Geoscience Bc Summary of Activities 2014
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Hydrothermal Characteristics of the Nechako Reservoir
Hydrothermal Characteristics of the Nechako Reservoir Phase 2 Report 2006/07 Gregory A. Lawrence, Ph.D., P.Eng. 1 Roger Pieters, Ph.D. 1,2 Tel: (604) 822 5371 Tel: (604) 822 4297 [email protected] [email protected] Bernard Laval, Ph.D., P.Eng. 1 Yasmin Nassar1 Tel: (604) 822 2204 Tel: (604) 827 5367 [email protected] [email protected] Yehya Imam1 Samuel Li, Ph.D. 1 Tel: (604) 822 4853 Tel: (250) 807 8145 [email protected] [email protected] 1Department of Civil Engineering 2 Department of Earth and Ocean Sciences University of British Columbia Vancouver, B.C. V6T 1Z4 Prepared for Nechako Enhancement Society c/o Suite 850-899 West Hasting Street Vancouver B.C. V6C 2W2 August 23, 2007 Executive Summary The Nechako Enhancement Society (NES), a joint partnership of Alcan Inc. and the Province of British Columbia, is considering building a Cold Water Release Facility (CWRF) at Kenney Dam on the Nechako Reservoir. The CWRF would draw cold deep water from the reservoir to reduce the temperature of the Nechako River for fish migration. The NES has requested an assessment of the ability of the CWRF to deliver up to 170 m3/s of 10 ºC water between July 20 and August 20 (a total of 0.47 km3). We have examined the physical limnology of the two basins adjacent to Kenney Dam (Knewstubb and Natalkuz lakes). In particular, we have: • Collected temperature profiles in the summer of 2005, 2006 and 2007; these were compared with data from 1990 (Limnotek) and 1994 (Triton). -
A. Proposed Northern Gateway Pipeline Route
(A47698) September 24, 2012 Richard A. Neufeld, Q.C. Richard.Neufeld@FMC‐Law.com National Energy Board Direct: (403) 268‐70203 File No.: 15084‐281 444 ‐ 7th Avenue SW Calgary, AB T2P 0X8 Attention: Ms. Sheri Young, Secretary to the Joint Review Panel Enbridge Northern Gateway Project Dear Ms. Young: RE: Northern Gateway Pipelines Inc. Enbridge Northern Gateway Project Application of 27 May 2010 Hearing Order OH‐4‐2011 In Ruling No. 91, the Joint Review Panel directed Northern Gateway to file photomosaics of the pipeline route at a scale no greater than 1:25,000 which indicate the pipeline route, aerial extent, location and ID number of the geohazards identified in the geohazard report filed as Exhibit B 69‐7. Maps for the pipeline route from the tunnels to the Kitimat Terminal (KP 1084 to KP 1176) are attached for filing with the Panel. Due to the amount of mapping required to complete the response to this ruling, Northern Gateway anticipates filing the remaining maps (which number approximately 120) by October 5, 2012. Yours truly, Fraser Milner Casgrain LLP Richard A. Neufeld, Q.C. Partner 130°0'0"W 125°40'0"W 121°20'0"W 117°0'0"W 112°40'0"W (A47698) N Beatton River a Mason Creek ! ver s ! Ch i s REDFERN-KEILY PARK incha ga R R Sikanni Chief i (PP) v ! Iskut River e TATLATUI PARK r n R (PP) atto iv CHINCHAGA Be e r S WILDLAND k e H Pink Mountain (WPP) 88 en Thutade Lake alfw ! a a ver R y i R iv R C Manning ± Thutade Creek a n e i i ! r v m e e w r r e o 97 British Columbia k i n t A l b e r t a R o i Buick ve Wonowon ! N r ! GRAHAM - LAURIER PARK SUSTUT PARK (PP) Murdale 88 37A ! (PP) r Alaska ive Trout R 56°0'0"N Alaska Nass River ! Stewart 64 uma Bear Flat ik R Charlie Lake t ive ! ! Peace River r Attachie ! U ! " Grimshaw Fort St. -
Pleistocene Volcanism in the Anahim Volcanic Belt, West-Central British Columbia
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2014-10-24 A Second North American Hot-spot: Pleistocene Volcanism in the Anahim Volcanic Belt, west-central British Columbia Kuehn, Christian Kuehn, C. (2014). A Second North American Hot-spot: Pleistocene Volcanism in the Anahim Volcanic Belt, west-central British Columbia (Unpublished doctoral thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/25002 http://hdl.handle.net/11023/1936 doctoral thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY A Second North American Hot-spot: Pleistocene Volcanism in the Anahim Volcanic Belt, west-central British Columbia by Christian Kuehn A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY GRADUATE PROGRAM IN GEOLOGY AND GEOPHYSICS CALGARY, ALBERTA OCTOBER, 2014 © Christian Kuehn 2014 Abstract Alkaline and peralkaline magmatism occurred along the Anahim Volcanic Belt (AVB), a 330 km long linear feature in west-central British Columbia. The belt includes three felsic shield volcanoes, the Rainbow, Ilgachuz and Itcha ranges as its most notable features, as well as regionally extensive cone fields, lava flows, dyke swarms and a pluton. Volcanic activity took place periodically from the Late Miocene to the Holocene. -
Have Broken Off Herald Staff Writer Bulkley System to Produce Power for New L I L I I HAZELTON- Talks Between the Aluminum Smelters
i i J I I II LEGISLATIVE LIBHARY : . :.: . ; ,' ; : , !!:, ~ ;~? : ,~.~.' ,! . ~,~, . i PARLINE~T BUILDINGS i' '"/ .., " "!"' ! i' 'i Victoria, B.C.. • vsv ,,/ i ii ¸¸ ii "~i~'F, ;: ' ~i ................ Ilit ..... " "=-- ' = .... 'q Lq .... i d ": ": q ~ " q ; ' , q" = P ' ~ " : " q; ;' # Iq I I q~ U :t = . # ~ + . ;:/~, '=:TERRACE '" j~int action, bY the Distdct,l'pf::. : ':~Ol~ing Off Chl!dren ~ I~sy~tre~is on either s!d e ~ '~,", : :,i '~dl~ bf'~[[:.paved bie~de pdt~c'~)r i-Jdldren'to,ude " : the.pi~blem/i : : " ,. ::. ~i~: .:; :i;: ...'i ?/ •/i Tei~aC~ and:'Scli~0t'Dbtrict ~its, ~Oi~ig part oLthe• :: .the school en~ancei"/• ./:/:~::. ;: i~;' i':/• ~::' * •:/ ,'Co/mefi ~cLded atiti laat meeting to' include the ' '~/~ said the traffic: ~iind •:would;,ha!p~• :' ":,: Par.~t Adyi~ory' C qnmRtee .ltiem~l' ~. ~lk~".: "!: • ..i' ;J.teil~.: fOl" :di~CtlS,.!Onill |is I ne~t, I~dget, Tha t I~.dget " rq"~e ~r~:. ~ ~ ~pping' d~:¢hil~ e~" :i' Way to meet demands by a local ~hoc! parents gredp ,,said .the. group feels: p ,oot, economic ce~ti..ms have :,. : wiLL be discussed in January i!nd' appr@ved i n May, busy Stre~. :, I)y /~1.ow~, 'g'.t~m: t9 be' dToj~l~ left. : ,' toiimprove .the traffic situafionaround.the school,--, • .." .'l'he~Uplande Elementary Sclioul Pa~m~ ~,dvisory ~ " resu!ted in L[itt]e m~ey.balng av#ilable xer. me Wor~ .,. ' • .: For the'next school ~ear thej district a~d the board 'in the. exintlng.scbooJ parking lot, " . ..., '.... :' they wo~d like to see done at the schaol, But Baker *.. : : have gotten t~gethar'and Will be ~mstructing a traffic While the lack of ~n~..rmulting from . -
The Cheslatta Lake Suite: Miocene Mafic, Alkaline Magmatism in Central British Columbia1
Color profile: Disabled Composite Default screen 697 The Cheslatta Lake suite: Miocene mafic, alkaline magmatism in central British Columbia1 Robert G. Anderson, Jonah Resnick, James K. Russell, G.J. Woodsworth, Michael E. Villeneuve, and Nancy C. Grainger Abstract: New mapping, mineralogical, and geochemical studies help characterize late Tertiary primitive, alkaline, sodic basanite, alkali olivine basalt, transitional basalt, and diabase in the Nechako River, Whitesail Lake, and McLeod Lake map areas of central British Columbia and distinguish the Miocene Cheslatta Lake suite. The suite encompasses scattered erosional remnants of topographically distinct, columnar-jointed, olivine-phyric basalt and diabase volcanic necks, dykes, and associated lava flows north of the Anahim volcanic belt and west of the Pinchi Fault. Volcanic cen- tres at Alasla Mountain and at Cutoff Creek, near Cheslatta Lake, are proposed as type areas. Olivine, plagioclase, and pyroxene phenocrysts, megacrysts, and (or) xenocrysts; common ultramafic xenoliths; and rare but significant plutonic and metamorphic xenoliths are characteristic. Basanite, transitional basalt, and alkali olivine basalt groundmass contain plagioclase, clinopyroxene, Fe-Ti oxides, feldspathoid, olivine, and apatite. The Cheslatta Lake suite is characterized by its alkaline character, olivine-rich (>10 wt.%) normative mineralogy, and silica-undersaturated nature (>1 wt.% norma- tive nepheline; hypersthene-normative rocks are uncommon). Mg numbers vary between 72–42. Some samples encom- pass -
Ridge Subduction and Slab Window Magmatism in Western North America
Cenozoic to Recent plate confi gurations in the Pacifi c Basin: Ridge subduction and slab window magmatism in western North America J.K. Madsen*† D.J. Thorkelson* Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia V5A 1S6, Canada R.M. Friedman* Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth and Ocean Science, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada D.D. Marshall* Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia V5A 1S6, Canada ABSTRACT Keywords: tectonics, magmatism, geochro- and temporally complex and spans Paleocene to nology, forearc, slab window, ridge subduc- Miocene time. The most spatially and tempo- Forearc magmatic rocks were emplaced in tion, western North America, Cordillera. rally coherent portion is the eastward-younging a semicontinuous belt from Alaska to Oregon Sanak-Baranof Belt in southern to southeastern from 62 to 11 Ma. U-Pb and 40Ar-39Ar dating INTRODUCTION Alaska (Bradley et al., 1993; Haeussler et al., indicates that the magmatism was concur- 1995; Bradley et al., 2003). The age progres- rent in widely separated areas. Eight new Forearcs are typically amagmatic with low sion has been attributed to the passage of an conventional isotope dilution–thermal ion- heat fl ow (Gill, 1981); however, subduction of a eastwardly migrating ridge-trench-trench triple ization mass spectrometry (ID-TIMS) U-Pb mid-ocean ridge imparts a thermal pulse into the junction related to the subduction of a mid-ocean zircon ages from forearc intrusions on Van- forearc, which may result in near-trench mag- spreading ridge in Paleocene to middle Eocene couver Island (51.2 ± 0.4, 48.8 ± 0.5 Ma, 38.6 matism (Marshak and Karig, 1977; DeLong et time (Hill et al., 1981; Bradley et al., 1993; Sisson ± 0.1, 38.6 ± 0.2, 37.4 ± 0.2, 36.9 ± 0.2, 35.4 al., 1979; Sisson et al., 2003). -
Inland Ferry Services
Inland Ferry Services t Ferry routes using n Ferry routes using cable ferries l Ferry routes using reaction ferries free-running vessels 5 Harrop on the Kootenay River (propelled by the current of the river) 1 Kootenay Lake 6 Glade on the Kootenay River 10 Lytton on the Fraser River 2 Upper Arrow Lake 7 Needles on the Lower Arrow Lake 11 Big Bar on the Fraser River INSET 2 3 Francois Lake 8 Arrow Park on the Columbia River 12 Usk on the Skeena River 4 Barnston Island on the Fraser River 9 Adams Lake 13 Little Fort on the North Thompson River 14 McLure on the North Thompson River LEGEND Numbered Highways Inland Ferry Town River INSET 1 INSET 1 INSET 2 1 Hazelton New Hazelton Middle River Bulkley River 24 13 23 Alberta 16/37 Little Fort Seymour Arm 97 93 Granisle 1 Skeena River 11 95 12 Babine Lake 97 Jesmond 14 Telkwa Terrace Usk 16 Big Bar Creek McLure 9 Adams Lake Sutherland River Fort St. James Salmon River 1 16 1 Sicamous Houston 5 Galena Bay 37 Morice River Burns Lake 27 Stuart River 99 Shelter Bay 1/97 Kamloops 97B 93/95 Salmon Arm 2 Kitimat 35 Francois Lake Vanderhoof Prince George 23 31 Kootenay Bay Francois Lake Fraser Lake 16 97 97A 3 Morice Lake Ootsa Lake 5A Fraser River 12 5 Vernon Ootsa Lake 97C Arrow Park 31A 8 8 Tahtsa Lake Lytton 6 Eutsuk Lake 10 97 Whitesail Lake 31 1 Knewstubb Lake Needles Fauquier 5 95A Kelowna 97 97C Kootenay Bay 7 6 Tetachuk lake Balfour Cranbrook Blackwater River 26 5A 3A Quesnel River Lower Arrow Lake Nelson 5 97 6 Longbeach River Fraser Squamish Summerland 3A 1 Castlegar 3/95 Penticton 3A Glade 3 6 Chilcotin River 3A 33 3 Marguerite 4 3 3B 3B 21 Bella Colla River 3 Maple Ridge 3 22 Mission Williams Lake Chilliwack KM 20 Delta Abbotsford Chilko River Detailed Inland Ferry Services Map 1 2. -
GEOLOGY of the FAWNIE and NECHAKO RANGES, SOUTHERN NECHAKO PLATEAU, CENTRAL BRITISH COLUMBIA (93F/2,3,6,7) by L.J
Ministry of Employment and Investment GEOLOGY OF THE FAWNIE AND NECHAKO RANGES, SOUTHERN NECHAKO PLATEAU, CENTRAL BRITISH COLUMBIA (93F/2,3,6,7) By L.J. Diakow and I.C.L. Webster, British Columbia Geological Survey, T.A. Richards, Geological Consultant, Calgary and H.W. Tipper, Geological Survey of Canada KEYWORDS: Nechako Plateau, Nechako River, Hazelton Nechako ranges and the connected east-west trending Group, Entiako formation, Naglico formation, Nechako ridges of the Entiako Spur and Naglico Hills. The ranges volcanics, Capoose batholith, Nechako uplift, Ootsa Lake are parallel, trending northwest and rise a maximum of 950 Group. metres above the intervening Chedakuz Creek valley with a base elevation of about 900 metres. The ranges drop abruptly to a surrounding plateau characterized by thickly INTRODUCTION-- ~ ~ - 0 forested hills. The ~echakoReservoir lies just beyond the Q The southern Nechako River map area (93F) was northern terminus of the ranges, marking the northern remapped at 1:50 000 scale to update stratigraphic, plutonic boundary of the study area. and structural relationships, building upon a regional geo- Access to the area from Vanderhoof, the closest major logical base published at 1:250 000 scale (Tipper, 1963). centre, is via the Kluskus-Ootsa forest service road. This This mapping provides a modem geological framework all-weather gravel road branches onto secondary logging which better defines Jurassic and Tertiary magmatic events roads suitable for two-wheel drive vehicles and provides associated with volcanic-hosted gold-hearing epithermal access to logged areas on the upper slopes of the Nechako veins and intrusion-related copper-molybdenum minerali- Range. -
PHYSICAL and CHEMICAL VOLCANOLOGY of the EOCENE MOUNT CLISBAKO VOLCANO, CENTRAL BRITISH COLUMBIA by P
Ministry of Employment andInvemnt PHYSICAL AND CHEMICAL VOLCANOLOGY OF THE EOCENE MOUNT CLISBAKO VOLCANO, CENTRAL BRITISH COLUMBIA By P. Metcalfe, T.A. Richards, M.E. Vieneuve, J.M. White and CJ. Hickson Geological Survey of Canada Geological Survey ofCum do Contribution 1996160 KEYWORDS: Interior Plateau, British Columbia, epither- began in September 1993. The purpose was to determine mal mineralization, clisbako, eocene, volcanic centre, calc- the stratigraphic succession and petrologic relationships of alkaline, potassic, pyroxene-phyric, intermediate, felsic, the Early Tertiary felsic volcanic rocks which host epither- biotite-phyric, pyroclastic e~ption,caldera, flowdomes, mal mineralization discovered on the Baez and Clisbako 40Ar/39~Isotopic ages, palynology, geochemistry, trace claim groups (MWFILE 093C 015 and 093C 016, respec- elements, chemical models. tively), near the headwaters of the Clisbako River. Results are compared with information from Tertiary volcanic rocks exposed to the north in the Nechako River area (93F; Green andDiakow, 1993; Diakow etal., 1993; Diakow and This paper summarizes current results of reconnais- Webster, 1994) and to the south in the Taseko Lakes area sance geological mapping, sampling and petrologic analy- (920; Hickson etal., 1991; Hickson, 1992,1993; Hickson sis of Tertiary volcanic rocks in the Clisbako River area of and Higman, 1993). central British Columbia, carried out as part of the (1991- The study area is part of the Chilcotin Plateau and 1995) Canada - British Columbia Agreement on Mineral comprises four 150 000 map sheets (93B112. B113, U9, Development (van der Heyden ez al., 1993, 1995). This C/16), bounded by latiNdes 52'30"N and 53"WN and by work complements other studies in this area such as drift longitudes 123°30W and 124'30"W @gum 2). -
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TREK Mapping Project Year 2: A Structural Framework for the northern Interior Plateau J.J. Angen1, C.J.R. Hart1, J.M. Logan2, R. Kim1,M. Rahimi1 1Mineral Deposit Research Unit, The University of British Columbia, Vancouver; 2Consulting Geologist 126°W 125°W 124°W 123°W ( ( a) Preliminary Bedrock Geology of the TREK Area IV. CRETACEOUS DEFORMATION b) ( ( 4 a) 4 ( Quesnel WMC4 4 ( ( 4 350000 E 375000 E 400000 E 425000 E Stikine ( The Jurassic strata south of the Tatuk Fault were deformed during ENE- ( ( Terrane 125°30'0"W 125°0'0"W 124°30'0"W 124°0'0"W 6000000 4 ( ( Terrane 4 4 Francois !( & ! VOLCANIC AND SEDIMENTARY ROCKS OTHER FEATURES ( 5Prince 4 !(!(NIT!(HI MOUNTAIN Vanderhoof 54°0'0"N and WSW-vergent fold and thrust deformation (Figure 5a). This is likely 4 4 Lake ! ( 4 !( !(!( Miocene to Holocene City ( 4 !(!( 4 !( !( 4 4 !( 54°N Plutonic 4 4 4 George Anahim Volcanics ( ( Pinchi Fault Road Fraser-Straight Creek Fault 4 4 4 !( 4 !( !( !( Basanites to basaltic trachyandesites and trachytes 4 4 ( River related to the 700 km long fold and thrust belt that anks the east side of ? ( 4 450000 E 4 4 4 4 4 Miocene to Pliocene 4 4 ( Lake 4 4 4 4 4 ( 5975000 N Cabin 5975000 N 4 4 Chilcotin Group 4 4 4 I. INTRODUCTION 4 Lake 4 4 4 4 the Coast Belt (Rusmore and Woodsworth, 1991; Evenchick et al., 1991; VMC 4 4 Olivine basalt lava flows ( 4 4 4 4 4 4 Mineral Occurrences 4 4 4 4 4 GF 4 Eocene to Oligocene 4 4 4 !( Tatuk Fault ( 5950000 4 4 4 4 4 Porphyry Cu-Au: vein, breccia Bobtail Shear Zone 4 ") 4 4 4 The Targeting Resources through Exploration and Knowledge 4 4 Endako Group !( Schiarizza et al., 1997; Rusmore et al., 2000). -
Summary of Activities 2015, Geoscience BC, Report 2016-1, P
TREK Geological Mapping Project, Year 2: Update on Bedrock Geology and Mineralization in the TREK Project Area, Central British Columbia (parts of NTS 093B, C, F, G) J.J. Angen, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC, [email protected] J.M. Logan, Consulting Geologist, North Saanich, BC C.J.R. Hart, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC R. Kim, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC Angen, J.J., Logan, J.M., Hart, C.J.R. and Kim, R. (2016): TREK geological mapping project, year 2: update on bedrock geology and min- eralization in the TREK project area, central British Columbia (parts of NTS 093B, C, F, G); in Geoscience BC Summary of Activities 2015, Geoscience BC, Report 2016-1, p. 1–16. Introduction The Interior Plateau region of British Columbia is con- sidered to have high exploration potential as it hosts a variety of deposit types including Late Cretaceous and Eocene epithermal Au and Ag deposits (e.g., Blackwa- ter, Capoose and Wolf) and porphyry Cu and Mo depos- its (e.g., Endako and Chu) ranging in age from Late Ju- rassic to Eocene. Exploration activity has historically been hindered by a limited understanding of the charac- ter and distribution of prospective units owing to the masking effects of overlying Eocene and Neogene ba- salt flows and extensive glacial till cover. The Targeting Resources through Exploration and Knowledge (TREK) project is a Geoscience BC initiative to inte- grate geophysical, geological and geochemical data in order to improve our geological understanding and, ul- timately, reduce the risk associated with exploration in such a poorly understood region (Clifford and Hart, 2014). -
Downloaded from the Geoscience Data Repository for ESS Geophysical and Geochemical Data 3.4 CGB Distribution Data Collation
DIsTRIBuTIoN OF THE CHILc0TIN GROUP BASALTS, BRITISH COLUMBIA by JACQUELINE ANNE MARIE DOHANEY B.Sc. (Honours), Carleton University, 2006 A THESIS SUBMITTED IN PARTIAL FULLFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER IN SCIENCE in The Faculty of Graduate Studies (Geological Sciences) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) August, 2009 © Jacqueline Anne Marie Dohaney, 2009 ABSTRACT The Chilcotin Group basalts (CGB) are Oligocene to Late Pleistocene, stratified olivine-phyric basaltic lavas that overlie a large proportion of the Interior Plateau of British Columbia. The distribution of the CGB is poorly understood regionally; the current distribution is based on compilations of previously published geological maps that employ a diverse set of lithostratigraphic definitions of the Group. Exposure of the basalts is typically poor, but the thickest and most extensive sections are exposed in the valley-margins of major rivers (e.g., the Fraser River). This study collates and interprets spatial datasets and reassesses the distribution of the CGB with the intent of producing a new, more robust distribution of the CGB within the Taseko Lakes (0920) and Bonaparte Lake (092P) map areas, with the goal of better characterizing their geological history and physical volcanology. The new distribution map demonstrates several important observations: (1) the distribution of the CGB is less extensive than previous compilations by up to 48%; this implies that, regionally, the CGB is probably significantly over-estimated; (2) there are abundant,