Loess Investigations in Mississippi

Total Page:16

File Type:pdf, Size:1020Kb

Loess Investigations in Mississippi Loess Investigations in Mississippi CEOLOCY OF MISSISSIPPI LOESS J. O. SNOWDEN, JR. RICHARD R. PRIDDY FORESTS OF WEST CENTRAL MISSISSIPPI AS AFFECTED BY LOESS C. D. CAPLENOR, ET AL BULLETIN 111 MISSISSIPPI GEOLOGICAL, ECONOMIC AND TOPOGRAPHICAL SURVEY WILLIAM HALSELL MOORE Director and State Geologist JACKSON, MISSISSIPPI 1968 PRICE $3.00 Loess Investigations in Mississippi CEOLOCY OF MISSISSIPPI LOESS J. O. SNOWDEN, JR. RICHARD R. PRIDDY FORESTS OF WEST CENTRAL MISSISSIPPI AS AFFECTED BY LOESS C. D. CAPLENOR, ET AL BULLETIN 111 MISSISSIPPI GEOLOGICAL, ECONOMIC AND TOPOGRAPHICAL SURVEY WILLIAM HALSELL MOORE Director and State Geologist JACKSON, MISSISSIPPI 1968 PRICE $3.00 STATE OF MISSISSIPPI Hon. John Bell Williams — Governor MISSISSIPPI GEOLOGICAL, ECONOMIC AND TOPOGRAPHICAL SURVEY BOARD BOARD Hon. Henry N. Toler, Chairman _— ..Jackson Hon. Don H. Echols, Vice Chairman — Jackson Hon. William E. Johnson — Jackson Hon. N. D. Logan - Oxford Hon. Richard R. Priddy _..Jackson STAFF William H. Moore Director and State Geologist Wilbur T. Baughman Geologist Alvin R. Bicker, Jr. Geologist Theo H. Dinkins, Jr _ - Geologist Thad N. Shows _ — Geologist Charles H. Williams, Jr Geologist Jean K. Spearman - Secretary Shirley J. Webb Secretary LETTER OF TRANSMITTAL Office of the Mississippi Geological, Economic and Topographical Survey Jackson, Mississippi August 15, 1968 Mr. Henry N. Toler, Chairman, and Members of the Board Mississippi Geological, Economic and Topographical Survey Gentlemen: Herewith is Mississippi Geological Survey Bulletin 111, "Loess Investigations in Mississippi," by J. O. Snowden, Jr., Richard R. Priddy, and others. This Bulletin is the result of eight years of study. It contains the results of intensive field and laboratory studies. The loess is examined from the standpoint of stratigraphy, mineralogy, chemistry and electrical character. In addition there are supporting articles on ceramic properties and the flora and fauna supported by the loess. Bulletin 111 is the most comprehensive study of the loess that has been made in this area. Respectfully submitted, William H. Moore Director and State Geologist WHM:js LOESS INVESTIGATIONS IN MISSISSIPPI 5 GEOLOGY OF MISSISSIPPI LOESS CONTENTS Page GEOLOGY OF MISSISSIPPI LOESS (Snowden and Priddy) 13 Abstract 13 Introduction 14 Review of Literature 15 Preliminary Statement 15 Summaries of Selected Reports on Loess 15 General Description of the Study Area 31 Location 31 Topography 31 Field Investigations 35 Preliminary Statement — 35 Methods of Field Investigations 35 Collection of samples 35 Exposed sections ~ 35 Roadcuts 35 Gravel pits 38 Hand auger holes 38 Core holes 38 Measuring sections 39 Measuring electrical properties 39 Exposed sections 39 Auger and core holes 39 Gamma ray emission logging — 40 Thickness and areal distribution 40 Preliminary Statement 40 Relation of Loess to Pre-Loess Topography 40 Relation of Loess Thickness and Areal Distribution to Distance from Bluff 44 Eastern Limit of Mississippi Loess Belt — 47 Laboratory Investigations 49 Preliminary Statement 49 Preparative Procedures 50 Analytical Methods—Mineralogical, Textural, Chemical, and Radiometric 51 Instrumentation—X-ray, Microscopes, Hydrometer, and Computer 53 Mineralogy 54 Preliminary Statement 54 Quartz and Feldspar 54 Carbonates 58 Accessory Heavy Minerals 67 Description of heavy minerals 68 Provenance of the loess based on its heavy mineral assemblage 73 Clay Mineralogy 74 Identification and classification of clay minerals 74 Quantitative estimation of clay minerals in Mississippi loess ~ 79 Distribution of clay minerals 82 Source of clay minerals in Mississippi loess 85 Mineralogical Classification 85 MISSISSIPPI GEOLOGICAL SURVEY Page Texture 89 Preliminary Statement 89 Textural Variability 89 Geographic variability 93 Interrelations among the textural parameters 94 Other Textural and Structural Characteristics 98 Shape and arrangement of grains 98 Cementation and structural stability of Mississippi loess .. 98 Electrical Measurements as an Aid in Stratigraphy 101 Preliminary Statement 101 Electrical Conductivity Logging of the Outcrops 101 Electrical Conductivity Logging of Holes Drilled into the Loess 103 Neltronic Gamma Ray Logging of Holes 108 Utilization of Physical, Electrical, and Chemical Variations in Loess Stratigraphy 109 Preliminary Statement 109 Physical Criteria for Zoning in the Field 110 Color 110 Moisture content 111 Effervescence with acid 111 Caliche content 112 Snail content 112 Grain size 113 Chemical Criteria for Zoning in the Field 113 Soluble carbonate determinations 113 pH and Eh determinations 113 pH readings—basicity of loess 114 Eh readings—reducing-oxidizing potential of loess ...114 Electrical Determinations of Loess in the Field 115 Between movable electrodes 115 Gamma ray logging 117 Stratigraphy 118 Preliminary Statement 118 Previous Stratigraphic Reports and General Observations 118 Radiocarbon Dating of Mississippi Loess 119 Standard Section and Stratigraphic Classification 124 Pre-Loess Stratigraphy 128 Orgin 129 Preliminary Statement 129 Source of Mississippi Loess 129 Mode of Loess Deposition 129 Eolian deposition of loess 130 Loessification 132 Observations on the genesis of Mississippi loess 132 Conclusions 138 Acknowledgments 140 Selected Bibliography 142 Appendix 170 Location and General Description of Loess Samples 170 Chemical Analyses of Loess 184 Texture of Loess and Related Sediments 190 Pyrophysical (Ceramic) and Plastic Properties of Mississippi Loess 195 Pulmonate Gastropods in the Loess 201 LOESS INVESTIGATIONS IN MISSISSIPPI 7 LIST OF TABLES Table Page 1. Accessory heavy minerals and non-carbonate light minerals in the loess and related sediments 55 2. Hornblende-kyanite ratios of mixed loess-Citronelle non opaque accessory heavy mineral assemblages _ 73 3. Average non-opaque heavy mineral assemblage of Mississippi loess compared with upper Mississippi Valley and Illinois Valley loesses 75 4. Record of hand auger hole drilled at footage 12,445, atop first bench of road cut, east side of U. S. Highway 61 bypass 107 5. Radiocarbon ages of fossil pulmonate gastropod shells and one fossil wood sample from loess deposits near Vicksburg, Mississippi 121 6. Location and general description of loess samples 170 7. Chemical analyses of loess —184 8. Texture of loess and related sediments 190 9. Pyrophysical properties of Mississippi loess 198 10. Dry and plastic properties of Mississippi loess 200 11. Fossil gastropods in Mississippi loess 202 LIST OF FIGURES Figure PaSe 1. Generalized distribution of loess in the central United States facing page 14 2. Sample stations and general topography in the central Mississippi loess belt — — 32 3. Sample stations in the Greenwood, Mississippi area — 33 4. Sample stations in the Louisiana-Mississippi border area — 34 5. Vertical, terraced highway cuts on U. S. Highway 61 bypass near Vicksburg, Mississippi — ~ - - 36 6. Highway profiles through the loess hills near Vicksburg, Mississippi 37 7. Section A-A': Loess distribution and bedrock stratigraphy near Vicksburg, Mississippi - — 41 8. Cross section of lower Mississippi Valley region near Natchez, Mississippi 42 9. Roadcut on U. S. Highway 61 bypass showing loess-pre-loess topographic relationship — — 43 10. Roadcut along U. S. Highway 61 bypass showing general topography and highway engineering practice 43 11. Roadcut on U. S. Highway 61 bypass showing a truncated loess-covered ridge facing the Mississippi Alluvial Plain 44 12. Relationship between ridge-top loess thickness and distance from Mississippi River bluffs, Vicksburg east to Jackson, Mississippi - 45 13. Thickness of loess in the lower Mississippi Valley 46 14. Roadcut on U. S. Highway 80 near Clinton, Mississippi showing typical thin leached loess near to east margin. The loess rests on gray silty sand of the Catahoula (Miocene) forma tion -— — - 48 15. Flow diagram of preparative procedures and mineralogical- textural analytical techniques .— 49 16. Flow diagram of preparative procedures and chemical analy tical techniques ——— - 52 17. MgO, CaO, and COo mole fractions in loess from auger hole 3, Warren County, Mississippi, revealing carbonate mineral zones - 59 8 MISSISSIPPI GEOLOGICAL SURVEY Figure Page 18. X-ray diffractograms of bulk loess from auger hole 3, show ing mineralogy of the three carbonate zones 61 19. X-ray diffractograms of bulk loess demonstrating the range of carbonate mineral variation 62 20. X-ray diffractogram of loess concretion showing high calcite content due to ground water concentration 63 21. X-ray diffractograms comparing shell mineralogy of fossil and living Allogona profunda 64 22. Loess concretions 65 23. MgO, CaO, and COL, mole fractions in loess at road cut 10 (Figure 6) showing cyclic carbonate mineral zones 67 24. Mean accessory heavy mineral assemblages of loess and re lated sediments 71 25. Mean non-opaque, non-micaceous accessory heavy mineral composition of loess and related sediments 72 26. X-ray powder diffractograms showing typical loess clay mineralogy 77 27. X-ray powder diffractograms showing mineralogical differ ences between the less-than-two micron and the 2-5 micron particle diameter fractions of the loess 80 28. X-ray powder diffractograms showing clay mineral differ ences among loess, "Citronelle", and mixtures of the two 83 29. Petrographic classification of Mississippi loess 87 30. Mean mineral composition of Mississippi loess 87 31. Grain-size distribution of Mississippi loess and related sediments .. 90 32. Typical cumulative
Recommended publications
  • Nichols Arboretum: Soil Types
    Nichols Arboretum: Soil Types Not Present in Arboretum Boyer Sandy Loam 0-6% Slopes Fox Sandy Loam 6-12% Slopes Miami Loam 2-6% Slopes Miami Loam 6-12% Slopes Miami Loam 12-18% Slopes Miami Loam 18-25% Slopes Miami Loam 25-35% Slopes Sloan Silt Loam, Wet Water Wasepi Sandy Loam 0-4% Slopes Mary Hejna : September 2012 0 0.125 0.25 Miles Data from NRCS Soil Survey t Soil Series Descriptions BOYER SERIES The Boyer series consists of very deep, well drained soils formed in USE AND VEGETATION sandy and loamy drift underlain by sand or gravelly sand outwash at Soils are cultivated in most areas. Principal crops are corn, small depths of 51 to 102 cm (20 to 40 inches). grain, soybeans, field beans, and alfalfa hay. A few areas remain in GEOGRAPHIC SETTING permanent pasture or forest. The dominant forest trees are oaks, hickories, and maples. Boyer soils are on outwash plains, valley trains, kames, beach ridges, river terraces, lake terraces, deltas, and moraines of Wisconsinan age. TYPICAL PEDON The slope gradients are dominantly 0 to 12 percent, but range from 0 Boyer loamy sand, on a 4 percent slope in a cultivated field. (Colors to 50 percent. Boyer soils formed in sandy and loamy drift underlain are for moist soil unless otherwise stated.) by sand or gravelly sand outwash at depths of 51 to 102 cm (20 to 40 inches). Quartz is the dominant mineral in the 3C horizon, which Ap--0 to 18 cm (7 inches); dark grayish brown (10YR 4/2) loamy contains, in addition, varying amounts of material from igneous and sand, light brownish gray (10YR 6/2) dry; weak fine granular metamorphic rocks, limestone, and dolomite.
    [Show full text]
  • Institutional Database of Staff Publications Tennessee Division of Archaeology
    Institutional Database of Staff Publications Tennessee Division of Archaeology Title: Archaeological Investigations at 40LK3 and Implications for Future Management Decisions at Reelfoot Lake, Tennessee. Year: 1991 Name(s): Robert C. Mainfort, Jr. and Michael C. Moore Source: Tennessee Archaeologist 16(2):180-197 Division of Archaeology • 1216 Foster Ave. • Cole Bldg #3 • Nashville, TN 37243 Tel: 615-741-1588 • Fax: 615-741-7329 • www.tennessee.gov/environment/section/arch-archaeology TENNESSEE ANTHROPOLOGIST VOLUME XVI, NUMBER 2 FALL 1991 ARCHAEOLOGICAL INVESTIGATIONS AT 40LK3 AND IMPLICATIONS REELFOOT LAKE 179 FOR FUTURE MANAGEMENT DECISIONS AT REELFOOT LAKE, TENNESSEE Robert C. Mainfort, Jr. and Michael C. Moore ~ .... ABSTRACT Archaeological investigations at mound site 40LK3 under drought conditions discovered intact features within an area submerged during the New Madrid earthquake of 1811-1812. Associated ceramic vessel forms suggest an occupation of post A.O. 1050 to 1150. The identification of intact prehistoric features explicitly illustrates that recently proposed water level changes pose a serious threat to archaeological sites below as well as above the current pool elevation. Introduction Archaeological investigations along the bluff s and bottoms near Reelfoot Lake in northwest Tennessee have recorded numerou s prehistori c sites (Mainfort 1989). · Temporally sensitive artifacts from these locales document habitation of the Reelfoot area primarily within the Late Woodland and Mississippian periods. Few indications of Paleo-Indian or Archaic use have been recorded to date. This article presents the results of limited test excavations at 40LK3, a late prehistoric mound and habitation site on the shores of Reelfoot Lake. In l addition, we will discuss the implications of these results for recently proposed \ •, management decisions at Reelfoot Lake.
    [Show full text]
  • Port Silt Loam Oklahoma State Soil
    PORT SILT LOAM Oklahoma State Soil SOIL SCIENCE SOCIETY OF AMERICA Introduction Many states have a designated state bird, flower, fish, tree, rock, etc. And, many states also have a state soil – one that has significance or is important to the state. The Port Silt Loam is the official state soil of Oklahoma. Let’s explore how the Port Silt Loam is important to Oklahoma. History Soils are often named after an early pioneer, town, county, community or stream in the vicinity where they are first found. The name “Port” comes from the small com- munity of Port located in Washita County, Oklahoma. The name “silt loam” is the texture of the topsoil. This texture consists mostly of silt size particles (.05 to .002 mm), and when the moist soil is rubbed between the thumb and forefinger, it is loamy to the feel, thus the term silt loam. In 1987, recognizing the importance of soil as a resource, the Governor and Oklahoma Legislature selected Port Silt Loam as the of- ficial State Soil of Oklahoma. What is Port Silt Loam Soil? Every soil can be separated into three separate size fractions called sand, silt, and clay, which makes up the soil texture. They are present in all soils in different propor- tions and say a lot about the character of the soil. Port Silt Loam has a silt loam tex- ture and is usually reddish in color, varying from dark brown to dark reddish brown. The color is derived from upland soil materials weathered from reddish sandstones, siltstones, and shales of the Permian Geologic Era.
    [Show full text]
  • Determination of Geotechnical Properties of Clayey Soil From
    DETERMINATION OF GEOTECHNICAL PROPERTIES OF CLAYEY SOIL FROM RESISTIVITY IMAGING (RI) by GOLAM KIBRIA Presented to the Faculty of the Graduate School of The University of Texas at Arlington in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE IN CIVIL ENGINEERING THE UNIVERSITY OF TEXAS AT ARLINGTON August 2011 Copyright © by Golam Kibria 2011 All Rights Reserved ACKNOWLEDGEMENTS I would like express my sincere gratitude to my supervising professor Dr. Sahadat Hos- sain for the accomplishment of this work. It was always motivating for me to work under his sin- cere guidance and advice. The completion of this work would not have been possible without his constant inspiration and feedback. I would also like to express my appreciation to Dr. Laureano R. Hoyos and Dr. Moham- mad Najafi for accepting to serve in my committee. I would also like to thank for their valuable time, suggestions and advice. I wish to acknowledge Dr. Harold Rowe of Earth and Environmental Science Department in the University of Texas at Arlington for giving me the opportunity to work in his laboratory. Special thanks goes to Jubair Hossain, Mohammad Sadik Khan, Tashfeena Taufiq, Huda Shihada, Shahed R Manzur, Sonia Samir,. Noor E Alam Siddique, Andrez Cruz,,Ferdous Intaj, Mostafijur Rahman and all of my friends for their cooperation and assistance throughout my Mas- ter’s study and accomplishment of this work. I wish to acknowledge the encouragement of my parents and sisters during my Master’s study. Without their constant inspiration, support and cooperation, it would not be possible to complete the work.
    [Show full text]
  • A Study of Unstable Slopes in Permafrost Areas: Alaskan Case Studies Used As a Training Tool
    A Study of Unstable Slopes in Permafrost Areas: Alaskan Case Studies Used as a Training Tool Item Type Report Authors Darrow, Margaret M.; Huang, Scott L.; Obermiller, Kyle Publisher Alaska University Transportation Center Download date 26/09/2021 04:55:55 Link to Item http://hdl.handle.net/11122/7546 A Study of Unstable Slopes in Permafrost Areas: Alaskan Case Studies Used as a Training Tool Final Report December 2011 Prepared by PI: Margaret M. Darrow, Ph.D. Co-PI: Scott L. Huang, Ph.D. Co-author: Kyle Obermiller Institute of Northern Engineering for Alaska University Transportation Center REPORT CONTENTS TABLE OF CONTENTS 1.0 INTRODUCTION ................................................................................................................ 1 2.0 REVIEW OF UNSTABLE SOIL SLOPES IN PERMAFROST AREAS ............................... 1 3.0 THE NELCHINA SLIDE ..................................................................................................... 2 4.0 THE RICH113 SLIDE ......................................................................................................... 5 5.0 THE CHITINA DUMP SLIDE .............................................................................................. 6 6.0 SUMMARY ......................................................................................................................... 9 7.0 REFERENCES ................................................................................................................. 10 i A STUDY OF UNSTABLE SLOPES IN PERMAFROST AREAS 1.0 INTRODUCTION
    [Show full text]
  • The Distribution of Silty Soils in the Grayling Fingers Region of Michigan: Evidence for Loess Deposition Onto Frozen Ground
    Geomorphology 102 (2008) 287–296 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph The distribution of silty soils in the Grayling Fingers region of Michigan: Evidence for loess deposition onto frozen ground Randall J. Schaetzl ⁎ Department of Geography, 128 Geography Building, Michigan State University, East Lansing, MI, 48824-1117, USA ARTICLE INFO ABSTRACT Article history: This paper presents textural, geochemical, mineralogical, soils, and geomorphic data on the sediments of the Received 12 September 2007 Grayling Fingers region of northern Lower Michigan. The Fingers are mainly comprised of glaciofluvial Received in revised form 25 March 2008 sediment, capped by sandy till. The focus of this research is a thin silty cap that overlies the till and outwash; Accepted 26 March 2008 data presented here suggest that it is local-source loess, derived from the Port Huron outwash plain and its Available online 10 April 2008 down-river extension, the Mainstee River valley. The silt is geochemically and texturally unlike the glacial fl Keywords: sediments that underlie it and is located only on the attest parts of the Finger uplands and in the bottoms of Glacial geomorphology upland, dry kettles. On sloping sites, the silty cap is absent. The silt was probably deposited on the Fingers Loess during the Port Huron meltwater event; a loess deposit roughly 90 km down the Manistee River valley has a Permafrost comparable origin. Data suggest that the loess was only able to persist on upland surfaces that were either Kettles closed depressions (currently, dry kettles) or flat because of erosion during and after loess deposition.
    [Show full text]
  • Tennessee Fish Species
    The Angler’s Guide To TennesseeIncluding Aquatic Nuisance SpeciesFish Published by the Tennessee Wildlife Resources Agency Cover photograph Paul Shaw Graphics Designer Raleigh Holtam Thanks to the TWRA Fisheries Staff for their review and contributions to this publication. Special thanks to those that provided pictures for use in this publication. Partial funding of this publication was provided by a grant from the United States Fish & Wildlife Service through the Aquatic Nuisance Species Task Force. Tennessee Wildlife Resources Agency Authorization No. 328898, 58,500 copies, January, 2012. This public document was promulgated at a cost of $.42 per copy. Equal opportunity to participate in and benefit from programs of the Tennessee Wildlife Resources Agency is available to all persons without regard to their race, color, national origin, sex, age, dis- ability, or military service. TWRA is also an equal opportunity/equal access employer. Questions should be directed to TWRA, Human Resources Office, P.O. Box 40747, Nashville, TN 37204, (615) 781-6594 (TDD 781-6691), or to the U.S. Fish and Wildlife Service, Office for Human Resources, 4401 N. Fairfax Dr., Arlington, VA 22203. Contents Introduction ...............................................................................1 About Fish ..................................................................................2 Black Bass ...................................................................................3 Crappie ........................................................................................7
    [Show full text]
  • Frequency and Magnitude of Selected Historical Landslide Events in The
    Chapter 9 Frequency and Magnitude of Selected Historical Landslide Events in the Southern Appalachian Highlands of North Carolina and Virginia: Relationships to Rainfall, Geological and Ecohydrological Controls, and Effects Richard M. Wooten , Anne C. Witt , Chelcy F. Miniat , Tristram C. Hales , and Jennifer L. Aldred Abstract Landsliding is a recurring process in the southern Appalachian Highlands (SAH) region of the Central Hardwood Region. Debris fl ows, dominant among landslide processes in the SAH, are triggered when rainfall increases pore-water pressures in steep, soil-mantled slopes. Storms that trigger hundreds of debris fl ows occur about every 9 years and those that generate thousands occur about every 25 years. Rainfall from cyclonic storms triggered hundreds to thousands of debris R. M. Wooten (*) Geohazards and Engineering Geology , North Carolina Geological Survey , 2090 US Highway 70 , Swannanoa , NC 28778 , USA e-mail: [email protected] A. C. Witt Virginia Department of Mines, Minerals and Energy , Division of Geology and Mineral Resources , 900 Natural Resources Drive, Suite 500 , Charlottesville , VA 22903 , USA e-mail: [email protected] C. F. Miniat Coweeta Hydrologic Lab , Center for Forest Watershed Research, USDA Forest Service, Southern Research Station , 3160 Coweeta Lab Road , Otto , NC 28763 , USA e-mail: [email protected] T. C. Hales Hillslope Geomorphology , School of Earth and Ocean Sciences, Cardiff University , Main Building, Park Place , Cardiff CF10 3AT , UK e-mail: [email protected] J. L. Aldred Department of Geography and Earth Sciences , University of North Carolina at Charlotte , 9201 University City Blvd. , Charlotte , NC 28223 , USA e-mail: [email protected] © Springer International Publishing Switzerland 2016 203 C.H.
    [Show full text]
  • Parametric Terracing As Optimization of Controlled Slope Intervention
    water Article Parametric Terracing as Optimization of Controlled Slope Intervention Tomaž Berˇciˇc and Lucija Ažman-Momirski * Faculty of Architecture, University of Ljubljana, Zoisova 12, 1000 Ljubljana, Slovenia; [email protected] * Correspondence: [email protected] Received: 31 December 2019; Accepted: 21 February 2020; Published: 26 February 2020 Abstract: With the introduction of mechanization in agriculture, the area of terraced slopes has increased. However, in most cases, the planning of terracing in practice remains experience-based, which is no longer effective from an agricultural, geological, and hydrological point of view. The usual method of building terraces, especially terraces with earth risers, is therefore outdated, and a new method must be found for planning and building terraced areas. In addition to geographical information system (GIS) tools, parametric design tools for planning terraced landscapes are now available. Based on the design approaches for a selected plot in the Gorizia Hills in Slovenia, where we used a trial-and-error method, we improved previous results by defining a model using a computer algorithm that generates a terraced landscape on a selected slope depending on various input parameters such as the height of the terrace slope, the inclination of the terrace slope, the width of the terrace platform, and the number of terraces. For the definition of the algorithm we used the visual program tool Grasshopper. By changing the values of the input data parameters, the algorithm was able to present combinatorial simulations through a variety of different solutions with all the corresponding statistics. With such results it is much easier to make a conscious decision on which combination of parameters is optimal to prevent landslides, plan adequate drainage, and control soil movements when building terraces.
    [Show full text]
  • Landform Regions of Iowa — 2000
    LANDFORM REGIONS OF IOWA LANDFORM REGIONS2000 OF IOWA — 2000 0 20 40 60 miles 0 20 40 60 miles 0 40 80 kilometers 0 40 80 kilometers 327 Trowbridge Hall Iowa Department of NaturalIowa City, Resources Iowa 52242-1319 Geological Survey Bureau 109 Trowbridge Hallwww.iowageologicalsurvey.org Iowa City, Iowa 52242-1319 319-335-1575 Hydroscience & Engineering www.igsb.uiowa.edu Printed on recycled paper A landscape is a collection of shapes or landforms. LANDFORM REGIONS In Iowa, these shapes are composed of earth materials OF IOWA derived from glacial, wind, river, and marine environments of the geologic past. This map is a guide to seeing the state’s remarkably diverse landscapes and www.iowageologicalsurvey.org landform features. 319-335-1575 The Des Moines Lobe Southern Iowa Drift Plain Paleozoic Plateau The last glacier to enter Iowa advanced in a series of surges This region is dominated by glacial deposits left by ice Narrow valleys deeply carved into sedimentary rock beginning just 15,000 years ago and reached its southern sheets that extended south into Missouri over 500,000 of Paleozoic age and a near-absence of glacial deposits limit, the site of modern-day Des Moines, 14,000 years years ago. The deposits were carved by deepening define this scenic region. Fossil-bearing strata originated ago. By 12,000 years ago, the ice sheet was gone, leaving episodes of stream erosion so that only a horizon line as sediment on tropical sea floors between 300 and 550 behind a poorly drained landscape of pebbly deposits of hill summits marks the once-continuous glacial plain.
    [Show full text]
  • Sand Dunes Computer Animations and Paper Models by Tau Rho Alpha*, John P
    Go Home U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Sand Dunes Computer animations and paper models By Tau Rho Alpha*, John P. Galloway*, and Scott W. Starratt* Open-file Report 98-131-A - This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this program has been used by the U.S. Geological Survey, no warranty, expressed or implied, is made by the USGS as to the accuracy and functioning of the program and related program material, nor shall the fact of distribution constitute any such warranty, and no responsibility is assumed by the USGS in connection therewith. * U.S. Geological Survey Menlo Park, CA 94025 Comments encouraged tralpha @ omega? .wr.usgs .gov [email protected] [email protected] (gobackward) <j (goforward) Description of Report This report illustrates, through computer animations and paper models, why sand dunes can develop different forms. By studying the animations and the paper models, students will better understand the evolution of sand dunes, Included in the paper and diskette versions of this report are templates for making a paper models, instructions for there assembly, and a discussion of development of different forms of sand dunes. In addition, the diskette version includes animations of how different sand dunes develop. Many people provided help and encouragement in the development of this HyperCard stack, particularly David M. Rubin, Maura Hogan and Sue Priest.
    [Show full text]
  • Cultural Resources Overview
    United States Department of Agriculture Cultural Resources Overview F.orest Service National Forests in Mississippi Jackson, mMississippi CULTURAL RESOURCES OVERVIEW FOR THE NATIONAL FORESTS IN MISSISSIPPI Compiled by Mark F. DeLeon Forest Archaeologist LAND MANAGEMENT PLANNING NATIONAL FORESTS IN MISSISSIPPI USDA Forest Service 100 West Capitol Street, Suite 1141 Jackson, Mississippi 39269 September 1983 TABLE OF CONTENTS Page List of Figures and Tables ............................................... iv Acknowledgements .......................................................... v INTRODUCTION ........................................................... 1 Cultural Resources Cultural Resource Values Cultural Resource Management Federal Leadership for the Preservation of Cultural Resources The Development of Historic Preservation in the United States Laws and Regulations Affecting Archaeological Resources GEOGRAPHIC SETTING ................................................ 11 Forest Description and Environment PREHISTORIC OUTLINE ............................................... 17 Paleo Indian Stage Archaic Stage Poverty Point Period Woodland Stage Mississippian Stage HISTORICAL OUTLINE ................................................ 28 FOREST MANAGEMENT PRACTICES ............................. 35 Timber Practices Land Exchange Program Forest Engineering Program Special Uses Recreation KNOWN CULTURAL RESOURCES ON THE FOREST........... 41 Bienville National Forest Delta National Forest DeSoto National Forest ii KNOWN CULTURAL RESOURCES ON THE
    [Show full text]