ATLAS of the SPAWNING and NURSERY AREAS of GREAT LAKES FISHES Volume II - Lake Superior
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WLSSB Map and Guide
WISCONSIN LAKE SUPERIOR SCENIC BYWAY (WLSSB) DEVILS ISLAND NORTH TWIN ISLAND MAP KEY ROCKY ISLAND SOUTH TWIN ISLAND CAT ISLAND WISCONSIN LAKE SUPERIOR SCENIC BYWAY APOSTLE ISLANDS BEAR ISLAND NATIONAL LAKESHORE KIOSK LOCATION IRONWOOD ISLAND SCENIC BYWAY NEAR HERBSTER SAILING ON LAKE SUPERIOR LOST CREEK FALLS KIOSKS CONTAIN DETAILED INFORMATION ABOUT EACH LOCATION SAND ISLAND VISITOR INFORMATION OUTER ISLAND YORK ISLAND SEE REVERSE FOR COMPLETE LIST µ OTTER ISLAND FEDERAL HIGHWAY MANITOU ISLAND RASPBERRY ISLAND STATE HIGHWAY COUNTY HIGHWAY 7 EAGLE ISLAND NATIONAL PARKS ICE CAVES AT MEYERS BEACH BAYFIELD PENINSULA AND THE APOSTLE ISLANDS FROM MT. ASHWABAY & NATIONAL FOREST LANDS well as a Heritage Museum and a Maritime Museum. Pick up Just across the street is the downtown area with a kayak STATE PARKS K OAK ISLAND STOCKTON ISLAND some fresh or smoked fish from a commercial fishery for a outfitter, restaurants, more lodging and a historic general & STATE FOREST LANDS 6 GULL ISLAND taste of Lake Superior or enjoy local flavors at one of the area store that has a little bit of everything - just like in the “old (!13! RED CLIFF restaurants. If you’re brave, try the whitefish livers – they’re a days,” but with a modern flair. Just off the Byway you can MEYERS BEACH COUNTY PARKS INDIAN RESERVATION local specialty! visit two popular waterfalls: Siskiwit Falls and Lost Creek & COUNTY FOREST LANDS Falls. West of Cornucopia you will find the Lost Creek Bog HERMIT ISLAND Walk the Brownstone Trail along an old railroad grade or CORNUCOPIA State Natural Area. Lost Creek Bog forms an estuary at the take the Gil Larson Nature Trail (part of the Big Ravine Trail MICHIGAN ISLAND mouths of three small creeks (Lost Creek 1, 2, and 3) where System) which starts by a historic apple shed, continues RESERVATION LANDS they empty into Lake Superior at Siskiwit Bay. -
Lake Superior South Watershed Monitoring and Assessment Report
Summary Monitoring and Assessment Lake Superior-South Watershed Why is it The undeveloped nature of the Lake Superior-South Watershed, along Minnesota’s North Shore within the Lake Superior Basin, is undoubtedly a key reason for the high important? water quality found in most parts of the watershed. This watershed covers 624 square miles of St. Louis and Lake counties, with nearly half of the land under state ownership (42%). Almost 90% is forested. The watershed is home to several small cities and supports diverse species of wildlife and fish populations. It contains 1,067 miles of streams of which 800 are designated as coldwater. Its immaculate waters produce some of the state’s highest-quality stream trout fisheries. The watershed is a valuable resource for drinking water, habitat for aquatic life, recreational opportunities and timber production. Key issues Overall, water quality conditions are good and can be attributed to the forest and wetlands that dominate the watershed’s land cover. Many stream segments have exceptional biological, chemical, and physical characteristics and should be considered for additional protections to preserve their high quality. The top five stream resources include: McCarthy Creek, Unnamed Creek (West Branch Little Knife River), Gooseberry River, Stewart River and Captain Jacobson Creek. Problem areas do occur but are typically limited to the lower reaches of streams where stressors from land use practices may accumulate. Impairments are likely a function of both natural and human-caused stressors. Historical and recent forest cover changes, along with urban/industrial development, draining of wetlands and damming of streams are likely stressors affecting biological communities within the watershed. -
MN History Magazine
THIS IS a revised version of a talk given before the St. Louis Ccninty Historical Society on February 23, 1954. The author, who teaches political science in the University of Minnesota, Duluth Branch, became interested in traces of early logging and mining operations while hunting and fishing in the Arrowhead region. Some Vanished Settlements of th£ ARROWHEAD COUNTRY JULIUS F. WOLFF, JR. FOR MORE THAN two centuries Minne in the 1840s in search of copper and other sota has been known to white men who minerals. Such prospecting, however, was were exploring, trading, mining, logging, really poaching, since the area was Indian fishing, or farming in the area. The thriving territory until it was ceded to the United communities of today are monuments to suc States by the treaty of La Pointe in 1854. cessful pioneer expansion in many fields. Yet One of the first accounts of white habitation there are numerous sites in Koochiching, on the shore dates from the fall of that Cook, Lake, and St. Louis counties that tell year, when R. B. McLean, a prospector who a different story — a story of failure, of at later became the area's first mail carrier, tempts at settlement that did not bear fruit. accompanied a party which scoured the White habitation in northeastern Minne shore for copper outcrops, McLean noted a sota is largely confined to the last hundred few settlers near the mouths of the French, years. To be sure, explorers, missionaries, Sucker, Knife, and Encampment rivers and and fur traders visited the area repeatedly at Grand Marais.^ after the seventeenth century and estab During the next two years a wave of lished scattered trading posts. -
Apostle Islands National Lakehore Geologic Resources Inventory
Geologic Resources Inventory Scoping Summary Apostle Islands National Lakeshore Geologic Resources Division Prepared by Trista L. Thornberry-Ehrlich National Park Service August 7, 2010 US Department of the Interior The Geologic Resources Inventory (GRI) provides each of 270 identified natural area National Park System units with a geologic scoping meeting and summary (this document), a digital geologic map, and a geologic resources inventory report. The purpose of scoping is to identify geologic mapping coverage and needs, distinctive geologic processes and features, resource management issues, and monitoring and research needs. Geologic scoping meetings generate an evaluation of the adequacy of existing geologic maps for resource management, provide an opportunity to discuss park-specific geologic management issues, and if possible include a site visit with local experts. The National Park Service held a GRI scoping meeting for Apostle Islands National Lakeshore on July 20-21, 2010 both out in the field on a boating site visit from Bayfield, Wisconsin, and at the headquarters building for the Great Lakes Network in Ashland, Wisconsin. Jim Chappell (Colorado State University [CSU]) facilitated the discussion of map coverage and Bruce Heise (NPS-GRD) led the discussion regarding geologic processes and features at the park. Dick Ojakangas from the University of Minnesota at Duluth and Laurel Woodruff from the U.S. Geological Survey presented brief geologic overviews of the park and surrounding area. Participants at the meeting included NPS staff from the park and Geologic Resources Division; geologists from the University of Minnesota at Duluth, Wisconsin Geological and Natural History Survey, and U.S. Geological Survey; and cooperators from Colorado State University (see table 2). -
What the “Trail Eyes” Pros Taught Us About the SHT P H
A publication oF the Superior Hiking TrAil AssoCiation SUmmEr 2019 What the “Trail Eyes” Pros Taught Us About the SHT P H o im Malzhan iS the trail operations director T o for our sister trail organization the ice Age B y Fr Trail Alliance in Wisconsin. Doing business as esh T “Trail Eyes,” Tim was one of four entities the SHTA Tr hired in the fall of 2018 to evaluate and recom- ac mend renewal strategies for what we have dubbed k S mE D “The Big Bad Five,” those sections of the SHT most damaged from heavy use and old age (or both). i A Though all four evaluators—malzhan, Critical Connections Ecological Services (Jason and Amy Husveth), the north Country Trail Association, and (Continued on page 2) What the “Trail Eyes” Taught Us About the SHT (continued from cover) Great Lakes Trail Builders (Wil- lie Bittner)—did what we asked (provide specific prescriptions for the Big Bad Five), their ex- pert observations gave us much more: they shed light on the en- tire Superior Hiking Trail. In other words, what they saw on the Split Rock River loop, or the sections from Britton Peak to Oberg Mountain and Oberg to the Lutsen ski complex, or the proposed reroute of the SHT north of Gooseberry Falls State Park, were microcosms of bigger, more systemic issues with the SHT. ❚ “keep people on the Trail and water off of it.” This suc- cinct wisdom comes from Matt no bridge is not the only problem at the Split rock river loop. -
Origin, Burial and Preservation of Late Pleistocene-Age Glacier Ice in Arctic
Origin, burial and preservation of late Pleistocene-age glacier ice in Arctic permafrost (Bylot Island, NU, Canada) Stephanie Coulombe1 2 3, Daniel Fortier 2 3 5, Denis Lacelle4, Mikhail Kanevskiy5, Yuri Shur5 6 1Polar Knowledge Canada, Cambridge Bay, X0B 0C0, Canada 5 2Department of Geography, Université de Montréal, Montréal, H2V 2B8, Canada 3Centre for Northern Studies, Université Laval, Quebec City, G1V 0A6, Canada 4Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, K1N 6N5, Canada 5Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5910, USA 6Department of Civil and Environmental Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5960, USA 10 Correspondence to: Stephanie Coulombe ([email protected]) Over the past decades, observations of buried glacier ice exposed in coastal bluffs and headwalls of retrogressive thaw slumps of the Arctic indicate that considerable amounts of late Pleistocene glacier ice survived the deglaciation and are still preserved in permafrost. In exposures, relict glacier ice and intrasedimental ice often coexist and look alike but their genesis is strikingly different. This paper aims to present a detailed description and infer the origin of a massive ice body preserved in the permafrost 15 of Bylot Island (Nunavut). The massive ice exposure and core samples were described according to the cryostratigraphic approach, combining the analysis of permafrost cryofacies and cryostructures, ice crystallography, stable O-H isotopes and cation contents. The ice was clear to whitish in appearance with large crystals (cm) and small gas inclusions (mm) at crystal intersections, similar to observations of englacial ice facies commonly found on contemporary glaciers and ice sheets. -
22 AUG 2021 Index Acadia Rock 14967
19 SEP 2021 Index 543 Au Sable Point 14863 �� � � � � 324, 331 Belle Isle 14976 � � � � � � � � � 493 Au Sable Point 14962, 14963 �� � � � 468 Belle Isle, MI 14853, 14848 � � � � � 290 Index Au Sable River 14863 � � � � � � � 331 Belle River 14850� � � � � � � � � 301 Automated Mutual Assistance Vessel Res- Belle River 14852, 14853� � � � � � 308 cue System (AMVER)� � � � � 13 Bellevue Island 14882 �� � � � � � � 346 Automatic Identification System (AIS) Aids Bellow Island 14913 � � � � � � � 363 A to Navigation � � � � � � � � 12 Belmont Harbor 14926, 14928 � � � 407 Au Train Bay 14963 � � � � � � � � 469 Benson Landing 14784 � � � � � � 500 Acadia Rock 14967, 14968 � � � � � 491 Au Train Island 14963 � � � � � � � 469 Benton Harbor, MI 14930 � � � � � 381 Adams Point 14864, 14880 �� � � � � 336 Au Train Point 14969 � � � � � � � 469 Bete Grise Bay 14964 � � � � � � � 475 Agate Bay 14966 �� � � � � � � � � 488 Avon Point 14826� � � � � � � � � 259 Betsie Lake 14907 � � � � � � � � 368 Agate Harbor 14964� � � � � � � � 476 Betsie River 14907 � � � � � � � � 368 Agriculture, Department of� � � � 24, 536 B Biddle Point 14881 �� � � � � � � � 344 Ahnapee River 14910 � � � � � � � 423 Biddle Point 14911 �� � � � � � � � 444 Aids to navigation � � � � � � � � � 10 Big Bay 14932 �� � � � � � � � � � 379 Baby Point 14852� � � � � � � � � 306 Air Almanac � � � � � � � � � � � 533 Big Bay 14963, 14964 �� � � � � � � 471 Bad River 14863, 14867 � � � � � � 327 Alabaster, MI 14863 � � � � � � � � 330 Big Bay 14967 �� � � � � � � � � � 490 Baileys -
Map 2, Lake Superior State Water Trail from Knife River to Split Rock
ROUTE DESCRIPTION - River miles 26 to 60 (34 miles) (0.0 at Minnesota Entrance – Duluth Lift Bridge). 48.0 Private resort. [47° 07.135' N / 91° 30.265' W] 57.7 Little Two Harbors at Split Rock Lighthouse State Park. Access to park and lighthouse, a MAP 2 - Knife River to Split Rock Lighthouse State Park 51.0 Gooseberry Falls State Park and Gooseberry Minnesota Historic Site. Trailer access, parking, River. Carry-in access, parking, campground, 2 campground, picnic area and trails. 26.5 Knife River Marina. Access at launch area. watercraft campsites (available on a first-come, [47° 11.865' N / 91° 22.620' W] Parking, toilets. [46° 56.705' N / 91° 46.950' W] first-served basis), picnic area and trails. [47° 08.560' N / 91° 27.500' W] 59.0 Gold Rock Point. Wreck of the Madeira, driven 26.6 Knife River Beach. Carry-in access, rest area, ashore in 1905, lies scattered on the bottom in parking, toilet. Sand and pebble beach. 53.0 Thompson Beach. Four watercraft campsites 10 to 100' of water with portions clearly visible [46° 56.785' N / 91° 46.845' W] and rest area, toilet. No fires. First-come, in calm water. A popular recreational diving site, first-served. [47° 09.480' N / 91° 26.230' W] please be alert to divers in the water. Rest area 30.2 Private resort. Rocky Beach. on small beach nearby. No facilities. [46° 59.025' N / 91° 44.170' W] 53.8 Twin Points. Rest area, trailer access, parking. [47° 12.410' N / 91° 21.520' W] No camping permitted. -
Population in Goulais Bay, Lake Superior
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/264864682 Identification of a robust Lake Sturgeon (Acipenser fulvescens Rafinesque, 1917) population in Goulais Bay, Lake Superior Article in Journal of Applied Ichthyology · August 2014 DOI: 10.1111/jai.12566 CITATIONS READS 0 33 5 authors, including: Thomas C. Pratt Jennie Pearce Fisheries and Oceans Canada Pearce & Associates Ecological Research 49 PUBLICATIONS 489 CITATIONS 42 PUBLICATIONS 3,610 CITATIONS SEE PROFILE SEE PROFILE All content following this page was uploaded by Thomas C. Pratt on 08 April 2016. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Journal of Applied Ichthyology J. Appl. Ichthyol. (2014), 1–7 Received: December 6, 2013 © 2014 Her Majesty the Queen in Right of Canada Accepted: February 24, 2014 Journal of Applied Ichthyology © 2014 Blackwell Verlag GmbH doi: 10.1111/jai.12566 ISSN 0175–8659 Identification of a robust Lake Sturgeon (Acipenser fulvescens Rafinesque, 1917) population in Goulais Bay, Lake Superior By T. C. Pratt1, W. M. Gardner1, J. Pearce2, S. Greenwood3 and S. C. Chong3 1Fisheries and Oceans Canada, Great Lakes Laboratory for Fisheries and Aquatic Sciences, Sault Ste Marie, ON, Canada; 2Pearce & Associates Ecological Research, Sault Ste Marie, ON, Canada; 3Upper Great Lakes Management Unit, Ontario Ministry of Natural Resources, Sault Ste Marie, ON, Canada Summary anthropogenic activities due to specific life history character- Lake Sturgeon (Acipenser fulvescens Rafinesque, 1917) in istics, including slow growth and late maturation, intermit- Lake Superior are greatly depressed from their historic abun- tent spawning intervals, and habitat requirements such as dance, and few populations meet the rehabilitation goals specific temperature, flow velocities and substrate require- identified by management agencies. -
N Shore L. Superior: Geology, Scenery
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”). -
Land Information Ontario Data Description OTN Trailhead
Unclassified Land Information Ontario Data Description OTN Trailhead Disclaimer This technical documentation has been prepared by the Ministry of Natural Resources (the “Ministry”), representing Her Majesty the Queen in right of Ontario. Although every effort has been made to verify the information, this document is presented as is, and the Ministry makes no guarantees, representations or warranties with respect to the information contained within this document, either express or implied, arising by law or otherwise, including but not limited to, effectiveness, completeness, accuracy, or fitness for purpose. The Ministry is not liable or responsible for any loss or harm of any kind arising from use of this information. For an accessible version of this document, please contact Land Information Ontario at (705) 755 1878 or [email protected] ©Queens Printer for Ontario, 2012 LIO Class Catalogue OTN Trailhead Class Short Name: OTNTHD Version Number: 1 Class Description: The point at which the trail starts. A trailhead exists for each trail. A trail may consist of one or more trail segments. Abstract Class Name: SPSPNT Abstract Class Description: Spatial Single-Point: An object is represented by ONE and ONLY ONE point. Examples: A cabin, bird nest, tower. Tables in LIO Class: OTN Trailhead OTN_TRAILHEAD_FT The point at which the trail starts. A trailhead exists for each trail. A trail may consist of one or more trail segments. Column Name Column Mandatory Short Name Valid Values Type OGF_ID NUMBER Yes OGF_ID (13,0) A unique numeric provincial identifier assigned to each object. TRAIL_NAME VARCHAR2 Yes TRAIL_NAME (200) The name that the trail is most commonly known as. -
Assessing Impacts of Climate Change on Vulnerability of Brook Trout in Lake Superior’S Tributary Streams of Minnesota
Assessing Impacts of Climate Change on Vulnerability of Brook Trout in Lake Superior’s Tributary Streams of Minnesota Lucinda B. Johnson, Natural Resources Research Institute, University of Minnesota Duluth William Herb, St. Anthony Falls Laboratory, University of Minnesota, Minneapolis Meijun Cai, Natural Resources Research Institute, University of Minnesota Duluth Report to Minnesota Department of Natural Resources, upon completion of contract # MN DNR/1229G WO 47578 Natural Resources Research Institute technical report number NRRI/TR-2013/05 1 Executive Summary Water temperature is generally considered one of the primary physical habitat parameter determining the suitability of stream habitat for fish species, with effects on the mortality, metabolism, growth, behavior, and reproduction of individuals. In this study we assessed the potential threats of climate change on stream temperatures and flow regimes in Lake Superior tributary streams in Minnesota, USA. The study included deterministic models for stream flow and temperature of three study streams (Amity Creek, Baptism River, Knife River), and regional (empirical) models for specific flow and temperature parameters to give better spatial coverage of the region. Information on stream flow, stream temperature, and land cover was used to develop a brook trout presence/absence model to understand the current pattern of distribution of brook trout and predict future distributions under future climate. The hydrology of north shore streams is mainly driven by air temperature and precipitation. Historical air temperatures in the region have a significant upward trend, particularly since 1980. Global climate model (GCM) outputs project a continued increasing trend in air temperature, with an increase in mean annual air temperature of 2 to 3 °C by 2089.