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Record #116369:
- #116369
Main publication details
MARC recordÉtudes préliminaires de la géologie du Quaternaire des régions de Big Bald Mountain et de Serpentine Lake, Nouveau-Brunswick / A. Doiron.
| Title: | Études préliminaires de la géologie du Quaternaire des régions de Big Bald Mountain et de Serpentine Lake, Nouveau-Brunswick / A. Doiron. |
| Translated title: | Preliminary studies on the Quaternary geology of the regions of Big Bald Mountain and of Serpentine Mountain, New Brunswick. |
| Author(s): | Doiron, A. |
| Date: | 1992. |
| Language: | French. |
| In: | Geological Survey of Canada. Paper. (1992.), Vol. 92-1D (1992) |
| Abstract: | Observed glacial striations suggest that Late Wisconsin glaciers flowing from west and originating from dispersion centre located in Notre Dame Mountains or ice divide in northern Maine veered to north-east in Curventon-Bathurst after contact with ice flowing from Gaspereau dispersion centre northwards, and from Escuminac dispersion centre westwards. Evidence suggests readvance towards north-east of glacier front, which might be associated with climatic deterioration during Late Dryas. |
| Notes: | Geological Survey of Canada. Paper. Vol. 92-1D :77-82 (1992). English abstract, p. 77. |
| Keywords: | 551.33 -- Glacial geology. 551.331.55 -- Rock, polished, grooved and striated by glacial action. 551.336 -- Ice ages. 551.79 -- Quaternary. 551.1/.4 -- Geology. E7 -- Glaciology: glacial geology and ice ages. (*41) -- Canada. (*415) -- New Brunswick. |
| SPRI record no.: | 116369 |
LDR 01700naa#a2200000#a#4500 001 SPRI-116369 005 20240418192656.0 007 ta 008 240418s1992####xx#ab#|##|###|0||#0|fre#d 035 ## ‡aSPRI-116369 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡afre 100 1# ‡aDoiron, A. 242 10 ‡aPreliminary studies on the Quaternary geology of the regions of Big Bald Mountain and of Serpentine Mountain, New Brunswick.‡yeng 245 10 ‡aÉtudes préliminaires de la géologie du Quaternaire des régions de Big Bald Mountain et de Serpentine Lake, Nouveau-Brunswick /‡cA. Doiron. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1992. 300 ## ‡ap. 77-82 :‡bdiag., maps. 500 ## ‡aGeological Survey of Canada. Paper. Vol. 92-1D :77-82 (1992). 500 ## ‡aEnglish abstract, p. 77. 520 3# ‡aObserved glacial striations suggest that Late Wisconsin glaciers flowing from west and originating from dispersion centre located in Notre Dame Mountains or ice divide in northern Maine veered to north-east in Curventon-Bathurst after contact with ice flowing from Gaspereau dispersion centre northwards, and from Escuminac dispersion centre westwards. Evidence suggests readvance towards north-east of glacier front, which might be associated with climatic deterioration during Late Dryas. 546 ## ‡aIn French. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.331.55 -- Rock, polished, grooved and striated by glacial action.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*415) -- New Brunswick.‡2udc 773 0# ‡7nnas ‡tGeological Survey of Canada. Paper. ‡gVol. 92-1D (1992) ‡wSPRI-16499 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418