|Statement||[by] A. S. MacLaren [and others.|
|Series||Geological Survey of Canada. Paper 67-38, Paper (Geological Survey of Canada) ;, 67-38.|
|Contributions||MacLaren, A. S.|
|LC Classifications||QE185 .A42 no. 67-38|
|The Physical Object|
|Pagination||vii, 48 p.|
|Number of Pages||48|
|LC Control Number||79400633|
The Moose River is a river in the Hudson Plains ecozone of northern Ontario, river flows km northeast from the junction of the Mattagami and Missinaibi Rivers into James drainage basin is , square kilometres (41, sq mi) and it has a mean discharge rate of 1, cubic metres (48, cu ft). Its full length is kilometres ( mi) if counted from the head of Country: Canada. Barnett, P.J., Yeung, K.H. and McCallum, J.D. Surficial geology of the Moose River area southeast, northern Ontario; Ontario Geological Survey, Preliminary Map P, scale Use and Reproduction of Content: The EIP and the Content may be used and reproduced only in accordance with applicable intellectual property laws. One is the damming of the east branch of the Moose River at Murray Island, less than fifty miles from Moose Factory, the erection of seventeen concrete piers across the west branch of the same river for a million-dollar steel bridge, so that the Temiskaming and Northern Ontario Railway – Ontario’s publicly owned railroad – may reach Moose. In northern Ontario, sedimentary rocks occur in the Hudson Bay and Moose River basins. In southern Ontario, sedimentary rocks occur within the Michigan and Appalachian Basins. Rocks in southern Ontario were originally flat-lying, but were tilted and deformed in a southwest-northeast trending ridge (anticline) referred to as the Algonquin Arch.
Abstract Exploration in the Moose River Basin of Northern Ontario has been conducted on an intermittent basis for almost years. Reconnaissance drilling during this period by v. Tectonophysics, 46 () T T7 Eisevier Scientific Publishing Company, Amsterdam Printed in The Netherlands Letter Section A gravity survey of James Bay and its bearing on the Kapuskasing Gneiss Belt, Ontario* R.A. GIBB Gravity and Geodynamics Division, Earth Physics Branch, Department of Energy, Mines and Resources, Ottawa, Ont. K1A OY3 (Canada) (Submitted August . Silica sand potential in eastern ontario, prelim. Rpt. 1: OFR: Preliminary report on trace element geochemistry of upper ordovician rocks of central southern ontario: OFR: Aggregate resources inventory of durham, map folio: OFR: Fossil fuel program - moose river basin drilling project: OFR: Precambrian geology of harvey. The Ontario Geological Survey is pleased to provide Summary of Field Work and Other Activities, (OFR ) for electronic distribution.. Summary of Field Work and Other Activities presents highlights of, and key new information from, mapping and geoscientific research conducted during the year.. The Summary of Field Work and Other Activities, publication can be viewed, .
Improvements are coming to moose management in Ontario that will ensure sustainable populations, while making moose hunting fairer and more consistent. COVID Get the latest updates, take a self-assessment or learn about the COVID Alert exposure-notification app. Moose Hunting Northern Ontario. by Bob (Ontario) This year marked my 45th anniversary of moose hunting in Northern Ontario! I can't believe it, and we were rewarded by a lb Bull Moose, not particularly big as moose go, but a real nice one none the less. This has been our 8th animal since The Ontario Geological Survey is pleased to provide Summary of Field Work and Other Activities, (OFR ) for electronic y of Field Work and Other Activities presents highlights of, and key new information from, mapping . Phlogopitization of pyroxenite is common in contact zones between clinopyroxenites and carbonatite dikes of the Cargill ultramafic rock—carbonatite complex near Kapuskasing, Ontario. The most typical development is a mica zone 1–10 cm wide but phlogopite is also developed in a more pervasive manner throughout the groundmass of several types.