|Title||Sedimentological models of the Waterloo Moraine for groundwater applications, southern Ontario|
|Author||Russell, H A J; Sharpe, D R; Bajc, A F|
|Source||2005 Salt Lake City Annual Meeting of the Geological Society of America: abstracts; Geological Society of America, Abstracts With Programs vol. 37, no. 7, 2005 p. 144|
|Links||Online - En ligne|
|Alt Series||Earth Sciences Sector, Contribution Series 2005187|
|Meeting||Geological Society of America 2005 Annual Meeting; Salt Lake City, Utah; US; October 16-19, 2005|
|File format||htm; pdf (Adobe® Reader®)|
|Subjects||surficial geology/geomorphology; sedimentology; hydrogeology; glaciolacustrine deposits; glacial landforms; moraines; groundwater; depositional models; depositional environment; aquifers; groundwater
flow; flow structures; flow rates; flow systems; boreholes; sediments; sands; muds; gravels; depositional trends; paleohydrology; sedimentary structures; fans; Waterloo Moraine; Catfish Creek Till; diamicton|
|Abstract||Source water protection legislation in Ontario will require significant improvement in the knowledge of aquifer units with respect to distribution, extent and internal heterogeneity. Moraines form
significant recharge areas of many watersheds in southern Ontario; however, in over 100 years of mapping moraine distribution, few studies have investigated moraine composition. The Waterloo Moraine provides ~60 % of the municipal water supply of the
Waterloo Region. The groundwater system of the moraine has been extensively modeled, yet it does not have a well-defined depositional model or understanding of the flow unit geometry. |
The Waterloo Moraine covers a 400 km2 area of dissected
hummocky terrain with a circular, spoke-like arrangement of stratified ridges. The moraine consists of up to 60 m of stratified sediment that overlies the regional Late Wisconsinan Catfish Creek Till. Borehole logs of the moraine indicate that the
gross sediment composition is silty sand with lesser amounts of mud, diamicton and gravel.
Subsurface analysis indicates that gravel within the moraine is concentrated in a northwest-trending mound flanked by extensive sand deposits. Paleoflow
measurements in gravel appears to parallel the northwest-trending structure. Sediment geometry and facies are arranged in two upward and laterally fining sequences that trend from gravel to mud.
Sediment facies and sediment architecture of
shallow aggregate sections (< 25 m) suggest deposition from a few high-energy flow events. Deeper deposits are characterized by evidence of rapid sedimentation, bed aggradation, and fluidal and hyperconcentrated flows. Shallower deposits, however,
contain a higher percentage of cut and fill structures suggesting lower rates of bed aggradation that are indicative of variable meltwater discharge to the moraine. The moraine was deposited in an ice-confined conduit with lateral subaqueous fan
sedimentation. Evidence of an glacilacustrine setting is provided by horizons of mud and abundant fine-grained silty sand lateral to the main paleoflow.