Annual Report, for the Year 1893

Total Page:16

File Type:pdf, Size:1020Kb

Annual Report, for the Year 1893 Digitized by the Internet Archive in 2010 with funding from University of Toronto http://www.archive.org/details/annualreport22geol w THE GEOLOGICAL AND NATURAL HISTORY SURVEY OF MINNESOTA. The Twenty-second Annual Report, for the Year 1893. State Geologist. MINNEAPOLIS: HARRISON & SMITH, STATE PRINTERS. 1894. ISL7 THE BOARD OF RECrENTS OF THE UNIVERSITY OF MINNESOTA. Hon. Stephen Mahoney, Minneapolis ]895 Hon. Sidney M. Owen, Minneapolis 1895 Hon. John Lind, New Ulm 1896 Hon. John S. Pillsbury, Minneapolis 1896 Hon. Ozora P. Stearns, Duluth 1897 Hon. William Liggett, Benson 1897 Hon. Joel P. Heatwole, Northfleld 1897 Hon. Greenleaf Clark, St. Paul 1898 Hon. Cushsian K. Davis, St. Paul 1898 Hon. Knute Nelson, Governor of the State Ex-officto Hon. W. W. Pendergast, Supt. of Public Instruction Ex-officin Dr. Cyrus Northrop, President of the University Ex-officio OFFICERS OF THE BOARD. Hon. John S. Pillsbijry President Hon. D. L. Kiehle Recording Secretary President Cyrus Northrop Cm-respoiiding Secretary Joseph E. Ware Treamrer - ADDRESS. Minneapolis, Minn., Aug. 1, 1894. To the President of the Board, of Regents: Dear Sir —I have the honor to offer herewith the twenty second annual report of the Geological and Natural History- Survey of Minnesota. It embraces preliminary field reports on a large amount of work, contributed by the various assist- ants who were engaged on the survey during the season of 1893. It also contains lists of additions to the library and to the museum. Respectfully submitted, N. H. WINCHELL, State Geologist and Curator of the General Museum. GEOLOGICAL CORPS. N. H. WiNCHEi.L State Geologist Warren Upham Assistant Geologist U. S. Grant Assistant Geologist L. A. Ogaard Surveyor and Draughtsman SPECIAL ASSISTANTS IN 1893. Paleontology. E. O. Ulrich, J. M. Clarke, W. H. Scofield. Field geology and topography, in charge of parties. J. E. Todd, G. E. Culver, J. E. Spurr. a. H. Elftman, A. D. Meeds, H. B. Ayres, C. P. Berkey. General assistants. A. N. Winchell, E. R. Barton, H. B. HovLAND, H. C. Carel, H. E. White, R. P. Johnson, R. M. Wheeler. CONTENTS. PAGE I. Summary statement 1 II. List of rock samples collected to illustrate the notes of N. H. WiNCHELL. 1893 5 III. Preliminary report of field work during 1893 in north- eastern Minnesota, chiefly relating to the glacial drift. By Warren Upham 18 Areas examined 19 Mapping accomplished 19 Sketch of results of geological work 26 IV. Preliminary report of field work during 1893 in north- eastern Minnesota. By U. S. Grant 67 V. List of rock samples collected in 1893. By U. S. Grant 79 VI. List of rock samples collected in 1893. By A. D. Meeds 87 VII. Preliminary report of a reconnoissance in northwest- ern Minnesota during 1893. By J. E. Todd 90 Itinerary 90 Summary of principal results 92 VIII. Notes on the geology of Itasca county, Minnesota. By G. E. Culver 97 Introduction 97 Topography 98 Rock systems observed 102 Glacial phenomena Ill IX. Preliminary report of field work done in 1893. By J. E. Spurr 115 Itinerary 116 Area mapped 118 Salient points in the geology 119 X. List of rock samples collected in 1893. By J. E. Spurr 125 XL Preliminary report of levelling party. By C. P. Berkey 134 XII. Preliminary report of field work during 1893 in north- eastern Minnesota. By A. H. Elftman 141 General report of field work 141 Geological notes on northeastern Minnesota 150 XIII. List of rock samples collected in 1893. By A. H. Elftman 181 XIV. Museum additions 190 XV. Additions to the library since the report of 1892 198 XVI. The exhibit of the Survey at the Columbian Expo- sition. By N. H. Winchell 201 ILLUSTKATIONS. PAGE Fig. 1. Sections of quartzyte blocks, showing mode of change of color 102 Pig. 3. Hand specimen of ore-bearing rock, T. 56-24, showing the irregular banding seen in cross sections 103 Pig. 3. Showing stratigraphic relations at the falls of Prairie river 105 FACING PAGE Pl. I. Map of the glacial geology of northern Minnesota 19 PL. II 44 Pig. 1. Section on the D. & I R. R. R. in the north part of sec. 1, T. 54, R. 12, 3 miles northwest of Highland station. Pig. 2. Section on the D. & I. R. R. R., in the south part of the S W. i of sec. 23, T. 55, R. 12, -k to i mile north of Thomas siding. Pig. 3. Section on the D. & I. R. R. R., in the southeastern part of sec. 15, T. 55. R. 12, 2^ miles southeast of Cloquet River station. Pig. 4. Section of part of the west side of the Biwabik Iron mine, Oct. 18, 1893; showing in the basal part of the drift two large masses of the red iron ore which were glacially uplifted and probably transported very short distances. Pl. III. Section across the Mesabi range 120 Pl. IV. Two profiles across Cook county, from Brul6 lake and from Grand Marais N. N. W. to the International boundary 138 Pl. V. Map of the west central part of Lake county..,. 150 Pl. VI 160 Pig. 1. Geological map of the western end of Birch lake and adjoining country southward. Pig. 2. Cross section from Moose lake to Snow- bank lake. I. SUMMARY STATEMENT. An effort was made in 1893 to finish that amount of field-work necessary to warrant the preparation of the final rejDort and maps of that portion of the state remaining unpublished. Al- though there are still many unknown elements in the geology of the northern part of the state, and some considerable tracts, remote from routes of travel, some of which have not been "subdivided"' by the township survey of the United States gov- ernment, which the parties of the geological survey have not been able to visit and map, yet it is thought best to close up the active work in the field and to enter upon the preparation of the last volume of the final report. It was with an earnest de- sire to round out the present survey with what might be called a final report, showing its completed results in systematic rela- tions, within the reasonable term of a single administration, that the writer, four years ago, volunteered to pledge the com- pletion of the field-work for the sum of twenty-five thousand dollars. This was stated to the appropriation committees of the Legislature of 1891. Fifteen thousand dollars were appro- priated by that Legislature. The last Legislature (1893) ap- propriated ten thousand dollars under similar representations. Although the full sum of twenty- five thousand dollars has not yet been expended on the field-work, yet so much has been done that nearly all the remaining plates, which will represent the geology in the final report, can be drawn. There will be need yet of special examination in some difficult and some important areas, where the opportunities of the past have not been favor- able to entirely and satisfactorily understand the geological structure. Practically, however, the campaign of 1893 may be said to have finished the field-work. The rest of the time to be devoted to this work by the writer will be given, as now con- templated, to the preparation of the last final volume, with the necessary accompanying maps. 2 TWENTY -SECOND ANNUAL REPORT During the last season parties were in the field under the fol- lowing assistants: Prof. J. E. Todd, in the northwestern portion of the state, north and east of Red lake. Prof. G. E. Culver, in Itasca county. Mr. Warren Upham, in Aitkin and Cass counties. Mr. J. E. Spurr, on the Mesabi range and southward in St. Louis county. Mr. A. D. Meeds, on the Mesabi range and southward in St. Louis county. Mr. A. H. Elftman, on the Mesabi range and southward in Lake county. Dr. U. S. Grant, on the Mesabi range and southward in Cook county. Mr. C. P. Berkey, from Grand Marais northward, in Cook county, and in co- operation with Dr. Grant. The writer also was in the field in different places, but chiefly in Cook county. Mr. H. B. Ayres began work in Carlton county, but was interrupted by sickness and afterward by other engage- ments, and accomplished but little. It is planned that he will finish his allotment of work in Carlton county the coming season. In view of the proposed final mapping of the rest of the state it was deemed highly desirable to obtain such hypsometric data as would warrant the approximate drawing of contour lines in the manner shown on the final plates already published in vol- umes I and II. Each party was furnished with the necessary instructions and apparatus for platting these lines en the field maps which they carried, while at the same time a continuous hourly reading of a mercurial barometer was recorded a>x, "Mesaba* station," by means of which the simultaneous aneroid readings of the different parties could be corrected and reduced to a uniform basis, and referred to the sea level. In this way a large mass of data was obtained which, when corrected and platted, will result in contour lines, 50 feet separate, over a large area in the northern part of the state. This will give an ex- pression of a preliminary topographical reconnaissance, and will serve as an introduction to the topographical map which it is hoped may yet be constructed. At the same time it is an in- * Tdore luiving been great diversity In the spelling of this word, the matter was brought before the United States Board of Qcouraphical Names, of which the Superin- tendent of the Coast and Geodetic Survey is president.
Recommended publications
  • 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.
    [Show full text]
  • Minnesota's Mineral Resources
    CHAPTER • 9 Minnesota's Mineral Resources IN MINNESOTA the production of iron ore is far more valuable economically than the total of all other mineral products, but im­ portant industries are based on Minnesota's other geological forma­ tions as well. Architectural, monumental, and structural stone are produced from granite, limestone, dolomite, and other Minnesota rocks. Gravel and sand are excavated and processed, and clay is used for many ceramic products. :Manganese in important amounts occurs in the iron ores of the Cuyuna district. Finally, although they are often not thought of as mineral products, two of our most im­ portant mineral resources are water and soil. The iron ores and mining operations of the Mesabi, Vermilion, and Cuyuna iron-bearing districts and of the southeastern lYlinnesota counties will be discussed in detail in later chapters, but a few sta­ tistics on Minnesota's iron ore industry may remind us how impor­ tant this geological heritage is. The following is an estimate of Min­ nesota's iron ore reserves, made on lYlay 1, 1961: Gross Tons Mesabi Range 500,799,179 Vermilion Range 9,755,974 Cuyuna Range 36,530,000 Fillmore County 'il,860,337 Total iron ore 549,945,490 172 MI NESOTA'S MINERAL RESOURCES The total production of iron ore in Minne ota to January 1, 1962, was 2,529,737,553 tons. Total taxes paid on iron ore to January 1, 1961 , were approximately $1,257,448,400, a very important source of funds for the state government. Slightly over 60 per cent of the total iron ore produced in the United States has come from l\1inne- ota.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • LAND USE and WATER RESOURCES in the MINNESOTA NORTH SHORE DRAINAGE BASIN Carol A. Johnston, Brian Allen, John Bonde, Jim Sal6s
    LAND USE AND WATER RESOURCES IN THE MINNESOTA NORTH SHORE DRAINAGE BASIN Carol A. Johnston, Brian Allen, John Bonde, Jim Sal6s, and Paul Meysembourg Natural Resources GIS Laboratory (NRGIS) NRRI Technical Report NRRI/TR-91/07 July 1991 Research funded by the Legislative Commission on Minnesota Resources INTRODUCTION Rivers and streams are an important feature of the Minnesota North Shore. A dozen state parks and waysides lie at the mouths of rivers that cascade down the steep slopes of Minnesota’s northern highlands into Lake Superior,-carving beautiful waterfalls out the basalt bedrock. But the rivers that drain the 5778 km2 North Shore drainage basin provide more than scenic beauty, delivering nutrients and other materials to Lake Superior. Lake Superior’s tributaries provide about half of its annual water input (Bennett 1978), more than 90% of its total dissolved solids, and 68% of its phosphorus (Upper Lakes Reference Group 1977). Moreover, the water from these tributaries is delivered to the nearshore zone, in which Lake Superior’s biological communities are concentrated (Rao 1978, Munawar and Munawar 1978, Watson and Wilson 1978). Since these communities of bacteria, algae, and zooplankton form the basis of the food web, the productivity and integrity of Lake Superior’s waters are heavily dependent on water supplied by the North Shore drainage basin. While some of the materials delivered by rivers and streams are essential to aquatic life, excessive inputs of sediment and nutrients can cause nonpoint source pollution, the flow of pollutants from land to water in stormwater runoff or from seepage through the soil.
    [Show full text]
  • Economic Analysis of Critical Habitat Designation for the Canada Lynx
    ECONOMIC ANALYSIS OF CRITICAL HABITAT DESIGNATION FOR THE CANADA LYNX Final Economic Analysis | October 31, 2006 prepared for: Division of Economics U.S. Fish and Wildlife Service 4401 N. Fairfax Drive Arlington, VA 22203 prepared by: Industrial Economics, Incorporated 2067 Massachusetts Avenue Cambridge, MA 02140 Final Economic Analysis – October 31, 2006 TABLE OF CONTENTS EXECUTIVE SUMMARY SECTION 1 FRAMEWORK FOR THE ANALYSIS 1-1 1.1 Approach to Estimating Economic Effects 1-2 1.2 Scope of the Analysis 1-6 1.3 Analytic Time Frame 1-11 1.4 Information Sources 1-11 1.5 Structure of Report 1-12 SECTION 2 BACKGROUND 2-1 2.1 Proposed Critical Habitat Designation 2-1 2.2 Threats to the Species and its Habitat 2-8 SECTION 3 TIMBER ACTIVITIES 3-1 3.1 Profiles of Regional Timber Industries 3-2 3.2 Changes in Timber Management Practices as a Result of Lynx Conservation Efforts 3-9 3.3 Pre-Designation Impacts to Timber Activities 3-12 3.4 Post-Designation Impacts to Timber Activities 3-13 3.5 Caveats 3-18 SECTION 4 DEVELOPMENT 4-1 4.1 Summary of Results 4-2 4.2 Methods and Assumptions 4-4 4.3 Unit by Unit Analysis 4-8 SECTION 5 RECREATION 5-1 5.1 Summary of Impacts to Recreation 5-1 5.2 Methods and Assumptions 5-5 5.3 Snowmobiling Scenario 2: Estimated Impacts by Unit 5-12 5.4 Hunting and Trapping 5-22 5.5 Other Recreational Projects 5-24 Final Economic Analysis – October 31, 2006 SECTION 6 PUBLIC LANDS MANAGEMENT AND CONSERVATION PLANNING 6-1 6.1 Summary of Impacts to Public Lands Management and Conservation Planning 6-1 6.2 Methods and Assumptions
    [Show full text]
  • Superior Hiking Trail Rises to Craggy Peaks and Plunges Into Forests of Birch, Maple, Spruce, Cedar, and Pine
    Photography by Gary Alan Nelson A Trail With a View For spectacular vistas, follow a footpath along the North Shore’s rocky ridge. Are you up for a day hike in one of Minnesota’s most dramatic landscapes? The Superior Hiking Trail rises to craggy peaks and plunges into forests of birch, maple, spruce, cedar, and pine. It crosses rushing streams and opens to panoramas of Lake Superior and the highlands. Built just for hiking and backpacking, the 296-mile footpath runs from Jay Cooke State Park to the Ontario border. Each year more than 50,000 hikers explore parts of this sensational trail. With 53 trailhead parking lots, one about every 5 to 10 miles, you can easily hop on and hike for an hour or a day. Here’s a look at some of the sights along three stretches. 26 Minnesota Conservation Volunteer July–August 2014 27 Gooseberry to Split Rock Gooseberry Falls State Park is a popular starting point. In the park, a bench overlooks the Gooseberry River. Markers assure hikers they’re on trail. This 6-mile section follows Bread Loaf Ridge. Atop a cliff, hikers gain a bird’s-eye view. During spring and fall, hikers can see migratory birds along this North Shore flyway. July–August 2014 29 Waterfalls on the Gooseberry River create a soundscape. From time to time, hikers get a view of the open sky over the big lake. In the late 1890s, lumber companies logged the land along the river. By the 1920s logging and fire had cleared the pines.
    [Show full text]
  • Survey and Fish Man- E Streams of the North Shore Watershed
    nical Bulletin Number 1 SURVEY AND FISH MAN- E STREAMS OF THE NORTH SHORE WATERSHED LLOYD L. SM ITH, JR. and JOHN B. MOYLE DEPARTMENT Of CONSERVATION ISION OF GAME AND FISH This document is made available electronically by the Minnesota Legislative Reference Library as part of an ongoing digital archiving project. http://www.leg.state.mn.us/lrl/lrl.asp (Funding for document digitization was provided, in part, by a grant from the Minnesota Historical & Cultural Heritage Program.) MINNESOTA DEPARTMENT OF CONSERVATION DIVISION OF GAME AND FISH A BIOLOGICAL SURVEY AND FISHERY MAN­ AGEMENT PLAN FOR THE STREAMS OF THE LAKE SUPERIOR NORTH SHORE WATERSHED LLOYD L. SMITH, JR. Research Supervisor and JOHN B. MOYLE Aquatic Biologist A CONTRIBUTION FROM THE MINNESOTA FISHERIES RESEARCH LABORATORY TECHNICAL BULLETIN NO. 1 1 9 4 4 STATE OF MINNESOTA The Honorable Edward J. Thye ................... Governor MINNESOTA DEPARTMENT OF CONSERVATION Chester S. Wilson ............................ Commissioner E. V. Willard ........................ Deputy Commissioner DIVISION OF GAME AND FISH Verne E. Joslin ............................. Acting Director E. R. Starkweather ........................ Law Enforcement Norman L. Moe ........................... Fish Propagation George Weaver ........................ Commercial Fisheries Stoddard Robinson .................... Rough Fish Removal Lloyd L. Smith,- Jr........................ Fisheries Research Thomas Evans ........................ Stream Improvement Frank Blair .......................... ~ .. Game Management
    [Show full text]
  • Ten Thousand Years of Population Relationships at the Prairie
    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 5-2001 Ten Thousand Years of Population Relationships at the Prairie- Woodland Interface: Cranial Morphology in the Upper Midwest and Contiguous Areas of Manitoba and Ontario Susan Mary Myster University of Tennessee - Knoxville Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Anthropology Commons Recommended Citation Myster, Susan Mary, "Ten Thousand Years of Population Relationships at the Prairie-Woodland Interface: Cranial Morphology in the Upper Midwest and Contiguous Areas of Manitoba and Ontario. " PhD diss., University of Tennessee, 2001. https://trace.tennessee.edu/utk_graddiss/3532 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Susan Mary Myster entitled "Ten Thousand Years of Population Relationships at the Prairie-Woodland Interface: Cranial Morphology in the Upper Midwest and Contiguous Areas of Manitoba and Ontario." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in Anthropology. Richard L. Jantz, Fred H. Smith, Major Professor We have read this dissertation and recommend its acceptance: Charles H. Faulkner, Lyle W. Konigsberg, David A. Gerard Accepted for the Council: Carolyn R.
    [Show full text]
  • North Shore Periphyton [Attached Algae] Survey
    North Shore Periphyton [Attached Algae] Survey July 2003 Jeff Jasperson MPCA Summer Intern Surveyed Streams: Tischer Creek Amity Creek and Lower Lester River Talmadge River French River Knife River Encampment River Gooseberry River Brule River General Trends · Periphyton abundance was greatest in the two Duluth urban streams (Tischer, Amity), and was not observed in the most rural stream (Brule) · Despite a few exceptions, periphyton levels were lower in streams farther from Duluth · Sunlight appears to be the limiting factor for periphyton growth in streams near the Duluth area. Essentially wherever adequate sunlight hit these streams, periphyton was observed · As expected, rivers with more pristine watersheds had lower levels of periphyton · In some survey streams, especially Knife River and Amity and Tischer Creeks, there was a noticeable increase in periphyton abundance near bridges or heavily used roads · Both epipelon (growth on soft sediments) and epilithion (growth on stones) periphyton were observed. Epilithion forms were by far the most common in North Shore streams. · Streamflow seems to factor into periphyton growth in North Shore streams. Riffles with moderate flow were found to support periphyton communities more often than stagnant backwaters or side pools. Growths along fast-flowing, shallow waterfalls were frequent. Stream: Tischer Creek Location of Survey: Greysolon Street to London Rd. Overpass (Duluth) Date/Time: July 24, 2003 @ 1345 In a survey of Tischer Creek from London Road to the St. Marie Street bridge, abundant growths of periphyton were observed. Nearly every region of the stream within the survey range exhibited very noticeable growths, making it difficult to establish any clear periphyton trends for this particular stream.
    [Show full text]
  • Gunflint Lake Cabin Property Guide
    PlansMatter architectural vacation rentals Welcome! Gunflint Lake Cabin 1 Essential Information 2 House Truths + Rules 3 Operating Instructions 4 Local Eats, Drinks + Provisions 5 Local Activities 2418 Bryant Avenue South | Minneapolis MN 55405 USA | 800.921.6067 | [email protected] | www.PlansMatter.com PlansMatter !1 of !6 architectural vacation rentals Essential Information Location Gunflint Lake Cabin is north! Canada is right across the lake. The cabin is 47 miles from the nearest town, Grand Marais, a 1.5 hour drive. We recommend you plan to arrive before nightfall and stop in Grand Marais on your way to the cabin for supplies and a bite to eat. If you forget a few things (like coffee or insect spray) there are general stores nearby that stock basic provisions. Gunflint Lake Cabin is a place to disconnect from technology. Cell phone service generally stops 10 miles up the Gunflint Trail out of Grand Marais and there is no internet service at the cabin. Address 611 South Gunflint Lake Road, Grand Marais MN 55604 Parking + Front Door There is exterior parking for 2 cars immediately adjacent to the cabin. The front door of the cabin is the single solid pine door. Not the multiple glass deck doors. Check-In 3pm Check-Out 2pm Check-In/Out Process The cabin will be unlocked when you arrive and you can leave it unlocked when you depart. There is no need to lock the cabin if you are on the water or exploring the area. Day-to-Day Contact PlansMatter, [email protected], 800.921.6067 Emergency Contact Greg and Barb Gecas, owners of Heston's Lodge, 218-338-2243 2418 Bryant Avenue South | Minneapolis MN 55405 USA | 800.921.6067 | [email protected] | www.PlansMatter.com PlansMatter !2 of !6 architectural vacation rentals Cabin Telephone The phone number for the cabin’s land line is 218.388.2211.
    [Show full text]