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Paleozoic Geology of the Carleton Place Area, Southern Ontario; Ontario Geological Survey, Preliminary Map P.2725, Scale 1:50 000

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Paleozoic Geology of the Carleton Place Area, Southern Ontario; Ontario Geological Survey, Preliminary Map P.2725, Scale 1:50 000 THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). Both your use of a linked Web site, and your right to use or reproduce information or materials from a linked Web site, are subject to the terms of use governing that particular Web site. Any comments or inquiries regarding a linked Web site must be directed to its Owner. Copyright: Canadian and international intellectual property laws protect the Content. Unless otherwise indicated, copyright is held by the Queen’s Printer for Ontario. It is recommended that reference to the Content be made in the following form: Williams, D.A. and Wolf R.R. 1984. Paleozoic geology of the Carleton Place area, southern Ontario; Ontario Geological Survey, Preliminary Map P.2725, scale 1:50 000. Use and Reproduction of Content: The Content may be used and reproduced only in accordance with applicable intellectual property laws. Non-commercial use of unsubstantial excerpts of the Content is permitted provided that appropriate credit is given and Crown copyright is acknowledged. Any substantial reproduction of the Content or any commercial use of all or part of the Content is prohibited without the prior written permission of MNDM. Substantial reproduction includes the reproduction of any illustration or figure, such as, but not limited to graphs, charts and maps. Commercial use includes commercial distribution of the Content, the reproduction of multiple copies of the Content for any purpose whether or not commercial, use of the Content in commercial publications, and the creation of value-added products using the Content. Contact: FOR FURTHER PLEASE CONTACT: BY TELEPHONE: BY E-MAIL: INFORMATION ON The Reproduction of MNDM Publication Local: (705) 670-5691 the EIP or Content Services Toll Free: 1-888-415-9845, ext. 5691 [email protected] (inside Canada, United States) The Purchase of MNDM Publication Local: (705) 670-5691 MNDM Publications Sales Toll Free: 1-888-415-9845, ext. 5691 [email protected] (inside Canada, United States) Crown Copyright Queen’s Printer Local: (416) 326-2678 Toll Free: 1-800-668-9938 [email protected] (inside Canada, United States) Carp 25 km Ministry of Hon. Alan W. Pope MARGINAL NOTES Minister Natural John R. Sloan Geological mapping of the Carleton Place area involved the re-examina­ Resources Deputy Minister tion of the area mapped by Wilson, Liberty and Reinhardt (1973) for the Geological Survey of Canada. The area lies partially within the Ottawa- Ontario St. Lawrence Lowland, which is characterized by Paleozoic bedrock transected by a system of normal faults striking northeast to southeast. The main physiographic feature is the Mississippi River (including Mis­ sissippi Lake), which flows generally northward through the map area. The eastern part of the area forms part of the Smiths Falls Limestone ONTARIO GEOLOGICAL SURVEY Plain (Chapman and Putnam 1951, 1966). MAP P. 2725 Paleozoic bedrock outcrop is generally abundant within the Smiths Falls Limestone Plain, and consists of areas of pavement (within which quar­ GEOLOGICAL SERIES - PRELIMINARY MAP ries have been developed). Surficial deposits consist of till (which occurs in till plains, drumlinized in PALEOZOIC GEOLOGY places), ice-contact stratified drift, marine (Champlain Sea) clay, sand, and gravel, and Recent alluvial sand and silt and organic bog deposits CARLETON PLACE AREA (Richard 1976). The Ontario Ministry of Natural Resources (Eastern Region) drilled the following wells within the map area: L-C (CP-1), drilled to a depth of 41.8 SOUTHERN ONTARIO m in Ramsay Township, (concession VIII, lot 2) (Powell and Klugman 1979; Rogers 1980, p. 38); and L-D (CP-2), drilled to 22.0 m in Ramsay Township (concession IX, lot 20) (Powell and Klugman 1979). The On­ Scale 1:50 000 tario Ministry of Transportation and Communications drilled 2 holes to a maximum depth of 10.4 m at locality Carleton Place 28 (CP-3) (Beckwith Township, concession VIII, lot 14) (Magni 1982). PRECAMBRIAN-PALEOZOIC BOUNDARY NTS Reference: 31F/1 ODM-GSC Aeromagnetic Map. 12G Precambrian rock is exposed in the western part of the map area, and the unconformably overlying Paleozoic rock is exposed in the eastern OGS Geological Compilation Map: 2418 part. Although a fault contact usually separates Precambrian and Paleo­ zoic outcrop areas, an unfaulted contact strikes generally north-south through Mississippi Lake. Bedding in the Paleozoic rock, normally close ©1984 Government of Ontario to horizontal, dips relatively steeply adjacent to contacts with Precam­ brian rock. Parts of this publication may be quoted if credit is given and the material PALEOZOIC STRATIGRAPHY is properly referenced. The logs for the Geological Survey of Canada Lebreton well (drilled in This map is published with the permission of V.G. Milne, Director, On­ the Ottawa area to the northeast), and for the Ontario Ministry of Natural tario Geological Survey. Resources (Eastern Region) L-C well, indicate that the maximum thick­ ness of Paleozoic rock occurring in the map area is approximately 240 m. The common occurrence of normal faults within the map area has resu lted in the exposure of Paleozoic rock at various levels within the sequence. Equivalent Paleozoic rock units occur in the Montreal area, and units equivalent to those of the uppermost part of the Ottawa Valley sequence occur in southern Ontario west of the Frontenac Axis. The uppermost units of the Carleton Place area are herein referred to as the Gull River Formation and the Bobcaygeon Formation (Units A to C and Unit D, re­ spectively, of Williams and Wolf 1982, p.133), in support of Liberty's (1967) recommendation that the lithostratigraphic nomenclature of the region to the west of the Frontenac Axis be applied to the Ottawa-St. Lawrence Lowland. It is recommended that the name "Ottawa" be ele­ vated to Group status. Covey Hill Formation (Cambro-Ordovician) Feldspathic conglomeratic quartz sandstone unconformably overlying the Precambrian basement, and tentatively assigned to the Covey Hill Formation (Unit 1) as proposed by Williams, Rae and Wolf (1984), occurs in areas to the east but may not exist in the Carleton Place map-area; it does not outcrop, and is absent from both wells (L-C an L-D) drilled into the Precambrian by the Ontario Ministry of Natural Resources (Eastern Region). Nepean Formation (Cambro-Ordovician) The Nepean Formation (Unit 2) (Wilson 1946, p.10-12) outcrops in sev­ eral fault blocks in the eastern part of the Carleton Place map area. The log for drillhole L-C indicates a total thickness of 31.1 m. The formation consists primarily of medium-grained well sorted quartz LEGEND sandstone. Fine-grained beds predominate in the upper part of the for­ mation, and interbeds up to a few metres thick of quartz-pebble con­ glomerate occur. The quartz grains are generally well rounded. The PHANEROZOIC fresh surface is white to light brown, and small rusty spots are common. PALEOZOIC The weathered surface ranges from pure white to dark brown to brick UPPER ORDOVICIAN red, and is usually cream to light brown. The unit is generally medium bedded, but beds range from very thin to massive (up to 2 m thick). Queenston Formation1: red to light greenish grey silt- Based on the nature of the cementing material, there are two common stone and shale, with interbeds of silty bioclastic lime­ types of sandstone: a hard quartzite (resulting from secondary quartz stone in lower part overgrowth) and a more friable rock (resulting from calcite cement). Crossbedding is common, and various types of trace fossils occur. Carlsbad Formation1: interbedded dark grey shale, The Nepean Formation is equivalent to the Cairnside Member of the fossiliferous calcareous siltstone, and silty bioclastic Chateauguay Formation of the Montreal area. limestone March Formation (Lower Ordovician) Billings Formation1: dark brown to black shale, with la­ The March Formation (Unit 3) (Wilson 1946, p.12-14) outcrops exten­ minations of calcareous siltstone sively in the eastern part of the map area. The log for drillhole L-C indi­ 1 cates a total thickness of 8.1 m. Eastview Formation : interbedded sublithographic to fine crystalline limestone and dark brown to dark grey The formation consists of interbedded quartz sandstone, sandy dolo- shale stone, and dolostone.
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