Relevant bibliographies by topics / Geology - Ontario - Kamiskotia area

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Academic literature on the topic 'Geology - Ontario - Kamiskotia area'

Author: Grafiati
Published: 4 June 2021
Last updated: 9 February 2022

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Journal articles on the topic "Geology - Ontario - Kamiskotia area"

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Finamore, S. M., H. L. Gibson, and P. C. Thurston. "Archean Synvolcanic Intrusions and Volcanogenic Massive Sulfide at the Genex Mine, Kamiskotia Area, Timmins, Ontario." Economic Geology 103, no. 6 (September 1, 2008): 1203–18. http://dx.doi.org/10.2113/gsecongeo.103.6.1203.

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Tucker Barrie, C., M. P. Gorton, A. J. Naldrett, and T. R. Hart. "Geochemical constraints on the petrogenesis of the Kamiskotia gabbroic complex and related basalts, Western Abitibi Subprovince, Ontario, Canada." Precambrian Research 50, no. 3-4 (May 1991): 173–99. http://dx.doi.org/10.1016/0301-9268(91)90020-b.

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Tucker Barrie, C., and Don W. Davis. "Timing of magmatism and deformation in the Kamiskotia-Kidd Creek area, Western Abitibi subprovince, Canada." Precambrian Research 46, no. 3 (February 1990): 217–40. http://dx.doi.org/10.1016/0301-9268(90)90003-9.

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McDougall, Raymond. "Mineral Highlights from the Bancroft Area, Ontario, Canada." Rocks & Minerals 94, no. 5 (August 5, 2019): 408–19. http://dx.doi.org/10.1080/00357529.2019.1619134.

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Kile, Daniel E. "Mineralogy of the Amethyst Mines in the Thunder Bay Area, Thunder Bay, Ontario, Canada." Rocks & Minerals 94, no. 4 (June 11, 2019): 306–43. http://dx.doi.org/10.1080/00357529.2019.1595939.

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Fralick, Philip W., and Andrew D. Miall. "Sedimentology of the lower huronian supergroup (early proterozoic), Elliot lake area, Ontario, Canada." Sedimentary Geology 63, no. 1-2 (June 1989): 127–53. http://dx.doi.org/10.1016/0037-0738(89)90075-4.

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Sharpe, David R., and Peter J. Barnett. "Significance of Sedimentological Studies on the Wisconsinan Stratigraphy of Southern Ontario." Géographie physique et Quaternaire 39, no. 3 (December 4, 2007): 255–73. http://dx.doi.org/10.7202/032607ar.

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ABSTRACTDetailed facies mapping along Lake Erie and Lake Ontario Bluffs, plus other studies illustrate that sedimentological studies, especially those with geomorphic or landform control, have had three main effects on the Wisconsinan stratigraphy of Ontario: (1) improved understanding of depositional processes and environments of several major rock stratigraphic units, without altering the stratigraphic framework, (2) aided correlation of drift sequences, and (3) questioned previous interpretations and stratigraphic correlations of drift sequences. Thus sedimentological analysis can not be separated from stratigraphy because the interpretation of depositional environnments of many mapped strata relies on their geometry and the inclusion of regional data. The geomorphic control provided by sedimentological study of surface landforms is also important because assessment of older buried sediments such as those at the Scarborough Bluffs has been hampered by the failure to determine landform control. The Late Wisconsinan stratigraphy of Southern Ontario generally remains unchanged, except for questions on the role of climate versus ice margin dynamics. The pre-Late Wisconsinan stratigraphy is scarce and not well defined, yet sedimentary studies support the presence of glacial ice in the Ontario Lake basin for all of the Middle Wisconsinan and possibly earlier, including the formation of the Scarborough delta. Large channel cut and fill sequences in the Toronto area (Pottery Road Formation), initially interpreted as resulting from subaerial erosion, were probably formed by subaqueous or subglacial meltwater erosion. If so, the pre-Late Wisconsinan stratigraphy in southern Ontario changes because the Pottery Road Formation may not be an Early Wisconsinan correlative of the St. Pierre beds. The channel example illustrates that stratigraphie correlation without sedimentological investigations may be misleading.
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Motazedian, Dariush, and James Hunter. "Development of an NEHRP map for the Orleans suburb of Ottawa, Ontario." Canadian Geotechnical Journal 45, no. 8 (August 2008): 1180–88. http://dx.doi.org/10.1139/t08-051.

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The average shear-wave velocity to a depth of 30 m (Vs30) has been obtained for 73 sites in the Orleans area in the northeast part of the City of Ottawa. Measurements of Vs30 were made using both ground surface reflection and refraction methods. In addition, borehole data was used to estimate Vs versus depth profiles using average Vs values assigned to distinct geological units. High values of Vs (>1500 m/s) were obtained in areas of thin surficial sediments overlying Paleozoic bedrock, and low Vs values (<180 m/s) were calculated in areas of thick late–post-glacial clay. The Vs30 values have been used to prepare an NEHRP map for the study area. Much of the suburb of Orleans is classified as NEHRP zone E, whereas the perimeter areas and some isolated central areas are classified as zones ranging from zone D to zone A. The presence of thick unconsolidated late–post-glacial sediments deposited in the Champlain Sea is the main contributing factor to the wide range of average shear-wave velocities in the study area.
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Mohajer, Arsalan A. "Seismicity and Seismotectonics of the Western Lake Ontario Region." Géographie physique et Quaternaire 47, no. 3 (November 23, 2007): 353–62. http://dx.doi.org/10.7202/032963ar.

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ABSTRACTThe western Lake Ontario region, a traditionally perceived area of low seismic risk, is densely populated and is home to, among other critical facilities, the nuclear reactors of Pickering and Darlington. These and other characteristics of the region call for improved estimates of seismic hazard. Due to a lack of understanding of the causative geological sources and recurrence characteristics of the reported seismic activity, there is considerable uncertainty regarding estimated ground motion parameters, a fundamental component of seismic hazard assessments. To attempt to improve the definition of the seismic source zones and, consequently, seismic hazard assessments, the hypocentres of about 30 local earthquakes were recomputed. A new data compilation, based on the revised locations or those with the least travel-time residuals, shows that local microearthquakes (ML"3.5) generally occur along, or at the intersection of, prominent aeromagnetic or gravity anomalies. A notable seismicity trend extends in a northeast-southwest direction between Toronto and Hamilton, and is bounded by magnetic lineaments. A major geological structure, the Central Metasedimentary Belt Boundary Zone (CMBBZ), coincides with a strong aeromagnetic anomaly which extends to the northeast into the Western Québec Seismic Zone. This magnetic lineament also extends to the south, across Lake Ontario, to join the Akron (Ohio) magnetic boundary that was associated with several historical earthquakes and with a mb=4.9 earthquake in 1986. Most of the seismic events recorded instrumentally in the 20th century have occurred within a depth range of 5 to 20 km. This observation supports the correlation of local earthquakes with deep geophysical and geological features, suggesting contemporary reactivation of basement structures. This may imply that a more conservative deterministic hazard estimate is needed to verify the probabilistic approach currently used to assess seismic hazard in southern Ontario.
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Cooper, A. J. "Waste disposal site selection techniques in Quaternary terraine Ontario, Canada." Geological Society, London, Engineering Geology Special Publications 7, no. 1 (1991): 211–17. http://dx.doi.org/10.1144/gsl.eng.1991.007.01.19.

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AbstractThick and predictable deposits of fine grained Quaternary materials have been used for the siting of waste management facilities in Ontario. The search for such sites is founded on the application of techniques in Quaternary geology and hydrogeology. Two examples are presented. Oxford County is located southwest of Toronto in an area of parallel morainic ridges separated by flat till plains. Conventional wisdom would focus on the till plains for thick, consistent fine grained Quaternary Sediments. However, the careful analysis of the Quaternary stratigraphy and glacial history revealed that better sites are located along the moraines. A site on the Ingersoll Moraine was studied in detail and defended at a public hearing. Concerns about the geology of the materials were allayed by the confirmation of homogeneous clayey silt materials exposed when the site opened in late 1986. A much wider ranging search was undertaken for a major hazardous and liquid industrial waste treatment and disposal facility for the Province of Ontario. Progressively more detailed investigations of the Quaternary geology were used to assist a multi-disciplinary site selection team. Initial interpretations covered an area of 75 000 km2 at a scale of 1:250 000. Eight candidate sites were then selected for further investigation with five continuously sampled stratigraphic boreholes. The chosen site is located in a depression in the bedrock filled with 40 m of glaciolacustrine clayey silt. Site specific hydrogeological and geotechnical studies were integrated with a detailed geological investigation.
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Dissertations / Theses on the topic "Geology - Ontario - Kamiskotia area"

1

Brown, Julie Louise. "Neoarchean evolution of the western-central Wabigoon boundary zone, Brightsand Forest Area, Ontario." Thesis, University of Ottawa (Canada), 2002. http://hdl.handle.net/10393/6451.

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The boundary between the western and central domains of the Wabigoon subprovince has been considered to represent a ca. 2.7 Ga suture between juvenile Neoarchean volcanic rocks in the west and granitoid rocks with Mesoarchean ancestry in the central Wabigoon. The nature and timing of interaction between these two terranes was examined southeast of the Sturgeon Lake greenstone belt within the central Wabigoon, where amphibolite-facies supracrustal remnants are dismembered by Neoarchean plutonic rocks and shear zones. Of the 4 preserved ductile deformation fabrics, D1 and D2 are bracketed by a 2718 +/- 7 Ma tonalite gneiss and crosscutting 2715 Ma tonalite dyke. The main penetrative S3 foliation affects most units, including quartz-rich sandstone deposited after 2701 Ma. A 2697 Ma granodiorite dyke cutting S3 in mafic and metasedimentary rocks provides a lower bracket on D3. Regional implications can be drawn from the observation of 2725--2715 Ma D1 and D2 deformation events in the central Wabigoon. These constraints overlap with an early deformation event in the Pipestone Lake area of the western Wabigoon (2727--2712 Ma; Edwards and Stauffer, 1999). (Abstract shortened by UMI.)
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Leblanc, Genevieve. "Geology and mineralization in the Big Four Lake area, Shining Tree, Abitibi greenstone belt, Ontario." Thesis, University of Ottawa (Canada), 2008. http://hdl.handle.net/10393/27699.

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The purpose of the research work (in partnership with the Ontario Geological Survey (OGS) and International KRL Resources Corp. (KRL)) was to better define the geology and mineralization of the Big Four Lake area, close to Shining Tree in Ontario, part of the southwesthern Abitibi greenstone belt. Rocks of the area belong to the Deloro assemblage a suite of calc-alkaline mafic to felsic metavolcanic rocks, tholeiitic mafic to intermediate metavolcanic rocks, iron formation plus komatiites of the Kidd-Munro and Pacaud assemblages, all cut by later intrusions. The rocks are metamorphosed to the greenschist facies and for the most part are only slightly deformed. A 1:10,000 scale geological map was produced in order to characterize the distribution of Deloro assemblage rocks and the Proterozoic intrusions. Seven different units were defined: (1) Mafic to intermediate metavolcanic rocks, (2) South rhyolite, (3) Volcanoclastic rocks, (4) Red Dome rhyolite, (5) Sulfide---rich chemical metasedimentary rocks, (6) Matachewan dike swarm, and (7) Nipissing gabbro. Major and trace element geochemistry shows that unit 1 rocks are tholeiitic whereas units 2 and 4 are calc-alkaline. Accordingly the Deloro assemblage rocks (units 1 to 5) are interpreted to have formed in a back-arc setting. The mafic to intermediate metavolcanic rocks have affinities with N-type MORB and a volcanic-arc environment. In the field, the Red Dome rhyolite has a characteristic hematization whereas the South rhyolite is strongly sericitized and has conspicuous alkali feldspar phenocrysts. Based on the presence of columnar jointing, autoclastic fades, and its massive form, the Red Dome rhyolite is interpreted to be a dome. The South rhyolite was earlier interpreted to be pyroclastic because of the presence of pumice fragments in a breccia that surrounds massive facies. However, there is no evidence of explosive and hot emplacement, and there are red chert clasts within the breccia which is itself located close to a conglomerate containing fragments of the South rhyolite. Because these two facies surround massive rhyolite, the South rhyolite is also interpreted to be a dome. Mineralization is characterized by pyrite, chalcopyrite, magnetite, hematite, malachite in quartz and carbonate veins that cut the Red Dome rhyolite. Exploration in the area focused on this mineralization because it was thought to be a VMS environment. The chlorite mineral chemistry is relatively iron-rich consistent with a metamorphic rather than hydrothermal origin and the rhyolites are not the Fill type typical of VMS. It is concluded that the mineralization may have been hydrothermal, possibly from a small, or aborted, VMS system, or related to later regional felsic intrusions or even the Proterozoic intrusions, which may have provided heat to remobilize metals.
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Chow, Andre M. C. (Andre Mu-Chin). "Sedimentology and paleontology of the Attawapiskat Formation (Silurian) in the type area, northern Ontario." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65494.

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Smyk, Mark Cory 1961 Carleton University Dissertation Geology. "Geology of Archean interflow sedimentary rocks and their relationship to Ag-Bi-Co-Ni-As veins, Cobalt area, Ontario." Ottawa.:, 1987.

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McMullen, Sarah Margaret. "Tectonic evolution of the Bark Lake area, eastern Central Gneiss Belt, Ontario Grenville, constraints from geology, geochemistry and U-Pb geochronology." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0010/MQ48503.pdf.

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McMullen, Sarah Margaret Carleton University Dissertation Earth Sciences. "Tectonic evolution of the Bark Lake area, Eastern Central Gneiss Belt, Ontario Grenville; constraints from geology, geochemistry and U-Pb geochronology." Ottawa, 1999.

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Murphy, Elena I. "Geology, metamorphism, and geochemistry of Southern and Grenville Province rocks in the vicinity of the Grenville Front, Timmins Creek area, near Sudbury, Ontario." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0018/MQ46496.pdf.

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Books on the topic "Geology - Ontario - Kamiskotia area"

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McKenzie, D. Ian. Quaternary geology of the Waterloo area, Ontario. Waterloo: Geological Association of Canada/Mineralogical Association of Canada, 1994.

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Stone, Denver. Geology of the northern Superior area, Ontario. [Sudbury]: Ontario Geological Survey, 2005.

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Stone, Denver. Precambrian geology of the Atikokan area, northwestern Ontario. Ottawa, Canada: Geological Survey of Canada, 1992.

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C, Kamineni D., Jackson M. C, and Geological Survey of Canada, eds. Precambrian geology of the Atikokan area, northwestern Ontario. Ottawa, Canada: Energy, Mines and Resources Canada, 1992.

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Karrow, P. F. Quaternary geology of the Hamilton - Cambridge area: Southern Ontario. Toronto: Ontario Ministry of Northern Development and Mines, 1987.

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Stone, Denver. Precambrian geology of the Berens River Area, Northwest Ontario. Toronto, Ont: Mines and Minerals Information Centre, 1998.

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A, Davidson. Grenville front relationships in the Sudbury area, Ontario. Waterloo: Geological Association of Canada/Mineralogical Association of Canada, 1994.

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Barnett, P. J. Quaternary geology of the Bancroft area: Southern Ontario. Toronto: Ontario Ministry of Northern Development and Mines, 1989.

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Thorleifson, L. Harvey. Quaternary geology and drift prospecting, Beardmore-Geraldton area, Ontario. Ottawa, Canada: Geological Survey of Canada, 1993.

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J, Frarey M. Proterozoic geology of the Lake Panache-Collins Inlet area, Ontario. Ottawa, Canada: Geological Survey of Canada, 1985.

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Book chapters on the topic "Geology - Ontario - Kamiskotia area"

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Sharpe, David R. "Quaternary geology of Toronto area, Ontario." In Centennial Field Guide Volume 5: Northeastern Section of the Geological Society of America, 339–44. Geological Society of America, 1987. http://dx.doi.org/10.1130/0-8137-5405-4.339.

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"Archean Au Quartz Vein Mineralization Hosted in a Tonalite-Trondhjemite Terrane, Renabie Mine Area, Wawa, North Ontario, Canada." In The Geology of Gold Deposits, 9–18. Society of Economic Geologists, 1989. http://dx.doi.org/10.5382/mono.06.01.

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Robbins, Eleanora I., and Michalann Harthill. "Life in a Copper Province." In Geology and Health. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195162042.003.0024.

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The North American Lake Superior region contains a world-class copper province nearly 300,000 km² in area. A dozen major copper deposits and hundreds of smaller mineral accumulations are located in Michigan, Minnesota, and Ontario (Morey and Sims 1996), many of which include As, nickel (Ni), platinum (Pt), palladium (Pd), Co, Mo, and Fe, as well as Cu (Nicholson et al. 1992). Historically, the province has hosted a variety of life forms; fossil biota have been traced as far back as 2.6-2.75 Ga. Palynological and microbial research (Robbins 1985, Robbins et al. 1994) prompts speculation about possible correlations between copper and the biota that evolved there. Because the region has been subjected to continental collisions, volcanism, glaciation, rifting, weathering, sea level rise and fall, waxing and waning of lakes, soil formation, and now to human settlement and development including mining, the fossil record is discontinuous. This review of the geologic formations in the Lake Superior region from the Precambrian to the present, and their copper and biotic occurrences and associations, attempts to illuminate some of those geologic/ biologic correlations, and includes mention of modern environmental concerns. Copper is one of nearly 75 chemical elements contributing to metabolic or structural functions of organisms (Dexter-Dyer et al. 1984). Bioassimilation varies and depends not only on availability from the environment, but also on the species, gender, and age of organism with specific concentrations also depending on diet, health, tissue assayed, and various synergisms with other trace elements such as Fe and Zn. Indeed, copper is an essential element and co-factor contributing to copper-associated polypeptides that provide catalytic and electron transfer functions in almost every known group of organisms alive today, from bacteria to humans. Copper proteins contribute to skin pigmentation, nerve coverings, and in mechanisms of development, maintenance, and repair of connective tissues important for well-functioning cardiovascular systems (Eisler 2000). Presently, over two dozen essential copper proteins, some with porphyrin-copper functional groups (similar to the porphyrin-iron association in hemoglobin), have been identified, each with its specific developmental or physiological function (Cowan 1998).
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"Landscape Influences on Stream Habitats and Biological Assemblages." In Landscape Influences on Stream Habitats and Biological Assemblages, edited by Les W. Stanfield and Bruce W. Kilgour. American Fisheries Society, 2006. http://dx.doi.org/10.47886/9781888569766.ch28.

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<em>Abstract.</em>—–We demonstrate the effects of percent impervious cover (PIC) on biophysical properties of Lake Ontario tributary streams. Biophysical data (fish assemblages, benthic invertebrate assemblages (benthos), instream physical habitat, and temperature) were collected from more than 575 wadeable stream sites. A geographic information system application was developed to characterize the landscape upstream of each site (i.e., drainage area, surficial geology, land use/land cover, slope, stream length, and climate). Total PIC of catchments was estimated from land use/land cover, and a base flow index was derived from the surficial geology. The relationship between PIC and biophysical responses was determined after statistically removing the effects of natural landscape features (i.e., catchment area, slope, base flow index) on those responses. Contrasts in PIC from natural conditions (<3% to 10%) were related to variations in fish and benthos assemblages. Both coldwater sensitive and warmwater tolerant fish and diverse benthos assemblages were found in catchments with low PIC. At more than 10 PIC (i.e., about 50% urban), both fish and benthos consisted of mainly warmwater or tolerant assemblages. For example, trout were absent and minnows were dominant. While some of the apparent PIC effect may have been confounded by land use/land cover and surficial geology, the consistency of the findings even after natural catchment conditions were considered suggests that the threshold response is valid. Percent impervious cover had a weaker effect on instream geomorphic variables than on biological variables. The models derived from this study can be used to predict stream biophysical conditions for catchments with varying levels of development.
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"Landscape Influences on Stream Habitats and Biological Assemblages." In Landscape Influences on Stream Habitats and Biological Assemblages, edited by Bruce W. Kilgour and Les W. Stanfield. American Fisheries Society, 2006. http://dx.doi.org/10.47886/9781888569766.ch30.

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<em>Abstract.</em>—Assessments of stream fish or benthos assemblages normally involve a contrast of conditions at test sites to conditions represented by regional reference sites that are either minimally or least disturbed. Identification of reference sites is difficult and normally involves a variety of subjective criteria. The development of reference models for stream fish and benthos in the Canadian tributaries of Lake Ontario is particularly challenging because there are few undeveloped areas and there is no consensus on criteria for a least-disturbed condition. Rather than identify sites as representing a least-disturbed condition, we developed a series of models that relate the existing biophysical condition of streams (i.e., the fish, benthos, and instream habitat) to landscape (i.e., slope, geology, catchment area) and land use/land cover (percent impervious cover [PIC]). Relationships between indices of biophysical condition and PIC can be used to hindcast or estimate the expected biophysical condition at a variety of land cover scenarios. The models cannot be used to predict conditions outside the calibration data range, but this approach does allow us to make use of a disturbance gradient and make predictions with a minimal number of least-disturbed sites. The difference between the hindcast reference and present day conditions is an estimate of present-day impacts. Results from this exercise provided an estimate of the magnitude of impairment of streams in the Canadian portion of the Lake Ontario region.
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Reports on the topic "Geology - Ontario - Kamiskotia area"

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Stone, D., and D. C. Kamineni. Geology, Atikokan area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127620.

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Morton, R. L., G. Hudak, and J. M. Franklin. Geology, south Sturgeon Lake area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210728.

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McClenaghan, M. B., R. C. Paulen, J. A. Ayer, N. F. Trowell, and S D Bauke. Regional till and humus geochemistry of the Timmins-Kamiskotia area, northeastern Ontario (NTS 42A/11, 12, 13, 14). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/210089.

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Percival, J. A., S. Castonguay, J. B. Whalen, J. L. Brown, V. McNicoll, and J. R. Harris. Geology, Sturgeon Lake-Obonga Lake area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210472.

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Sanborn-Barrie, M., and T. Skulski. Structural geology, central Sturgeon Lake area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209936.

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Stone, D., C. Kamineni, M. Jackson, and W. Shanks. Geology of the Atikokan area, Northwestern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130128.

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St-Onge, D. A. Quaternary geology of the Cornwall area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/223019.

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Brennand, T. A. Preliminary surficial geology site attributes, Oshawa area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194144.

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Matile, G. L. D., and L. H. Thorleifson. Surficial geology, Falcon Lake area, Manitoba and Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207499.

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Stone, D., D. C. Kamineni, and M. C. Jackson. Precambrian geology of the Atikokan area, northwestern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/134053.

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