Surficial geology of Taseko Lakes map area (92-0) British Columbia by J. A. Heginbottom

Cover of: Surficial geology of Taseko Lakes map area (92-0) British Columbia | J. A. Heginbottom

Published by Department ofEnergy, Mines and Resources in Ottawa .

Written in English

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Edition Notes

Folded map in back pocket.

Book details

StatementJ.A. Heginbottom.
SeriesPaper / Geological Survey of Canada -- 72-14
ContributionsCanada. Department of Energy, Mines and Resources.
ID Numbers
Open LibraryOL14850464M

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Get this from a library. Surficial geology of Taseko Lakes map-area () British Columbia (Report, 2 figures and Map ). [J A Heginbottom]. Soils of the Taseko Lakes area, British Columbia Report No. 36 of the British Columbia Soi1 Survey K.W.G.

Valentine, W. Watt, and A.L. Bedwany. The Taseko Lakes are a pair of lakes, Upper Taseko Lake and Lower Taseko Lake, which are expansions of the upper Taseko River in the southern Chilcotin District of the Central Interior of British Columbia, Canada.

Their name is based on the original in the Chilcotin language, Dasiqox Biny, where "Desiqox" means "Mosquito River" and is cognate to the name of the river as in Location: British Columbia. This ,scale map depicts the surficial geology of the Cadotte Lake area of Alberta (NTS 84C/SE) and includes point, line and area features in GIS files.

McMartin, I. Surficial geology, Hargrave Lake, Manitoba; Geological Survey of Canada, "A" Series Map, Map A, scale:1 0. McMartin, I. Surficial geology of the Mitishto River area, Manitoba; Geological Survey of Canada, Open Filescale R i ngros e,SQ u a tyG lfhK k-HL ;Mb c dEv m.

Variability of till in the McAdam (NTS 21 G/11) map area, York County, New Brunswick. in Geoscience ResearchNB Department of Natural Resources, Miscellaneous Report Weary, G.F., Giles, T.R., Levson, V.M. and Broster, B.E. Surficial geology and Quaternary stratigraphy of the Chedakuz Creek area (NTS 93F/7).

The data were created in geodatabase format and output for public distribution in shapefile format. These data comprise the line features of Alberta Geological Survey MapSurficial Geology of the South Whitemud Lake Area (NTS 84D/NE). GEOSCAN supports the mission of Natural Resources Canada through the timely access to information.

Surficial geology, geomorpholog y, g ran ula r resource evaluation and geo ha zar d assess m ent for t he M a x ham ish Lake map area (N TS 94 -O), northea ster n.

This GIS dataset depicts the surficial geology of the Ray Lake Area (NTS 84D/NW) (GIS data, line features).

The data were created in geodatabase format and output for public distribution in shapefile format. These data comprise the line features of Alberta Geological Survey MapSurficial Geology of the Ray Lake Area (NTS 84D/NW).

This GIS dataset depicts the surficial geology of the Crooked Lake area (NTS 83K/SW) (GIS data, polygon features). The data were created in geodatabase format and output for public distribution in shapefile format. These data comprise the polygon features of Alberta Geological Survey MapSurficial Geology of the Crooked Lake Area (NTS 83K/SW).

The Surficial Geology of the Fraser Lowland, originally published by J.E. Armstrong and S.R. Hicock atscale, is released in digital format under the auspices of the Geological Survey of Canada, Vancouver Hydrogeology Program.

Surficial Geology of Charlie Lake Area Date: December Projection:UTM Zone 10N Datum: NAD 83 Scale: 1: 50 Map 2 PETREL ROBERTSON CONSULTING LTD. Compiled by: Victor M. Levson, Quaternary Geosciences Inc. GIS and Cartography by: Mike A.

Fournier, MAF Geographix, Martin Perra, Petrel Roberston Consulting Ltd. The dry matrix colors of the surficial deposits in the map area Surficial geology of Taseko Lakes map area book determined by comparison with a Munsell Soil Color Chart (Munsell Color, ). DESCRIPTION OF MAP UNITS SURFICIAL DEPOSITS Artificial fill deposits Artificial fill (latest Holocene)—Compacted and uncompacted fill mapped only beneath the Alaska Highway.

Lakes. The two large lakes in the valley are Men­ denhall and Auke. Mendenhall Lake, formed by Menden­ hall Glacier, has a maximum depth of feet and covers a surface area of about square miles.

Its maximum volume is ab acre-feet and is normally high in summer and low in the winter. TheCited by: 7. Surficial geology, Skeena River-Bulkley River area, British Columbia; Geological Survey of Canada, Map A;93 L14 Victoria Sheet. Bridge River is an east-flowing tributary of Fraser River originating in the Coast Mountains of British Columbia.

Its confluence with the Fraser River is near the village of Lillooet. This study encompasses the lower 15 miles (24 km) of Bridge River Valley. The purpose of the study is: (1) to describe and reconstruct the local Quaternary events and relate them to the regional.

The Taseko -Bridge River map area covers about square kilometres of mountainous terrain centred kilo- metres north of Vancouver. It lies between latitudes SO"45' and 5l'lS'north and longitudes "OO'and "3O'west, and covers NTS map areas /2 and /3 and portions of map areas /1,92J/14,92J/IS and 92J/ Geologic exposures in the Salt Lake City region record a long history of sedimentation and tectonic activity extending back to the Precambrian Era.

Today, the city lies above a deep, sediment-filled basin flanked by two uplifted range blocks, the Wasatch Range and the Oquirrh Mountains. The Wasatch Range is the easternmost expression of major Basin and Range.

Geoscience Map Geology of British Columbia: Parts of NTS E/5,6,9,10,11,12,13,14 and Geoscience Map GM Diakow, L.J. Geology of the Tahtsa Ranges Between Eutsuk Lake and Morice Lake Area, Whitesail Lake Map Area West-Central British Columbia (Parts of NTS 93E/5,6,) L/10, Open File OF 1.

Plate 3, Surficial Geology of Kanabec County (Mb application/pdf) Plate 4, Quaternary Stratigraphy (Mb application/pdf) Plate 5, Bedrock topography, Depth to bedrock and Sand Distribution maps (Mb application/pdf)Author: Terrence J.

Boerboom. Preliminary Geologic Map of the Sedillo Quadrangle, Bernalillo County, New Mexico By A.S. Read, B.D. Allen, G.R. Osburn, C.A. Ferguson, R.M. Chamberlin May, New Mexico Bureau of Geology and Mineral Resources Open-file Digital Geologic Map OF-GM 20 Scalethe bedrock mapping area (Matile, GS, this volume).

Bedrock and surficial mapping in the Kasmere and Putahow lakes areas was carried out to support mineral exploration activities in the region and to advance and update the currently limited understanding of the geology of a large part of Manitoba’s far northwest.

The Above: Location of presented geologic map (grey-square) in %relation to the major rift bounding faults and Lake Turkana. Geology of the Magadi Area, Kenya 0 5 10 20 30 ² Kilometers GEOLOGIC HISTORY HOLOCENE Evaporite Series ( ka): trona with interbedded clays. The Magadi Soda Company at Lake Magadi currently mines the trona.

PLEISTOCENE. CRATER LAKE WEST, OR, minute USGS topographic map Unknown Binding – January 1, by United States Geological Survey (Editor) See all formats and editions Hide other formats and editions. Enter your mobile number or email address below and we'll send you a link to download the free Kindle App.

Manufacturer: USGS. Huntley DH, Broster BE () The Late Wisconsinan deglacial history of the east-central Taseko Lakes area, British Columbia. Can J Earth Sci – CrossRef Google Scholar Huscroft CA () Surficial geology, Criss Author: Tracy A. Brennand, Andrew J.

Perkins. Geology of the Kajiado area: Degree sh S. quarter, with coloured geological map (Report - Geological Survey of Kenya ; no. 70) [F. J Matheson] on *FREE* shipping on qualifying offers. Marine Geology Map of The Vicinity of Northern Okinawa-Jima Island» Geological Map» Sedimentological Map» Appendix 1, 2, 3» Explanatory Notes Pub: Price: ¥1, No (CD) Marine Geology Map of The Vicinity of Southern Okinawa-Jima Island» Geological Map» Sedimentological Map» Appendix 1, 2, 3» Explanatory Notes Pub.

This map is the result of field investigations by DGGS in and This geologic map and report supersede the previously released Public Data File B, Preliminary interpretive bedrock geologic map of the Healy A-6 Quadrangle, southcentral Alaska. The current map has been updated to include mapping of areas adjacent to the Healy A-6 Quadrangle, newly.

Trip stops (numbered circles), population centers, and physiographic features on and around the southern Fraser Plateau. Inset shows elevation, non-synchronous Cordilleran Ice Sheet extent at local Last Glacial Maximum (white solid line; Clague and James, ), the extent of the Fraser Plateau (gray solid line; Holland, ), and the location of the main map (white dashed box).

Area extends from the Koobi Fora Ridge Road on the northwest to the edge of exposures along Kolom Malbe in the northeast, where the boundary is an arbitrary line placed through a large area of surficial deposits. The eastern boundary is along the divide between two branches of small tributary to Il Alia east of Kolom Malbe which join before.

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. Surtsey, administratively not (yet) part of the Geopark, though geologically very much so, caused an uproar of volcanism in During its formation it was already protected as a natural conservation site, and inUNESCO declared the island a World Heritage Site in recognition of the great scientific value it presented.

Below is a 20 minute documentary celebrating 50. We make available the scoreboard for soil erosion indicators including SDG Soil erosion indicator, CAP Context indicator.

A recent publication proposes the use of those indicators for agricultural, environmental, climate policies. The Taranaki Region of New Zealand is built upon the Median Batholith in the West, and Greywacke Rocks in the East.

However, no rocks older than Miocene times are visible at the surface. The dominant feature of the Taranaki Region is the andesitic stratovolcano of Mount Taranaki, which is only aboutyears dissected hill country to the East of the.

The lavas and eruptive history of Mt. Bailey, Mt. Thielsen, and Howlock Mountain are very similar, and are representative of the other High Cascade peaks in the area.

These volcanoes will be discussed in some detail, and occasional references will. part of Kutai Basin based on detail surficial mapping and laboratory analyses. It provides the valuable information to support exploration activities regarding many hydrocarbon fields located in and around this area.

The East Kutai Basin is bounded to the north by the Mangkaliat Ridge, to the south by WNW-ESE trending. Geology of the Kiandra Area Datum: G A94 Data Source: Geoscience Australia. Created Date: + The Laguna Pedernal–Salar de Aguas Calientes area lies to the immediate south of the Llullaillaco–Corrida de Cori volcanic lineament, and northwest of, and on trend with, the Antofalla volcanic complex (Fig.

1, Fig. 2).The geology is characterized by typical Neogene Andean sequences of basaltic andesite, andesite, dacite, and rhyolite lava flows and ignimbrite Cited by: The site is secure. The https:// ensures that you are connecting to the official website and that any information you provide is encrypted and transmitted securely.

The Geology and Mineral Resources of the Agros-Akrotiri Area. Geological Survey Department, Cyprus, Memoir No. 7. Published by authority of the Government of Cyprus. 88pp. with maps. Part 1: The Geology and Mineral Resources of the Agros-Apsiou Area, by L.M.

Bear; Part 2: The Geology and Mineral Resources of the Apsiou-Akrotiri Area, by S.W. Morel.Notice - The USGS Water Resources Mission Area's priority is to maintain the safety and well-being of our communities, including providing critical situational awareness in times of flooding in all 50 U.S.

states and additional territories. Our hydrologic monitoring stations continue to send data in near real-time to NWISWeb, and we are continuing critical water monitoring activities to.These rocks cover at least 10 km 2 but extend far beyond the map area and average – m in thickness hence their minimum eruptive volume would have been – km 3.

These are characteristics of super eruptions (e.g. Bryan and Ferrari, ) and jointly with the seismic data underpin our interpretation that Tana is a caldera Cited by:

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