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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.
The batch of ingredients is dominated by sand, which contains silica. [1] Other ingredients such as soda ash, potash, and lime are added. [2] The batch is placed inside a pot or tank that is heated by a furnace to roughly 3090 °F (1700 °C). [1] In the glass–making industry, the melted batch is called "metal". [3]
Brown to tan in color. [23] Cranberry Opalescent 1956-1989 Mainly made in hobnail and coin dot pattern molds. [23] French Opalescent 1956-68, 1980 Also called Crystal. Clear class. Made in hobnail, Coin Dot molds, also Mandarin and Empress vases. [22] [23] Green Opalescent 1959-61 Can be a jade color to a lime green. [22] [23] Plum Opalescent ...
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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]
This pattern was produced in crystal from the 1930s until 1983. It was reissued as Maypole in the 1980s using colored glass. [58] Patterns can be a style of glass, an etching on the glass, or a cutting on the glass. [Note 10] Some of the most successful Fostoria patterns were American, Kashmir, June, Trojan, and Versailles. [55]
Framework grains are sand-sized (0.0625-to-2-millimeter (0.00246 to 0.07874 in) diameter) detrital fragments that make up the bulk of a sandstone. [ 16 ] [ 17 ] Most framework grains are composed of quartz or feldspar , which are the common minerals most resistant to weathering processes at the Earth's surface, as seen in the Goldich ...
Quartzite can have a grainy, glassy, sandpaper-like surface. Quartzite is a hard, non-foliated metamorphic rock which was originally pure quartz sandstone. [1] [2] Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts.
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