• Geology of the Forrest Kerr-Mess Creek Area, Northwestern British Columbia (Nts 104b/10, 15 & 104g/2 & 7w)

    Geology of the Forrest Kerr-Mess Creek Area, Northwestern British Columbia (Nts 104b/10, 15 & 104g/2 & 7w). James Metcalfe Logan
    Geology of the Forrest Kerr-Mess Creek Area, Northwestern British Columbia (Nts 104b/10, 15 & 104g/2 & 7w)


    Author: James Metcalfe Logan
    Date: 31 Dec 2000
    Publisher: GOVERNMENT OF BRITISH COLUMBIA
    Format: Hardback::164 pages
    ISBN10: 0772640386
    Download: Geology of the Forrest Kerr-Mess Creek Area, Northwestern British Columbia (Nts 104b/10, 15 & 104g/2 & 7w)


    Download free book Geology of the Forrest Kerr-Mess Creek Area, Northwestern British Columbia (Nts 104b/10, 15 & 104g/2 & 7w). Chapter 7 Geology 105. STUDY. Flashcards. Learn. Write. Spell. Test. PLAY. Match. Gravity. Created . Seo4015. Sediment and Sedimentary Rocks. Terms in this set (49) An area that is large enough to be mappable. Distinguishable from surrounding formations, can be composed of more than one bed. The Stikine Project: Geology of Western Telegraph Creek Map Area, Northwestern British Columbia (NTS 104G/5, 6, 11W, 12, and 13): British Columbia, Geology of the McConnell Range Serrated Peak to Jensen Creek, Parts of NTS 94E/2 and 94D/15, in Geological Fieldwork 1997: British Columbia Ministry of Energy and Mines Paper 1998 1, p. 8a-1 Geology of the Mess Lake area, northwestern British Columbia:NTS 104G/7W. Responsibility J.M. Logan and J.R. Drobe. Imprint [Victoria]:BC, Province of British Columbia, Ministry of Energy, Mines, and Petroleum Resources, Mineral Resources Division, Geological Survey Branch, [1993] (British Columbia. Geological Survey Branch);1993-6 The high-grade (8.1 million ounces of gold; 15.6 Mt grading 16.1 g/t Au; Pretium, 2016) Brucejack epithermal Au-Ag deposits are located in the Canadian Cordillera of northwestern British Columbia, and formed in association with extensive early Mesozoic island arc magmatism. Forrest Kerr Gold Project in British Columbia's Golden Triangle Region. Heart of a region called the GOLDEN TRIANGLE in northwestern British Columbia. Pretium (Brucejack), Eskay Creek, Snip, Galore Creek, Copper Canyon, Schaft Creek, According to recent geologic studies BC Geological Survey personnel, Geology of the Forrest Kerr Mess Creek area, northwestern British Columbia (NTS 104B/10, 15 and 104G/2 & 7W);. BC Ministry of Energy Geology of the Forrest Kerr-Mess Creek area, northwestern. British Columbia (NTS 104B/10, 15 & 104G/2 & 7W). (Bulletin;104). Issued Geological Survey PDF | On Jan 1, 2013, David Huntley and others published Surficial Geology, Two Island Lake, British Columbia (NTS 94O/08) The mid-Carboniferous Arctic Lake Formation, northwestern Stikine terrane, British Columbia Article (PDF Available) in Bulletin of Canadian Petroleum Geology 55(1):21-50 Structural constraints for oil and gas assessment in the Whitehorse trough: new results from seismic profiling northwestern B ritish Columbia (NTS 104B/10 GEOLOGY OF THE FORREST KERR CREEK NTS 104G/1,2,7,8,9,10; 104B/9,10,15,16; 104H/4,5,12; 104A/12,13 Lake area, northwestern British Columbia; BC Ministry of Energy, Mines and and McClelland, W.C. (2000): Geology of the Forest Kerr - Mess Creek Area. Northwestern British Columbia (104B/10,15 & 104G/2 & 7W); BC Ministry of Energy, Mines and. gold-silver-molybdenum and related deposits in northwest BC. The Delta West Grid is located on NTS Map Sheets 104A/052, 053, 062, Logan, J.M., Drobe, J.R. And McClelland, W.C., 2000, Geology of the Forest Kerr - Mess. Creek Area, Northwestern British Columbia (104B/10,15 & 104G/2 & 7W). The Forrest Kerr-Mess Creek map area straddles the boundary between the Intermontane and the Coast belts in north- west British Columbia. This region is underlain rocks comprising the western boundary of the Stikine Terrane(Stikinia). (Telegraph Creek NTS 104G/1, 2, 7, 8, 9, 10). Geology of the Forest Kerr - Mess Creek area. Northwestern British Columbia (104B/10,15 & 104G/2 & 7W). Much of today's focus on dams centers around the large dams on the main stem of the Columbia and Snake. Were dams a threat to salmon habitat before these large projects came along in the 1930s? 1900s: water storage dams were built that did not allow for the passage of salmon and didn't screen for irrigation channels so salmon ended up in fields. NTS 104G/2W Jim Logan SCALE 1:20 000 a GEOLOGY AND GEOCHEMISTRY OF THE FOREMORE AREA, MORE CREEK, NORTHWESTERN BRITISH COLUMBIA 0 1 2 Kilometres 3 4.01.1 1 10.01.1 1 Basalt Andesite/Basalt Rhyolite/Dacite Alkali Basalt Trachy-Andesite Trachyte Alkali Rhyolite Phonolite Tephri-phonolite Foidite Nb/Y Zr /T iO 2 0 20 40 60 80 100 120.5 1 10 50 Formation for rift-related and volcanic facies in the Eskay rift area. British Columbia Geological Survey, 5th Floor 1810 Blanshard St, Victoria, BC NTS 104G/1, 2; Iskut River NTS 104B/9, 10, 15, 16). In the Forest Kerr - Mess Creek area, Northwestern British Columbia. (104B/10,15 & 104G/2 & 7W).





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