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  2. List of quarries in the United States - Wikipedia

    en.wikipedia.org/wiki/List_of_quarries_in_the...

    Walczak-Wontor Quarry Pit Workshop, near Cataract, Wisconsin, NRHP-listed. Address-restricted archeological site. Krukowski Quarry, a sandstone quarry near Mosinee, Wisconsin. It yields late Cambrian period fossils, in the course of quarrying rock slabs for countertops and other purposes.

  3. Roofing slates - Wikipedia

    en.wikipedia.org/wiki/Roofing_slates

    The world's biggest consumer of slate is France, followed by the UK, USA and Germany. In 2012, Spain produced more than 580,000 tonnes (570,000 long tons; 640,000 short tons) of slate worth about $380 million. This made it the largest slate producer in the world, followed by China and Brazil. [3]

  4. Marble Cliff Quarry Co. - Wikipedia

    en.wikipedia.org/wiki/Marble_Cliff_Quarry_Co.

    In 1985, the Kaufmans sold the 2,000-acre (8.1 km 2) quarry to investors who filled in and developed the quarry for residential use, including Marble Cliff Commons [6] [2] [3] apartments and Marble Cliff Crossing, a 100 single-family and 60 double-family subdivision built between 1998 and 2003. [7]

  5. Engineered stone - Wikipedia

    en.wikipedia.org/wiki/Engineered_stone

    The most common slab format is 3040 mm x 1440 mm for Quartz and 3050 mm x 1240 mm for Breton-based marbles, but other sizes like 3040 mm x 1650 mm are produced according to market demand. Engineered stone is non porous, [ 7 ] more flexible, and harder than many types of natural stone.

  6. Slate industry - Wikipedia

    en.wikipedia.org/wiki/Slate_industry

    Slate mines are found around the world. 90% of Europe's natural slate used for roofing originates from the Slate Industry in Spain. [1] The major slate mining region in the United Kingdom is the Lake district, with Honister slate mine being the last working slate mine, the only producers of the world famous Westmorland greenslate.

  7. Slate - Wikipedia

    en.wikipedia.org/wiki/Slate

    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.

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