72. Interior River Valleys and Hills 39. Ozark Highlands 47. Western Corn
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Upper Mississippi River Conservation Opportunity Area Wildlife Action Plan
Version 3 Summer 2012 UPPER MISSISSIPPI RIVER CONSERVATION OPPORTUNITY AREA WILDLIFE ACTION PLAN Daniel Moorehouse Mississippi River Pool 19 A cooperative, inter-agency partnership for the implementation of the Illinois Wildlife Action Plan in the Upper Mississippi River Conservation Opportunity Area Prepared by: Angella Moorehouse Illinois Nature Preserves Commission Elliot Brinkman Prairie Rivers Network We gratefully acknowledge the Grand Victoria Foundation's financial support for the preparation of this plan. Table of Contents List of Figures .............................................................................................................................. ii Acronym List .............................................................................................................................. iii I. Introduction to Conservation Opportunity Areas ....................................................................1 II. Upper Mississippi River COA ..................................................................................................3 COAs Embedded within Upper Mississippi River COA ..............................................................5 III. Plan Organization .................................................................................................................7 IV. Vision Statement ..................................................................................................................8 V. Climate Change .......................................................................................................................9 -
Delta Soils of Southeast Missouri
Delta Soils of Southeast Missouri he Mississippi River Alluvial Valley is called the shifts in stream channels, sometimes with clay over sand Delta region. The Delta includes parts of and vice versa (Figure 2). Missouri, Tennessee, Arkansas, Mississippi and Louisiana.T This report focuses on the Upper Delta in Southeast Missouri. It is one of the most fertile places for growing crops in the United States (Figure 1). The high crop productivity is due to the soils, climate and abundant ground water for irrigation. Delta soils were formed by alluvial sediments from the Mississippi and Ohio rivers and smaller rivers from the Ozark Highlands. Temperatures in the growing season are warm enough for producing cotton and rice, but also suited for producing high yields of corn and soybeans. Farmers often apply water with furrow and center pivot irrigation systems during periods of low rainfall. Figure 2. Delta soils were formed from river sediment deposits. They have slight to moderate profile layer development because of their young geologic age. Farmers should remember that the present prosperity of the region was preceded by the toil and struggle of the pioneers who cleared the land and constructed the first drainage ditches. There were many failures in capital investment for reclamation before the land became Figure 1. Most fields in the Delta region are 80 or more acres in size and productive. The physical, agricultural and cultural have been mechanically graded to about 0.1% slope for water drainage. development of the Delta forms a special chapter in the The slope on a given field usually depends on what required the least history of Missouri. -
The Naming, Identification, and Protection of Place in the Loess Hills of the Middle Missouri Valley
The Naming, Identification, and Protection of Place in the Loess Hills of the Middle Missouri Valley David T. McDermott B.A., Haverford College, 1979 B.S., State University of New York, 1992 M.A., University of Kansas, 2005 Submitted to the graduate degree program in Geography and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Doctor of Philosophy. _________________________________ James R. Shortridge, Ph. D., Chair _________________________________ J. Christopher Brown, Ph. D. _________________________________ Linda Trueb, Ph. D. _________________________________ Terry A. Slocum, Ph. D. _________________________________ William Woods, Ph. D. Date defended: October 22, 2009 The Dissertation Committee for David T. McDermott certifies that this the approved version of the following dissertation: THE NAMING, IDENTIFICATION, AND PROTECTION OF PLACE IN THE LOESS HILLS OF THE MIDDLE MISSOURI VALLEY Committee: _________________________________ James R. Shortridge, Ph. D., Chair _________________________________ J. Christopher Brown, Ph. D. _________________________________ Linda Trueb, Ph. D. _________________________________ Terry A. Slocum, Ph. D. _________________________________ William Woods, Ph. D. Date approved: October 27, 2009 ii It is inconceivable to me that an ethical relation to land can exist without love, respect, and admiration for land, and a high regard for its value. By value, I of course mean something broader than mere economic value; I mean value in the philosophical -
Ecological Regions of Minnesota: Level III and IV Maps and Descriptions Denis White March 2020
Ecological Regions of Minnesota: Level III and IV maps and descriptions Denis White March 2020 (Image NOAA, Landsat, Copernicus; Presentation Google Earth) A contribution to the corpus of materials created by James Omernik and colleagues on the Ecological Regions of the United States, North America, and South America The page size for this document is 9 inches horizontal by 12 inches vertical. Table of Contents Content Page 1. Introduction 1 2. Geographic patterns in Minnesota 1 Geographic location and notable features 1 Climate 1 Elevation and topographic form, and physiography 2 Geology 2 Soils 3 Presettlement vegetation 3 Land use and land cover 4 Lakes, rivers, and watersheds; water quality 4 Flora and fauna 4 3. Methods of geographic regionalization 5 4. Development of Level IV ecoregions 6 5. Descriptions of Level III and Level IV ecoregions 7 46. Northern Glaciated Plains 8 46e. Tewaukon/BigStone Stagnation Moraine 8 46k. Prairie Coteau 8 46l. Prairie Coteau Escarpment 8 46m. Big Sioux Basin 8 46o. Minnesota River Prairie 9 47. Western Corn Belt Plains 9 47a. Loess Prairies 9 47b. Des Moines Lobe 9 47c. Eastern Iowa and Minnesota Drift Plains 9 47g. Lower St. Croix and Vermillion Valleys 10 48. Lake Agassiz Plain 10 48a. Glacial Lake Agassiz Basin 10 48b. Beach Ridges and Sand Deltas 10 48d. Lake Agassiz Plains 10 49. Northern Minnesota Wetlands 11 49a. Peatlands 11 49b. Forested Lake Plains 11 50. Northern Lakes and Forests 11 50a. Lake Superior Clay Plain 12 50b. Minnesota/Wisconsin Upland Till Plain 12 50m. Mesabi Range 12 50n. Boundary Lakes and Hills 12 50o. -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
Pecatonica River: Targeting Conservation Practices in a Watershed to Improve Water Quality
Pecatonica River: Targeting conservation practices in a watershed to improve water quality Madison 151 Partners discuss new stream crossing on the Judd farm. © TNC Pleasant Valley Watershed One of the challenges facing landowners and managers in Wisconsin and nationwide is keeping sediment and phosphorus on the land and out of streams. Too much phosphorus leads to excessive algae growth, which consumes oxygen in the water and can contaminate The group tested this approach in the Pecatonica River drinking water. watershed in southwest Wisconsin, and the results are in. Farmers working with the project cut their estimated Since 2009, farmers and conservation groups in average phosphorus runoff and erosion almost in half, Wisconsin have worked together to test whether it is keeping an estimated average 4,400 pounds of phosphorus possible to target efforts to improve water quality to and 1,300 tons of sediment out of the water each year. have the greatest impact at the lowest possible cost. Just one year after fully implementing targeted changes The idea was to use science to target conservation to agricultural practices on approximately one third practices on those fields and pastures with the greatest of the crop and pasture acres in the watershed, water potential for contributing nutrients to streams. quality has improved. Launching a Pilot Project in Driftless Area Bypassed by the glaciers, the Driftless Area in southwest Wisconsin is characterized by steep- sided ridges and miles of rivers and smaller tributary streams that eventually drain into the Mississippi River. The pilot project took place in two sub-watersheds Changing crop rotations to increase cover on fields in winter gives the Kellers to the Pecatonica River: Pleasant Valley Branch another source of feed for some of their herd. -
Lake of the Ozarks Regional Housing Study Acknowledgments
LAKE OF THE OZARKS REGIONAL HOUSING STUDY ACKNOWLEDGMENTS The project team would like to acknowledge the contributions of the residents of the Lake Region, who gave their time, ideas, and exper- tise for the creation of this plan. It is only with their assistance and direction the plan gained the depth necessary to truly represent the spirit of the Lake Region and it is with their commitment that the plan will be implemented. We would also like to thank the partner organizations, Lake of the Ozarks Regional Economic Development Council who financially sup- ported this study and provided their leadership. A special thanks to everyone involved. Project Manager LOREDC BOARD Roger Corbin Tim Jacobsen Jeana Woods COMMITTEE Jacob Neusche Kim Willey Corey ten Bensel Linda Conner Brent Depeé Colleen Richey Debbie Hurr Russell Clay Jeff Hancock Cary Patterson Lori Hoelscher Vicki Devine Dennis Croxton Vicki Brown Kevin McRoberts Stan Schultz Roger Corbin CONSULTING TEAM RDG Planning & Design Omaha and Des Moines www.RDGUSA.com CHAPTER 1: INTRODUCTION 7 CHAPTER 2: PROFILE OF THE REGION 11 CHAPTER 3: CAMDEN COUNTY 49 CHAPTER 4: MORGAN COUNTY 79 CHAPTER 5: MILLER COUNTY 103 CHAPTER 6: LACLEDE COUNTY 127 CHAPTER 7: DEFINING HOUSING ISSUES / DIRECTIONS FORWARD 153 CHAPTER 1: Introduction 1 LAKE OF THE OZARKS REGIONAL HOUSING STUDY | Introduction INTRODUCTION The Lake of the Ozarks Regional Housing Study represents an in-depth study of the housing conditions of the three counties that constitute the Lake of the Ozarks Regional Economic Development Council (LOREDC). This includes the counties of Camden, Miller, and Morgan and the commercial centers of Camdenton, Eldon, Lake Ozark, Osage Beach, and Versailles. -
NATURAL RESOURCES (Updated Excerpt from Jo Daviess Comprehensive Plan Baseline Data)
ATTACHMENT F: NATURAL RESOURCES (Updated excerpt from Jo Daviess Comprehensive Plan Baseline Data) The natural resources in Jo Daviess County are unique relative to the rest of the state and much of the mid-west because the county is part of the Wisconsin Driftless Region bypassed by continental glaciers of the Ice Age. This region covers parts of southern Minnesota and Wisconsin, Northwestern Illinois and Northeastern Iowa. Glaciated areas were leveled, strewn with glacial debris or "drift" and dotted with lakes and ponds. The driftless areas, on the other hand, have bedrock close to the surface into which deep valleys have been carved by millions of years of weather and erosion. In Jo Daviess County, streams are numerous and the only two lakes are man-made. The relief from the higher ridges to the valley floors is typically 300 feet or more creating a rugged and scenic landscape. Ecosystems can be found in this landscape that are older than those found in glaciated areas. Geology The topography of Jo Daviess County is characterized by rugged relief unique to most of Illinois. Our county, located in the far northwestern corner of the state, is in an area spared by the major glaciations of the last two million years. It is, accordingly, called the "Driftless Area" by geologists, the term "drift" referring to material deposited by glacial activity. The visible landscape that we see today began during the Paleozoic Era (570 to 245 million years ago) when shallow seas repeatedly inundated the interior of the continent. Shells of marine animals, along with muds, silts and sands from eroding highlands, were periodically deposited in those sea bottoms. -
Characterization of Ecoregions of Idaho
1 0 . C o l u m b i a P l a t e a u 1 3 . C e n t r a l B a s i n a n d R a n g e Ecoregion 10 is an arid grassland and sagebrush steppe that is surrounded by moister, predominantly forested, mountainous ecoregions. It is Ecoregion 13 is internally-drained and composed of north-trending, fault-block ranges and intervening, drier basins. It is vast and includes parts underlain by thick basalt. In the east, where precipitation is greater, deep loess soils have been extensively cultivated for wheat. of Nevada, Utah, California, and Idaho. In Idaho, sagebrush grassland, saltbush–greasewood, mountain brush, and woodland occur; forests are absent unlike in the cooler, wetter, more rugged Ecoregion 19. Grazing is widespread. Cropland is less common than in Ecoregions 12 and 80. Ecoregions of Idaho The unforested hills and plateaus of the Dissected Loess Uplands ecoregion are cut by the canyons of Ecoregion 10l and are disjunct. 10f Pure grasslands dominate lower elevations. Mountain brush grows on higher, moister sites. Grazing and farming have eliminated The arid Shadscale-Dominated Saline Basins ecoregion is nearly flat, internally-drained, and has light-colored alkaline soils that are Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and America into 15 ecological regions. Level II divides the continent into 52 regions Literature Cited: much of the original plant cover. Nevertheless, Ecoregion 10f is not as suited to farming as Ecoregions 10h and 10j because it has thinner soils. -
Missouri Master Naturalist a Summary of Program Impacts and Achievements During 2017
Missouri Master Naturalist A summary of program impacts and achievements during 2017 Robert A. Pierce II Syd Hime Extension Associate Professor Volunteer and Interpretive Programs Coordinator and State Wildlife Specialist Missouri Department of Conservation University of Missouri 1 “The mission of the Missouri Master Naturalist program is to engage Missourians in the stewardship of the state’s natural resources through science-based education and community service.” Introduction Program Objectives The Missouri Master Naturalist program results 1. Improve public understanding of natural from a partnership created in 2004 between the resource ecology and management by Missouri Department of Conservation (MDC) developing a pool of local knowledge that and University of Missouri Extension. These can be used to enhance and expand two organizations are the sponsors of the educational efforts within local communities program at the state level. Within MU Extension, the Missouri Master Naturalist 2. Enhance existing natural resources Program has the distinction of being recognized education and outreach activities by as a named and branded educational program. providing natural resources training at the The MU School of Natural Resources serves as local level, thereby developing a team of the academic home for the program. dedicated and informed volunteers The program is jointly administered by state 3. Develop a self-sufficient Missouri Master coordinators that represent the MDC and MU Naturalist volunteer network through the Extension. The state program coordinators Chapter-based program. provide leadership in conducting the overall program and facilitate the development of An increasing number of communities and training and chapter development with Chapter organizations across the state have relied on Advisors representing both organizations as these skilled volunteers to implement natural interest is generated within a local community. -
Ecoregions of the Mississippi Alluvial Plain
92° 91° 90° 89° 88° Ecoregions of the Mississippi Alluvial Plain Cape Girardeau 73cc 72 io Ri Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and quantity of This level III and IV ecoregion map was compiled at a scale of 1:250,000 and depicts revisions and Literature Cited: PRINCIPAL AUTHORS: Shannen S. Chapman (Dynamac Corporation), Oh ver environmental resources; they are designed to serve as a spatial framework for the research, subdivisions of earlier level III ecoregions that were originally compiled at a smaller scale (USEPA Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Omernik, J.M., 1987, Ecoregions of the conterminous United States (map Barbara A. Kleiss (USACE, ERDC -Waterways Experiment Station), James M. ILLINOIS assessment, management, and monitoring of ecosystems and ecosystem components. By recognizing 2003, Omernik, 1987). This poster is part of a collaborative effort primarily between USEPA Region Ecoregions and subregions of the United States (map) (supplementary supplement): Annals of the Association of American Geographers, v. 77, no. 1, Omernik, (USEPA, retired), Thomas L. Foti (Arkansas Natural Heritage p. 118-125, scale 1:7,500,000. 71 the spatial differences in the capacities and potentials of ecosystems, ecoregions stratify the VII, USEPA National Health and Environmental Effects Research Laboratory (Corvallis, Oregon), table of map unit descriptions compiled and edited by McNab, W.H., and Commission), and Elizabeth O. Murray (Arkansas Multi-Agency Wetland Bailey, R.G.): Washington, D.C., U.S. Department of Agriculture - Forest Planning Team). 37° environment by its probable response to disturbance (Bryce and others, 1999). -
Level III Ecoregions of the Continental United States 3
1. Coast Range 2. Puget Lowland Level III Ecoregions of the Continental United States 3. Willamette Valley 4. Cascades (Revised August 2002) 5. Sierra Nevada National Health and Environmental Effects Research Laboratory 6. Southern and Central California 77 Chaparral and Oak Woodlands 77 U.S. Environmental Protection Agency 7. Central California Valley 1 2 2 8. Southern California Mountains 9. Eastern Cascades Slopes and Foothills 15 41 42 10. Columbia Plateau 10 11. Blue Mountains 49 17 48 12. Snake River Plain 82 10 17 13. Central Basin and Range 1 3 17 14. Mojave Basin and Range 4 17 15. Northern Rockies 11 58 16. Idaho Batholith 16 17 17. Middle Rockies 43 50 17 58 18. Wyoming Basin 51 19. Wasatch and Uinta Mountains 50 9 46 51 58 20. Colorado Plateaus 17 21. Southern Rockies 83 59 78 12 17 84 22. Arizona/New Mexico 4 80 57 58 Plateau 52 60 42 53 62 23. Arizona/New Mexico 56 Mountains 62 84 24. Chihuahuan Deserts 18 44 47 25. Western High Plains 57 61 57. Huron/Erie Lake Plains 26. Southwestern Tablelands 64 84 58. Northeastern Highlands 5 19 69 27. Central Great Plains 54 59. Northeastern Coastal Zone 28. Flint Hills 13 60. Northern Appalachian Plateau 55 29. Central Oklahoma/Texas Plains 70 63 and Uplands 25 40 30. Edwards Plateau 1 7 61. Erie Drift Plain 20 31. Southern Texas Plains 21 27 62. North Central Appalachians 32. Texas Blackland Prairies 67 63. Middle Atlantic Coastal Plain 66 33. East Central Texas Plains 64.