Quaternary geology : Coquitlam-Port Moody area, British Columbia
During Quaternary time the Coquitlam-Port Moody area underwent two and possibly three major glaciations separated by nonglacial intervals. Each glaciation was accompanied by eustatic and isostatic sea-level changes of up to 230 m, relative to present sea level, and probably some tectonic adjustment....
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| Language: | English |
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2010
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| Online Access: | http://hdl.handle.net/2429/20068 |