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Blue chalcedony (1967) Nevada [46] [47] Metal: Silver (1977); Nevada's nickname is the Silver State: Sandstone (1987) Precious Gemstone: Virgin Valley black fire opal (1987) Semiprecious Gemstone: Nevada turquoise (1987) New Hampshire [48] Beryl (1985) Granite (1985); New Hampshire's nickname is the Granite State: Smoky quartz (1985) New Jersey ...
Baraboo Quartzite is a Precambrian geological formation [1] of quartzite, found in the region of Baraboo, Wisconsin. While pure quartzite is usually white or gray, Baraboo Quartzite is typically dark purple to maroon in color, due to the presence of iron ( hematite ) and other impurities. [ 2 ]
Prasiolite (also known as green quartz, green amethyst or vermarine) is a green variety of quartz. Since 1950, almost all natural prasiolite has come from a small Brazilian mine, [citation needed] but it has also been mined in the Lower Silesia region of Poland. Naturally occurring prasiolite has also been found in the Thunder Bay area of ...
The quartzite in the range was formed as sandstone during the Precambrian Supereon; then a greenschist phase changed it to quartzite. The monolith is located in a wayside on Wisconsin Highway 136, about 3/4 mile north of the intersection with Wisconsin Highway 154 near the village of Rock Springs.
Sioux Quartzite at Falls Park, Sioux Falls, South Dakota Cross-bedding in the Sioux Quartzite, Blue Mounds State Park, Minnesota, United States.. The Sioux Quartzite is a Proterozoic quartzite that is found in the region around the intersection of Minnesota, South Dakota, and Iowa, and correlates with other rock units throughout the upper midwestern and southwestern United States.
Viola Garfield, Seattle's Totem Poles (Bellevue, WA: Thistle Press, 1996), 9; Seattle Department of Parks and Recreation, Data on the History of Seattle Park System Vol. 4 (Seattle: Seattle Parks Department, 1978); James William Clise, "Personal Memoirs 1855-1935" Mimeograph, Altadena, California, 1935, Seattle Public Library.
History of Seattle, Washington 1900–1940: Seattle experienced rapid growth and transformation in the early 20th century, establishing itself as a leader in the Pacific Northwest. The Klondike Gold Rush led to massive immigration, diversifying the city's ethnic mix with arrivals of Japanese, Filipinos, Europeans, and European-Americans.
[5]: 7–8 The construction of the locks profoundly reshaped the topography of Seattle and the surrounding area, lowering the water level of Lake Washington and Lake Union by 8.8 feet (2.7 m), adding miles of new waterfront land, reversing the flow of rivers, and leaving piers in the eastern half of Salmon Bay high and dry. [5]
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