Granite Mills
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Granite Mills
Granite Mills are two historic cotton textile mills located on Bedford Street in Fall River, Massachusetts, consisting of Granite Mill No. 2 and Granite Mill No. 3. The site was determined eligible to be listed on the National Register of Historic Places in 1983, but was omitted due to owner's objection. The mills were organized in 1863 with William Mason as president and Charles O. Shove as treasurer. The original Mill No. 1 was built 1864. It was long by wide and five stories high with a barn roof. The mill did not begin operation until January 1865, however. Mill No. 1 was destroyed by fire on September 19, 1874. Twenty three workers were killed in the disaster, and thirty three more were injured. Workers on the upper floors faced a desperate choice, either jump five stories to the ground, or be burned to death. The Granite Mill fire was widely publicized in the press and became the subject of several folk songs found throughout New England and New York (state), New York ...
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Granite Mill No 2
Granite () is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contai ...
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