DOCSLIB.ORG

Bedrock Geology (5.250Mb Application/Pdf)

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Bedrock Geology (5.250Mb Application/Pdf) Prepared and Published with the Support of COUNTY ATLAS SERIES THE HENNEPIN COUNTY BOARD OF COMMISSIONERS, ATLAS C-45, PART A MINNESOTA GEOLOGICAL SURVEY Hennepin County Harvey Thorleifson, Director THE MINNESOTA ENVIRONMENT AND NATURAL RESOURCES TRUST FUND SHERBURNE AS RECOMMENDED BY THE LEGISLATIVE-CITIZEN COMMISSION ON MINNESOTA RESOURCES, Plate 2—Bedrock Geology COUNTY ANOKA AND THE MINNESOTA LEGACY AMENDMENT'S CLEAN WATER FUND COUNTY WRIGHT 93°30' COUNTY 275 U 31tm D j Mississippi 6 s 1 R. 22 W. j 275 s R. 23 W. s tm M 275 M )101 CORRELATION OF MAP UNITS 93°37'30" 275 D275 D Lake tm Laura River U U s tl w 275F BEDROCK GEOLOGY North Twin Diamond j Od 275 w tl Lake Cowley Lake tl Upper Ordovician 275 Lake w U T. 120 N. j T. 120 N. Opg s D LOCATION DIAGRAM 275 Sylvan 275 tm By Prairie Lake tm 275 Os Middle Ordovician Lake tl D tl ¤52 j U 93°22'30" unconformity 300 tm Rogers French s Ops F s D Hayden Andrew J. Retzler Lake U Lake Lemans tm 94 F tm unconformity s ¦§ Lake s Lower Ordovician tl j Henry s Champlin U Lake s Opo 2018 D s Powers unconformity Lake R. 21 W. 31 s PALEOZOIC 36 31 36 31 j j 275 w 275 27536 j Dayton Goose B Lake s U tm s tm tl F j ¤169 D RiverOs tm 1 6 j tm 1 6 Mud 1 6 Upper Cambrian M j Lake R. 24 W. F j tl j tm w e s s unconformity tl 275 w s 300 j tm 45°7'30" Crow s j e Osseo 250 45°7'30" 275 tl Middle Cambrian j 275 s Rice Lake m Schwappauff s tm LakeOs j s unconformity T. 119 N. Os tm Weaver T. 119 N. Greenfield w Lake j Mss INTRODUCTION Most layers designated as aquitards in the county have a much lower permeability in the vertical Schendel M MESOPROTEROZOIC Os Brooklyn Park direction than do aquifers. Examples in Hennepin County include the lower Jordan Sandstone, and s Lake Corcoran tl tm j tm The geologic map, cross sections, and stratigraphic column on this plate depict the type, D Mbv St. Lawrence and Eau Claire Formations, whose rocks are composed mostly of very fine-grained U s Mcv distribution, and structure of the bedrock units in Hennepin County that are either exposed at the Hafften 275 s sandstone and shale with small, poorly connected pore spaces. Carbonate rock with relatively sparse Lake 300 s land surface or lie beneath unconsolidated Quaternary glacial sediments of variable thickness Os fractures, such as the lower part of the Prairie du Chien Group (Oneota Dolomite), are also aquitards. 325 300 Fish j U Lake Opo (see cross sections and Plate 3, Surficial Geology; Plate 4, Quaternary Stratigraphy; and Plate 6, Os However, layers designated as aquitards with very low permeability in the vertical direction may Os 300 300 D300 )252 93°45' Jubert 300 Scott Os Os 275 Bedrock Topography and Depth to Bedrock). The map shows how the bedrock surface would appear Lake F locally contain horizontal fractures that are conductive enough to yield large quantities of water, Lake j tm 275 ¦§94 Ops if it was viewed from an aerial perspective and the overlying Quaternary sediments were stripped 275 Os Cedar Island including the St. Lawrence Formation. Lake ¤52 Ops Palmer Lake away. The bedrock units near the land surface in Hennepin County consist of sedimentary rocks 300 sRattail j Eagle Brooklyn Center Horizontal and vertical fractures are more common where bedrock layers are at or near the tl Lake 325 31 j Lake Opo of Paleozoic age that form distinguishable and mappable layers designated as formations. Some of 31 36 36 31 36 Lake 300 s 36 31 bedrock surface. As a result, aquitards in such conditions are likely to have higher permeability Os Morin F these units are commonly exposed along the Mississippi River bluffs within the county. Several of Lake Lake Sarah F Maple Grove Opo compared with more deeply buried portions of the same formation, and may have a diminished 300 s s Os Pike the Paleozoic bedrock formations are major reservoirs for water supply in the county, and provide 275 Lake ability to retard water flow to underlying aquifers. There is no precise boundary between shallow Rebecca s 300 a stable platform that supports major metropolitan buildings and bridges. 300 275 Os j Os and deep conditions of burial, but in most areas of southeastern Minnesota, about 50 feet (15 meters) 1 6 tl Peter Lake 6 Lithostratigraphic 6 Lake 1 6 Mud Lake 1 Meadow Lake 1 Characteristics of each formation are given in the stratigraphic column (Fig. 1) and in the Os Loretto Medina Bass unit Composite natural gamma log of depth below the bedrock surface is a best approximation (Runkel and others, 2006a, 2014a). tm j 300 300 Era )55 Os Pomerleau Lake description of map units. The accompanying bedrock geologic cross sections add the dimension of s Lake Twin Os Group, Formation, In addition to this hydrostratigraphic classification, the Minnesota Department of Natural j 300 Lithology Map symbol API M Lakes depth and illustrate the stratigraphic, structural, and topographic relationships of the bedrock units; System-Series Member Haughey s 300 T. 118 N. Resources, as Part B of the Hennepin County atlas, will conduct a thorough hydrogeologic study Hydrostratigraphic properties F Thomas Lake 494 0 100 Thickness (in feet) Lake Os Os 300¦§ as well as the variable thickness of the overlying Quaternary sediments. Surfaces representing the ¤169 Opo of the groundwater flow system, aquifer capacity, and aquifer sensitivity that may or may not result Robina Winterhalter Lake 300 elevation of the tops of the mapped formations are also available as digital elevation models for 275 RAMSEY Decorah 300 Od 12 Edward <40 in modifications or additions to this classification. Furthermore, designations of aquifers versus Lake 275 ANOKA Shale ¤ COUNTY Group 300 Spurzem 93°15' Galena use in GIS programs. The geologic formations are thin in relation to their aerial extent, and would 300 Lake Hamel Lake New Hope Ardmore300 tm Lake Os Crystal R. 24 W. COUNTY R. 23 W. aquitards made here may not correspond precisely with those made for regulatory purposes by the Opo only be one-tenth as thick as shown on the cross sections if no vertical exaggeration were used. The Os F Opo Platteville and Minnesota Department of Health. j Ops Opg 300 Lake Halfmoon j exaggeration necessary to show the thin rock formations gives the appearance of steeper slopes on Os 300 Os Glenwood Formations 30-35 Lake s Lost Lake275 Ph bedrock unit contacts, the land surface, and bedrock topography. Most of the Paleozoic units shown 300 Independence Medina Opo 1 St. 6 300 DESCRIPTION OF MAP UNITS Independence School Lake s Anthony T. 118 N. tl Plymouth on this plate, with the exception of the Platteville Formation, Glenwood Formation, and St. Peter Os j Robbinsdale Crystal Lake 250 Opg Os Holy Name Os Upper Ordovician Sandstone, are buried by Quaternary sediments and cannot be seen at the land surface in Hennepin PALEOZOIC j Maple Lake Os 52 County. The sedimentary rocks differ in their resistance to weathering and erosion, as depicted tl 275 ¤ Plain300 F Medicine )100 Od Decorah Shale (Late Ordovician)—Dominantly grayish-green shale interbedded with Opo Ops graphically by the weathering profile on the lithology column of Figure 1. The units that cover the 300 Katrina Thies Lake Ops Lake Opg 275 thin beds of fossiliferous limestone. Fossiliferous, yellowish-brown limestone beds Irene s Os largest areas of the map are the most resistant to weathering and commonly form plateaus composed Lake Lake Wolsfeld Medicine Tonti are most common at the base of the Decorah Shale, and are recognized as the basal 300 Lake Os Os 300 of carbonate rock (limestone and dolostone). The soft sandstone and shale units erode more easily Os Mooney 300Snyder Lake Carimona Member (Mossler, 2008). The Decorah Shale is present as erosional j Lake 94 St. Peter 45° ¦§ and typically occur as thin veneers atop the carbonate rock plateaus or lie along valley walls. Lake Sandstone Os s 275 275 Od 45° remnants capping buried mesas of Platteville Limestone in the eastern part of the s Parkers 150-175 Production of the map and associated products relied on several data sources, including outcrops, Lake 250 county. Although not fully preserved in the county, water-well logs in adjacent 300 275 35W 300 394 300 300 ¦§ ¦§ Opo water-well and scientific drilling records from the County Well Index data base, rock core, drill j Ops 275 T. 29 N. counties indicate the Decorah Shale has a maximum preserved thickness of 90 feet Long Lake 300 250 cutting samples, borehole geophysical logs, seismic soundings, geophysical images, and previously Os Middle Odrovician 300 Ops Opg (27 meters). 31 w 36 31 j Os 31 Plymouth )55 Od 300 300 36 36 31 published geologic maps of Hennepin and adjacent counties (Olsen and Bloomgren, 1989; Mossler and WRIGHT 300 300 275 Pigs Platteville Formation and Glenwood Formation (Late Ordovician)—The carbonate Os 300 Gleason Opg COUNTY 300 Eye Tipping, 2000; Runkel and others, 2006a; Mossler, 2013; Steenberg and Chandler, 2013; Steenberg 300 Lake Golden Valley Platteville Formation and underlying shale of the Glenwood Formation are combined CARVER 300 Opg 250 and Retzler, 2016). This map supersedes the previous bedrock geology map of Hennepin County tl 300 Minneapolis 300 into a single map unit with a full thickness of 30 to 35 feet (9 to 11 meters).
Load more

Recommended publications
  • 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]
  • Review & Evaluation of Groundwater Contamination & Proposed Remediation
    -1 r r n CONFIDENTIAL REVIEW AND EVALUATION r OF GROUND-WATER CONTAMINATION AND PROPOSED REMEDIATION AT THE REILLY TAR SITE, ST. LOUIS PARK, MINNESOTA r. c Prepared by L Dr. James W. Mercer GeoTrans, inc. 209 Elden Street Herndon, Virginia 22070 [ Report to L U.S. Environmental Protection Agency Region V, Remedial Response Branch (5HR-13) Chicago, Illinois 60604 December 1984 L ieoT L GEOTRANS, INC. lrran« s P.O. Box 2550 Reston.Virginia 22090 USA (703)435-4400 EPA Region 5 Recorcte Ctr. i inn minium iflBiniiiiiiiw L 234542 r. CONFIDENTIAL REVIEW AND EVALUATION OF GROUND-WATER CONTAMINATION AND PROPOSED REMEDIATION AT THE REILLY TAR SITE, ST. LOUIS PARK, MINNESOTA Prepared By Dr. James W. Mercer GeoTrans, Inc. 209 El den Street Herndon, Virginia 22070 Report To U.S. Environmental Protection Agency Region V, Remedial Response Branch (5HR-13) Chicago, Illinois 60604 December 1984 TABLE OF CONTENTS Page LIST OF FIGURES v LIST OF TABLES vii 1.0 INTRODUCTION 1 1.1 PURPOSE AND SCOPE 1 1.2 SITE HISTORY 2 2.0 CONCLUSIONS AND RECOMMENDATIONS 4 2.1 CONCLUSIONS 4 2.2 RECOMMENDATIONS 6 3.0 SITE HYDROGEOLOGY 7 3.1 GEOLOGY 7 3.1.1 Stratigraphy 7 3.1.2 Geomorphic Features 14 3.2 GROUND-WATER HYDROLOGY 17 3.2.1 Flow Directions 17 3.2.1.1 Mount Simon-Hinckley Aquifer 17 3.2.1.2 Ironton-Galesville Aquifer 25 3.2.1.3 Prairie du Chien-Jordan Aquifer 25 3.2.1.4 St. Peter Aquifer 29 3.2.1.5 Drift-Platteville Aquifers 33 3.2.1.6 Vertical Gradients 35 3.2.2 Flow Properties 35 3.3 CHEMISTRY 39 4.0 GROUND-WATER MODELING 42 4.1 CODE SELECTED 42 4.2 GEOMETRY 43
    [Show full text]
  • Pre-Pennsylvanian Stratigraphy of Nebraska
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 12-1934 PRE-PENNSYLVANIAN STRATIGRAPHY OF NEBRASKA Alvin Leonard Lugn University of Nebraska-Lincoln Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Lugn, Alvin Leonard, "PRE-PENNSYLVANIAN STRATIGRAPHY OF NEBRASKA" (1934). Papers in the Earth and Atmospheric Sciences. 360. https://digitalcommons.unl.edu/geosciencefacpub/360 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. BULLETIN OF THE AMERICAN ASSOCIATION OF PETROLEUM GEOLOGISTS VOL. 18. NO 12 'DECEMBER, 1934). PP 1597-1631, 9 FIGS PRE-PENNSYLVANIAN STRATIGRAPHY OF NEBRASKA1 A. L. LUGN2 liincoln, Nebraska ABSTRACT Sioux quartzite, granite, and schistose metamorphic rocks have been recognized in the pre-Cambrian. The present irregularities, the "basins and highs," on the pre- Cambrian surface are the result of erosion and a long structural history. In general succeedingly younger rocks rest unconformably by overlap against the pre-Cambrian "highs." The principal erosional and structural "highs" are: the "Nemaha moun­ tains," the Cambridge anticline, the Chadron dome, and the Sioux Falls area. "Basins," or saddle-like depressions, occur on the pre-Cambrian surface between the "highs." The largest of these trends from southeast to northwest across the central part of Nebraska. The history of each ridge or "high" is more or less individualistic, but it seems certain that the structural framework of Nebraska came into existence in late pre-Cambrian time and has dominated the structural and depositional history of the state ever since.
    [Show full text]
  • Geology of Winneshiek County
    GEOLOGY OF WINNESHIEK COUNTY. BY SAMUEL CALVIN. • GEOLOGY OF WINNESHIEK COUNTY. BY SAMUEL CALVIN. CONTENTS. PA.GE . Introduction . .. " .. ... .. ..... ....... ....... .. .. , ...... ... .. .. ... ... 43 Geographic and Geologic Rt:lations . .. .. ...... ...... .. 43 Area.. .............. .. .. .. ........... ..... .... ... .. ....... .. 43 Boundaries . ... .. ... ......... .. .... .... ... ..... ..... 43 Relations to topographic areas . .. ..... .. ... .... .. ... 43 Relations to dist~ibution of geological formations .... .. ... 44 Previous geological work . .... .. ..... ... .. ......... 45 PhYliography .... .. ........ ....• , . .. .... ... ....... 47 Topography. .. .. .. ... 47 Preglacial topography. ... .... ..... .... .. .. .. ... ... 47 Topographic effects of the several rock formations.... ... 48 Topography controlled by Pleistocene deposits......... .. ..... 53 The area of Kansas drift. .. ... ... .. .. ... ... ..... 53 The Iowan-Kansas border. .. 54 The area of Iowan drift . , ....... .. .. .. .. .... .... ... 54 Topography due to recent shifting of mantle rocks. ....... 55 The larger topographic features. .. .......... .. ... .. ... ... 56 The Cresco-Calmar ridge. .. ... .. .... ......... .... 56 Drainage ba&in of the Ox.Eota, or Upper Iowa river..... .. 56 Drainage basin of the Yellow river.... •. .... .. ..... .. .... 56 Drainage basin of the Turkey river. .. ... .. .. ....... 56 Elevations.... .......... .. .... .. .. .... .. .. .... .. ... 56 Drainage ..... ... .... .. ... .................. ........ '" 57 The Oneota, or
    [Show full text]
  • Number 6 GEOLOGICAL and NATURAL HISTORY SURVEY
    ~.. J X Information Circular Number 6 1 University of Wisconsin GEOLOGICAL AND NATURAL HISTORY SURVEY George F. Hanson, State Geologist and Director CAMBRO-ORDOVICIAN STRATIGRAPHY OF SOUTHWEST WISCONSIN by M. E. Ostrom Assistant State Geologist Prepared as a Guidebook for the 29th Annual Tri-State Field Conference WISCONSIN October 9 and 10, 1965 Information Circular Number 6 University of Wisconsin GEOLOGICAL AND NATURAL HISTORY SURVEY George F. Hanson, State Geologist and Director CAMBRO-ORDOVICIAN STRATIGRAPHY OF SOUTHWEST WISCONSIN by M. E. Ostrom Assistant State Geologist Prepared as a Guidebook for the 29th Annual Tri-State Field Conference WISCONSIN October 9 and 10, 1965 Available from University of Wisconsin, Geological and Natural History Survey, 170 Science Hall, Madison, Wis. 53706. Price - 759. 13. Vertical Scale GENERALIZED CROSS SECTION feet Decorah Fm. 200 OF STOPS Platteville Fm. SINNIPEE' GP. 50 3. 12. Glenwood Mbr. I .-- - - , Tonli Mbr. i}(': 4. Sf. Peter Fm. 100 ... --- ~-, ,,--------- >-:'-;;.." ~,,,- "..,.. - __ "'SHAKOPEE FM,~ , " -s~ i - ....... _ _ _, ...... '--,~,- - ~'.~ I 50 2. PRAIRIE DU CHIEN GP. 10. II. " I o W 5. Oneota Fm. I 9. I Van Ose r Mbr. Jordan Fm. ---- ---- Norwalk Mbr. ---- ~ I...uui Mbr. - - - v Black Earlh Mbr. st LO'<'lrence frn. 1""":<.'-"1 IYluzomonie Mbr. - - --- ---- ..----- - - _ .·ZlI_ - - R@no Mbr. Franconia Fm. 8. 7. ~ Jomah Mbr. Birkmose Mbr. IranIan Mbr_ Mbr. - DRESBACH GP. Generalized Geologic Column for Southwestern Wisconsin Ordovician System Cincinnatian Series Maquoketa Shale Formation Champlainian Series Sinnipee Group Galena Dolomite Formation Dubuque Member Stewartville Member Prosser Member Decorah Shale Formation Ion Member Guttenberg Member Spechts Ferry Member Platteville Limestone Formation Quimby's Mill Member MacGregor Member Pecatonica Member 1 Ancell Group St.
    [Show full text]
  • Description of the Minneapolis and St. Paul District
    DESCRIPTION OF THE MINNEAPOLIS AND ST. PAUL DISTRICT. By Frederick W. Sardeson. INTRODUCTION. district described in this folio lies in the northwestern part and southern Wisconsin, in Illinois, and in Iowa, but not of the Upper Mississippi basin subprovince and embraces the in Minnesota. They are chiefly dolomitic limestones, which LOCATION AND RELATIONS OF THE DISTRICT. junction of the Mississippi and Minnesota valleys. (See fig. 2.) include many coral reefs. They were laid down in clear, shal­ The district here described is bounded by parallels 44° 45' low seas while this region was a low coastal plain between the and 45° 15' and by meridians 93° and 93° 30' and comprises OUTLINE OF THE GEOLOGY AND GEOGRAPHY OF THE UPPEE Laurentian highlands on the north and the sea on the south. the Anoka, White Bear, Minneapolis, and St. Paul quad­ MISSISSIPPI BASIN SUBPROVINCE. The Devonian system covers the Silurian and overlaps it on rangles, an area of 846 square miles. It is in southeastern Extent and general relations. The Upper Mississippi basin the north so that it rests on the Ordovician in southern Minnesota (see fig. 1) and includes nearly the whole of subprovince lies west of Lake Michigan, east of the Coteau Minnesota (see fig. 3), but elsewhere it has been more strongly Ramsey County, the greater part of Hennepin County, and des Prairies, north of the Carboniferous basin or coal fields of eroded away and is less extensive than the Silurian system. smaller parts of Anoka, Dakota, Scott, and Washington coun­ Illinois and Iowa, and south of The Ranges, a southward It consists of limestones and clay shales, which were laid down ties.
    [Show full text]
  • WELL and BORING RECORD 221072 Quad Brush Creek Update Quad ID 12A Minnesota Statutes Chapter 1031 Received Date 08/18/2014
    Minnesota Unique Well No. MINNESOTA DEPARTMENT OF HEALTH County Faribault Entry Date 11/16/1987 WELL AND BORING RECORD 221072 Quad Brush Creek Update Quad ID 12A Minnesota Statutes Chapter 1031 Received Date 08/18/2014 Well Name Township Range Dir Section Subsection Use Status Well Depth Depth Completed Date Well Completed Lic/Reg. No. WL-7 103 25 W 13 CDCCDB test well 1246 ft. 1246 ft. 10/13/1978 Elevation 1133 ft. Elev. Method Surveyed Aquifer Depth to Bedrock 100 ft Open Hole - ft Static Water Level ft Field Located By Minnesota Geological Survey Locate Method Digitized - scale 1:24,000 or larger (Digitizing Universal Transverse Mercator (UTM) - NAD83 - Zone 15 - Unique No. Verified Information from owner-site Input Source Minnesota Geological Survey UTM Easting (X) 437020 Geological Interpretation John Mossler Input Date 01/01/1990 UTM Northing (Y) 484084 Agency (Interpretation) Interpretaion Method Geologic study 1:24k to 1:100k Depth (ft.) Elevation (ft.) Geological Material Color Hardness From To Thickness From To Stratigraphy Primary Lithology Secondary Minor Lithology DRIFT 0 100 100 1133 1033 Quaternary deposit drift GALENA LIMESTONE 100 178 78 1033 955 Stewartville- limestone DECORAH SHALE 178 227 49 955 906 Decorah Shale shale PLATTEVILLE LIMESTONE 227 236 9 906 897 Platteville Formation limestone GLENWOOD SHALE 236 245 9 897 888 Glenwood Formation shale ST. PETER SANDSTONE 245 338 93 888 795 St.Peter Sandstone sandstone SHAKOPEE DOLOMITE 338 595 257 795 538 Prairie Du Chien dolomite JORDAN SANDSTONE 595 679 84 538 454 Jordan
    [Show full text]
  • WELL and BORING RECORD 231730 Quad Bricelyn Update Quad ID 12D Minnesota Statutes Chapter 1031 Received Date 10/03/2018
    Minnesota Unique Well No. MINNESOTA DEPARTMENT OF HEALTH County Faribault Entry Date 05/15/1996 WELL AND BORING RECORD 231730 Quad Bricelyn Update Quad ID 12D Minnesota Statutes Chapter 1031 Received Date 10/03/2018 Well Name Township Range Dir Section Subsection Use Status Well Depth Depth Completed Date Well Completed Lic/Reg. No. BURT FLO 1 101 25 W 11 CCDDCC observation well A 1413 ft. 1386 ft. 10/09/1979 Elevation 1176 ft. Elev. Method Surveyed Aquifer Mt.Simon Depth to Bedrock 79 ft Open Hole 125 - 126 ft Static Water Level 265.1 ft Field Located By Minnesota Geological Survey Locate Method Digitization (Screen) - Map (1:24,000) (15 meters Universal Transverse Mercator (UTM) - NAD83 - Zone 15 - Unique No. Verified Information from owner-site Input Source Minnesota Geological Survey UTM Easting (X) 435028 Geological Interpretation John Mossler Input Date 05/30/2001 UTM Northing (Y) 482308 Agency (Interpretation) Interpretaion Method Geologic study 1:24k to 1:100k Depth (ft.) Elevation (ft.) Geological Material Color Hardness From To Thickness From To Stratigraphy Primary Lithology Secondary Minor Lithology DRIFT 0 79 79 1176 1097 Quaternary deposit drift GALENA 79 228 149 1097 948 Stewartville- limestone DECORAH SHALE 228 278 50 948 898 Decorah Shale shale PLATTEVILLE LIMESTONE 278 285 7 898 891 Platteville Formation limestone GLENWOOD SHALE 285 293 8 891 883 Glenwood Formation shale ST. PETER SANDSTONE 293 378 85 883 798 St.Peter Sandstone sandstone SHAKOPEE 378 629 251 798 547 Prairie Du Chien dolomite JORDAN SANDSTONE 629 740
    [Show full text]
  • 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.
    [Show full text]
  • Geology to the Cost of Underground Projects 9
    MN DEPTOF TRANSPORTATION IIIIllIlR3 0314 00024IlA llIl 5513 AN EXAMINATION OF THE POTENTIAL TO REDUCE THE COST OF AN UNDERGROUND LRT ALIGNMENT THROUGH GEOLOGIC PLANNING AND TECHNOLOGICAL INNOVATION PHASE 1 Draft Prepared for CENTER FOR TRANSPORTATION STUDIES UNIVERSITY OF MINNESOTA September 1987 By AMERICAN UNDERGROUND-SPACE ASSOCIATION 511 11th Avenue South Box 320 Minneapolis, MN 55415 (612) 339-5403 Susan Nelson, Executive Director ACKNOWLEDGEMENTS Technical input was received from AUA members: Russell K. McFarland Vice President, Operations UTD, Incorporated 8220 Russell Road Alexandria, VA 22309 Charles R. Nelson Vice President, Engineering CNA Consulting Engineers 2800 University Avenue S.E. Minneapolis, MN 55414 Funding for is project has been provided through the Federal Department Exxon Petroleum Violations Escrow Fund. / I/-h yrx / c TABLE OF CONTENTS Page List of Figures 4 Introduction 5 Underground Construction Methods 7 The Importance of Geology to the Cost of Underground Projects 9 The Importance of Planning 12 Geology of the Twin Cities Metropolitan Region 13 Bedrock Geology 15 Hydrogeology 17 Geologic Hazards 18 Existing Structures 22 Minneapolis Data 24 Geology 24 Existing Structures in Bedrock 24 Existing Structures in Soils 26 Suitability of Proposed Transit Routes for an Underground Alignment 31 3 LIST OF FIGURES Figure 1 Geologic Column Figure 2 Areas of "Good" and "Fair" Soils Types, Minneapolis-St. Paul Urban Area, Minnesota Figure 3 Occurrence of Platteville limestone and St. Peter sandstone, Seven County Metropolitan Region, Minnesota Figure 4 Cross-section of Surficial Geology, Lake Harriet to U.S. 10-61 Figure Minneapolis Bedrock Geology Figure Minneapolis Surficial Geology Figure Existing Structures in St.
    [Show full text]
  • The Glenwood Beds As a Horizon Marker at the Base of the Platteville Formation
    C&flUifl W» 1H If QLluc wlH MS] mmIBS $Bft IK STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION A. M. SHELTON, Director DIVISION OF THE STATE GEOLOGICAL SURVEY M. M. LEIGHTON, Chief REPORT OF INVESTIGATIONS -NO. 9 THE GLENWOOD BEDS AS A HORIZON MARKER AT THE BASE OF THE PLATTEVILLE FORMATION BY ARTHUR BEVAN PRINTED BY AUTHORITY OF THE STATE OF ILLINOIS URBANA, ILLINOIS 192 6 STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION A. M. SHELTON. Director DIVISION OF THE STATE GEOLOGICAL SURVEY M. M. LEIGHTON. Chief Committee of the Board of Natural Resources and Conservation A. M. Shklton, Chairman Director of Registration and Education Kendric C. Babcock Representing the President of the Uni- versity of Illinois Edson S. Bastix Geologist Schnepp& Barnes, Printers Springfield, Ii.i.. 1926 1G416—2M THE GLENWOOD BEDS AS A HORIZON MARKER AT THE BASE OF THE PLATTEVILLE FORMATION By Arthur Bevan OUTLINE PAfiE Introduction 5 Purpose of the report 5 General statement 5 The Glenwood beds 6 General character and stratigraphic relations 6 Distribution and character in Illinois 7 Character in the Oregon basin 8 Stratigraphic relations in Illinois . 11 Geologic history 12 ILLUSTRATIONS FIGURE 1. Map of northern Illinois showing the approximate line of outcrop of the Glenwood beds beneath the glacial drift 4 2. Microphotographs of Glenwood sandstone in the vicinity of Oregon 9 3. Unconformity between the St. Peter sandstone and Platteville-Galena dolomite at Deer Park 12 TABLE 1. Geologic time divisions of the Paleozoic era and epochs of the Ordovician period 5 GLKNWOOI) BEDS AS A HORIZON MARKER Area underlain by Platteville and (or) later formations Area underlain by St.
    [Show full text]
  • Seeps and Springs at a Platteville-Observatory-On the River
    SEEPS AND SPRINGS AT A PLATTEVILLE “OBSERVATORY” ON THE RIVER BLUFFS BJ Bonin Independent Contract Geologist, 284 Macalester Street, St. Paul, MN, 55105 USA [email protected] Greg Brick Department of Earth Sciences, University of Minnesota, Minneapolis, MN, 55455 USA [email protected] Julia Steenberg Minnesota Geological Survey, 2609 Territorial Road, St. Paul, MN, 55114 USA [email protected] Abstract teville–Glenwood Shale contact. Overall, the hydro- Residential building construction along the Mississip- stratigraphic attributes of this site are consistent with pi River bluffs in the 1970s created a unique enclosed how the Platteville has been recently characterized in the outcrop of the Late Ordovician Platteville Formation TCM area in a fractured bluff edge setting (Anderson et at Lilydale, Minnesota. This outcrop was examined in al., 2011). early 2013 after a newly-formed spring flooded an el- evator shaft the previous year, drawing attention to the The enclosed outcrop features many seep- and spring- foundation conditions. related mineral deposits. Most notable were the iron- stained flowstone and microgours near the seeps and The Lexington Riverside property is a six story condo- springs along fractures in the limestone, and calcite rafts minium complex constructed within the top of the bluff. on the surfaces of the pools. At some damp locations a A two-level underground parking garage was built into fungal ecosystem has developed. Gypsum beards have the bluff. Bedrock was mechanically excavated to ac- grown in dry portions of the cavern. commodate the construction of the building, creating This man-made cavern, and others nearby, present an unweathered rock surface.
    [Show full text]