Calibration and Validation of SWAT for the Upper Maquoketa River Watershed
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The Prettiest Dam on the Maquoketa River
The Prettiest Dam on the Maquoketa River The Quaker Mill Dam at Manchester, Iowa Published by Office of the State Archaeologist University of Iowa Iowa City OSA Booklet 2017 Title quote “The Prettiest Dam on the Maquoketa River” is taken from Kinney (1967). Cover images Front— Quaker Mill Dam and bridge, circa 1900–1910 (Robert Ungs). Front inside—Quaker Mill Dam and bridge, circa 1900–1910 (Robert Ungs). Back—various historic postcards (Robert Ungs). The Prettiest Dam on the Maquoketa River The Quaker Mill Dam at Manchester, Iowa By Richard J. Carlson With contributions by Chérie E. Haury-Artz and layout by Angela R. Collins (Office of the State Archaeologist, University of Iowa) Prepared for and funded by the Iowa Department of Natural Resources 1869 map of Manchester area with Quaker Mill circled (Thompson and Everts, Library of Congress, Geography and Map Division). Quaker Mill, dam, and bridge circa 1900–1910 (Robert Ungs). Introduction The Maquoketa River in northeast Iowa has long been one earliest dam was a wooden struc- of state’s premier rivers, both for the water power that sup- ture built in 1852 to supply power ported its many industries and for its scenic beauty and rec- to a saw mill and later to a flour reational opportunities. The river’s water power was a major mill. After a series of wooden dams attraction for early settlers. Dams were constructed at many were built in this location, only to points along the river from the 1840s through the 1930s. be destroyed by floods, a more permanent concrete dam The first dams powered grist mills and saw mills. -
Maquoketa River Access to Retz Park
Photos courtesy of Larry Reis Maquoketa LINDSEY BRIDGE TO MANCHESTER WHITEWATER PARK MAQUOKETA RIVER ACCESS TO RETZ PARK SEGMENT ONE SEGMENT THREE H W 165th St. 165th St. Y e e e v 1 v 6 1 v 5 A th A 3 HIGHLIGHTS St. MAQUOKETA RIVER ACCESS A LINDSEY BRIDGE ACCESS h h River Mile: 1036 h t 124.6 t River Mile: 124.6 Constructed in 2015, t Lindsey 5 5 0 F 2 2 Bridge i Manchester Whitewater Park 3 r 2 2 e t. 2 S P fl Red-Tailed Hawk Snapping Turtle has six 18-inch drops over d r i y 3 o R 6 d 800 feet, and is the largest . n 2 . e v e t S whitewater paddling nd A e 2 1 6 d r 2 6 n course in Iowa! R 2 2 HIGHLIGHTS 1 RIVER 3 d n 2 4 . This segment has been 124 d Delhi PADDLER’S GUIDE 5 DANGER: DAM A t Dam known to hold more bass h v Hartwick e S per mile and a higher percentage Lake t . of mature bass than any other Shearer 104 river stretch in Iowa! Wildlife Area Mallard Drake e 1 v 1 13 8 A 5 0 0 h t 103 t h t F 9 h i A 2 r S e 2 v t fl e . y 123 The Yellow Highlighed R d segment is a black bass . catch-and-release zone 180th St. RETZ PARK 180th 267th St. St 180th St. Mile LANDMARK (3) PADDLE TIME . -
Driftless Area - Wikipedia Visited 02/19/2020
2/19/2020 Driftless Area - Wikipedia Visited 02/19/2020 Driftless Area The Driftless Area is a region in southwestern Wisconsin, southeastern Minnesota, northeastern Iowa, and the extreme northwestern corner of Illinois, of the American Midwest. The region escaped the flattening effects of glaciation during the last ice age and is consequently characterized by steep, forested ridges, deeply carved river valleys, and karst geology characterized by spring-fed waterfalls and cold-water trout streams. Ecologically, the Driftless Area's flora and fauna are more closely related to those of the Great Lakes region and New England than those of the broader Midwest and central Plains regions. Colloquially, the term includes the incised Paleozoic Plateau of southeastern Minnesota and northeastern Relief map showing primarily the [1] Iowa. The region includes elevations ranging from 603 to Minnesota part of the Driftless Area. The 1,719 feet (184 to 524 m) at Blue Mound State Park and wide diagonal river is the Upper Mississippi covers 24,000 square miles (62,200 km2).[2] The rugged River. In this area, it forms the boundary terrain is due both to the lack of glacial deposits, or drift, between Minnesota and Wisconsin. The rivers entering the Mississippi from the and to the incision of the upper Mississippi River and its west are, from the bottom up, the Upper tributaries into bedrock. Iowa, Root, Whitewater, Zumbro, and Cannon Rivers. A small portion of the An alternative, less restrictive definition of the Driftless upper reaches of the Turkey River are Area includes the sand Plains region northeast of visible west of the Upper Iowa. -
Grant-Little Maquoketa
Grant–Little Maquoketa River Watershed (WI) HUC: 7060003 Wisconsin Rapid Watershed Assessment Grant–Little Maquoketa River Rapid watershed assessments provide initial estimates of where conservation investments would best address the concerns of landowners, conservation districts, and other community organizations and stakeholders. These assessments help landowners and local leaders set priorities and determine the best actions to achieve their goals. Wisconsin October 2007 The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, sex, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To fi le a complaint of discrimination, write USDA, Director, Offi ce of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington DC 20250-9410, or call (202) 720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Grant–Little Maquoketa River Watershed (WI) HUC: 7060003 Contents Introduction 1 Common Resource Area Descriptions 2 Physical Description 2 Assessment of Waters 3 Soils 5 Drainage Classifi cation 5 Farmland Classifi cation 6 Hydric Soils 7 Highly Erodible Land (HEL) 8 Land Capability Classifi cation 9 Resource Concerns/Watershed Assessment 10 PRS and Other Data 11 Census and Social Data (Relevant) 12 Watershed Projects, Studies, Monitoring, Etc SW Savannah Ecological Landscape 13 Management Opportunities Partner Groups 14 Footnotes/Bibliography 15 Grant–Little Maquoketa River Watershed (WI) HUC: 7060003 Introduction The Grant–Little Maquoketa River Watershed is located in the Driftless Region of Southwest Wisconsin and northeast Iowa. -
Upper Mississippi River National Wildlife and Fish Refuge
UPPER MISSISSIPPI RIVER NATIONAL WILDLIFE AND FISH REFUGE McGregor District McGregor, Iowa ANNUAL NARRATIVE REPORT 1998 ·e Upper Mississippi River National Wildlife and Fish Refuge,McGregor District McGregor, Iowa 1998 Date INTRODUCTION Table of Contents Highlights Page 1. Monitoring and Studies a. Surveys and Censuses. 1 b. Studies and Investigation................................. 2 2. Habitat Restoration a. Wetland Restoration...................................... NTR b. Upland Restoration....................................... 2 c. Deep Water/Riverine Restoration.......................... 2 d. Environmental Management Program......................... 2 3. Habitat Management a. Water Level Management. 3 b. Moist Soil Management. 3 c. Graze/Mow/Hay. NTR d. Farming. 4 e. Forest Management.. 4 f. Fire Management. 4 g. Pest Plant Control....................................... 5 h. Other Habitat Management................................. 5 4. Fish and Wildlife Management a. Bird Banding ............................................ 5 b. Disease Monitoring and Treatment ........................ NTR c. Reintroductions ......................................... NTR d. Nest Structures ......................................... NTR e. Pest, Predator and Exotic Animal Control ................ 5 5. Coordination Activities a. Interagency Coordination................................. 6 b. Private Lands Activities................................. 7 6. Resource Protection a. Law Enforcement. 8 b. Permits and Economic Use Management ..................... -
Iowa Low-Head Dam Modification Success Stories
AFTER Vernon Springs (during low water) IOWA LOW-HEAD DAM MODIFICATION SUCCESS STORIES BEFORE by Vernon Springs d This booklet is dedicated to the 163 people known to have tragically lost their lives at Iowa’s low-head dams since 1900. a ACKNOWLEDGEMENTS Researched, written, and designed by Erica Lynn Blair. Thank you especially to Linda Appelgate and Bob Brammer for their generous and sustained editorial assistance throughout the process; to DNR’s Nate Hoogeveen for providing the map, photos, contacts, and many insights; and to Lyle Danielson, Robin Fortney, Roz Lehman, Teresa Opheim, and John Wenck for their guidance, advice, and feedback. Special thanks to the individuals who provided community success stories for this booklet: Anita Arnold, Anthony Bardgett, Dan Beck, Joel Bryan, Mimi Cameron, Harvey Chesmore, Jennifer Cowsert, Jim Cusick, Rick Dietz, David Finck, Bob Garms, Greg Gelwicks, Tom Gifford, Ty Graham, Doug Hawker, Willard Hawker, Dale Hein, Sonna Johnson, Dan Kirby, Bob Kloberdanz, Bonnie Koel, Jeff Korsmo, Steve Lindaman, Bruce Lindner, Troy Loeckle, Corinne Love, Orlan Love, Sean McEnany, Brian Moore, John Moran, Marcy Palmer, Mike Plumley, Cletus Ries, Kyle Sands, Adam Sears, Doug Schroeder, Wayne Schwartz, Randy Schweitzer, Gary Siegwarth, Greg Simmons, Ryan Sindelar, Joe Skinner, Greg Soenen, Chad Staton, Roger Thomas, Craig Van Otterloo, Timothy Vick, Piper Wall, Gene Warner, Ryan Wicks, Carol Williams, Ginger Williams, and Ronnie Wolfe. FUNDING This publication was made possible by grants from Iowa’s Resource Enhancement and Protection Conservation Education Program (REAP-CEP) and from the McKnight Foundation. by Iowa Rivers Revival P.O. Box 72 Des Moines, Iowa 50301 Phone: (515) 724-4093 Email: [email protected] Website: www.iowarivers.org PHOTO CREDITS Front cover: Iowa DNR. -
Iowa Trout Management Plan to Better Reflect Today’S Anglers and Coldwater Conservation Challenges
Iowa Department of Natural Resources A Plan for Iowa Trout Management Prepared by: Dan Kirby, Fisheries Management Biologist, Manchester District Michael Siepker, Fisheries Management Biologist, Decorah District Mike Steuck, Trout Program Supervisor Approved by: Joe Larscheid, Chief of Fisheries, Iowa Department of Natural Resources Approved January 2020 PLAN DEVELOPMENT This plan was informed by the long history of trout management in Iowa. Discussions with Iowa DNR trout program staff, as well as trout fisheries professionals in Minnesota, Missouri, and Wisconsin guided the development of this plan. Trout angler opinions, habits, and demographics measured as part of the Iowa Trout Angler Survey informed plan goals, as did angler suggestions and feedback gathered over recent years through meetings, phone, email, creel survey, social media, and direct personal interactions with staff. The authors consulted historic Iowa DNR planning documents and interviewed retired program personnel. Authors also incorporated comments from Fisheries Bureau’s leadership team before final approval in January 2020. EXECUTIVE SUMMARY Karst geological features of northeast Iowa create coldwater streams that support unique aquatic species including trout. Brook Trout are native to the region and Brown and Rainbow Trout are now common due to intensive stocking and management programs that have been refined over the past 140 years. Trout fishing is increasingly popular in streams of northeast Iowa, as well as the most populated communities of Iowa where trout are seasonally stocked into ponds. Trout fishery management over the past 50 years has focused on expanding fisheries through stocking, development of public access, habitat and watershed improvement, fish culture refinements, and diversifying fishing opportunities. -
Evolution of the Driftless Area and Contiguous Regions of Midwestern USA Through Pleistocene Periglacial Processes Michael Iannicelli*
The Open Geology Journal, 2010, 4, 35-54 35 Open Access Evolution of the Driftless Area and Contiguous Regions of Midwestern USA Through Pleistocene Periglacial Processes Michael Iannicelli*,# 1429 76 Street, Brooklyn, New York, NY 11228, USA Abstract: In the Driftless Area region and contiguous regions (Paleozoic Plateau and Iowan Erosion Surface) within the U.S.A., there are a variety of northwest to southeast oriented landforms. They are interpreted to have been formed by periglacial nival and cryoplanation erosion processes during the Pleistocene. It is proposed that the oriented landforms are initiated by erosion focused along the edges of northwest-southeast trending snow dunes. Over time, cryopedimentation/cryoplanation widens some of the landforms into broad pediments or planed surfaces. These processes left other landforms standing as narrow, northwest-southeast trending, isolated ridges (paha and rock paha). Oriented valleys were carved in bedrock in some areas and were also carved in loess or loess underlain by till within other areas. An overall regional northeast to southwest trend of increasing amounts of pre-Illinoian till cover is interpreted to form by different degrees of widespread nival erosion. The Pleistocene wind was an important, indirect cofactor in the development of both the till pattern and the previously mentioned landforms. Determining these events not only helps us to formulate an evolutionary model for all three regions as a unit but also justifies speculation that the Driftless Area may have been glaciated during pre-Illinoian times. Keywords: Driftless area, snow dunes, rock paha, cryopedimentation, cryoplanation. 1. INTRODUCTION about why the Driftless Area is “driftless”. -
Geologic Overview of the Paleozoic Plateau Region of Northeastern Iowa
Proceedings of the Iowa Academy of Science Volume 91 Number Article 4 1984 Geologic Overview of the Paleozoic Plateau Region of Northeastern Iowa George R. Hallberg Iowa Geological Survey E. Arthur Bettis III Iowa Geological Survey Jean C. Prior Iowa Geological Survey Let us know how access to this document benefits ouy Copyright ©1984 Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/pias Recommended Citation Hallberg, George R.; Bettis, E. Arthur III; and Prior, Jean C. (1984) "Geologic Overview of the Paleozoic Plateau Region of Northeastern Iowa," Proceedings of the Iowa Academy of Science, 91(1), 5-11. Available at: https://scholarworks.uni.edu/pias/vol91/iss1/4 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Proceedings of the Iowa Academy of Science by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. Hallberg et al.: Geologic Overview of the Paleozoic Plateau Region of Northeastern Proc. Iowa Acad. Sci. 91(1): 5-11, 1984 3 Geologic Overview of the Paleozoic Plateau Region of Northeastern Iowa GEORGE R. HALLBERG, E. ARTHUR BETTIS III, JEAN C. PRIOR Iowa Geological Survey, Iowa City, Iowa 52242 Steep slopes, varied slope aspects, and entrenched stream valleys carved into Paleozoic-age rocks provide the geologic framework for the unique and diverse ecology of northeastern Iowa. Differential weathering and erosion of these variable rock types resulted in irregular surface slopes in a multi-stepped, high-relief landscape. -
Quaker Mill Dam.Pdf
TC 557 .182 Q35 2017 The Prettiest Dam on the Maquoketa River The Quaker Mill Dam at Manchester, Iowa Pub Iished by Office of the State Archaeologist University of Iow a Iowa City OSA Booklet 2017 Title quote "The Prettiest Dam on the Maquoketa River" is taken from Kinney (1967). Cover images Front- Quaker Mill Dam and bridge, circa 1900-1910 (Robert Ungs). Front inside-Quaker Mill Dam and bridge, circa 1900-1910 (Robert Ungs). ' . The Prettiest Dam on the Maquoketa River The Quaker Mill Dam at Manchester, Iowa By Richard j. Carlson With contributions by Cherie E. Haury-Artz and layout by Angela R. Collins (Office of the State Archaeologist, University of Iowa) Prepared for and funded by the Iowa Department of Natural Resources ,-~ 1869 map of Manchester area with Quaker Mill circled (Thompson and Everts, Library of Congress, Geography and Map Division). <, . a. I/. _ -~ - - ~""'- IHE l}UAKER MILL. MANUHtSTtH, WW~ Quaker Mill, dam, and bridge circa 1900-191 o (Robert Ungs). Introduction The Maquoketa River in northeast Iowa has long been one earliest dam was a wooden struc of state's premier rivers, both for the water power that sup ture built in 1852 to supply power IOWA * ported its many industries and for its scenic beauty and rec to a saw mill and later to a flour reational opportunities. The river's wat er power was a major mill. After a series of wooden dams attraction for early settlers. Dams were construct ed at many were built in this location, only to points along the river from the 1840s through the 1930s. -
Floods of July 23–26, 2010, in the Little Maquoketa River and Maquoketa River Basins, Northeast Iowa
Prepared in cooperation with the Iowa Department of Transportation and Iowa Highway Research Board (Project HR–140) Floods of July 23–26, 2010, in the Little Maquoketa River and Maquoketa River Basins, Northeast Iowa Little Maquoketa River Basin Maquoketa River Basin IOWA Open-File Report 2011–1301 U.S. Department of the Interior U.S. Geological Survey Cover. Map of Iowa showing location of Little Maquoketa River and Maquoketa River Basins. Floods of July 23–26, 2010, in the Little Maquoketa River and Maquoketa River Basins, Northeast Iowa By David A. Eash Prepared in cooperation with the Iowa Department of Transportation and Iowa Highway Research Board (Project HR–140) Open-File Report 2011–1301 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. -
Flood of August 2, 1972, in the Little Maquoketa River Bas In, Dubuque County, Iowa
UN I TED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY FLOOD OF AUGUST 2, 1972, IN THE LITTLE MAQUOKETA RIVER BAS IN, DUBUQUE COUNTY, IOWA By Albert J. Heinitz, Hydrologist United States Geological Survey Prepared in cooperation with the IOWA STATE HIGHWAY COMMISSION Open-file Report 18 -- d.. Iowa City, Iowa September 1973 U.S. GEOLOGICAL SURVEY P.O. BOX 1230 c. :r ::-1 IOWA CITY, lA 52244 c. I - . _, UBRARY COPY 'lt U NI TED STATES _ _, i- DEPARTMENT OF THE INTER lOR'··· GEO LOGI CAL SURV EY FLOOD OF AUGUST 2, 1972, IN THE LITTLE MAQUOKETA RIVER BAS IN , DUBUQUE COUNTY, IOWA c_. By Albert J . Heinitz, Hydrologist -::. United States Ge ological Survey Prepa red in cooperat ion with the IOWA STATE HIGHWAY CO M MISSION Open- f ile Re p ort Iowa City, Iowa Septe mber 1973 CONTENTS Page Abstract. • . 1 Introduction. 2 Acknowledgments 4 Basin description 4 Flood history . 5 Flood of August 2, 1972 8 Description. • • • . • • . • . • . • • • . • 8 Peak stages and discharges . 9 Flood frequency • • • . 13 Selected references • 16 Appendix. • . • • • 17 Gaging-station records 5-4143.5 Little Maquoketa River near Graf. 18 5-4144 Middle Fork Little Maquoketa River near Rickardsville. 20 5-4144.5 North Fork Little Maquoketa River near Rickardsville. 22 5-4145 Little Maquoketa River near Durango . 24 5-4146 Little Maquoketa River tributary at Dubuque •.•.•••.••.•• 27 iii ILLUSTRATIONS Page Figure 1. Map of Little Maquoketa River basin showing location of flood-measurement sites and isohyetal data .••••••• 3 2. Maximum flood peaks in northeast Iowa •• 6 3. Stage and discharge hydrographs for Little! Maquoketa River near Durango, August 1-3, 1972 •••.••.•••• 12 4.