Engineering Aspects of the St. Peter Sandstone in the Minneapolis-St

Total Page:16

File Type:pdf, Size:1020Kb

Engineering Aspects of the St. Peter Sandstone in the Minneapolis-St Engineering aspects of the St. Peter sandstone in the Minneapolis-St. Paul area of Minnesota Item Type text; Thesis-Reproduction (electronic) Authors Payne, Charles Marshall, 1937- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 17:41:05 Link to Item http://hdl.handle.net/10150/551926 ENGINEERING ASPECTS OF THE ST. PETER SANDSTONE IN THE MINNEAPOLIS - ST. PAUL AREA OF MINNESOTA by Charles Marshall Payne A Thesis. Submitted to the Faculty of. the DEPARTMENT OF GEOLOGY In Partial Fulfillment of the Requirements. For the Degree of - —• j ' MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 6 ? The St. Peter sandstone at the Minnesota Silica Company quarry, Minneapolis. STATEMENT BY AUTHOR This thesis has been submitted in partial fulfill­ ment of requirements for an advanced degree at The Univer­ sity of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Li brary. Brief quotations from this thesis are allowable without special permission, provided that accurate acknow­ ledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department of the Dean of the Graduate College when in his judgment the proposed use of the material is in the inter­ est of scholarship. In all other instances, however, per­ mission must be obtained from the author. SIGNED: APPROVAL BY THESIS DIRECTOR This thesis has been approved on the date shown below Date Professor of Mining & Geological Engineering ACKNOWLEDGMENTS The writer wishes to acknowledge with gratitude the able assistance given by Dr. George M0 Schwartz in the col­ lection of studies and literature needed to compile this p&- per. The writer wishes also to express his indebtedness to Dr. Paul K. Sims, director of the Minnesota Geological Sur­ vey, for allowing the time and facilities to conduct this study and fo r the preparation and use of the Bedrock Geologic Map of Minneapolis, St. Paul and Vicinity. Dr. John E. Stone, of- the Minnesota Geological Survey, was' very helpful in supplying general information regarding the engineering properties of the St. Peter sandstone. Recognition is given to' Dr. Willard C. Lacy, professor at the University of Ari­ zona, for his patience and assistance in organization and preparation of this thesis. i l l TABLE OF CONTENTS P a g e LIST OF ILLUSTRATIONS ................. vl LIST OF TABLES .................... v i i i J—_L 1^ . ^ . e o o . ". o o o o . 2-5C INTRODUCTION 1. Description of the Thesis Area .......... 2 General Geology .................. 4 PHYSICAL CHARACTERISTICS OF THE ST. PETER SANDSTONE . 9 General Description ................ 9 F r ia b ility and Cementation ............ 13 Mineralogy and Lithology .............. 16 Textural and Grain Size Analyses ......... 19 Roundness5 F rosting, and P ittin g ......... 25 Silt Horizon ..................... 26 Green Sand Horizon . ^ . 27 Shakopee Dolomite - St. Peter Sandstone Contact . 28 Glenwood Shale - St. Peter Sandstone Contact . 29 Jointing and. Fracturing .............. 29 Sandstone Caves .................. 36 Origin of the St. Peter Sandstone 37 HYDROLOGIC ASPECTS OF THE ST. PETER. SANDSTONE ..... 4l GENERAL GROUNDWATER CONDITIONS IN THE ST. PETER SANDSTONE .................. 44 ENGINEERING ASPECTS OF THE ST. PETER SANDSTONE .... 53 Previous Engineering Studies ........... 53 Sampling Techniques ................. 54- Unit Weight . ................. 56 Unconfined Compression Tests ........... 56 Triaxial Compression Tests ............ 62 Plate Bearing Tests ................ 70 Consolidation and Settlement ........... 73 Penetration Resistance Tests ........... 75 Bearing Capacities ................ 78 FOUNDATION USE OF THE ST. PETER SANDSTONE ....... 80 i v V TABLE OF CONTENTS--Continued Page Potential Problems 80 Bridges 83 Locks and Dams „ „ 85 Buildings „ „ „ „ , 87 E O a d S o o o o e o o o \ 91 TUNNELING IN THE ST. PETER SANDSTONE 92 Problems in Tunneling . „ . < 92 Tunnel Description .............. 95 Arching and Stress Distribution ........ 96 Tunnel Supports ................ 99 Mining Methods ................ 104 Case Histories of Tunneling in the St. Peter 1C ^3 S o 1C . ...... ...... 108 Eastman Tunnel .............. 108 Wabasha S tre e t In tercep to r Sewer . , 109 Roblyn Avenue Interceptor Sewer, St. Paul , 110 Dayton's Bluff Interceptor Sewer, St. Paul 111 Rondo Street Tunnel Cave-in ........ ill Stevens Avenue Sewer Tunnel Cave-in, Minneapolis ............... 113 CONCLUSIONS AND RECOMMENDATIONS ............ 119 LIST OF REFERENCES ................ 124 LIST OF ILLUSTRATIONS Figure Page 1. Index map of Minnesota showing location of thesis area <,„<,.<, «».<>„ 6 „ = <,«>.<, „ 3 2 „ Rock formations of the Minneapolis-St.Paul 3. Photograph of a fresh exposure of the St-. ' Peter sandstone ............... 10 4. Photograph of a fresh exposure of the St. Peter sandstone 10 5. Photograph of the river bluff at Holiday Harbor in St, Paul ............. 11 6 . Photograph of a mine d r i f t a t Holiday Harbor in St. Paul ................. 12 7. Photomicrograph showing grain relationships in the St. Peter Sandstone ........... 15 8 . Grain size analysis, vertical section ...... 21 9. Grain size analysis, horizontal section ..... 23 10. Histogram showing the bimodal distribution of grain sizes ................. 24 1 1 . Rose diagram showing joint directions in the St. Peter sandstone ............... 31 12. Photograph of the river bluff below the Soldier’s Home in Minneapolis (1932) . ... 7 . 34 13. Photograph of the river bluff below the Soldier's Home in Minneapolis (1964) ......... 35 14. Sketch of the natural sandstone cave, Minneapolis ................. 38 15. Moisture - density relationships ........ 57 1 6 . Stress-strain curves for unconfined compression te s ts . 0 . a . e .0 o o o o 0 o 00000 59 v i v i i LIST OF ILLUSTRATIONS--Continued Figure Page 17. Undisturbed triaxial compressions tests 64 18. Triaxial compression tests--disturbed O OOOOO 69 19o .Triaxial compression tests5 disturbed sand - S tone OOO 0 90 0 00 OO OOC OO o'o 71 20. Field bearing tests 72 21 o Consolidation tests 0.=., ,,o . 76 22. Photograph of an excavation in the St. Peter sandstone at the Dayton’s Department Store in St. Paul o,. ..L 90 Photograph of placing lagging in a sandstone t unne1 .. ....... ..a.... 101 24. .Photograph of an unsupported tunnel driven in competent sandstone ............. 102 25. Photograph of full ring beam supports in a sandstone tunnel .............. 102 2 6 . Photograph of hydraulicly mining the St. Peter sandstone .............. 105 27. Sketch and photograph of the Rondo Street Tunnel Cave-in ............... 114 28. Geologic section, Stevens Avenue Sewer Tunnel, Minneapolis ................. 117 1 . 29. Photograph of the Stevens Avenue cave-in .... 118 30. Bedrock geologic map of Minneapolis- St. Paul and v ic in ity ........ Map Pocket 31. North-South cross section of the Minneapolis-St. Paul area ...... Map Pocket 32. East-West cross section of the Minneapolis-St. Paul area ...... Map Pocket LIST OF TABLES T a b le P a g e 1 . Textural characteristics of the St. Peter sandstone .................. 25 2. Coefficient of Transmissibility ......... 4-2 3. Test results - unconfined compression tests . 60 4. Triaxial compression tests conditions, undisturbed St. Peter sandstone ........ 66 v i i i ABSTRACT In the Twin City area a variety of heavy structures and tunnels have been built on or in the St„ Peter sand­ stone. The rock in situ, though friable, is competent and capable of withstanding high bearing loads. Because the soft sandstone is easily excavated and supported,.tunnels can be constructed- at below normal tunneling costs. Buried river channels, groundwater problems, and the unique physical properties of the sandstone have caused numerous engineering perplexities. The sandstone normally lacks cohesion, has a low shear stren g th , but has a high angle of internal friction. If the rock is disturbed or exposed to running water, the material loses its strength, and structural failure results. The engineering properties of the sandstone have not been thoroughly defined. The formation is unusual be­ cause it is neither a soil nor rock. The elastic properties of the sandstone categorize it as a rock; cohesionless characteristics are more typical of soils. The objectives of this paper have been to compile all available engineering data in an attempt to better un­ derstand the engineering properties of the St. Peter sand­ stone. i x X Several case histories are reviewed to demonstrate the necessity of adequate exploration and testing of the sandstone. In addition 5 a subsurface geologic map of the Twin City area was made to show the distribution of the various rock types present. INTRODUCTION For over one hundred years the St. Peter sandstone5 In the Twin City area, has been utilized for foundation purposes and for the excavation of utility and sewer tun­ nels . As the cities expand and grow skyward, an ever in­ creasing use of the sandstone will become evident. As succeeding projects become larger and more extensive, the number and complexity of engineering problems w ill increase.
Recommended publications
  • A Hydrogeologic and Mapping Investigation of the St. Lawrence Formation in the Twin Cities Metropolitan Area Executive Summary T
    Minnesota Geological Survey (MGS) Open File Report 06-04 (Open File Reports are not subjected to conventional MGS editorial standards) A HYDROGEOLOGIC AND MAPPING INVESTIGATION OF THE ST. LAWRENCE FORMATION IN THE TWIN CITIES METROPOLITAN AREA Runkel, A.C., Mossler, J.H., Tipping, R.G., and Bauer, E.J. Minnesota Geological Survey 2642 University Ave W., St. Paul, Minnesota 55114-1057 EXECUTIVE SUMMARY This report summarizes the results of a two year project conducted by the Minnesota Geological Survey to map the Upper Cambrian St. Lawrence Formation and investigate its hydrologic properties in the Twin Cities Metropolitan area (TCMA). Funding was provided by the Minnesota Department of Health. Final products are a map delivered in electronic format that can be used with Arcview 3.2 GIS software, and this informal report. Our hydrogeologic study indicates that the St. Lawrence Formation commonly has a moderate to high horizontal hydraulic conductivity across all of the study area. In conditions of shallow burial beneath younger bedrock it is most similar in the development of secondary pores and measured hydraulic properties to fractured carbonate rock aquifers. Discrete intervals with secondary pores have a high horizontal hydraulic conductivity whereas rock between these intervals are orders of magnitude lower in conductivity. The properties of the St. Lawrence Formation in a vertical direction are not as well- understood, but available data are consistent with the traditional classification of the formation as an aquitard. However, the integrity of the formation as an aquitard in a vertical direction, particularly under conditions of shallow burial such as where it is uppermost bedrock, has not been rigorously tested, and may be markedly variable across the TCMA.
    [Show full text]
  • Geologic Atlas of Blue Earth County, Minnesota
    Prepared and Published with the Support of COUNTY ATLAS SERIES THE BLUE EARTH COUNTY BOARD OF COMMISSIONERS AND ATLAS C-26, PART A MINNESOTA GEOLOGICAL SURVEY the Minnesota ENVironment and Natural Resources Trust Fund Blue Earth County Harvey Thorleifson, Director as recommended by the LEGislatiVE-CitiZen Commission on Minnesota Resources Plate 2—Bedrock Geology NIC OLL ET COU NTY 7 Minnesota B BEDROCK GEOLOGY Ka 44°15' N. 285 300 R. 29 W. Kd m STRATIGRAPHIC COLUMN River 285 By 240 s 94° W. e i Lithostratigraphic r Composite natural gamma log 255 NICOLLET LE SUEUR COUNTY R. 26 W. COUNTY R. 25 W. e unit S 270 - e 315 Increasing count 330 Era m Lithology Kd e T. 109 N. sl Os 315 Julia R. Steenberg t Group, 0 100 s 24 Map symbol 19 y 300 300 24 24 Formation 270 lr 19 S API-G units Oo Thickness (in feet) 300 River 285 LIME JAMESTOWN 345 94°15' W. 255 Kd Wita Kd Creek 315 2012 315 )68 j Kd Lake j Dakota Kd 5-90 m.y.) Upper Formation Os Y 300 (99.6-93.5 T Duck Cretaceous 300 lr Morgan Os Lake N T. 109 N. CAMBRIA U 315 O 300 Minnesota 240 Ballantyne C LOCATION DIAGRAM Oo 300 Lake R 270 Madison MESOZOIC R. 28 W. U 31 Kd 300 31 Oo Unnamed Ka Os E Kd 30-90 36 31 Eagle Lake lr lr 36 315 36 U 36 S Cretaceous 300 ) 31 300 22 (112-93.5 m.y.) (112-93.5 Gilfillin 315 E Lower to Upper Lake L Judson Lake 315 300 lr 240 1 6 Y 6 240 Os Platteville Formation 255 315 T Opg 6 Madison 5-20 1 1 N 6 Glenwood Formation Ph 1 255 U sl 255 1 CORRELATION OF MAP UNITS O )60 Upper 315 315 C Lake A j (450 m.y.) 315 C ? E Kd Upper Cretaceous 285 14 Kd S Lithology Key 315 A St.
    [Show full text]
  • Hydrogeology and Stratigraphy of the Dakota Formation in Northwest Iowa
    WATER SUPPLY HYDROGEOLOGY AND J.A. MUNTER BULLETIN G.A. LUDVIGSON NUMBER 13 STRATIGRAPHY OF THE B.J. BUNKER 1983 DAKOTA FORMATION IN NORTHWEST IOWA Iowa Geological Survey Donald L. Koch State Geologist and Director 123 North Capitol Street Iowa City, Iowa 52242 IOWA GEOLOGICAL SURVEY WATER-SUPPLY BULLETIN NO. 13 1983 HYDROGEOLOGY AND STRATIGRAPHY OF THE DAKOTA FORMATION IN NORTHWEST IOWA J. A. Munter G. A. Ludvigson B. J. Bunker Iowa Geological Survey Iowa Geological Survey Donald L. Koch Director and State Geologist 123 North Capitol Street Iowa City, Iowa 52242 Foreword An assessment of the quantity and quality of water available from the Dakota (Sandstone) Formation 1n northwest Iowa is presented in this report. The as sessment was undertaken to provide quantitative information on the hydrology of the Dakota aquifer system to the Iowa Natural Resources Council for alloca tion of water for irrigation, largely as a consequence of the 1976-77 drought. Most area wells for domestic, livestock, and irrigation purposes only partial ly penetrated the Dakota Formation. Consequently, the long-term effects of significant increases in water withdrawals could not be assessed on the basis of existing wells. Acquisition of new data was based upon a drilling program designed to penetrate the entire sequence of Dakota sediments at key loca tions, after a thorough inventory and analysis of existing data. Definition of the distribution, thickness, and lateral and vertical changes in composition of the Dakota Formation has permitted the recognition of two mem bers. Additionally, Identification of the rock units that underlie the Dakota Formation has contributed greatly to our knowledge of the regional geology of northwest Iowa and the upper midwest.
    [Show full text]
  • Cement in Cambrian Sandstone : Assessing the Potential for the Generation of Respirable Silica
    Cement in Cambrian Sandstone : Assessing the Potential for the Generation of Respirable Silica J. Brian Mahoney Kent M. Syverson Department of Geology University of Wisconsin-Eau Claire • Geologic Setting • Industrial Silica Sand • Community Concerns • Identifying Particulate Matter • Geologic Setting • Industrial Silica Sand • Community Concerns • Identifying Particulate Matter Mt. Simon Formation Eau Claire Eau Claire/Wonewoc Formation contact Tilden, WI Wonewoc/Lone Rock Formation contact Colfax, WI Jordan Formation Arcadia, WI A' A northwest Iowa southeastern west-central Minnesota Wisconsin Paleoseaward Oneota Dolomite RSL Paleolandward Jordan Ss FSL Jordan Ss St Lawrence Fm St Lawrence Fm FSL Mazom anie RSL RSL Wonewoc Ss Wonewoc Ss FSL FSL Wonewoc Ss Eau Claire Fm 100 ft 25 m Eau Claire Fm RSL Mt Simon Ss 25 miles RSL 0 40 km Fine- to coarse-grained, quartzose sandstone: nonmarine Fine- to coarse-grained, quartzose sandstone: nearshore marine Very fine grained, feldspathic sandstone, siltstone, shale: offshore siliciclas Carbonate: "offshore" subtidal and peritidal carbonate parasequence boundary or parallel to inferred parasequence boundaries unconformity correlative conformity • Geologic Setting • Industrial Silica Sand • Community Concerns • Identifying Particulate Matter Minnesota Grain Size Distribution Wisconsin Grain Size Distribution 50 50 s s e e v v e e i i S 40 s 40 n n o o ST. PETER d 30 ST. PETER d e e 30 n n i i JORDAN a JORDAN a t t e 20 e r 20 WONEWOC R WONEWOC % % MT. SIMON e e g g 10 10 a a r r e e v v A A 0 0
    [Show full text]
  • Algal Stromatolites in the Willow River Member of the Lower Ordovician Shakopee Formation Near Chatfield, Minnesota, USA
    The Compass: Earth Science Journal of Sigma Gamma Epsilon Volume 84 Issue 1 Article 6 1-6-2012 Algal Stromatolites in the Willow River Member of the Lower Ordovician Shakopee Formation near Chatfield, Minnesota, USA Sophia L. May College of St. Benedict / St. John's University, [email protected] Larry E. Davis College of St. Benedict / St. John's University, [email protected] David G. Brown College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/compass Part of the Paleontology Commons Recommended Citation May, Sophia L.; Davis, Larry E.; and Brown, David G. (2012) "Algal Stromatolites in the Willow River Member of the Lower Ordovician Shakopee Formation near Chatfield, Minnesota, USA," The Compass: Earth Science Journal of Sigma Gamma Epsilon: Vol. 84: Iss. 1, Article 6. Available at: https://digitalcommons.csbsju.edu/compass/vol84/iss1/6 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in The Compass: Earth Science Journal of Sigma Gamma Epsilon by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. ON THE OUTCROP Algal Stromatolites in the Willow River Member of the Lower Ordovician Shakopee Formation near Chatfield, Minnesota, USA Sophia L. May, Larry E. Davis, and David G. Brown Department of Biology College of Saint Benedict/Saint John’s University Collegeville, Minnesota, 56321 USA [email protected] LOCATION From the intersection of (Olmsted) Co. Hwy 2 and U.S. 52 Rochester I-90 (Main Street) in Chatfield, MN drive N south-southeast on U.S.
    [Show full text]
  • Bedrock Geology of Altenburg Quadrangle, Jackson County
    BEDROCK GEOLOGY OF ALTENBURG QUADRANGLE Institute of Natural Resource Sustainability William W. Shilts, Executive Director JACKSON COUNTY, ILLINOIS AND PERRY COUNTY, MISSOURI STATEMAP Altenburg-BG ILLINOIS STATE GEOLOGICAL SURVEY E. Donald McKay III, Interim Director Mary J. Seid, Joseph A. Devera, Allen L. Weedman, and Dewey H. Amos 2009 360 GEOLOGIC UNITS ) ) ) 14 Qal Alluvial deposits ) 13 18 Quaternary Pleistocene and Holocene 17 360 ) 15 360 16 14 0 36 ) 13 Qf Fan deposits ) Unconformity Qal ) & 350 tl Lower Tradewater Formation Atokan ) ) Pennsylvanian 360 ) &cv Caseyville Formation Morrowan 24 360 ) Unconformity ) 17 Upper Elviran undivided, Meu ) Waltersburg to top of Degonia 19 20 Qal 21 22 23 ) 24 ) Mv Vienna Limestone 360 o ) 3 Mts ) 350 Mts Tar Springs Sandstone ) 20 360 ) Mgd 360 30 ) Mgd Glen Dean Limestone ) 21 350 360 Mts 29 ) Qal Hardinsburg Sandstone and J N Mhg Chesterian ) Golconda Formations h Æ Qal Mav anc 28 27 Br ) N oJ 26 25 JN 85 N ) Cypress Sandstone through J Mcpc Dsl 500 Paint Creek Formation JN N ) J o Mts N 5 J s ) Dgt 600 J N 70 J N Mgd Yankeetown Formation s ) Myr Db 80 28 Æ and Renault Sandstone N J 29 N J N ) Sb J Mgd Mississippian o Dgt Ssc 25 Clines o N 25 Msg 27 ) Qal J 80 s 3 Mav Aux Vases Sandstone N J N Mts o MILL J MISSISSIPPI 34 ) Qal J N ) N J Dsl 35 N 26 J o N 25 J Mgd Mgd ) Msg Ste. Genevieve Limestone 500 o Db DITCH J 20 Mgd N N N ) J J o RIVER o N 600 J 80 N ) 10 o J Mav Æ Msl St.
    [Show full text]
  • Download Printable Version of the Geology and Why It Matters Story
    Geology and Why it Matters This story was made with Esri's Story Map Journal. Read the interactive version on the web at http://arcg.is/qrG8W. The geology, landforms and land features are extremely important components of watersheds. They influence water quality, hydrology and watershed resiliency. Every watershed has critical areas where water interacts with and mobilizes contaminants, including non-point and point source contributions to surface water bodies. Where and how nutrients, bacteria and/or pesticides are mobilized to reach surface water can be better understood through a careful study of subsurface hydrology, or hydrogeology, which, according to the Iowa Geological and Water Survey Bureau, “allows better identification for sources, pathways and delivery points for groundwater and contaminants transported through the watershed’s subsurface geological plumbing system.” Diagram courtesy of Iowa DNR Iowa Geological Survey The highly developed karst topography and highly permeable bedrock layers of the Upper Iowa River increase the depth from which actively circulating groundwater contributes to stream flows, making an understanding of the hydrogeology even more important. Fortunately, the Iowa Geological and Water Survey Bureau completed a detailed mapping project of bedrock geologic units, key subsurface horizons, and surficial karst features in the Iowa portion of the Upper Iowa River watershed in 2011. The project “provides information on the subsurface part of the watersheds, which is necessary for evaluating the vulnerability of groundwater to nonpoint-source contamination, the groundwater contributions to surface water contamination, and for targeting best management practices for water quality improvements.” The map on the right shows the surface elevation of bedrock in the state of Iowa and the Upper Iowa River Watershed.
    [Show full text]
  • Petrography and Origin of Illinois Nodular Cherts
    View metadata, citation and similar papers at core.ac.ukG^tA S^svjlx-^ brought to you by CORE provided by Illinois Digital Environment for Access to Learning and Scholarship... STATE OF ILLINOIS c a WILLIAM G. STRATTON, Governor DEPARTMENT OF REGISTRATION AND EDUCATION VERA M. BINKS, Director PETROGRAPHY AND ORIGIN OF ILLINOIS NODULAR CHERTS Donald L. Biggs DIVISION OF THE ILLINOIS STATE GEOLOGICAL SURVEY JOHN C. FRYE, Chief URBANA CIRCULAR 245 1957 ILLINOIS GEOLOGICAL SURVEY LIBRARY JAN 9 1958 ILLINOIS STATE GEOLOGICAL SURVEY 3 3051 00004 4572 PETROGRAPHY AND ORIGIN OF ILLINOIS NODULAR CHERTS Donald L. Biggs ABSTRACT Seventy-eight samples of nodular chert from 18 Illinois lime- stone and dolomite formations, ranging from Cambrian through Mississippian age, were investigated todetermine the petrography and mode of origin of the nodules. Regardless of geologic age or type of host rock, the nodules were similar in mode of occurrence and in principal textural characteristics. The cherts are dominantly microcrystalline or cryptocrys- talline quartz with a lesser amount of fibrous quartz. No opal or hydrated silica was detected. Almost all the cherts contain re- sidual masses of their host rock. Field relationships and a varie- ty of evidence for replacement leads to the conclusion that the cherts are epigenetic concretions formed by metasomatic proc- esses operating during diagenesis and involving the aggregation of silica that originally had been deposited syngenetically with, and dispersed through, the host rocks. INTRODUCTION Chert is found in many limestones that crop out in Illinois and range in age from Cambrian to Mississippian. The chert may appear as nodules, len- ses, or beds, and some Devonian rocks in extreme southern Illinois are entire- ly chert.
    [Show full text]
  • Stratigraphic Succession in Lower Peninsula of Michigan
    STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation
    [Show full text]
  • Early Ordovician Strata Along Fox River in Northern Illinois
    URBANA jf-.'-INOIS STATE GEOLOGICAL SURVEY 3 3051 00003 5240 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/earlyordovicians100will STATE OF ILLINOIS DWIGHT H. GREEN, Governor DEPARTMENT OF REGISTRATION AND EDUCATION FRANK G. THOMPSON, Director DIVISION OF THE STATE GEOLOGICAL SURVEY M. M. LEIGHTON, Chief URBANA CIRCULAR 100 EARLY ORDOVIC1AN STRATA ALONG FOX RIVER IN NORTHERN ILLINOIS H. B. WILLMAN AND J. NORMAN PAYNE Reprinted from the Journal of Geology Vol. LI, No. 8, November-December, 1943 PRINTED BY AUTHORITY OF THE STATE OF ILLINOIS URBANA, ILLINOIS 1943 EARLY ORDOVICIAN STRATA ALONG FOX RIVER IN NORTHERN ILLINOIS H. B. WILLMAN AND J. NORMAN PAYNE Illinois State Geological Survey ABSTRACT A nearly complete sequence of Ordovician strata along Fox River, southwest of Aurora, indicates the presence of the Kankakee arch—a major structure trending northwest-southeast across northeastern Illinois —and the probable location of the Sandwich fault, which parallels the arch for many miles and had been found previously by studies of well records. Outcrops of sandstone and dolomite which have long been corre- lated with the St. Peter and Galena-Platteville formations have been found to belong to the New Richmond sandstone and the Shakopee dolomite. Study of the outcrops and well records shows that the anticlinal struc- ture underwent major movements both before and after deposition of the St. Peter sandstone. INTRODUCTION subsurface data showed that this struc- ture, termed the "Kankakee arch," In the earliest geological studies of this (1) 2 had its greatest deformation before, rather area the sandstone and the dolomite out- than since, St.
    [Show full text]
  • Deep Oil Possibilities of the Illinois Basin
    s Ccc 36? STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell Elwood Atherton T. C. Buschbach David H. Swann ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 368 1964 . DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell, Elwood Atherton, T. C. Buschbach, and David H. Swann ABSTRACT The Middle Ordovician and younger rocks of the Illinois Basin, which have yielded 3 billion barrels of oil, are underlain by a larger volume of virtually untested Lower Ordovician and Cambrian rocks. Within the region that has supplied 99 percent of the oil, where the top of the Middle Ordovician (Trenton) is more than 1,000 feet be- low sea level, less than 8 inches of hole have been drilled per cubic mile of the older rocks. Even this drilling has been near the edges; and in the central area, which has yielded five- sixths of the oil, only one inch of test hole has been drilled per cubic mile of Lower Ordovician and Cambrian. Yet drilling depths are not excessive, ranging from 6,000 to 14,000 feet to the Precambrian. More production may be found in the Middle Ordovician Galena Limestone (Trenton), thus extending the present productive regions. In addition, new production may be found in narrow, dolomitized fracture zones in the tight limestone facies on the north flank of the basin . The underlying Platteville Limestone is finer grained and offers fewer possibilities. The Joachim Dolomite oil- shows occur in tight sandstone bodies that should have commercial porosity in some re- gions.
    [Show full text]
  • Mechanical Properties of St. Peter Sandstone a Comparison of Field and Laboratory Results a Thesis Submitted to the Faculty of T
    MECHANICAL PROPERTIES OF ST. PETER SANDSTONE A COMPARISON OF FIELD AND LABORATORY RESULTS A THESIS SUBMITTED TO THE FACULTY OF THE GRADUATE SCHOOL OF THE UNIVERSITY OF MINNESOTA BY MICHAEL EUGENE DITTES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DECEMBER, 2015 This thesis contains previously published material (Appendix E) in the “Journal of Geotechnical and Geoenvironmental Engineering” © 2002 ASCE. All other material © 2015 Michael E. Dittes All Rights Reserved. ACKNOWLEDGMENTS I would like to extend my thanks to those, who without their help I would not have been able to bring this project to completion. First and foremost, I thank Professor Joseph Labuz who took a chance on me, by offering me a TA-ship. Through my time in school, Joe helped me stay focused when I started to move off on tangents, offered timely advice, and over the years has become much more than my advisor. I am proud to think of him as a friend. Professors Andrew Drescher and Peter Huddleston also deserve special thanks for providing critical review of my work, and agreeing to sit on my thesis committee. To Ms. Tiffany Ralston who had an uncanny way of knowing what I needed to do, and how, before I knew myself. To Charles Nelson who helped me streamline my thesis project and helped me gain access to the Minnesota Library Archives construction site. To my fellow graduate students with whom I debated, joked and laughed, you helped me see things that I was missing. Your input was invaluable and you have my deep appreciation.
    [Show full text]