. [6] The direction of cleavage is independent of any sedimentary structures in the original mudrock, reflecting instead the direction of regional compression. [7]

Slaty cleavage is continuous, meaning that the individual cleavage planes are too closely spaced to be discernible in hand samples. The texture of the slate is totally dominated by these pervasive cleavage planes. Under a microscope, the slate is found to consist of very thin lenses of quartz and feldspar (QF-domains) separated by layers of mica (M-domains). [8] These are typically less than 100 μm (micron) thick. [4] Because slate was formed in low heat and pressure, compared to most other metamorphic rocks, some fossils can be found in slate; sometimes even microscopic remains of delicate organisms can be found in slate. [9] [10]

The process of conversion of mudrock to slate involves a loss of up to 50% of the volume of the mudrock as it is compacted. Grains of platy minerals, such as clay minerals, are rotated to form parallel layers perpendicular to the direction of compaction, which begin to impart cleavage to the rock. Slaty cleavage is fully developed as the clay minerals begin to be converted to chlorite and mica. Organic carbon in the rock is converted to graphite. [11]

Slate is mainly composed of the minerals quartz, illite, and chlorite, which account for up to 95% of its composition. The most important accessory minerals are iron oxides (such as hematite and magnetite), iron sulfides (such as pyrite), and carbonate minerals. Feldspar may be present as albite or, less commonly, orthoclase. [12] Occasionally, as in the purple slates of North Wales, ferrous (iron(II)) reduction spheres form around iron nuclei, leaving a light-green, spotted texture. These spheres are sometimes deformed by a subsequent applied stress field into ovoids, which appear as ellipses when viewed on a cleavage plane of the specimen. However, some evidence shows that reduced spots may also form after deformation and acquire an elliptical shape from preferential infiltration along the cleavage direction, so caution is required in using reduction ellipsoids to estimate deformation. [13]

Terminology

Before the mid-19th century, the terms "slate", "shale", and "schist" were not sharply distinguished. [14] 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. [15] 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. [16]

The British Geological Survey recommends that the term "slate" be used in scientific writings only when very little else is known about the rock that would allow a more definite classification. For example, if the characteristics of the rock show definitely that it was formed by metamorphosis of shale, it should be described in scientific writings as a metashale. If its origin is uncertain, but the rock is known to be rich in mica, it should be described as a pelite. [2]

Uses

Construction

A slate roof in Cardiff, Wales St Fagans Tannery 7.jpg
A slate roof in Cardiff, Wales
A slate-faced church and homes in Wurzbach, Germany Kirche wurzbach.jpg
A slate-faced church and homes in Wurzbach, Germany
A fine slate tile work, Saint Leonhard's Church in Frankfurt am Main, Germany St.leonhard-ffm002.jpg
A fine slate tile work, Saint Leonhard's Church in Frankfurt am Main, Germany
Slates with holes at a farm in Tremedda, Cornwall, England SlateTremedda.jpg
Slates with holes at a farm in Tremedda, Cornwall, England

Slate can be made into roofing slate, a type of roof tile which are installed by a slater. Slate has two lines of breakability—cleavage and grain—which make it possible to split the stone into thin sheets. When broken, slate retains a natural appearance while remaining relatively flat and easy to stack. A series of "slate booms" occurred in Europe from the 1870s until the First World War following improvements in railway, road and waterway transportation systems. [17]

Slate is particularly suitable as a roofing material as it has an extremely low water absorption index of less than 0.4%, making the material resistant to frost damage. [18] Natural slate, which requires only minimal processing, has an embodied energy that compares favorably with other roofing materials. [19] Natural slate is used by building professionals as a result of its beauty and durability. Slate is incredibly durable and can last several hundred years, [20] often with little or no maintenance. [18] Natural slate is also fire resistant and energy efficient. [21]

Slate roof tiles are usually fixed (fastened) either with nails or with hooks (as is common with Spanish slate). [22] In the UK, fixing is typically with double nails onto timber battens (England and Wales) [23] or nailed directly onto timber sarking boards (Scotland and Northern Ireland).[ citation needed ] Nails were traditionally of copper, although there are modern alloy and stainless steel alternatives. [24] Both these methods, if used properly, provide a long-lasting weathertight roof with a lifespan of around 60–125 years. [18]

Some mainland European slate suppliers suggest that using hook fixing means that: [25]

The metal hooks are, however, visible and may be unsuitable for historic properties.

Slate tiles are often used for interior and exterior flooring, [27] stairs, [28] walkways [29] and wall cladding. [30] Tiles are installed and set on mortar and grouted along the edges. Chemical sealants are often used on tiles to improve durability and appearance, [31] increase stain resistance, [27] reduce efflorescence, and increase or reduce surface smoothness. Tiles are often sold gauged, meaning that the back surface is ground for ease of installation. [31] Slate flooring can be slippery when used in external locations subject to rain.

Slate tiles were used in 19th century UK building construction (apart from roofs) and in slate quarrying areas such as Blaenau Ffestiniog and Bethesda, Wales there are still many buildings wholly constructed of slate. Slates can also be set into walls to provide a rudimentary damp-proof membrane. Small offcuts are used as shims to level floor joists. In areas where slate is plentiful it is also used in pieces of various sizes for building walls and hedges, sometimes combined with other kinds of stone.

Other uses

Because it is a good electrical insulator and fireproof, it was used to construct early-20th-century electric switchboards and relay controls for large electric motors. [32] Because of its thermal stability and chemical inertness, slate has been used for laboratory bench tops and for billiard table tops.

Slate was used by earlier cultures as whetstone to hone knives, [33] [34] but whetstones are nowadays more typically made of quartz. [35] In 18th- and 19th-century schools, slate was extensively used for blackboards and individual writing slates, for which slate or chalk pencils were used. [32] In modern homes slate is often used as table coasters.

In areas where it is available, high-quality slate is used for tombstones and commemorative tablets. [36] In some cases slate was used by the ancient Maya civilization to fashion stelae. [37] Slate was the traditional material of choice for black Go stones in Japan, alongside clamshell for white stones. It is now considered to be a luxury. [38]

Pennsylvania slate is widely used in the manufacture of turkey calls used for hunting turkeys. The tones produced from the slate, when scratched with various species of wood striker, imitates almost exactly the calls of all four species of wild turkey in North America: eastern, Rio Grande, Osceola and Merriam's.

Extraction

The Fell Exhibition Slate Mine in Rhineland-Palatinate, Germany Bergwerk-fell-hoffnung.jpg
The Fell Exhibition Slate Mine in Rhineland-Palatinate, Germany
The historical Vogelsberg 1 pit at Fell Exhibition Slate Mine Bergwerk-fell-stollen2.jpg
The historical Vogelsberg 1 pit at Fell Exhibition Slate Mine
Mules carrying slate roof tiles on their backs in Dharamshala, India, in 1993 Mules carrying slate. Dharamsala.jpg
Mules carrying slate roof tiles on their backs in Dharamshala, India, in 1993

Slate is found in the Arctic and was used by Inuit to make the blades for ulus. China has vast slate deposits; in recent years its export of finished and unfinished slate has increased. Deposits of slate exist throughout Australia, with large reserves quarried in the Adelaide Hills in Willunga, Kanmantoo, and the Mid North at Mintaro and Spalding. Slate is abundant in Brazil, the world's second-largest producer of slate, around Papagaios in Minas Gerais, which extracts 95 percent of Brazil's slate. However, not all "slate" products from Brazil are entitled to bear the CE mark. [39]

Workers mining slate at Mintaro Quarry in Mintaro, South Australia, c. 1880 Mintaro Slate Quarry 1880.jpeg
Workers mining slate at Mintaro Quarry in Mintaro, South Australia, c. 1880

Most slate in Europe today comes from Spain, the world's largest producer and exporter of natural slate, and 90 percent of Europe's natural slate used for roofing originates from the slate industry there. Lesser slate-producing regions in present-day Europe include Wales (with UNESCO landscape status and a museum at Llanberis), Cornwall (famously the village of Delabole), Cumbria (see Burlington Slate Quarries, Honister Slate Mine and Skiddaw Slate) and, formerly in the West Highlands of Scotland, around Ballachulish and the Slate Islands in the United Kingdom. Parts of France (Anjou, Loire Valley, Ardennes, Brittany, Savoie) and Belgium (Ardennes), Liguria in northern Italy, especially between the town of Lavagna (whose name is inherited as the term for chalkboard in Italian) and Fontanabuona valley; Portugal especially around Valongo in the north of the country. Germany's Moselle River region, Hunsrück (with a former mine open as a museum at Fell), Eifel, Westerwald, Thuringia and north Bavaria; and Alta, Norway (actually schist, not a true slate). Some of the slate from Wales and Cumbria is colored slate (non-blue): purple and formerly green in Wales and green in Cumbria.

In North America, slate is produced in Newfoundland, eastern Pennsylvania, Buckingham County, Virginia, and the Slate Valley region in Vermont and New York, where colored slate is mined in the Granville, New York, area. A major slating operation existed in Monson, Maine, during the late 19th and early 20th centuries, where the slate is usually dark purple to blackish, and many local structures are roofed with slate tiles. The roof of St. Patrick's Cathedral in New York City and the headstone of John F. Kennedy's gravesite in Arlington National Cemetery are both made of Monson slate. [40]

See also

Related Research Articles

<span class="mw-page-title-main">Gneiss</span> Common high-grade metamorphic rock

Gneiss is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. This rock is formed under pressures anywhere from 2 to 15 kbar, sometimes even more, and temperatures over 300°C (572°F). Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage.

<span class="mw-page-title-main">Schist</span> Easily split medium-grained metamorphic rock

Schist is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture reflects a high content of platy minerals, such as mica, talc, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz.

<span class="mw-page-title-main">Shale</span> Fine-grained, clastic sedimentary rock

Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2Si2O5(OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite. Shale is characterized by its tendency to split into thin layers (laminae) less than one centimeter in thickness. This property is called fissility. Shale is the most common sedimentary rock.

<span class="mw-page-title-main">Metamorphic rock</span> Rock that was subjected to heat and pressure

Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than 150 to 200 °C and, often, elevated pressure of 100 megapascals (1,000 bar) or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock.

<span class="mw-page-title-main">Rock (geology)</span> Naturally occurring mineral aggregate

In geology, rock is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects.

<span class="mw-page-title-main">Quartzite</span> Hard, non-foliated metamorphic rock

Quartzite is a hard, non-foliated metamorphic rock which was originally pure quartz sandstone. Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals.

<span class="mw-page-title-main">Lithology</span> Description of the physical characteristics of a rock unit

The lithology of a rock unit is a description of its physical characteristics visible at outcrop, in hand or core samples, or with low magnification microscopy. Physical characteristics include colour, texture, grain size, and composition. Lithology may refer to either a detailed description of these characteristics, or a summary of the gross physical character of a rock. Examples of lithologies in the second sense include sandstone, slate, basalt, or limestone.

<span class="mw-page-title-main">Siltstone</span> Sedimentary rock which has a grain size in the silt range

Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.

<span class="mw-page-title-main">Phyllite</span> Type of foliated metamorphic rock

Phyllite is a type of foliated metamorphic rock formed from slate that is further metamorphosed so that very fine grained white mica achieves a preferred orientation. It is primarily composed of quartz, sericite mica, and chlorite.

<span class="mw-page-title-main">Dimension stone</span> Natural stone that has been finished to specific sizes and shapes

Dimension stone is natural stone or rock that has been selected and finished to specific sizes or shapes. Color, texture and pattern, and surface finish of the stone are also normal requirements. Another important selection criterion is durability: the time measure of the ability of dimension stone to endure and to maintain its essential and distinctive characteristics of strength, resistance to decay, and appearance.

<span class="mw-page-title-main">Greenschist</span> Metamorphic rock

Greenschists are metamorphic rocks that formed under the lowest temperatures and pressures usually produced by regional metamorphism, typically 300–450 °C (570–840 °F) and 2–10 kilobars (29,000–145,000 psi). Greenschists commonly have an abundance of green minerals such as chlorite, serpentine, and epidote, and platy minerals such as muscovite and platy serpentine. The platiness gives the rock schistosity. Other common minerals include quartz, orthoclase, talc, carbonate minerals and amphibole (actinolite).

<span class="mw-page-title-main">Mudrock</span> Type of sedimentary rock

Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone and shale. Most of the particles of which the stone is composed are less than 1⁄16 mm and are too small to study readily in the field. At first sight, the rock types appear quite similar; however, there are important differences in composition and nomenclature.

<span class="mw-page-title-main">Foliation (geology)</span> Repetitive layering in metamorphic rocks

Foliation in geology refers to repetitive layering in metamorphic rocks. Each layer can be as thin as a sheet of paper, or over a meter in thickness. The word comes from the Latin folium, meaning "leaf", and refers to the sheet-like planar structure. It is caused by shearing forces, or differential pressure. The layers form parallel to the direction of the shear, or perpendicular to the direction of higher pressure. Nonfoliated metamorphic rocks are typically formed in the absence of significant differential pressure or shear. Foliation is common in rocks affected by the regional metamorphic compression typical of areas of mountain belt formation.

<span class="mw-page-title-main">Clastic rock</span> Sedimentary rocks made of mineral or rock fragments

Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock. A clast is a fragment of geological detritus, chunks, and smaller grains of rock broken off other rocks by physical weathering. Geologists use the term clastic to refer to sedimentary rocks and particles in sediment transport, whether in suspension or as bed load, and in sediment deposits.

<span class="mw-page-title-main">Slate industry</span> Industry of the extraction and processing of slate

The slate industry is the industry related to the extraction and processing of slate. Slate is either quarried from a slate quarry or reached by tunneling in a slate mine. Common uses for slate include as a roofing material, a flooring material, gravestones and memorial tablets, and electrical insulation.

<span class="mw-page-title-main">Yorkstone</span> Variety of sandstone from Yorkshire, England

Yorkstone or York stone is a variety of sandstone, specifically from quarries in Yorkshire that have been worked since the middle ages. Yorkstone is a tight grained, Carboniferous sedimentary rock. The stone consists of quartz, mica, feldspar, clay and iron oxides.

<span class="mw-page-title-main">Cleavage (geology)</span> Planar fabric in rock

Cleavage, in structural geology and petrology, describes a type of planar rock feature that develops as a result of deformation and metamorphism. The degree of deformation and metamorphism along with rock type determines the kind of cleavage feature that develops. Generally, these structures are formed in fine grained rocks composed of minerals affected by pressure solution.

This glossary of geology is a list of definitions of terms and concepts relevant to geology, its sub-disciplines, and related fields. For other terms related to the Earth sciences, see Glossary of geography terms.

<span class="mw-page-title-main">Slate industry in Spain</span>

90% of Europes's natural slate used for roofing originates from the slate industry in Spain, with the region of Galicia being the primary source of production.

References

  1. 1 2 3 4 5 Marshak, Stephen. Essentials of Geology (3rd ed.).[ page needed ]
  2. 1 2 Robertson, S. (1999). "BGS Rock Classification Scheme, Volume 2: Classification of metamorphic rocks" (PDF). British Geological Survey Research Report. RR 99-02. Archived (PDF) from the original on 3 April 2018. Retrieved 27 February 2021.
  3. ↑ Allaby, Michael (2013). "Slate". A Dictionary of Geology and Earth Sciences (4th ed.). Oxford: Oxford University Press. ISBN   9780199653065.
  4. 1 2 Jackson, Julia A., ed. (1997). "Slate". Glossary of Geology (4th ed.). Alexandria, VA: American Geological Institute. ISBN   0922152349.
  5. 1 2 Blatt, Harvey; Tracy, Robert J. (1996). Petrology: Igneous, Sedimentary, and Metamorphic (2nd ed.). New York, NY: W.H. Freeman. p. 365. ISBN   0716724383.
  6. ↑ Yardley, B. W. D. (1989). An Introduction to Metamorphic Petrology. Harlow, Essex: Longman Scientific & Technical. p. 22. ISBN   0582300967.
  7. ↑ Potter, Paul Edwin; Maynard, J. Barry; Pryor, Wayne A. (1980). Sedimentology of Shale. New York: Springer-Verlag. p. 17. ISBN   0387904301.
  8. ↑ Fossen, Haakon (2016). Structural Geology (2nd ed.). Cambridge: Cambridge University Press. pp. 287–289. ISBN   9781107057647.
  9. ↑ BBC Video: David Attenborough: Lost Worlds, Vanished Lives
  10. ↑ Glass, Alexander; Blake, Daniel B. (April 2004). "Preservation of tube feet in an ophiuroid (Echinodermata) from the Lower Devonian Hunsrück Slate of Germany and a redescription of Bundenbachia beneckei and Palaeophiomyxa grandis". Paläontologische Zeitschrift. 78 (1): 73–95. Bibcode:2004PalZ...78...73G. doi:10.1007/BF03009131. S2CID   140689763.
  11. ↑ Yardley 1989, pp. 64, 170.
  12. ↑ Walsh, Joan A. (November 2007). "The use of the scanning electron microscope in the determination of the mineral composition of Ballachulish slate". Materials Characterization. 58 (11–12): 1095–1103. doi:10.1016/j.matchar.2007.04.013.
  13. ↑ Fossen 2016, p. 61.
  14. ↑ Raymond, R. W. (1881). "Slate". A Glossary of Mining and Metallurgical Terms. American Institute of Mining Engineers. p. 78.
  15. ↑ Fay, Albert H. (1920). "Slate". A Glossary of the Mining and Mineral Industry. United States Bureau of Mines. p. 622.
  16. ↑ Weller, J. Marvin, ed. (1960). Supplement to the Glossary of Geology and Related Sciences. American Geological Institute. p. 18.
  17. ↑ Schunck, Eberhard; Oster, Hans Jochen (2003). Roof Construction Manual Pitched Roofs (print ed.). Basel: De Gruyter. p. 12.
  18. 1 2 3 Chavez, Mark (2013). "Should I Replace My Slate Roof with a Synthetic?". National Park Service. Retrieved 28 June 2021.
  19. ↑ Crishna, N.; Banfill, P.F.G.; Goodsir, S. (October 2011). "Embodied energy and CO2 in UK dimension stone". Resources, Conservation and Recycling. 55 (12): 1265–1273. doi:10.1016/j.resconrec.2011.06.014.
  20. ↑ Cárdenes, Víctor; Cnudde, Jean Pierre; Wichert, Jörn; Large, David; López-Mungira, Aurora; Cnudde, Veerle (July 2016). "Roofing slate standards: A critical review". Construction and Building Materials. 115: 93–104. doi:10.1016/j.conbuildmat.2016.04.042.
  21. ↑ Natural Slate, the natural option Archived 10 March 2014 at the Wayback Machine
  22. ↑ "Slate Design and Fixing Guide" (PDF). SSQ Group. Retrieved 28 June 2021.
  23. ↑ "Natural roofing slate design and fixing guide" (PDF). SSQ Group. p. 8. Archived (PDF) from the original on 26 June 2019. Retrieved 28 June 2021.
  24. ↑ "6 Basic Principals of Slate Roofing". National Slate Association. 3 August 2017. Retrieved 28 June 2021.
  25. ↑ Galician and Spanish Slate website "Hook Fixing". Retrieved on 26 January 2010 archived
  26. 1 2 "Hook fixing" (PDF). SSQ Group. Archived (PDF) from the original on 26 June 2019. Retrieved 28 June 2021.
  27. 1 2 Taylor, Glenda; Vila, Bob (11 August 2016). "All You Need to Know About Slate Floors". bob vila. Action Media, Inc. Retrieved 28 June 2021.
  28. ↑ Robinson, Kristy (2 July 2012). "Installing Slate Tiles on Front Stairs". SFGate. Hearst. Retrieved 28 June 2021.
  29. ↑ "How to Lay a Walkway with Slate Pavers". doityourself. Retrieved 28 June 2021.
  30. ↑ Asaff, Sarabeth (December 2013). "How to Install Exterior Slate Tile". SFGate. Hearst. Retrieved 28 June 2021.
  31. 1 2 Lewitin, Joseph. "Everything You Need to Know About Slate Flooring Tiles". The Spruce. Dotdash. Retrieved 28 June 2021.
  32. 1 2 Bowles, Oliver (1922). The Technology of Slate. U.S. Government Printing Office.
  33. ↑ Taylor, William B. (2009). "Whetstones Found in Southeastern Massachusetts" (PDF). Bulletin of the Massachusetts Archaeological Society. 70 (2): 79–80. Archived (PDF) from the original on 28 June 2021. Retrieved 28 June 2021.
  34. ↑ Arbel, Yoav (2020). "Miscellaneous Finds from the Magen Avraham Compound, Yafo (Jaffa)". 'Atiqot. 100: 363–372. JSTOR   26954598.
  35. ↑ Adam Cherubini (12 October 2011). "What is an Oilstone?". Popular Woodworking magazine. Retrieved 22 February 2017.
  36. ↑ Born, Anne (November 1988). "Blue Slate Quarrying in South Devon: An Ancient Industry". Industrial Archaeology Review. 11 (1): 51–67. doi:10.1179/iar.1988.11.1.51.
  37. ↑ Healy, Paul F.; Awe, Jaime J.; Iannone, Gyles; Bill, Cassandra (June 1995). "Pacbitun (Belize) and ancient Maya use of slate". Antiquity. 69 (263): 337–348. doi:10.1017/S0003598X00064735. S2CID   162523022.
  38. ↑ Fairbairn, John (1992). "A Survey of the best in Go Equipment". In Bozulich, Richard (ed.). The Go Player's Almanac (2nd ed.). Kiseido Publishing Company (published 2001). pp. 142–155. ISBN   978-4-906574-40-7.
  39. ↑ Fundación Centro Tecnológico de la Pizarra. Report into the "Technical properties of Bambui Slate from the State of Minas Gerais (Brazil) to ascertain its compliance with the Standard EN12326". Brazilian Slate Report Archived 14 February 2010 at the Wayback Machine , retrieved on 27 January 2010
  40. ↑ Granville: Facts Archived 8 January 2011 at the Wayback Machine accessed 23 March 2011

Further reading


This page is based on this Wikipedia article
Text is available under the CC BY-SA 4.0 license; additional terms may apply.
Images, videos and audio are available under their respective licenses.