000
| 03179cem 2200457za 4500 |
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001 | 9.834452 |
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003 | CaOODSP |
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005 | 20221107150434 |
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006 | m go c f |
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007 | cr ||||||||||| |
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008 | 170818s2017 onca bd a fo 0 eng d |
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020 | |a978-0-660-08104-5 |
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034 | 1 |aa|b100000|dW0650000|eW0640000|fN0543000|gN0540000 |
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040 | |aCaOODSP|beng |
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041 | |aeng|bfre |
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043 | |an-cn-nl |
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086 | 1 |aM183-1/315-2017E-PDF |
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100 | 1 |aPaulen, Roger C., |d1970- |
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245 | 10|aSurficial geology, northwest Smallwood Reservoir, Newfoundland and Labrador, NTS 23-I southeast |h[electronic resource] / |c[authors, R.C. Paulen, J.M. Rice, and M.B. McClenaghan]. |
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250 | |aPrelim. |
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255 | |aScale 1:100,000 ; |buniversal transverse Mercator proj., zone 20 |c(W 65°00’--W 64°00'/N 54°30'--N 54°00’). |
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260 | |a[Ottawa] : |bNatural Resources Canada, Geological Survey of Canada, |c2017. |
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300 | |a1 map. : |bcol. + |e1 map information document ([7] p.). |
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490 | 1 |aCanadian geoscience map ; |v315 |
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500 | |aRelief shown by contours and shading. |
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500 | |aIncludes text, index map and location map. |
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500 | |aThis record only includes the map and the “Map information document” in PDF, the complete data set with all the files in various formats is available for free download at http://geoscan.nrcan.gc.ca/ |
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504 | |aIncludes bibliographical references. |
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520 | 3 |a"Approximately 60% of the map-area is covered by the Smallwood Reservoir, created in 1974 with the damming of the Churchill River at Churchill Falls. The terrain is of moderate relief, with higher elevation regions in the northeast that correspond to the southern extent of the Paleoproterozoic De Pas Batholith and Late Archean Orma domain intrusive rocks. Three general phases of ice flow are observed in the map-area: to the northeast, southeast, and east. Meltwater corridors and eskers crosscut the southeasterly oriented glacial landforms and drained to the southeast and east towards the former ice margin. A large shallow glacial lake filled the Smallwood Reservoir basin. This glacial lake was previously unmapped. This lake is herein informally referred to as ‘glacial Lake Low’ named after A.P. Low of the Geological Survey of Canada, who first recognized that the final disintegration of the continental ice sheet occurred in this region"--Abstract. |
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546 | |aIncludes abstract in French. |
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692 | 07|2gccst|aGeological maps |
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692 | 07|2gccst|aGeomorphology |
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692 | 07|2gccst|aSurficial geology |
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700 | 1 |aRice, J. M. |q(Jessey Murray) |
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700 | 1 |aMcClenaghan, Margaret Beth, |d1960- |
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710 | 1 |aCanada. |bNatural Resources Canada. |
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710 | 2 |aGeological Survey of Canada. |
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830 | #0|aCanadian geoscience map ;|v315.|w(CaOODSP)9.506260 |
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856 | 40|qPDF|s18.15 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1/M183-1-315-2017-eng.pdf|zMap |
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856 | 40|qPDF|s444 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1/M183-1-315-2017-1-eng.pdf|zMap information document |
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856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/300685|zGEOSCAN DOI |
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