Implications of Photogeologic Linears in the South Long Lake Area, Alpena and Presque Isle Counties, Michigan

Total Page:16

File Type:pdf, Size:1020Kb

Implications of Photogeologic Linears in the South Long Lake Area, Alpena and Presque Isle Counties, Michigan Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 4-1973 Implications of Photogeologic Linears in the South Long Lake Area, Alpena and Presque Isle Counties, Michigan Richard E. Kimmel Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons, Geomorphology Commons, and the Hydrology Commons Recommended Citation Kimmel, Richard E., "Implications of Photogeologic Linears in the South Long Lake Area, Alpena and Presque Isle Counties, Michigan" (1973). Master's Theses. 615. https://scholarworks.wmich.edu/masters_theses/615 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. IMPLICATIONS OF PHOTOGEOLOGIC LINEARS IN THE SOUTH LONG LAKE AREA, ALPENA AND PRESQUE ISLE COUNTIES, MICHIGAN by Richard E. Kimmel A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the Degree of Master of Arts Western Michigan University Kalamazoo, Michigan April 1973 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. IMPLICATIONS OF PHOTOGEOLOGIC LINEARS IN THE SOUTH LONG LAKE AREA, ALPENA AND PRESQUE ISLE COUNTIES, MICHIGAN Richard Elmer Kimmel, M. A. Western Michigan University, 1973 There are numerous linear features in Alpena and Presque Isle Counties, Michigan, which are generally visible on aerial photographs. These photolinears trend in two general directions, northeast-southwest and northwest-southeast. These two sets are perpendicular to each other, and represent vector means of two fracture sets. The development of the photolinears began in Early Devonian. Throughout its history, ground water flowed along underground channels connecting fracture intersections. This underground drainage network is responsible for many of the photolinears. Some of the photolinears can be attributed tb Early Devonian ground water activity and subsequent collapse of the Salina Salt basin, and some are attributable to more re­ cent ground water activity. Some photolinears are the result of differential erosional resistance between different beds of rock, or the result of progressive stages of Pleistocene lakes. with permission of the copyright owner. Further reproduction prohibited without permission. INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again — beginning below the first row and continuing on until complete. 4. The majority of users indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation. Silver prints of "photographs" may be ordered at additional charge by writing the Order Department, giving the catalog number, title, author and specific pages you wish reproduced. 5. PLEASE NOTE: Some pages may have indistinct print. Filmed as received. Xerox University Microfilms 300 North Zeeb Road Ann Arbor. Michigan 48106 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. I I MASTERS THESIS M-480M- KIMMEL, Richard Elmer IMPLICATIONS OF PH0T06E0L0GIC LINEARS IN THE SOUTH LONG LAKE AREA, ALPENA AND PRESQUE ISLE COUNTIES, MICHIGAN. Western Michigan University, M.A., 1973 Geology University Microfilms, A XEROX Company, Arm Arbor, Michigan Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. TABLE OF CONTENTS chapter page Acknowledgements vii I. Introduction ........................................................................... 1 Geographic Location of the Area ...................................... 1 Geologic Position of Traverse G ro u p .............................. 4 Scope of Investigation ........................................................... 4 Previous W ork .................................................................... 5 I I. Stratigraphy ............................................................................ 9 Definition of the Traverse Group ...................................... 9 Descriptive Stratigraphy ................................................... 11 Bell Shale .................................................................... 11 Rockport Quarry Lim estone .................................. 12 Ferron Point Formation .......................................... 14 Genshaw F o rm a tio n ............................................... 15 Newton Creek Lim estone ...................................... 21 Alpena Limestone . .......................................... 23 Fourmile Dam Form ation ...................................... 24 Norway Point F o rm a tio n ............................................25 Potter Farm Form ation ................................................ 26 Thunder Bay Limestone .......................................... 27 Squaw B3y Limestone ...............................................27 Surface formations ................................................... 28 III. Photolinears ...................................................................................32 Definitions and Descriptions of Linears ............................... 32 Methods of S t u d y .................................................................33 Statistical Analysis ........................................................... 38 Photolinears of the South Long Lake A re a ...........................49 Opechee and Little Opechee Lines ............................... 50 Killians L i n e ........................................................... 51 Three Lakes Line ....................................................... 51 Mindock L in e ........................................................... 55 Algonquin L i n e .............................................................56 Dagett Line ..................................................................... 57 Bolton Line.....................................................................58 Cathro Line .....................................................................59 Weide L in e.....................................................................59 Other photolinears ........................................................ 60 — i i — Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. TABLE OF CONTENTS (CONT'D) chapter page Origins of P h o to lin e ars .......................................... 61 Significance of Photolinears ...................................... 66 IV . Ground Water and Karst F e a tu re s .......................................... 68 Surface Drainage ............................................................... 68 Karst Features of Alpena and Presque Isle Counties . 69 Sinkholes ................................................................... 69 Devil's Lake ............................................................... 73 Rainy L a k e ............................................................... 74 Sunken Lake—Mystery V a lle y .................................. 75 Summary of Karst Features .............................................. 76 V. Conclusions ................................................................................ 78 Suggested Future W o r k .................................................. 79 References C ite d ....................................................................... 81 Appendix i ................................................................................ 85 Appendix i i................................................................................ 90 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. LIST OF ILLUSTRATIONS figure page 1. Location of study a r e a ............................................................................. 2 2. Bedrock geology of the South Long Lake area, M ich ig an ...................... 3 3. Stratigraphic column of the Traverse Group of Alpena and . Presque Isle Counties, Michigan ...............................................................
Recommended publications
  • Basement Control on the Development of Selected Michigan Basin Oil and Gas Fields As Constrained by Fabric Elements in Paleozoic Limestones
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 6-1991 Basement Control on the Development of Selected Michigan Basin Oil and Gas Fields as Constrained by Fabric Elements in Paleozoic Limestones Robert Thomas Versical Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Versical, Robert Thomas, "Basement Control on the Development of Selected Michigan Basin Oil and Gas Fields as Constrained by Fabric Elements in Paleozoic Limestones" (1991). Master's Theses. 1010. https://scholarworks.wmich.edu/masters_theses/1010 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. BASEMENT CONTROL ON THE DEVELOPMENT OF SELECTED MICHIGAN BASIN OIL AND GAS FIELDS AS CONSTRAINED BY FABRIC ELEMENTS IN PALEOZOIC LIMESTONES by Robert Thomas Versical A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan June 1991 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. BASEMENT CONTROL ON THE DEVELOPMENT OF SELECTED MICHIGAN BASIN OIL AND GAS FIELDS AS CONSTRAINED BY FABRIC ELEMENTS IN PALEOZOIC LIMESTONES Robert Thomas Versical, M.S. Western Michigan University, 1991 Hydrocarbon bearing structures in the Paleozoic section of the Michigan basin possess different structural styles and orientations. Quantification of the direction and magnitude of shortening strains by applying a calcite twin-strain analysis constrains the mechanisms by which these structures may have developed.
    [Show full text]
  • A Framework for in Northwest Michigan
    A Framework For Energy In Northwest Michigan 2014 REPORT 1 A Framework for Transportation in planning, and decision-making and adopted goals from local plans Northwest Michigan was prepared as processes, and will help to identify and planning initiatives. Strategies are part of the Framework for Our Future: A the steps a community can take to not intended as recommendations, Regional Prosperity Plan for Northwest address a local issue, if desired. nor do they supersede and local Michigan, a regional resource for local government decision-making. governments, community organizations The Framework for Our Future was Moreover, the Framework is not working to meet local goals. developed by Networks Northwest intended for, nor shall it be used (formerly the Northwest Michigan for, infringing upon or the taking of The Framework was developed with Council of Governments) with input personal property rights enjoyed by support from the US Department and partnerships from a variety of the residents of Northwest Michigan. of Housing and Community community stakeholders and members Rather, the information included in Development’s Office of Economic of the public. An intensive community the Framework is instead intended Resilience and Partnership for outreach process featured a wide to serve as a compilation of best Sustainable Communities, the Michigan variety of opportunities for participation practices to help guide local decision- Department of Transportation, the from the public: events, surveys, focus makers who would like to address the Michigan State Housing Development groups, online forums, and public issues identified in the Framework. Authority, and the State of Michigan discussions were held region-wide Regional Prosperity Initiative, as well as throughout the process.
    [Show full text]
  • Cambrian Ordovician
    Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation.
    [Show full text]
  • Radio Stations in Michigan Radio Stations 301 W
    1044 RADIO STATIONS IN MICHIGAN Station Frequency Address Phone Licensee/Group Owner President/Manager CHAPTE ADA WJNZ 1680 kHz 3777 44th St. S.E., Kentwood (49512) (616) 656-0586 Goodrich Radio Marketing, Inc. Mike St. Cyr, gen. mgr. & v.p. sales RX• ADRIAN WABJ(AM) 1490 kHz 121 W. Maumee St. (49221) (517) 265-1500 Licensee: Friends Communication Bob Elliot, chmn. & pres. GENERAL INFORMATION / STATISTICS of Michigan, Inc. Group owner: Friends Communications WQTE(FM) 95.3 MHz 121 W. Maumee St. (49221) (517) 265-9500 Co-owned with WABJ(AM) WLEN(FM) 103.9 MHz Box 687, 242 W. Maumee St. (49221) (517) 263-1039 Lenawee Broadcasting Co. Julie M. Koehn, pres. & gen. mgr. WVAC(FM)* 107.9 MHz Adrian College, 110 S. Madison St. (49221) (517) 265-5161, Adrian College Board of Trustees Steven Shehan, gen. mgr. ext. 4540; (517) 264-3141 ALBION WUFN(FM)* 96.7 MHz 13799 Donovan Rd. (49224) (517) 531-4478 Family Life Broadcasting System Randy Carlson, pres. WWKN(FM) 104.9 MHz 390 Golden Ave., Battle Creek (49015); (616) 963-5555 Licensee: Capstar TX L.P. Jack McDevitt, gen. mgr. 111 W. Michigan, Marshall (49068) ALLEGAN WZUU(FM) 92.3 MHz Box 80, 706 E. Allegan St., Otsego (49078) (616) 673-3131; Forum Communications, Inc. Robert Brink, pres. & gen. mgr. (616) 343-3200 ALLENDALE WGVU(FM)* 88.5 MHz Grand Valley State University, (616) 771-6666; Board of Control of Michael Walenta, gen. mgr. 301 W. Fulton, (800) 442-2771 Grand Valley State University Grand Rapids (49504-6492) ALMA WFYC(AM) 1280 kHz Box 669, 5310 N.
    [Show full text]
  • G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine
    DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY GEOLOGY OF THE CRAIG QUADRANGLE, ALASKA By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Open-File Report 83-91 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and strati graphic nomenclature Menlo Park, California 1983 Geology of the Craig Quadrangle, Alaska By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Introduction This report consists of the following: 1) Geologic map (1:250,000) (Fig. 1); includes Figs. 2-4, index maps 2) Description of map units 3) Map showing key fossil and geochronology localities (Fig. 5) 4) Table listing key fossil collections 5) Correlation diagram showing Silurian and Lower Devonian facies changes in the northwestern part of the quadrangle (Fig. 6) 6) Sequence of Paleozoic restored cross sections within the Alexander terrane showing a history of upward shoaling volcanic-arc activity (Fig. 7). The Craig quadrangle contains parts of three northwest-trending tectonostratigraphic terranes (Berg and others, 1972, 1978). From southwest to northeast they are the Alexander terrane, the Gravina-Nutzotin belt, and the Taku terrane. The Alexander terrane of Paleozoic sedimentary and volcanic rocks, and Paleozoic and Mesozoic plutonic rocks, underlies the Prince of Wales Island region southwest of Clarence Strait. Supracrustal rocks of the Alexander terrane range in age from Early Ordovician into the Pennsylvanian, are unmetamorphosed and richly fossiliferous, and aopear to stratigraphically overlie pre-Middle Ordovician metamorphic rocks of the Wales Group (Eberlein and Churkin, 1970).
    [Show full text]
  • Middle Devonian Formations in the Subsurface of Northwestern Ohio
    STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 SCIENTIFIC AND TECHNICAL STAFF OF THE OHIO DIVISION OF GEOLOGICAL SURVEY ADMINISTRATIVE SECTION Horace R. Collins, State Geologist and Di v ision Chief David K. Webb, Jr., Geologist and Assistant Chief Eleanor J. Hyle, Secretary Jean S. Brown, Geologist and Editor Pauline Smyth, Geologist Betty B. Baber, Geologist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, Geologist and Section Head William J. Buschman, Jr., Geologist and Section Head Richard M. Delong, Geologist Michael J. Clifford, Geologist G. William Kalb, Geochemist Adriaan J anssens, Geologist Douglas L. Kohout, Geologis t Frederick B. Safford, Geologist David A. Stith, Geologist Jam es Wooten, Geologist Aide Joel D. Vormelker, Geologist Aide Barbara J. Adams, Clerk· Typist B. Margalene Crammer, Clerk PUBLICATIONS SECTION LAKE ERIE SECTION Harold J. Fl inc, Cartographer and Section Head Charles E. Herdendorf, Geologist and Sectwn Head James A. Brown, Cartographer Lawrence L. Braidech, Geologist Donald R. Camburn, Cartovapher Walter R. Lemke, Boat Captain Philip J. Celnar, Cartographer David B. Gruet, Geologist Aide Jean J. Miller, Photocopy Composer Jean R. Ludwig, Clerk- Typist STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 GEOLOGY SERVES OHIO CONTENTS Page Introduction . 1 Previous investigations .. .. .. .. .. .. .. .. .. 1 Study methods . 4 Detroit River Group . .. .. .. ... .. ... .. .. .. .. .. .. .. ... .. 6 Sylvania Sandstone ..........................
    [Show full text]
  • PROGRAMME ABSTRACTS AGM Papers
    The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important.
    [Show full text]
  • Cheboygan County Local Ordinance Gaps Analysis
    Cheboygan County Local Ordinance Gaps Analysis An essential guide for water protection Tip of the Mitt Watershed Council Written and compiled by Grenetta Thomassey, Ph.D. Cheboygan County Local Ordinance Gaps Analysis An essential guide for water protection Tip of the Mitt Watershed Council Written and compiled by Grenetta Thomassey, Ph.D. This publication is designed to provide accurate and authoritative information in regard to the subject matter covered. Mention of specific companies, organizations, or authorities in this book do not imply endorsement by the author or publisher, nor does the mention of specific companies, organizations or authorities imply that they endorse this book, its author or publisher. Internet addresses and phone numbers given in this book were accurate at the time of printing. Library of Congress Catalog Thomassey, Grenetta Cheboygan County Local Ordinance Gaps Analysis ISBN 978-1-889313-07-8 1. Government 2. Water Protection 3. Cheboygan County, Michigan © 2014 Tip of the Mitt Watershed Council All rights reserved. Printed in the United States of America Photography by: Kristy Beyer If you want to reproduce this book or portions of it for reasons consistent with its purpose, please contact the publisher: Tip of the Mitt Watershed Council 426 Bay Street Petoskey, MI 49770 (231) 347-1181 phone (231) 347-5928 fax www.watershedcouncil.org This work should be cited as follows: Thomassey, Grenetta. Cheboygan County Local Ordinance Gaps Analysis 2014. Tip of the Mitt Watershed Council, Petoskey, MI 49770 ~ ACKNOWLEDGEMENTS
    [Show full text]
  • Schmitz, M. D. 2000. Appendix 2: Radioisotopic Ages Used In
    Appendix 2 Radioisotopic ages used in GTS2020 M.D. SCHMITZ 1285 1286 Appendix 2 GTS GTS Sample Locality Lat-Long Lithostratigraphy Age 6 2s 6 2s Age Type 2020 2012 (Ma) analytical total ID ID Period Epoch Age Quaternary À not compiled Neogene À not compiled Pliocene Miocene Paleogene Oligocene Chattian Pg36 biotite-rich layer; PAC- Pieve d’Accinelli section, 43 35040.41vN, Scaglia Cinerea Fm, 42.3 m above base of 26.57 0.02 0.04 206Pb/238U B2 northeastern Apennines, Italy 12 29034.16vE section Rupelian Pg35 Pg20 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 145.8 m above base 31.41 0.03 0.04 206Pb/238U 145.8, equivalent to GSSP), northeastern Apennines, Italy 12 28003.83vE of section MCA/84-3 Pg34 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 142.8 m above base 31.72 0.02 0.04 206Pb/238U 142.8 GSSP), northeastern Apennines, Italy 12 28003.83vE of section Eocene Priabonian Pg33 Pg19 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 14.7 m above base of 34.50 0.04 0.05 206Pb/238U 14.7, equivalent to Ancona, northeastern Apennines, 13.6011 E section MAS/86-14.7 Italy Pg32 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.9 m above base of 34.68 0.04 0.06 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E section Italy Pg31 Pg18 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.7 m above base of 34.72 0.02 0.04 206Pb/238U
    [Show full text]
  • Eurasian Ruffe (Gymnocephalus Cernua), Native to Northern Europe and Asia, Have Threatened the Great Lakes and Surrounding States Since the Late 1980S
    State of Michigan’s Status and Strategy for Eurasian Ruffe Management Scope Invasive Eurasian ruffe (Gymnocephalus cernua), native to northern Europe and Asia, have threatened the Great Lakes and surrounding states since the late 1980s. The goals of this document are to: • Summarize the current understanding level of the biology and ecology of Eurasian ruffe. • Summarize the current management options for Eurasian ruffe in Michigan. • Identify possible future directions of Eurasian ruffe management in Michigan. Biology and Ecology I. Identification Eurasian ruffe, also known as blacktail Gary Cholwek – National Biological Service or river ruffe, is a member of genus Gymnocephalus within Percidae. Eurasian ruffe is a small, aggressive, benthic fish native to Europe and Asia. The species resemble yellow perch with distinct walleye markings (McLean 1997). The Eurasian ruffe can be distinguished from other perch by their large, jointed dorsal fin composed of 11 to 16 spines with rows of dark spots between each spine. Adult ruffe are typically five to six inches long with large individuals rarely exceeding 10 inches. They have a small, downturned mouth, lack scales on their head, and are slimy when handled (McLean 1997). Eurasian ruffe have two dorsal fins, one spiny (anterior) and one soft (posterior), and are commonly mistaken for troutperch, which have only a single dorsal fin. Their coloration consists of an olive-brown dorsal surface, pale sides, and a yellow underside (Fuller 2014, Hajjar 2002). Eurasian ruffe have two ventral fins with sharp spines on the leading edges; the anterior fin has only one spine where the posterior fin has two spines.
    [Show full text]
  • Introduction Paxton Quarry
    Geological Society of America Centennial Field Guide— limestones followed by deep-water anaerobic black North-Central Section, 1987 shales of a euxinic basin. Devonian shelf-basin, Michigan Basin, Alpena, Michigan Raymond C Gutschick, Department of Earth Sciences, University of Notre Dame, Notre Dame, Indiana 46556- 1020 INTRODUCTION This chapter cites two localities, Paxton Quarry and Partridge Point (Fig. 1), and combines field observations from both to illustrate important stratigraphic relations and principles. Focus is on litho- and biostratigraphy of Middle and Late Devonian rocks as they relate to the Michigan Basin (Fig. 2). Black organic-rich shales deserve our attention due to Figure 2. Chart to relate the chrono- and biostratigraphy of the their energy potential a source rocks and fracture rock sequence in the Paxton Quarry and Partridge Point area reservoirs for petroleum and natural gas. The Paxton to standard accepted stratigraphic nomenclature. Chart shows relationship of the Antrim Shale to other widespread Late Quarry offers the opportunity to examine an exceptional Devonian black shale units for parts of the United States and exposure of black shale (large area in Fig. 3; thick Canada. In the conodont zonation column, Si stands for section in Fig. 4) as part of the formational sheet that Siphonodella; P,, Polygnathus, A., Ancyrognathus, and S., continues into the Michigan Basin subsurface. These Schmidtognathus; other zones refer to species of special rocks offer a challenge to observe and test their Palmatolepis. physical, chemical, and organic composition and structure to decipher origin, paleoenvironments, diagenesis, history, and economic value. A spectacular PAXTON QUARRY display of numerous, large calcareous concretions, in situ and free of shale matrix, is present in the quarry.
    [Show full text]
  • Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1990 Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan Brendan Ciaran Curran Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Curran, Brendan Ciaran, "Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan" (1990). Master's Theses. 1053. https://scholarworks.wmich.edu/masters_theses/1053 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. RESERVOIR GEOLOGY OF THE DUNDEE LIMESTONE, WEST BRANCH FIELD, MICHIGAN by Brendan Ciaran Curran A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan December 1990 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. RESERVOIR GEOLOGY OF THE DUNDEE LIMESTONE, WEST BRANCH FIELD, MICHIGAN Brendan Ciaran Curran, M.S. W estern Michigan University, 1990 West Branch field is a low-relief, NW-SE-trending anticline near the center of the Michigan basin. Since 1934, the Dundee Limestone (Middle Devonian) has produced over 12 million barrels of oil from this field. From core studies, six depositional facies types were recognized in the Dundee. These are dominated by bioclastic carbonate sand facies deposited in normal- marine shelf settings. Although burial cements have occluded some porosity, carbonate sand facies have retained significant primary interparticle porosity and are the most important reservoir rocks.
    [Show full text]