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Port Moody British Columbia

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Journal Article
Published: 11 June 2001
Canadian Journal of Earth Sciences (2001) 38 (6): 943–952.
...Olav B. Lian; Rolf W. Mathewes; Stephen R. Hicock Abstract New palynological data from peaty sediments deposited during the Port Moody Interstade, at about 18 000 14 C years, indicate that the environment in the western Fraser Lowland of British Columbia consisted of subalpine forest and parkland...
FIGURES | View All (8)
Journal Article
Published: 01 April 1985
Canadian Journal of Earth Sciences (1985) 22 (4): 498–505.
...R. F. Miller; A. V. Morgan; S. R. Hicock Abstract Samples of organic silt from post-Coquitlam Quadra sand at Port Moody and Mary Hill, British Columbia (dated at 18 300 and 18 700 years BP, respectively) were examined for insect remains and yielded small assemblages of beetles.At Port Moody species...
Journal Article
Published: 01 June 1995
Canadian Journal of Earth Sciences (1995) 32 (6): 758–767.
...Stephen R. Hicock; Olav B. Lian Abstract Sisters Creek Formation is formally defined, stratotypes are established for it, and the time–space chart is updated for the Fraser Lowland, southwestern British Columbia. The Sisters Creek is a Pleistocene formation comprising in situ and reworked organic...
Journal Article
Published: 07 January 2016
Canadian Journal of Earth Sciences (2016) 53 (3): 304–320.
... . Canadian Journal of Earth Sciences , 32 : 1194 – 1207 . 10.1139/e95-098 . Lian, O.B., Mathewes, R.W., and Hicock, S.R. 2001. Palaeoenvironmental reconstruction of the Port Moody Interstade, a nonglacial interval in southwestern British Columbia at about 18 000 14 C years BP. Canadian Journal...
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Image
Southwestern British Columbia with location of the study area. Squares represent where both Coquitlam Stade and Port Moody Interstade deposits have been discovered. The triangle represents a site where only Coquitlam Stade deposits have been observed. SC, Sisters Creek; HC, Hollyburn Creek; SV, Seymour valley; PM, Port Moody; MH, Mary Hill; SS, S&S Gravel Pit; CR, Chehalis River.
Published: 28 July 2004
Fig. 1. Southwestern British Columbia with location of the study area. Squares represent where both Coquitlam Stade and Port Moody Interstade deposits have been discovered. The triangle represents a site where only Coquitlam Stade deposits have been observed. SC, Sisters Creek; HC, Hollyburn
Image
Photograph of modern Engelmann Spruce – Subalpine Fir parkland vegetation from Mt. Stoyoma in the northernmost Cascade range of British Columbia (Fig. 1). On the ridge in the distance is a subalpine forest of fir and spruce, with herb-dominated wet meadow vegetation in the foreground. This subalpine parkland mosaic is a suggested analogue for the Port Moody Interstade.
Published: 11 June 2001
Fig. 8. Photograph of modern Engelmann Spruce – Subalpine Fir parkland vegetation from Mt. Stoyoma in the northernmost Cascade range of British Columbia (Fig.  1 ). On the ridge in the distance is a subalpine forest of fir and spruce, with herb-dominated wet meadow vegetation in the foreground
Image
Ordination, using detrended correspondence analysis, of modern pollen surface samples from coastal British Columbia (Pellatt et al. 1997), showing clustering of the five study area samples from Sisters Creek Formation near the Engelmann Spruce – Subalpine Fir zone samples, suggesting strong similarities. MH, Mary Hill; PM, Port Moody; SV, Seymour Valley; HC, Hollyburn Creek; SC, Sisters Creek. CWH, coastal western hemlock; ESSF, Engelmann spruce – subalpine fir. MH-Q, -G, -Ba, -NS, and -Be refer to mountain hemlock zones from Queen Charlotte Islands, Mount Garibaldi, Mount Baker, North Shore (Vancouver), and Berendon Bog, respectively. See Pellat et al. (1997) for locations and elevations.
Published: 11 June 2001
Fig. 7. Ordination, using detrended correspondence analysis, of modern pollen surface samples from coastal British Columbia ( Pellatt et al. 1997 ), showing clustering of the five study area samples from Sisters Creek Formation near the Engelmann Spruce – Subalpine Fir zone samples, suggesting
Journal Article
Published: 28 July 2004
Canadian Journal of Earth Sciences (2004) 41 (7): 881–895.
...Fig. 1. Southwestern British Columbia with location of the study area. Squares represent where both Coquitlam Stade and Port Moody Interstade deposits have been discovered. The triangle represents a site where only Coquitlam Stade deposits have been observed. SC, Sisters Creek; HC, Hollyburn...
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Journal Article
Published: 28 September 2001
Canadian Journal of Earth Sciences (2001) 38 (10): 1387–1401.
... that the Kechika Formation and Road River Group are broadly similar to the lithologies of the miogeoclinal succession observed east of the NRMT in northern British Columbia (Macdonald Platform) and may have originally been continuous with the Kakwa Platform to the south ( Cecile and Norford 1993 ). The lack...
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Journal Article
Published: 01 September 1981
Canadian Journal of Earth Sciences (1981) 18 (9): 1443–1451.
...Stephen R. Hicock; John E. Armstrong Abstract Coquitlam Drift is formally defined and stratotypes established for it in the Coquitlam – Port Moody area, B.C. It is a Pleistocene formation consisting of till, glaciofluvial, ice-contact, and glaciomarine sediments deposited between 21 700 and 18 700...
Journal Article
Published: 27 June 2023
Canadian Journal of Earth Sciences (2023) 60 (11): 1544–1572.
... mean 40 Ar/ 39 Ar ages to glacial events recorded in southwest British Columbia. We suggest an optimal eruption age of between 20 and 18 ka, perhaps, coinciding with the Port Moody interstade ( Lian et al. 2001 ). While there is evidence for ice-free conditions in the Fraser Lowland at this time (e.g...
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Series: GSA Field Guide
Published: 01 January 2014
DOI: 10.1130/2014.0038(01)
EISBN: 9780813756387
.... Figure 10. Columnar jointing (horizontal) in Oligocene volcanic on Great Northern Way, Vancouver. Outcrop height ~1 m. Figure 11. Lionel Jackson (left) and Devon Woods at exposure of pre-Vashon organic bed on South Schoolhouse Creek, Port Moody, British Columbia. Exposure is just above Woods...
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Journal Article
Published: 23 July 2010
Canadian Journal of Earth Sciences (2010) 47 (8): 1029–1036.
... Head. However, on the lower mainland of British Columbia the sand has been dated to between 18 300 ± 170 BP (GSC-2322) at Port Moody and 26 100 ± 320 BP (GSC-1635) at Point Grey (radiocarbon dates in Clague 1980 ). Cowichan Head Formation sediment was deposited during the Olympia Interglacial...
FIGURES
Journal Article
Published: 01 September 1921
Bulletin of the Seismological Society of America (1921) 11 (3-4): 205–217.
... University, Library of Sandai, Japan University of Arizona, Library of Tucson, Ariz. University of British Columbia, Library of Vancouver, B. C. University of Chicago, General Library of Chicago, Ill. University of California, Southern Branch, Library of 895 North Vermont Ave., Los Angeles, Cal. MEMBERS...
Journal Article
Published: 23 September 2005
Canadian Journal of Earth Sciences (2005) 42 (6): 999–1031.
... en filtrant les effets tectoniques–eustatiques globaux et régionaux et en proposant des causes pour quelques événements. [Traduit par la Rédaction] Lower Paleozoic strata that accumulated on the margin extend from southwest Alberta to northeastern British Columbia into the western Northwest...
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Journal Article
Published: 01 January 1937
Bulletin of the Seismological Society of America (1937) 27 (1): 55–71.
..., Geology Department Fayetteville, Ark. University of British Columbia, The Library . . . . . . . . Point Grey, British Columbia University of California, Geological Department . . . . . . . . . . . . . . . Berkeley, Calif. University of California at Los Angeles, Library of 405 Hilgard Ave., Los Angeles...
Journal Article
Published: 01 March 1980
Bulletin of Canadian Petroleum Geology (1980) 28 (1): 59–79.
... of British Columbia (Fulton and Halstead, 1972, p. 34; Fulton and Smith, 1978, fig. 4) and Denmark (C. Heinberg and J. M. Hansen,pers. com., 1979), and undoubtedly are common elsewhere. An example is i l lustrated in Figure 3C. These cycles are similar to coarsening-upward cycles of tectonic origin (Figs. 3A...
Journal Article
Published: 01 October 1948
Bulletin of the Seismological Society of America (1948) 38 (4): 307–330.
... British Columbia, The Library. Point Grey, British Columbia, Canada. University of California, Library . . . . . . . . . . . 405 Hilgard Ave., Los Angeles 24, Calif. University of California, Geological Sciences Dept . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Bacon Hall, Berkeley 4...
Journal Article
Journal: SEG Discovery
Published: 01 April 2013
SEG Discovery (2013) (93): 1–56.
... that the British Columbia Securities minerals are part of the national patri- subject to a range of new taxes, royal- Commission has proposed to revoke the mony. Exploration, exploitation, and ties, laws, and regulations by the gov- Northwest Exemption, which will beneficiation of minerals receive prefer- ernments...
Journal Article
Published: 01 July 1951
Bulletin of the Seismological Society of America (1951) 41 (3): 263–294.
... of Arizona, Library . . . . . . . . . . . . Tucson, Ariz. University of Arkansas, General Library Fayetteville, Ark. University of British Columbia, Library Point Grey, British Columbia, Canada. University of California, General Library, Serials Dept Berkeley 4, Calif. University of California, Library 405...