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- Q5166740 subject Q8498844.
- Q5166740 abstract "Conway granite is a typically pink mineral-rich igneous (or mesoperthitic) biotite granite. It is amphibole-free and of coarse particle size (with portions of the rock fine-grained or porphyritic).Conway granite has a relatively high concentration of thorium, at about 56 (±6) PPM; this amount is not enough to make the granite dangerously radioactive, but it is sufficient to make the rock a low-grade (almost certainly not economic, at least in the early years) source of thorium for a thorium fuel cycle.Geologist Edward Hitchcock named the granite in 1877 after the town of Conway, New Hampshire, which is near where it is mined. The Old Man of the Mountain, a famous geologic feature in New Hampshire (which collapsed in 2003) was made of Conway granite. The formation is found throughout the lower areas of the central White Mountains, such as Franconia Notch, Crawford Notch, the center of the Pemigewasset Wilderness, and the Saco River valley. Other exposures of the formation include the Belknap Mountain Range south of Lake Winnipesaukee.".
- Q5166740 wikiPageWikiLink Q105794.
- Q5166740 wikiPageWikiLink Q1115.
- Q5166740 wikiPageWikiLink Q1156105.
- Q5166740 wikiPageWikiLink Q1508103.
- Q5166740 wikiPageWikiLink Q1556007.
- Q5166740 wikiPageWikiLink Q17159.
- Q5166740 wikiPageWikiLink Q2076159.
- Q5166740 wikiPageWikiLink Q2210898.
- Q5166740 wikiPageWikiLink Q224872.
- Q5166740 wikiPageWikiLink Q302806.
- Q5166740 wikiPageWikiLink Q322185.
- Q5166740 wikiPageWikiLink Q3374600.
- Q5166740 wikiPageWikiLink Q3774256.
- Q5166740 wikiPageWikiLink Q41177.
- Q5166740 wikiPageWikiLink Q4883048.
- Q5166740 wikiPageWikiLink Q5484708.
- Q5166740 wikiPageWikiLink Q7140503.
- Q5166740 wikiPageWikiLink Q759.
- Q5166740 wikiPageWikiLink Q8498844.
- Q5166740 comment "Conway granite is a typically pink mineral-rich igneous (or mesoperthitic) biotite granite.".
- Q5166740 label "Conway granite".