Last edited by Maukasa
Tuesday, July 21, 2020 | History

3 edition of Geology of Woodburn Lake map area, District of Keewatin found in the catalog.

Geology of Woodburn Lake map area, District of Keewatin

J. A. Fraser

Geology of Woodburn Lake map area, District of Keewatin

by J. A. Fraser

  • 158 Want to read
  • 7 Currently reading

Published by Geological Survey of Canada in Ottawa, Ont .
Written in English

    Subjects:
  • Geology -- Northwest Territories -- Keewatin

  • Edition Notes

    StatementJ.A. Fraser.
    SeriesPaper (Geological Survey of Canada) -- 87-11.
    ContributionsGeological Survey of Canada
    Classifications
    LC ClassificationsCGSPAP87-11 1988
    The Physical Object
    Pagination12 p. :
    Number of Pages12
    ID Numbers
    Open LibraryOL22073291M
    ISBN 100660126419
    LC Control Number88-209584

    Full Title: Province of Manitoba, District of Keewatin, North West Territory Full Atlas Title: Middlesex County Copy 1 State: Ontario Location 1: Unattributed Location 2: Unattributed Publish Date: Publisher: H.R. Page & Co. Number Maps in the Atlas: 75 Map Original Width: " Map Original Height: " Item Number: CA Collection: Historic Map Works Rare Historic Maps Collection. The area of this data set includes the classic geology and mineral deposits of the Keweenaw Peninsula, renowned for the occurrence of great volumes of Middle Proterozoic flood basalts and the world's largest concentration of native copper. Native copper was mined there continuously from the 's to the 's. For the earlier part of that period the Keweenawan native copper district was the Author: W.F. Cannon, Michele E. McRae, S.W. Nicholson.

    Historical Weather. Below are weather averages from to according to data gathered from the nearest official weather station. The nearest weather station for both precipitation and temperature measurements is CHILOQUIN 7 NW which is approximately 14 miles away and has an elevation of 4, feet (1, feet lower than Seven Lakes Basin).Calpella, CA: mi. Ok I am biased but I much prefer North Wales to the Lake District. Don't get me wrong I understand why people love the area, the scenery,the out door pursuits (if you like that kind of thing) but I just find it a bit dull, sorry. That said I am not a great one for walking up and down hills for the sake of it. There is more variety in North Wales.

    The Keewatin River area, where the MacLellan Au-Ag and Lynn Lake Ni-Cu-Co deposits occur, contains a variety of volcanic rocks comprising basalt, andesite, dacite and rhyolite and related volcaniclastic rocks, along with sedimentary rock units. Carmacks Map; Coastal Alaska Gustavus Map; Dawson City Map; Dempster Highway Map; Faro Map; Fort Nelson British Columbia Map; Haines Alaska Map; Haines Junction Map; Inuvik Map; Juneau Maps; Ketchikan Map; Kluane Region Map; Marsh Lake Map; Mayo Map; Northwest North America; Prince of Wales Island Map; Ross River Map; Silver Trail Map; Sitka.


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Geology of Woodburn Lake map area, District of Keewatin by J. A. Fraser Download PDF EPUB FB2

The District of Keewatin was a territory of Canada and later an administrative district of the Northwest was created in by the Keewatin Act, and originally it covered a large area west of Hudsonit became a part of the Northwest Territories and inits southern parts were adjoined to the provinces of Manitoba and Ontario, leaving the remainder, now called.

Geology of the Chantrey Belt and its environs, lower Hayes River and Darby Lake map areas, northern District of Keewatin Chapter (PDF Available) January with 28 Reads How we measure 'reads'.

PDF | On Jan 1,C.M. Cunningham and others published Surficial geology of the Baker Lake area, District of Keewatin | Find, read and cite all the research you need on ResearchGate. Welcome to the Keewatin google satellite map.

This place is situated in Kenora District, Ontario, Canada, its geographical coordinates are 49° 46' 0" North, 94° 33'. Geology of High Lake-Rush Bay Area By J.

Da vies1 Introduction The map-area lies immediately north of Shoal Lake and adjacent to the Manitoba border. The proximity of the southern part of the area to Shoal Lake, and the existence of a number of minor canoe routes, have been important factors in the long history of prospecting in the Size: 9MB.

The Keewatin Region was a region of the Northwest Territories, in use as an administrative and statistical division until the creation of Nunavut in The majority of Keewatin Region fell on the Nunavut side of the boundary and was reconstituted as Kivalliq Region within the new territory, while a strip on the region's west side remaining in the NWT was transferred to Fort Smith Region.

Kenora - Head Office 4th Floor - Veterans Drive, Kenora, ON P9N 3Y5 Phone: Fax: Toll Free: Lake District Sheet 54 N - 04 W Solid Geology. Map type: Solid: Scale: Publication year: Published statement: Published Made and Published by the Ordnance Survey for the Institute of Geological Sciences.

Print code: / View map. It would be difficult in a few pages to com- bine an attempt to give a general account of the geology of the district with adequate attention to the work carried out in the last thirty years, and the reader is, therefore, referred to Geology of the Lake District (Marr, S.E.

HOLLINGWORTH ) and to the Regional Geology: Northern Cited by: Grant Lake Site, Keewatin District, Northwest Territories Books by this Author History of the Native People of Canada, Volume III (A.D. – European Contact). Flanders Lake area and the Steven-Kagiano Lake area, on the south by the Black River area and the Dayohessarah Lake area, on the west by the Manitouwadge area, and it extends as far east as Obakamiga Lake.

This present report describes the geology, structure, and economic geology of the area. Figure 1—Key map showing location of the File Size: 5MB.

Keewatin Region hotels: low rates, no booking fees, no cancellation fees. in partnership with offers highly competitive rates for all types of hotels in Keewatin Region, from affordable family hotels to the most luxurious ones.

being established inis longtime Europe’s leader in online hotel reservations. Originally published inthis book contains a condensed account of the geology of the Lake District and how geology has influenced its visible features. The text is illustrated with a number of drawings and photographs showing significant geological structures, and points of interest to the trained geologist are printed in smaller : J.

Marr. Keewahtin is southeast of Forest Lake at the southwest corner of Scandia Trail N. (MN. Highway 97) and North Shore Trail N.

There is no boat access to this lake. The area along Keewahtin Avenue is posted no parking and no boat launching. Anglers fish from shore of the shoulder of MN Hwy. 97 and.

thicker toward the rift axis which lies beneath Lake Superior north of the map area (see, for example, Ypl (Portage Lake Volcanics) in sections A-A', B-B', and C-C').

Near the rift axis the flow sequence is as much as 20 km thick but has a maximum thickness of about 10 km in the map area (Cannon and others, ).Cited by: 5. Buy The Geology of the Lake District - And Introduction by Westwood, Robert, Westwood, Robert (ISBN: ) from Amazon's Book Store. Everyday low Author: Robert Westwood.

The Lake of the Woods District Hospital is located at 21 Sylvan Street West and is directly located across from the Kenora Harbourfront.

They can be reached at The Hospital meets the immediate healthcare needs of residents of the City of Kenora, as well as a large surrounding area, including several First Nations Communities.

Lake Keewahtin. Lake Keewahtin (formerly known as Sylvan or Halfbreed Lake) is a deep lake with excellent water quality. The lake does not drain (it's landlocked) and it has rich fen floating mats south of the lake that have been identified for preservation in past studies (CLFLWD, ).

Lake Keewahtin is known for its excellent water quality. Locally a late Hemingfordian age indicated by mammalian fauna (Woodburn and Robinson, ). May include some rocks of middle Miocene age in the area west and northwest of Lakeview.

Potassium-argon ages on rocks from unit range from about 36 Ma (Swanson and Robinson, ) to about 20 Ma. At the western shore of Mono Lake we will slip into salty, alkaline waters, past tufa-coated pumice boulders, and begin a leisurely swim of about 13 miles across the surface of the lake.

After several miles we will navigate the channel between Negit and Paoha, Mono Lake's volcanic islands. The ca. – Ma Middle Sequence correlates with metasedimentary rocks, which stratigraphically overlie metavolcanic rocks in the Meadowbank area (Sequence 3 of the Woodburn Lake group), Dubawnt Lake area (Clarke River schist), and Barclay belt (Peterson,Hinchey et al.,Hinchey et al.,Pehrsson et al., ).Author: R.C.

Hunter, B. Lafrance, L.M. Heaman, G. Zaluski, D. Thomas.Borrowdale Volcanic Group, Derwentwater Independent Hostel is perfectly located for studying the oldest rocks in the Lake District. We have million years of geological history on our doorstep!

The Skiddaw Group lies to the north of the hostel, while to the south you will File Size: KB.Historical Weather. Below are weather averages from to according to data gathered from the nearest official weather station.

The nearest weather station for both precipitation and temperature measurements is ENTERPRISE 20 which is approximately 22 miles away and has an elevation of 3, feet (1, feet lower than Three Lakes Country).Dayton, NV: mi.