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Journal articles on the topic 'Superior, Lake, Region – Biography'

Author: Grafiati

Published: 27 July 2024

Last updated: 31 July 2025

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1

HUBBARD, C. D. "Geology of the Lake Superior Region." Environmental & Engineering Geoscience I, no. 1 (1995): 111–12. http://dx.doi.org/10.2113/gseegeosci.i.1.111.

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2

Mulligan, William H., and Kathryn Bishop Eckert. "The Sandstone Architecture of the Lake Superior Region." Michigan Historical Review 27, no. 2 (2001): 181. http://dx.doi.org/10.2307/20173935.

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3

Schulz, Klaus J., and William F. Cannon. "The Penokean orogeny in the Lake Superior region." Precambrian Research 157, no. 1-4 (2007): 4–25. http://dx.doi.org/10.1016/j.precamres.2007.02.022.

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4

Howkins, Adrian, Stephen Chignell, and Andrew Fountain. "Vanda Station, Antarctica: a biography of the Anthropocene." Journal of the British Academy 9s6 (2021): 61–89. http://dx.doi.org/10.5871/jba/009s6.061.

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This article uses the history of New Zealand�s Vanda Station in Antarctica as a case study of the inseparability of human history and environmental change in the age of the Anthropocene. Vanda Station was built in the late 1960s to promote New Zealand�s sovereignty claims to Antarctica and to promote scientific research in the predominantly ice-free McMurdo Dry Valleys region. Over the course of the 1970s and 1980s, the levels of the nearby Lake Vanda rose dramatically, and in the early 1990s the decision was taken to close the station. Rather than seeing the closure of Vanda simply as a conse

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5

Kaups, Matti E. "Finnish Meadow-Hay Barns in the Lake Superior Region." Journal of Cultural Geography 10, no. 1 (1989): 1–18. http://dx.doi.org/10.1080/08873638909478451.

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6

Glass, Gary E., Edward N. Leonard, Walter H. Chan, and Daniel B. Orr. "Airborne Mercury in Precipitation in the Lake Superior Region." Journal of Great Lakes Research 12, no. 1 (1986): 37–51. http://dx.doi.org/10.1016/s0380-1330(86)71698-5.

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7

Ojakangas, R. W., G. B. Morey, and J. C. Green. "The Mesoproterozoic Midcontinent Rift System, Lake Superior Region, USA." Sedimentary Geology 141-142 (June 2001): 421–42. http://dx.doi.org/10.1016/s0037-0738(01)00085-9.

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8

Cengiz, Taner. "Periodic structures of Great Lakes levels using wavelet analysis." Journal of Hydrology and Hydromechanics 59, no. 1 (2011): 24–35. http://dx.doi.org/10.2478/v10098-011-0002-z.

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Periodic structures of Great Lakes levels using wavelet analysisThe recently advanced approach of wavelet transforms is applied to the analysis of lake levels. The aim of this study is to investigate the variability of lake levels in four lakes in the Great Lakes region where the method of continuous wavelet transform and global spectra are used. The analysis of lake-level variations in the time-scale domain incorporates the method of continuous wavelet transform and the global spectrum. Four lake levels, Lake Erie, Lake Michigan, Lake Ontario, and Lake Superior in the Great Lakes region were

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9

Fisher, Shannon J., and Bruce L. Swanson. "Diets of Siscowet Lake Trout from the Apostle Islands Region of Lake Superior, 1993." Journal of Great Lakes Research 22, no. 2 (1996): 463–68. http://dx.doi.org/10.1016/s0380-1330(96)70970-x.

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10

Zuccarino-Crowe, Chiara M., William W. Taylor, Michael J. Hansen, Michael J. Seider, and Charles C. Krueger. "Effects of lake trout refuges on lake whitefish and cisco in the Apostle Islands Region of Lake Superior." Journal of Great Lakes Research 42, no. 5 (2016): 1092–101. http://dx.doi.org/10.1016/j.jglr.2016.07.011.

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11

Manson, Matthew L., and Henry C. Halls. "Proterozoic reactivation of the southern Superior Province and its role in the evolution of the Midcontinent rift." Canadian Journal of Earth Sciences 34, no. 4 (1997): 562–75. http://dx.doi.org/10.1139/e17-045.

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Major reverse faults associated with the late compressional phase of the 1.1 Ga Midcontinent rift in the western Lake Superior region appear to cut across the rift at the eastern end of the lake and join with reverse faults on the eastern shoreline, defined on the basis of geological and potential field data. The continuation of the faults across eastern Lake Superior is inferred on evidence drawn from nearshore shipborne magnetic surveys together with new interpretations of published bathymetric and GLIMPCE aeromagnetic data. In the Archean Superior Province about 100 km east of Lake Superior

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12

Rodriguez, Yarice, David A. R. Kristovich, and Mark R. Hjelmfelt. "Lake-to-Lake Cloud Bands: Frequencies and Locations." Monthly Weather Review 135, no. 12 (2007): 4202–13. http://dx.doi.org/10.1175/2007mwr1960.1.

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Abstract Premodification of the atmosphere by upwind lakes is known to influence lake-effect snowstorm intensity and locations over downwind lakes. This study highlights perhaps the most visible manifestation of the link between convection over two or more of the Great Lakes lake-to-lake (L2L) cloud bands. Emphasis is placed on L2L cloud bands observed in high-resolution satellite imagery on 2 December 2003. These L2L cloud bands developed over Lake Superior and were modified as they passed over Lakes Michigan and Erie and intervening land areas. This event is put into a longer-term context th

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13

Detenbeck, Naomi E., Colleen M. Elonen, Debra L. Taylor, Leroy E. Anderson, Terri M. Jicha, and Sharon L. Batterman. "REGION, LANDSCAPE, AND SCALE EFFECTS ON LAKE SUPERIOR TRIBUTARY WATER QUALITY." Journal of the American Water Resources Association 40, no. 3 (2004): 705–20. http://dx.doi.org/10.1111/j.1752-1688.2004.tb04454.x.

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14

Hinze, William J. "The Meter Reader: Early magnetic studies in the Lake Superior region." Leading Edge 42, no. 8 (2023): 566–68. http://dx.doi.org/10.1190/tle42080566.1.

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In the mid-19th century, the quality of life in the United States was improving rapidly with widespread electrification of the nation and growth in the industrial revolution. These advances were dependent on the increasing availability of copper for instruments and electric wires and iron ore for the production of iron and steel. Accordingly, reconnaissance geologic investigations in the Lake Superior region of North America that discovered copper and iron-rich rocks in the 1840s rapidly attracted the attention of prospectors and mining companies. However, ore deposits were a challenge to find

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15

Vall, Kathryn, Collin Murphy, David P. Pompeani, et al. "Ancient mining pollution in early to middle Holocene lake sediments from the Lake Superior region, USA." Anthropocene 39 (September 2022): 100348. http://dx.doi.org/10.1016/j.ancene.2022.100348.

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16

Kenyeres, Zoltán, and Tibor Kovács. "Aki a Mátrában is otthon volt: Tóth Sándortól búcsúzunk." Folia historico-naturalia Musei Matraensis, no. 48 (2024): 5–12. https://doi.org/10.69595/folianatmatra.2024.48.01.

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Sándor Tóth, one of the last significant figures of Hungarian classical entomology, passed away on 17 May 2024. His long career focused mainly on the Bakony Region and Lake Balaton. Still, he also conducted intensive research in many other areas of the country, including the Mátra Mts. He summarized his results on Odonata and Dipteran families of Bombyliidae, Conopidae, Culicidae, Stratiomyidae, Syrphidae, Tabanidae, and Tachinidae from the Mátra Region in 17 publications, 3 of which are monographs. In the name of the whole profession, the authors bid farewell their tireless and exemplary coll

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17

Reavie, Euan D., John A. Robbins, Eugene F. Stoermer, et al. "Paleolimnology of a fluvial lake downstream of Lake Superior and the industrialized region of Sault Saint Marie." Canadian Journal of Fisheries and Aquatic Sciences 62, no. 11 (2005): 2586–608. http://dx.doi.org/10.1139/f05-170.

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A paleolimnological study was undertaken to describe the past environment of the St. Mary's River downstream of Lake Superior. Two sediment cores were obtained from the deepest part of Lake George, a fluvial lake in the river system. Rigorous analyses of radionuclides (210Pb, 226Ra, and 137Cs) and chemical properties provided an accurate sediment chronology. More than 450 diatom species from 47 genera were identified. Diatom and geochemical data indicated gradual environmental change in response to anthropogenic activities, including logging, hydrologic manipulation, and steel, leather, and pa

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18

Morey, G. "Early Geologic Studies in the Lake Superior Region-the Contributions of H.R. Schoolcraft, J.J. Bigsby, and H.W. Bayfield." Earth Sciences History 8, no. 1 (1989): 36–42. http://dx.doi.org/10.17704/eshi.8.1.03r5858k56041196.

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Charles Lyell published a geologic map of the Lake Superior region in 1845 as an appendix to his epochal Travels in North America. One of the published sources Lyell used to compile this map was an 1829 report by H.W. Bayfield, who as a surveyor for the Royal Navy spent the years 1823 to 1825 circumnavigating the lake. Bayfield's report, in turn, included the geologic observations of two other travelers on the lake: H.R. Schoolcraft and J.J. Bigsby, both of whom, like Bayfield, had taken part in some of the earliest government-sponsored explorations in the region. Although Schoolcraft had rece

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19

Morey, G. B., and D. L. Southwick. "Allostratigraphic relationships of early Proterozoic iron-formations in the Lake Superior region." Economic Geology 90, no. 7 (1995): 1983–93. http://dx.doi.org/10.2113/gsecongeo.90.7.1983.

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20

Craddock, John P., Alex Konstantinou, Jeffrey D. Vervoort, et al. "Detrital Zircon Provenance of the Mesoproterozoic Midcontinent Rift, Lake Superior Region, U.S.A." Journal of Geology 121, no. 1 (2013): 57–73. http://dx.doi.org/10.1086/668635.

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21

LARUE, D. K., and W. L. UENG. "Florence-Niagara terrane: An early Proterozoic accretionary complex, Lake Superior region, U.S.A." Geological Society of America Bulletin 96, no. 9 (1985): 1179. http://dx.doi.org/10.1130/0016-7606(1985)96<1179:ftaepa>2.0.co;2.

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22

Ojakangas, R. W., G. B. Morey, and D. L. Southwick. "Paleoproterozoic basin development and sedimentation in the Lake Superior region, North America." Sedimentary Geology 141-142 (June 2001): 319–41. http://dx.doi.org/10.1016/s0037-0738(01)00081-1.

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23

Ojakangas, R. W. "Upper Keweenawan Stratigraphy: Reservoir Characteristics of the Keweenawan Supergroup, Lake Superior Region." Geoscience Wisconsin 11 (1986): 25–31. https://doi.org/10.54915/wlun9708.

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24

Halls, H. C., and E. G. Shaw. "Paleomagnetism and orientation of Precambrian dykes, eastern Lake Superior region, and their use in estimates of crustal tilting." Canadian Journal of Earth Sciences 25, no. 5 (1988): 732–43. http://dx.doi.org/10.1139/e88-069.

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Archean rocks form the eastern margin of the 1.1 Ga old Central North American rift along the eastern shore of Lake Superior and have been tilted westwards in response to rifting. Paleomagnetic and structural data from 2.6 Ga old Matachewan dykes suggest a westward crustal tilt of about 60°, which agrees well with dips recorded in nearby Keweenawan volcanics that rest directly on basement rocks. The Matachewan dyke swarm occurs throughout the east shore region of Lake Superior, whereas Keweenawan supracrustal sequences, which give a more precise estimate of tilt, are restricted to a few isolat

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25

Griffiths, Ronald W., Donald W. Schloesser, Joseph H. Leach, and William P. Kovalak. "Distribution and Dispersal of the Zebra Mussel (Dreissena polymorpha) in the Great Lakes Region." Canadian Journal of Fisheries and Aquatic Sciences 48, no. 8 (1991): 1381–88. http://dx.doi.org/10.1139/f91-165.

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Dreissena polymorpha (Pallas), a small mussel common throughout most of Europe, was discovered in June of 1988 in the southern part of Lake St. Clair. Length–frequency analyses of populations from the Great Lakes and review of historical benthic studies suggest that the mussel was introduced into Lake St. Clair in late 1986, probably as a result of the discharge of ballast water from an ocean-crossing vessel. Following the 1990 reproductive season, Dreissena populations ranged from the head of the St. Clair River, through Lake St. Clair, the Detroit River, Lake Erie, the Welland Canal, and the

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26

Bajc, Andrew F., Alan V. Morgan, and Barry G. Warner. "Age and paleoecological significance of an early postglacial fossil assemblage near Marathon, Ontario, Canada." Canadian Journal of Earth Sciences 34, no. 5 (1997): 687–98. http://dx.doi.org/10.1139/e17-055.

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Organic materials recovered from deltaic deposits confined to the Black River Valley near Marathon, Ontario, provide information on lake-level history and local ecology for the region. Radiocarbon samples provide the first age determinations (ca. 8200 BP) for the post-Minong III – IV lake phases along the northeast corner of the Lake Superior basin. A minimum of 49 Coleoptera taxa and 22 vascular plant taxa indicate coniferous-forest and riparian communities. Overbank deposition along rivers flowing from the ice margin provided temporary ponds colonized by sedges and other aquatic plants and a

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27

Schram, Stephen T., Timothy B. Johnson, and Michael J. Seider. "Burbot Consumption and Relative Abundance in the Apostle Islands Region of Lake Superior." Journal of Great Lakes Research 32, no. 4 (2006): 798. http://dx.doi.org/10.3394/0380-1330(2006)32[798:bcarai]2.0.co;2.

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28

Pufahl, Peir K., and Philip W. Fralick. "Depositional controls on Palaeoproterozoic iron formation accumulation, Gogebic Range, Lake Superior region, USA." Sedimentology 51, no. 4 (2004): 791–808. http://dx.doi.org/10.1111/j.1365-3091.2004.00651.x.

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29

Holm, Daniel, L. Gordon Medaris, Kalin T. McDannell, et al. "Growth, overprinting, and stabilization of Proterozoic provinces in the southern Lake Superior region." Precambrian Research 339 (April 2020): 105587. http://dx.doi.org/10.1016/j.precamres.2019.105587.

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30

Bockheim, J. G., and S. E. Crowley. "Ion Cycling in Hemlock-Northern Hardwood Forests of the Southern Lake Superior Region." Journal of Environmental Quality 31, no. 5 (2002): 1623–29. http://dx.doi.org/10.2134/jeq2002.1623.

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31

Van Den Broeke, Matthew. "Seasonally and Diurnally Varying Cold Front Effects along the Minnesotan North Shore of Lake Superior." Atmosphere 13, no. 3 (2022): 441. http://dx.doi.org/10.3390/atmos13030441.

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Cold fronts are typically associated with cooling, drying and a strengthening wind that shifts to have a northerly component. Cold front effects at a particular point, however, are dependent upon pre-existing air mass characteristics. Here, we examine 634 passages of synoptic-scale cold fronts in northeastern Minnesota from 2010 to 2018. While these fronts are associated with the expected effects in some areas, they are often associated with warming and enhanced drying in the region directly influenced by an air mass from Lake Superior (coastal sites). Coastal sites experience warming during m

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32

Corfu, F., and G. M. Stott. "U–Pb geochronology of the central Uchi Subprovince, Superior Province." Canadian Journal of Earth Sciences 30, no. 6 (1993): 1179–96. http://dx.doi.org/10.1139/e93-100.

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U–Pb zircon and titanite ages for rocks of the central Uchi Subprovince in northwestern Ontario indicate a late Archean magmatic and tectonic development spanning over 200 Ma. An early period at 2900–2800 Ma formed volcano-plutonic complexes, presumably linked to 3.1–2.8 Ga terrains of the northwestern Superior Province. A later period of southward growth by magmatic and tectonic accretion occurred at 2750–2710 Ma and was concluded by large scale compression and plutonism at 2700 Ma.The oldest 2890–2860 and 2840–2820 Ma components occur in the Pickle Lake and Meen–Dempster greenstone belts and

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33

Manson, Matthew L., and Henry C. Halls. "Post-Keweenawan compressional faults in the eastern Lake Superior region and their tectonic significance." Canadian Journal of Earth Sciences 31, no. 4 (1994): 640–51. http://dx.doi.org/10.1139/e94-057.

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GLIMPCE aeromagnetic data in eastern Lake Superior are characterized by a series of strong easterly- and northeasterly-oriented gradients that relate to mapped post-Keweenawan faults occurring along the eastern shore. The reversed nature of three of the faults is established through field observations and potential field modelling. Middle Keweenawan volcanic rocks at Mamainse Point are in fault contact on their south side with upper Keweenawan sandstone of Bayfield–Jacobsville type. Gravity modelling suggests that the fault is a low angle thrust dipping to the north. Field observations and hig

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34

Polat, Ali, Robert Frei, Hao Deng, Xue-Ming Yang, and Paul Sotiriou. "Anatomy of a Neoarchean continental arc-backarc system in the Cross Lake-Pipestone Lake region, northwestern Superior Province, Canada." Precambrian Research 370 (March 2022): 106556. http://dx.doi.org/10.1016/j.precamres.2021.106556.

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35

Dixit, Sushil S. "Diatom-inferred pH calibration of lakes near Wawa, Ontario." Canadian Journal of Botany 64, no. 6 (1986): 1129–33. http://dx.doi.org/10.1139/b86-155.

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In the absence of long-term pH records for lakes, sedimentary diatoms have often been used to detect the extent of recent lake acidification. Although various methods have been used to relate surface-sediment diatom remains to contemporary lake-water pH, their usefulness and selection criteria have not been clearly defined for Canadian lakes. Surface-sediment diatoms of 28 lakes (pH 4.0–8.13) located northeast of Lake Superior were identified and enumerated. Lake-water pH estimates were made using multiple regression analyses of selected diatom taxa and Hustedt's pH indicator groups, as well a

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36

Hansen, Dennis L., Satoshi Ishii, Michael J. Sadowsky, and Randall E. Hicks. "Escherichia coli Populations in Great Lakes Waterfowl Exhibit Spatial Stability and Temporal Shifting." Applied and Environmental Microbiology 75, no. 6 (2009): 1546–51. http://dx.doi.org/10.1128/aem.00444-08.

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ABSTRACT Populations of Escherichia coli from juvenile and adult ring-billed gulls, juvenile common terns, and adult Canada geese were sampled over 6 years at five locations on Lake Superior (Duluth, MN, and Wisconsin) and Lake Michigan (Wisconsin, Illinois, and Indiana) to determine the extent of spatial and temporal variability in E. coli strains. Strain identity was determined using horizontal fluorophore-enhanced repetitive element palindromic DNA fingerprinting. Multivariate statistics were used to determine if spatial or temporal changes in E. coli populations occurred in waterfowl speci

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37

Berthelette, Scott. "“Les Sçioux n’étoient bons qu’à manger”: La Colle and the Anishinaabeg-Dakota War, 1730–1742." Ethnohistory 69, no. 1 (2022): 1–27. http://dx.doi.org/10.1215/00141801-9404118.

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Abstract La Colle was an influential Anishinaabe ogimaa (leader) and mayosewinini (war chief) who led the Monsoni (moose) doodem (clan) in the Rainy Lake region during the 1730s and 1740s. A biographical study of La Colle not only restores an individual Indigenous voice to the tapestry of Native North America but also provides insight into a conflict between the Anishinaabeg, Nêhiyawak (Crees), Nakoda (Assiniboines), and Očhéthi Šakówiŋ (Dakota, Yankton, Yanktonai, and Lakota) that took place in the borderlands between Lake Superior and the Upper Missouri Valley. Ultimately, the conflict saw t

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38

Foley, Carolyn J., Gabriel J. Bowen, Thomas F. Nalepa, Marisol S. Sepúlveda, and Tomas O. Höök. "Stable isotope patterns of benthic organisms from the Great Lakes region indicate variable dietary overlap of Diporeia spp. and dreissenid mussels." Canadian Journal of Fisheries and Aquatic Sciences 71, no. 12 (2014): 1784–95. http://dx.doi.org/10.1139/cjfas-2013-0620.

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Competition between native and invasive species may bring about a suite of ecological and evolutionary outcomes, including local extirpations. In the Laurentian Great Lakes, competition for food may explain the dramatic decline of Diporeia spp. amphipods following the introduction of dreissenid mussels. This hypothesis has not been confirmed, in part because dreissenids and Diporeia appear to co-exist and flourish in other systems, including the Finger Lakes of New York. We used carbon, nitrogen, hydrogen, and oxygen stable isotope ratios to examine resource use by Diporeia from three spatiall

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39

Miller, Christina, Gerald J. Niemi, JoAnn M. Hanowski, and Ronald R. Regal. "Breeding Bird Communities Across an Upland Disturbance Gradient in the Western Lake Superior Region." Journal of Great Lakes Research 33, sp3 (2007): 305–18. http://dx.doi.org/10.3394/0380-1330(2007)33[305:bbcaau]2.0.co;2.

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40

Ueng, Wen-long C., and Dave K. Larue. "The Early Proterozoic structural and tectonic history of the south central Lake Superior Region." Tectonics 7, no. 3 (1988): 369–88. http://dx.doi.org/10.1029/tc007i003p00369.

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41

Cannon, William F. "The Midcontinent rift in the Lake Superior region with emphasis on its geodynamic evolution." Tectonophysics 213, no. 1-2 (1992): 41–48. http://dx.doi.org/10.1016/0040-1951(92)90250-a.

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42

Hill, Christopher L. "Geoarchaeology and late glacial landscapes in the western lake superior region, Central North America." Geoarchaeology 22, no. 1 (2006): 15–47. http://dx.doi.org/10.1002/gea.20145.

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43

Geiger, C. A., and C. V. Guidotti. "Precambrian Metamorphism in the Southern Lake Superior Region and Its Bearing on Crustal Evolution." Geoscience Wisconsin 13 (1989): 1–33. https://doi.org/10.54915/buih3897.

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44

Oyadomari, Jason K., and Nancy A. Auer. "Transport and growth of larval cisco (Coregonus artedi) in the Keweenaw Current region of Lake Superior." Canadian Journal of Fisheries and Aquatic Sciences 65, no. 7 (2008): 1447–58. http://dx.doi.org/10.1139/f08-068.

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Larval cisco ( Coregonus artedi ) were sampled from Lake Superior off the western coast of the Keweenaw Peninsula (Michigan, USA) to determine if the Keweenaw Current influences their distribution and growth. Bongo net tows were conducted during April–June 2000 from four transects extending from 0.1 to 17 km offshore. For most sampling dates, cisco tended to be slightly more abundant, larger, and older at inshore locations. Later-hatched larvae appeared at the western-most transects first, during which time earlier-hatched larvae disappeared from the study area. This pattern followed what woul

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45

Ihssen, P. E., J. M. Casselman, G. W. Martin, and R. B. Phillips. "Biochemical Genetic Differentiation of Lake Trout (Salvelinus namaycush) Stocks of the Great Lakes Region." Canadian Journal of Fisheries and Aquatic Sciences 45, no. 6 (1988): 1018–29. http://dx.doi.org/10.1139/f88-125.

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Allelic frequencies for lake trout (Salvelinus namaycush) samples collected from 27 small lakes or spawning shoals on larger lakes did not show significant annual changes. Levels of genetic variability were in the high range for Salmonidae, with 57% of the loci examined polymorphic (1% criterion) and 4.7% average heterozygosity per locus. Twenty-one percent of the total genetic variability was due to differences between stocks. Highly significant allelic frequency differences were found among allopatric as well as sympatric stocks. Genetic differences among sympatric stocks of Lake Superior in

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46

Lemoine, Rick M., and James T. Teller. "Late Glacial Sedimentation and History of the Lake Nipigon Basin, Ontario." Géographie physique et Quaternaire 49, no. 2 (2007): 239–50. http://dx.doi.org/10.7202/033039ar.

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ABSTRACTThe Lake Nipigon basin lies north of the Lake Superior basin and was the hydrological link between glacial Lake Agassiz and the Great Lakes during part of the last deglaciation. A sequence of glaciolacustrine sediments, composed mainly of silt-clay rhythmites and sand, was deposited in the offshore waters of glacial Lake Nipigon by overflow from Lake Agassiz and meltwater from the retreating glacier margin. Sections from six long sediment cores and four lake bluff exposures reveal a sandy (early deglacial) lower section that is overlain by 300 to 850 silt-clay rhythmites (varves). Depo

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47

Percival, John A., and Herwart Helmstaedt. "The Western Superior Province Lithoprobe and NATMAP transects: introduction and summary." Canadian Journal of Earth Sciences 43, no. 7 (2006): 743–47. http://dx.doi.org/10.1139/e06-063.

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The Special Issue on the Western Superior Province Lithoprobe and NATMAP transects presents a wide spectrum of contributions from coordinated, multidisciplinary research projects on the western region of Earth's largest Archean craton. Articles include aspects of the geophysical, stratigraphic, geochemical, geochronological, petrological, and structural evidence bearing on the accretionary history of this classic, well-exposed piece of ancient continental crust, as well as analyses of the prospectivity and seismic character of the gold-rich Red Lake greenstone belt.

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48

Heaman, L. M., R. M. Easton, T. R. Hart, P. Hollings, C. A. MacDonald, and M. Smyk. "Further refinement to the timing of Mesoproterozoic magmatism, Lake Nipigon region, Ontario." Canadian Journal of Earth Sciences 44, no. 8 (2007): 1055–86. http://dx.doi.org/10.1139/e06-117.

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The Midcontinent Rift in the Lake Superior region of North America is one of the best preserved examples of an aborted Precambrian intercontinental rift, one that hosts a diverse suite of rock types in addition to the well-studied and voluminous rift-fill flood basalts. Although there is a growing database of high-precision age information for the main volcanic packages and the largest mafic intrusions, there is relatively little information available on the absolute timing of mafic-ultramafic intrusions, dyke swarms, and alkaline complexes, especially in the Ontario portion of the rift. We re

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Bullock, Ryan. "Reframing Forest-Based Development As First Nation–Municipal Collaboration: Lessons from Lake Superior’s North Shore." Journal of Aboriginal Economic Development 7, no. 2 (2011): 78–89. http://dx.doi.org/10.29173/jaed305.

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Changes in Northern Ontario's planning and policy context (e.g., forest tenure reform, Far North Act) are creating opportunities and obligations for First Nations and towns that often are not matched by the local capacity, resources, and governance structures requisite for effective and equitable participation. This paper documents the early stages of a First Nation-municipal forestbased development initiative in the Northeast Superior Region and interprets evolving perspectives of 27 First Nation and non-First Nation interviewees concerning the establishment of counterpart regional governance

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Rook, Benjamin J., Michael J. Hansen, and Charles R. Bronte. "Are Cisco and Lake Whitefish Competitors? An Analysis of Historical Fisheries in Michigan Waters of the Upper Laurentian Great Lakes." Journal of Fish and Wildlife Management 12, no. 2 (2021): 524–39. http://dx.doi.org/10.3996/jfwm-20-062.

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Abstract Historically, Cisco Coregonus artedi and Lake Whitefish Coregonus clupeaformis were abundant throughout the Laurentian Great Lakes, but overharvest, habitat degradation, and interactions with exotic species caused most populations to collapse by the mid-1900s. Strict commercial fishery regulations and improved environmental and ecological conditions allowed Cisco to partially recover only in Lake Superior, whereas Lake Whitefish recovered in all the upper Great Lakes (Superior, Michigan, and Huron). The differential responses of Cisco and Lake Whitefish to improved environmental and e

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