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^ Florida's state gem, moonstone, was adopted to highlight Florida's role in the United States' Lunar program, which landed the first astronauts on the Moon. [81] ^ Since 1983, Massachusetts has had 3 other official state rocks: State Historical Rock (Plymouth Rock), State Explorer Rock (Dighton Rock), and State Building and Monument Stone . In ...
Fletcher Granite Company is a granite quarry that opened in 1881 in Westford, Massachusetts. History. In 2003, the company rebuilt their rail line, ...
A block of granite in 2017 from the Fletcher Granite Company. The granite is described as a light gray or light pinkish-gray to a medium, slightly pinkish or pinkish and greenish-gray biotite granite with spots from 0.2 to 0.5 inches (5.1 to 12.7 mm) across and in some cases tapering out to 1 inch (25 mm) in length. [1]
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 "Granite Railway" was designed and built by railway pioneer Gridley Bryant and began operations on October 7, 1826. [3] The granite from these quarries became famous throughout the nation, and stone cutting quickly became Quincy's principal economic activity.
Helenite set in an earring. Helenite, also known as Mount St. Helens obsidian, emerald obsidianite, and ruby obsidianite, is a glass made from the fused volcanic rock dust from Mount St. Helens and marketed as a gemstone.
The Dedham granite was formed during the Ediacaran Period of the Precambrian era about 610 million years ago and is one of the oldest rocks in the Boston basin. [2] Dedham granites to the south and west of the basin are older outcrops from around 630 million years ago, while outcrops to the north of the basin are younger and closer to 596 million years old. [2]
Greisen fluids are formed by granites as the last highly gas- and water-rich phases of complete crystallisation of granite melts. This fluid is forced through the interstitial spaces of the granite into veins and pools at the upper margins, where boiling and rock alteration occur.