|Title||Ice flow indicators in the Timmins and Kirkland Lake areas, northeastern Ontario|
|Author||McClenaghan, M B; Veillette, J J; DiLabio, R N W|
|Source||Geological Survey of Canada, Open File 3014, 1995, 1 sheet, https://doi.org/10.4095/203616 (Open Access)|
|Links||Canadian Database of Geochemical Surveys, downloadable
|Links||Banque de données de levés géochimiques du Canada,
|Map Info.||surficial geology, landforms, 1:200,000|
|Media||paper; diskette; digital; on-line|
|File format||pdf; JPEG2000|
|NTS||42A; 32D/04; 32D/05; 32D/12; 32D/13|
|Area||Kirkland Lake; Lake Abitibi; Timmins|
|Lat/Long WENS||-82.0000 -79.5000 49.0000 48.0000|
|Subjects||surficial geology/geomorphology; eskers; glacial striations; ice movement directions; drumlinoids; glacial deposits; Munro Esker; Quaternary|
|Program||Canada-Ontario Subsidiary Agreement on Northern Ontario Development, 1991-1995|
|Released||1995 05 01|
|Abstract||The Timmins and Kirkland Lake mining camps are in the western part of the Abitibi Greenstone Belt, the world's largest greenstone belt and Canada's primary source of precious and base metals (Figure
1). Because most of the region is covered by a thick and often complex sequence of glacial deposits, till geochemistry and indicator mineral tracing are principal exploration methods. To be effective, however, these methods require an understanding
of ice flow patterns that transported mineralized material down-ice. |
Until recently, drift prospecting programs in the region relied on an ice-flow model based primarily on the orientation of striations and glacial landforms produced by the final
south and southeast ice flows that prevailed during deglaciation. The prolonged use of this simple but incomplete model may explain the disenchantment with drift prospecting methods. In later years, extensive overburden drilling for mineral
exploration and stratigraphic purposes, revealed evidence for older southwest ice flows that better explained anomalies of glacial dispersal incompatible with the first model.
Striations can reveal useful information about ice flow patterns
across the region, however, the published striation information for the region was inadequate. Most measurements on surficial geology maps record only the final south and southeast ice flows. Therefore, between 1992 and 1994, freshly stripped
outcrops on mineral exploration and mine properties and freshly exposed outcrops along lake shorelines were examined to look for evidence of older ice flows. These new measurements were combined with existing striation and fluting data from surficial
and bedrock geology maps published over the last 60 years to produce a map showing the distribution eskers, flutings and individual striations and cross-striation measurements. These data, when combined with our existing knowledge of the Quaternary
stratigraphy of the region, provide a reasonable ice flow model for drift prospecting.
From bottom to top, the Quaternary stratigraphy of the Timmins- Kirkland Lake region consists of: 1) older tills and associated sediments, one of which is a
carbonate-rich till transported south from the Hudson Bay Lowlands; 2) organic-bearing non glacial sediments of the Owl Creek Formation; 3) sandy Matheson till, deposited by ice flowing southwest, then south and finally southeast; 4) Barlow-Ojibway
glaciolacustrine deposits; 4) clay-rich Cochrane Till, in the north part of the area, deposited by south and southeastward ice flows (DiLabio et al. 1988; Veillette and McClenaghan, 1995).
Three major ice flows that predate the Cochrane
readvances are preserved in the striation record for the region (Figure 2). The oldest ice flow (blue arrow; Photos B, C, D) crossed the area towards the west-southwest (240). This flow likely is associated with the main phase of the Laurentide Ice
Sheet (Veillette and McClenaghan, 1995). Towards the end of glaciation, ice flow shifted southward (green arrows; Photos A, B,C, D). As the Laurentide Ice Sheet thinned in the final stage of glaciation, ice flow (red arrows; Photo D) shifted
southeast (120-160) towards the Harricana Moraine (Veillette, 1989). Minor shifts (red arrows) in ice flow occurred at the end of glaciation; ice flow shifted southwestward (180-200) towards the Chapleau Moraine in the Timmins area (Photo A) and
shifted eastward (120-150) in the Kirkland Lake area. All three phases of ice flow (blue, green and red) likely are associated with the deposition of Matheson Till, the youngest and most ubiquitous till sheet. Older tills that underlie Matheson Till
may be associated with older southwest or southeast ice flows (Veillette and McClenaghan, 1995), not shown in Figure 2.
Any combination of all three phases of ice flow may be preserved on an outcrop in the region. Four striated sites showing
various combinations of the three ice flow events are shown in Photos A to D. The blue, green and red ice flow arrows on the photos are associated with the blue, green and red ice flow arrows in Figure 2. These four sites are highlighted here
because they display well preserved striations and they are accessible to geologists working in the region.
Implications for Exploration
Ice flow across the region shifted through time from southwestward to southeastward. It is important to
consider all of these ice flow patterns for Matheson and older tills when using till geochemistry and indicator minerals to explore for gold, base metals and diamonds in the region. This map is the first detailed and comprehensive dataset of
striations for the Timmins - Kirkland Lake region. These data should be used for future till sampling programs as well as for reinterpreting the vast quantity of existing overburden drill hole data from previous exploration projects.