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A SEDIMENTOLOGICAL AND GEOMORPHICAL INVESTIGATION OF THE PARIS MORAINE IN THE GUELPH AREA, ONTARIO, CANADA
McGill;Michael
出版年2012
英文摘要A sedimentological and geomorphologic investigation southeast of the City of Guelph, Ontario was undertaken to determine the nature, trends in distribution, and origin of subsurface sediments in the Paris moraine. Sediments were investigated by drilling five cored-holes, mapping geomorphic elements, and creating a database of existing data. Nine broadly encompassing and reoccurring lithofacies were identified, ranging from gravel to clayey silt. The general transverse trend of geomorphic elements across the moraine consists of a frontslope, hummocky, and backslope element. Sediment-landform associations were identified from the synthesis of cored-hole, geomorphic element mapping, and lithologic cross-section data. Based on these results, the Paris Moraine is thought to be the remnants of an ice-cored controlled moraine. The relief inversion process responsible for the formation of the controlled moraine creates a horizontally and vertically variable distribution of lithofacies. Hydrogeologic properties of the moraine sediments will likely be similarly spatially variable and difficult to predict. Ontario Research Fund, NSERC, OMAFRA
英文关键词Paris Moraine Moraine Sedimentology Guelph Lithofacies Hydrogeology Relief Inversion Quaternary Glacial Supraglacial End Moraine
语种英语
URLhttp://hdl.handle.net/10214/3865
资源类型学位论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/247097
推荐引用方式
GB/T 7714
McGill;Michael. A SEDIMENTOLOGICAL AND GEOMORPHICAL INVESTIGATION OF THE PARIS MORAINE IN THE GUELPH AREA, ONTARIO, CANADA[D],2012.
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