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1 edition of Aiken Lake and Osilinka River areas. by F. Ferri [and others] found in the catalog.

Aiken Lake and Osilinka River areas. by F. Ferri [and others]

Aiken Lake and Osilinka River areas. by F. Ferri [and others]

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Published by Ministry of Energy, Mines and Petroleum Resources in Victoria .
Written in English

    Subjects:
  • Geology - British Columbia

  • Edition Notes

    11

    The Physical Object
    Pagination2 maps Scale 1:50,000 & 1:100,000
    Number of Pages100
    ID Numbers
    Open LibraryOL22020854M

    a): Geology and mineral occurrences of Quesnel Terrane, Kliyul Creek to Johanson Lake Article December with 24 Reads How we measure 'reads' Practical Guide to the Care of the Ambulatory Patient, Michael D. Stein, Fred F. Ferri, Tom J. Wachtel Friendly Matches - A Play in Two Halves!, Vicky Ireland, Allan Ahlberg, Steve Markwick,

    OSILINKA RIVER Cu Porphyry Showing 21 C DETNI CREEK OMINECA RIVER Cu Porphyry Showing 22 C HAWK (HSW) HSW Au, Cu Au-quartz veins Showing Full text of "Bibliographic index of North American archaeocyathids" See other formats

    1. Ábrahám, Levente; Mihoci, Iva; Šašić, Martina. Protokol za istraživanje danjih leptira (Lepidoptera) duž rijeke Drave // Priručnik za istraživanje bioraznolikosti duž rijeke Drave / Purger, J. Jenő (ur.). Pečuh/Pécs: Sveučilište u Pečuhu/University of Pécs, Str?sif_podr=&period= This banner text can have markup.. web; books; video; audio; software; images; Toggle navigation


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Aiken Lake and Osilinka River areas. by F. Ferri [and others] Download PDF EPUB FB2

The Aiken Lake map area inchldsss most of N TS map stu:el 94ClS together with parts of 94C16 and)4Cll2. -The Osilinka River map area includes parts of 94C’2 and 94U3 These areas are located to kilolxtres no?h~ northwest of Fon St.

James (Figure l). F oad acccs~~ i!:   References Ferri, F. (): Devono-Mississippian Felsic Volcanism Along the Western Edge of the Cassiar Terrane, North-Central British Columbia in Geological FieldworkB.C.

Ministry of Energy and Mines, Paperpages Ferri, F., Dudka, S., Rees, C. and Meldrum, D.G. (): Preliminary Geology and Geochemistry of the Aiken Lake   F 17 18 F 19 F20 F21 F 22 F27 F 28 F29 GSC Locality c c c c c C c c c c c c Ferri and Melville (In Preparation).

Arthropod, brachiopod, graptolites: Ordovician, probably Early; B.S. Norford, Personal Middle Cambrian to Permian; B.S. Norford. Personal   lake p mp qat sss whole rock samples - major oxides a of the aiken lake and osilinka river areas, british columbia nts 94c/2, 3, 5, 6 and 12 filippo ferri, steve dudka, chris rees and dan mel-drum scale (sheet 2 of 2) legend regional geochemical   Ferri,F.

et al Geology of the Uslika Lake Area: B.C. Ministry of Energy, Mines and Petroleum Resources,Open File 1 Ferri, a], a: Geology of the Aiken Lake and Osilinka River Areas, Northern Quesnel Trough (94C/2,3,5,6 &I 2); in   on the Osilinka Project during September.

The Osilinka Project is located in northeast British Columbia approximately km NW of Prince George. The property consists of nine pairs of lines, each line being 1 km in length, and separated by ://   Preliminary Geology of the Aiken Lake and Osilinka River Areas, British Columbia (NTS 94C/2,3,5,6 and 12); Ministry of Energy, Mines and Petroleum Resources, Open File MP LA MP LA MP LA MP LA e-OPx HD HPx   the soil surface but in many areas, O horizon was sampled in bogs and wet sediment the S Ferri, F., Dudka, S., Rees, C., and Meldrum, D.

(): Geology of the Aiken Lake and Osilinka River Areas, North Quesnel Trough; B.C. Ministry of Energy and Mines, Geoscience. Lehtinen, J., () Geology and Geochemical survey on the NTS YEAR PUBLICATION SCALE AUTHOR TITLE; ; Bulletin B Griffin, D.L.

The Devonian Slave Point, Beaverhill Lake, and Muskwa Formations of Northeastern British Columbia and Adjacent ?NTS=   The paper is named "Geology of the Usilika Lake Area, Northern Quesnel Trough, B.C.7'y (94C/3,4, 6) byS. Dudka and C. Rees. In Cominco Ltd. completed a reconnaissance silt and soil geochemical survey on the stratigraphic extensions of the Lower Cambrian to Middle Devonian carbonates that host the known mineral   road, which is located on the west side of Williston Lake, north for kilometres, and then west for 22 kilometres to the junction of the Osilinka and Wasi Lake Forest Access roads.

Driving another 18 kilometres along the south side of the Osilinka River on the Wasi Lake Forest access road accesses the Wasi Creek ://   smaller areas underlain by andesitic flow-rocks and intercal- ated sediments that do not exhibit the same degree of metamor- phism, and are presumably younger.

Near Uslika Lake, close to the left bank of the Osilinka River, are several exposures of bedded conglomerate, which must represent a former drainage   m m s ea lev l (0m)m C C'm sea level (0m) m m B B' D m m sea leve (0m) m m s ea lev l (0m) E E' D'm sea level (0m)   Dease Lake Geoscience Project, Part I: Geology and Mineralization of the Dease Lake (NTS J/08) and East-Half of the Little Tuya River (NTS J/07E) Map Sheets, Northern British Columbia.

In: Geological FieldworkBritish Columbia Ministry of Energy, Mines and Natural Gas, British Columbia Geological Survey Paperpp. /british-columbia-geological-survey/publications/fieldwork. Geology of the Aiken Lake and Osilinka River Areas, Northern Quesnel Trough.

In: Geological FieldworkBritish Columbia Ministry of Energy, Mines and Petroleum Resources, British Columbia Geological Survey Paperpp. /publications/papers   George F. Simmons: with portraits by Maceo Mitchell. by David Eugene Smith.

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You would be Winning praise for its free -form nature and spinning every-thing from the Ramones to the Thrills, commercial English - language Indie made room in June for a weekly program   In this area, Big Creek argillites can be traced around a broad syncline south of the Osilinka River (Figure 2).

East of Wasi Lake, anomalous levels of Pb, Zn and Ba in stream silts were reported by Ferri et al. (a) and from the RGS survey for 94C (Jackaman, ).

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GREGGS B.A., Queen's University, A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF APPLIED SCIENCE i n the Department of GEOLOGY AMD GEOGRAPHY We accept t h i s t h e s i s as