3 edition of The trap minerals of Nova Scotia found in the catalog.
The trap minerals of Nova Scotia
|Statement||by Edwin Gilpin.|
|Series||CIHM/ICMH microfiche series -- no. 33687.|
|The Physical Object|
|Number of Pages||296|
Curatorial Report No. 90 The Nova Scotia Museum Isle Haute Expedition, July , Parrsboro ⓘ Wasson Bluff (Wasson's Bluff) Mineralogy of Nova Scotia, . Pe-Piper, G. and Miller, L. () Zeolite minerals from the North Shore of the Minas Basin, Nova Scotia. Atlantic Geology: 11– Digby Co. ⓘ Digby Gut. [Summary Report, Department of Mines, Ottawa, ] The property was acquired by the Nova Scotia Steel and Coal Company, but does not appear to be of any great extent. The mineral has many uses among which an important one is that for lining furnaces where great heat is required. Some Other Minerals
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Additional Physical Format: Print version: Gilpin, Edwin, or Trap minerals of Nova Scotia. [Place of publication not identified]: [publisher not identified], [?]. ISBN: X OCLC Number: Notes: Caption title. "Read March 7th, " Reproduction of original in: University of Toronto.
throughout the world. To the mineralogist the New Jersey trap rocks rank with similar occurrences in Nova Scotia, Iceland, and the Deccan of India for the quality and variety of their zeolites and associated minerals. The literature on the minerals of the New Jersey trap rocks is ex tensive.
Reference: How, H., () Contributions to the Mineralogy of Nova Scotia (VII. Some Triassic Trap Minerals). Some Triassic Trap Minerals). The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science: 1: Canada. From Cache Lake Country to The Loyalists Of New Brunswick, from Pulse Of the Community to The Buffalo Head, we can help you find the canada books you are looking the world's largest independent marketplace for new, used and rare books, you always get the best in service and value when you buy fromand all of your purchases are backed.
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Examples of the form of fig. 13 have been found at Chesterfiled, Mass.; they have also been brought from Nova Scotia and New Holland, in both instances attached to masses of trap rock. Perfectly transparent crystals of dodecahedral form have also been found in Nova Scotia.
The first is a very interesting, nearly rhombic crystal shown below. () On Natro-boro-calcite and another Borate occurring in the Gypsum of Nova Scotia. The American Journal of Science and Arts, Second Series, 32, () On mordenite, a new mineral from the trap of Nova Scotia.
Journal of the Chemical Society, 17, () Contributions to the Mineralogy of Nova Scotia, Pt. I, Manganite Alma mater: Royal College of Chemistry. It was discovered in by Henry How, who name it for the town of Morden, Nova Scotia, Canada, on Bay of Fundy, where it was first found.
Mordenite forms fine sprays of radial acicular crystal clusters that look like pincushions or snowballs. On top of other interesting and beautiful associated minerals, mordenite can be extremely striking.
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According to them, inthree teenagers—Daniel MacGinnis, Anthony Vaughan and John Smith—were exploring Oak Island, an uninhabited island in Mahone Bay, Nova Scotia when they noticed a depression in the ground beneath an oak tree, which is usually said to have an old rusty piece of ship’s tackle hanging from one of its branches.
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History.—Nova Scotia may well have been the Markland of early Norse and Icelandic voyages, and Cape Breton was visited by the Cabots in –, but not till was any attempt at permanent colonization made by that year an expedition was headed by a Frenchman, Pierre de Guast, Sieur de Monts (–c.
16 30), who had received. Matthew (, p. 48), a long time curator of the Natural History Society of New Brunswick, stated, "The most valuable parts of the Gesner and Institute Museum are the ethnological collections now in the lecture hall of the Natural History Society, and the collection of minerals from the Jurassic Trap of Nova Scotia, made by Dr.
Gesner. On Mordenite a New Mineral from the Trap of Nova Scotia By Prof How. Additional Experiments on the Density of Certain Minerals By A.
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