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  2. Jacobsville Sandstone - Wikipedia

    en.wikipedia.org/wiki/Jacobsville_Sandstone

    Jacobsville Sandstone is a red sandstone formation, marked with light-colored streaks and spots, primarily found in northern Upper Michigan, portions of Ontario, and under much of Lake Superior. Desired for its durability and aesthetics, the sandstone was used as an architectural building stone in both Canada and the United States.

  3. Red beds - Wikipedia

    en.wikipedia.org/wiki/Red_beds

    Red beds (or redbeds) are sedimentary rocks, typically consisting of sandstone, siltstone, and shale, that are predominantly red in color due to the presence of ferric oxides. Frequently, these red-colored sedimentary strata locally contain thin beds of conglomerate , marl , limestone , or some combination of these sedimentary rocks.

  4. New Red Sandstone - Wikipedia

    en.wikipedia.org/wiki/New_Red_Sandstone

    Exeter, Devon, ancient city walls of Isca Dumnoniorum with medieval and Roman elements. The New Red Sandstone, chiefly in British geology, is composed of beds of red sandstone and associated rocks laid down throughout the Permian (300 million years ago) to the end of the Triassic (about 200 million years ago), that underlie the Jurassic-Triassic age Penarth Group. [1]

  5. Dakota Formation - Wikipedia

    en.wikipedia.org/wiki/Dakota_Formation

    Over the range of the usage of the Dakota name, the unit is primarily known for its massive beds of sandstone, which commonly shows shades of red, but also gray, yellow, or white. The sand was carried and deposited by rivers or accumulated in dunes or shoreline strands, and later cemented by red iron oxide or white calcite , depending on the ...

  6. Bloomsburg Formation - Wikipedia

    en.wikipedia.org/wiki/Bloomsburg_Formation

    The Bloomsburg is defined as a grayish-red and greenish-gray claystone, argillaceous siltstone, shale, and very fine to fine-grained sandstone, [4] arranged in fining-upward cycles. [5] Although the Bloomsburg can sometimes be green to gray, its most dominant color is red and they are often called "The Bloomsburg Red Beds".

  7. Geology of Alderley Edge - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Alderley_Edge

    The Upper Mottled Sandstone – now the lower Wilmslow Member – is a medium- to coarse-grained friable false-bedded sandstone with abrupt colour changes from bright red to white. It is composed mainly of rounded grains but sub-angular grains also occur.

  8. List of sandstones - Wikipedia

    en.wikipedia.org/wiki/List_of_sandstones

    Bollingen Sandstone (also Buchberg Sandstone, Uznaberg Sandstone, Bollinger-Lehholz Sandstone and Güntliweid Sandstone): Rapperswil-Jona by the Upper Lake Zürich Grès à cailloux roulés : near Avenches

  9. Medina sandstone - Wikipedia

    en.wikipedia.org/wiki/Medina_sandstone

    Medina sandstone is a geographic subset of the Medina Group stratigraphic formation in New York State and beyond. The name refers specifically to sandstone first quarried in Medina, New York , and later quarried in other locations in Orleans County and adjacent quarries in Monroe County to the east and Niagara County to the west.