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ROOT RIVER ONE WATERSHED, ONE PLAN -I- SWCD Soil and Water Conservation District
Cold Snap Photography Prepared For: Root River Planning Partnership Prepared By: Houston Engineering, Inc. Photo by Bob Joachim Root River Watershed | ONE WATERSHED, ONE PLAN List of PLan Abbreviations i Plan Definitions iii Executive Summary iv 1. INTRODUCTION 1-1 1.1 Preamble 1-1 1.2 Plan Area 1-1 1.3 Watershed Characteristics 1-4 1.4 Plan Overview 1-4 1.5 Plan Partners and Roles in Plan Development 1-5 1.6 Incorporating Comments into the Plan __________________1-7 2. ANALYSIS AND PRIORITIZATION OF RESOURCES, CONCERNS, AND ISSUES CAUSING CONCERN 2-1 2.1 Definitions 2-1 2.2 Identifying Potential Resource Concerns and Issues 2-2 2.3 Prioritizing Potential Resource Concerns and Issues 2-13 2.4 Priority Resource Concerns and Issues 2-14 2.4.1 "A" Level Priorities 2-14 2.4.1.1 Description and Resource Concern Locations 2-14 2.4.1.2 Issues Affecting "A" Level Priority Resource Concerns 2-18 2.4.2 "B" Level Priorities 2-18 2.4.2.1 Description and Landscape Locations 2-18 2.4.2.2 Issues Affecting “B” Level Priority Resource Concerns 2-26 2.4.3 "C" Level Priorities 2-26 2.4.3.1 Issues Affecting “C” Level Priority Resource Concerns 2-35 2.5 Use of Priority Categories in Plan Implementation 2-35 2.6 Emerging Issues 2-35 2.6.1 "Scientific and Technical Emerging Issues 2-36 2.61.1 Climate Change and Infrastructure Resilience 2-36 2.6.1.2 Endocrine Active Compounds 2-37 2.6.1.3 Water Movement Within a Karst Landscape 2-37 2.6.1.4 Improving Soil Health 2-37 2.6.1.5 Buffers for Public Waters and Drainage Systems 2-38 2.6.1.6 Invasive Species 2-38 2.6.1.7 -
Classifying Rivers - Three Stages of River Development
Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion. -
Stream Channel and Vegetation Monitoring Reportreport,,,, 2005 Through 2008
Resurrection Creek Stream and Riparian Restoration Project Stream Channel and Vegetation Monitoring ReportReport,,,, 2005 through 2008 USDA Forest Service Chugach National Forest January 2009 Resurrection Creek Restoration Monitoring Report January 2009 Resurrection Creek Stream and Riparian Restoration Project Stream Channel and Vegetation Monitoring Report 2005 through 2008 USDA Forest Service Chugach National Forest Seward Ranger District Bill MacFarlane, Chugach National Forest Hydrologist Rob DeVelice, Chugach National Forest Ecologist Dean Davidson, Chugach National Forest Soil Scientist (retired) January 2009 1 Resurrection Creek Restoration Monitoring Report January 2009 Summary______________________________________________________________ The Resurrection Creek Stream Restoration project was implemented in 2005 and 2006, with project area revegetation continuing through 2008. Stream channel morphology and vegetation have been monitored in 2005, 2006, 2007, and 2008. This report compiles the 2008 data and summarizes the 4 years of monitoring data and the short-term response of the project area to the restoration. Each of the project objectives established prior to the implementation of this project were fully or partially accomplished. These included variables that quantify channel pattern, channel profile, side channels, aquatic habitat, and riparian vegetation. While the target values may not have been met in all cases, the intent of each objective was met through restoration. The response of the project area in the 3 years following restoration represents the short- term response to restoration. While numerous changes can occur in this period as the morphology and vegetation adjusts to the new conditions, no major channel changes have occurred on Resurrection Creek or its side channels, and vegetation growth in the riparian area has occurred as expected. -
Delineation Percentage
Lake Superior - North Rainy River - Headwaters Lake Superior - South Vermilion River Nemadji River Cloquet River Pine River Rainy River - Rainy Lake Little Fork River Mississippi River - Headwaters Leech Lake River Upper St. Croix River Root River Big Fork River Mississippi River - Winona Upper/Lower Red Lake Kettle River Mississippi River - Lake Pepin Mississippi River - Grand Rapids Mississippi River - La Crescent Crow Wing River Otter Tail River Mississippi River - Reno Mississippi River - Brainerd Zumbro River Redeye River Upper Big Sioux River Mississippi River - Twin Cities Snake River Des Moines River - Headwaters St. Louis River Rum River Lower Big Sioux River Lower St. Croix River Cottonwood River Minnesota River - Headwaters Cannon River Mississippi River - St. Cloud Long Prairie River Lake of the Woods Lower Rainy North Fork Crow River Mississippi River - Sartell Lac Qui Parle River Buffalo River Wild Rice River Minnesota River - Mankato Sauk River Rock River Redwood River Snake River Chippewa River Watonwan River Clearwater River East Fork Des Moines River Red River of the North - Sandhill River Upper Red River of the North Blue Earth River Red River of the North - Marsh River Roseau River Minnesota River - Yellow Medicine River Le Sueur River Little Sioux River Bois de Sioux River Cedar River Lower Minnesota River Pomme de Terre River Red Lake River Lower Des Moines River Upper Iowa River Red River of the North - Tamarac River Shell Rock River Two Rivers Rapid River Red River of the North - Grand Marais Creek Mustinka River South Fork Crow River Thief River Winnebago River Upper Wapsipinicon River 0% 10% 20% 30% 40% 50% 60% 70% 80% 90% 100% %Altered %Natural %Impounded %No Definable Channel wq-bsm1-06. -
Johnson Creek Restoration Project Effectiveness Monitoring
Bureau of Environmental Services • City of Portland Johnson Creek Restoration Projects Effectiveness Monitoring Reporting on data collected from 1997 through 2010 DECEMBER 2012 Dan Saltzman, Commissioner Dean Marriott, Director Dan Saltzman, Commissioner • Dean Marriott, Director Acknowledgements Implementation of the effectiveness monitoring program for restoration projects in the Johnson Creek Watershed has drawn on the expertise, support, and dedication of a number of individuals. We thank them for making this report possible. City of Portland, Environmental Services Staff Jennifer Antak, Johnson Creek Effectiveness Monitoring Program Lead Sean Bistoff Trevor Diemer Mathew Dorfman Steven Kass Theophilus Malone Chris Prescott Gregory Savage Wendy Sletten Maggie Skenderian Ali Young Supporting Organizations and Consultants Oregon Watershed Enhancement Board Salmon River Engineering ‐ Janet Corsale, PE CPESC Portland State University ‐ Denisse Fisher Contents Introduction .........................................................................................................................1 Johnson Creek Overview ...................................................................................................1 Project Effectiveness Monitoring Program....................................................................12 Overview ........................................................................................................................12 Monitoring Methods.....................................................................................................13 -
Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota Dylan Babiracki
University of North Dakota UND Scholarly Commons Undergraduate Theses and Senior Projects Theses, Dissertations, and Senior Projects 2015 Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota Dylan Babiracki Follow this and additional works at: https://commons.und.edu/senior-projects Recommended Citation Babiracki, Dylan, "Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota" (2015). Undergraduate Theses and Senior Projects. 114. https://commons.und.edu/senior-projects/114 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Undergraduate Theses and Senior Projects by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. | 1 Lateral migration of the Red River, in the vicinity of Grand Forks, North Dakota Dylan Babiracki Harold Hamm School of Geology and Geologic Engineering, University of North Dakota, 81 Cornell St., Grand Forks, ND 58202-8358 1. Abstract River channels are dynamic landforms that play an important role in understanding the alluvial changes occurring within this area. The evolution of the Red River of the North within the shallow alluvial valley was investigated within a 60 river mile area north and south of Grand Forks, North Dakota. Despite considerable research along the Red River of the North, near St. Jean Baptiste, Manitoba, little is known about the historical channel dynamics within the defined study area. A series of 31 measurements were taken using three separate methods to document the path of lateral channel migration along areas of this highly sinuous, low- gradient river. -
Root River Watershed Monitoring and Assessment Report
z c Root River Watershed Monitoring and Assessment Report June 2012 Acknowledgements MPCA Watershed Report Development Team: Michael Koschak, Mike Walerak, Pam Anderson, Dan Helwig, Bruce Monson, Dave Christopherson, David Duffey, Andrew Streitz Contributors: Citizen Stream Monitoring Program Volunteers Minnesota Department of Natural Resources Minnesota Department of Health Minnesota Department of Agriculture Fillmore County Soil and Water Conservation District The MPCA is reducing printing and mailing costs by using the Internet to distribute reports and information to a wider audience. Visit our Website for more information. MPCA reports are printed on 100% post-consumer recycled content paper manufactured without chlorine or chlorine derivatives. Project dollars provided by the Clean Water Fund (from the Clean Water, Land and Legacy Amendment). Minnesota Pollution Control Agency 520 Lafayette Road North | Saint Paul, MN 55155-4194 | www.pca.state.mn.us | 651-296-6300 Toll free 800-657-3864 | TTY 651-282-5332 This report is available in alternative formats upon request, and online at www.pca.state.mn.us Document number: wq-ws3-070400086 Contents Executive Summary ................................................................................................................. 1 I. Introduction ....................................................................................................................... 2 II. The Watershed Monitoring Approach ................................................................................ 3 -
2020 Root River Soil and Water Conservation District Annual Report
2020 Root River Soil and Water Conservation District Annual Report Larry Ledebuhr Family 1 TABLE OF CONTENTS INTRODUCTION..……….……….……………………………………………………………………………………………………..3 MISSION STATEMENT.….................................................................................................................3 ORGANIZATIONAL BOUNDARIES.…….………………………………………………………………………………………...4 COUNTY LAND DESCRIPTION……………………………………………………………………………………………………..4 ORGANIZATIONAL HISTORY.………………………………………………………………………………………………………6 SWCD & NRCS STAFF 2020.……………………………………......................................................................7 ROOT RIVER SOIL & WATER CONSERVATION DISTRICT SUPERVISORS.…….…………………………….…..8 SUPERVISORS NOMINATION DISTRICT ….……………………………………………………………………………….….9 DISTRICT ACCOMPLISHMENTS.………………………………………………………………………………………………..10 EDUCATIONAL OUTREACH……………………………………………………………………………………………………….24 MEETINGS…………………………………….…………………………………………………………………………………….……24 STAFF DEVELOPMENT…….……………………….……………………………………………………………………………….25 PARTNERSHIPS………….…….……………………………………………………………………………………………………….26 2 INTRODUCTION This annual report is to assist and present an overview of the accomplishments and activities of the Root River Soil and Water Conservation District in a manner consistent to the District’s policies and long-range goals. MISSION STATEMENT The Root River Soil and Water Conservation District’s mission is to provide assistance to cooperators in managing the natural resources on their land. In addition, the district will continue to educate people on local conservation -
Southeastern Minnesota Floods from Record Rains, August 2007
Floods from Record Rains in Illinois, Iowa, Minnesota, and Wisconsin, August 17−30, 2007 1 2 3 4 By J.D. Fallon , H.S. Garn , M.L. Harris , and K.D. Lund 1USGS Minnesota Water Science Center, 2 USGS Wisconsin Water Science Center, 3 USGS Illinois Water Science Center, 4 USGS Iowa Water Science Center INTENSE PRECIPITATION USGS MONITORING FLOOD STATISTICS FLOOD AFFECTS Provisional summary of peak stages and discharges at selected streamflow-gaging stations in the upper Midwest Flood of August 2007 Previous maximum discharge Approximate Peak recurrrence Peak Station Drainage area Peak discharge Date interval Peak stage discharge Years of State number Station name (mi2) stage (ft) (ft3/s) (2007) (years) (ft) (ft3/s) Date record Illinois 05439000 S. Br. Kishwaukee River at Dekalb, IL 77.7 15.34 3,100 Aug. 24 100 15.80 3,500 July 1983 28 Illinois 05440700 Rock River at Byron, IL 7990 15.50 32,100 Aug. 25 nd 16.12 35,400 June 2000 7 Illinois 05529000 Des Plaines river near Des Plaines, IL 360 8.62 3,800 Aug. 24 10 10.88 4,900 Oct. 1986 67 Illinois 05530990 Salt Creek at Rolling Meadows, IL 30.5 10.57 1,350 Aug. 23 10 - 25 14.03 1,650 Aug 1987 34 Illinois 05536000 North Branch Chicago River at Niles, IL 100 9.61 1,800 Aug. 24 10 11.35 2,590 Aug. 1987 57 2 Illinois 05536235 Deer Creek near Chicago Heights, IL 23.1 12.37 1,320 Aug. 24 100 12.15 1,380 July 1957 59 1 2 Illinois 05539900 W. -
Ink Bayou Prospectus
Prospectus for the ARDOT Ink Bayou Mitigation Bank Pulaski County, Arkansas Arkansas Department of Transportation January 2019 The Arkansas Department of Transportation (ARDOT) proposes the establishment of a wetland mitigation bank in Pulaski County, Arkansas. The mitigation area is located just west of Interstate 440, southeast of Highway 161 and north of Interstate 40 near McAlmont, Arkansas (Figure 1). ARDOT’s Rixey Bayou Mitigation Area is located approximately 0.7 mile north of the proposed bank site. This 436.86-acre site includes portions of sections 14, 15, and 16, Township 2 North, Range 11 West (Figure 2). The property was purchased by ARDOT expressly to mitigate wetland impacts resulting from highway construction and maintenance activities. The property would be used for compensatory mitigation for unavoidable impacts resulting from ARDOT highway activities authorized under Section 404 of the Clean Water Act. A. Management Goal and Objectives: The management goal for the mitigation bank is the restoration, enhancement, and preservation of wetlands and associated uplands. Objectives include the preservation of existing forested wetlands and the enhancement of existing wetlands through reforestation of agricultural land with bottomland hardwood tree species. The past, associated agricultural practices will be removed from the property. There is a total of 269.99 acres of wetlands on the proposed mitigation bank site. There is a 0.6-acre permittee responsible mitigation area that is not included as part of the mitigation bank acreage. Eligible acreage includes: 137.01 acres of wetland preservation, and 132.38 acres of wetland enhancement that will be reforested with bottomland hardwood trees (Figure 3). -
Multi-Millennial Record of Erosion and Fires in the Southern Blue Ridge Mountains, USA
Chapter 8 Multi-millennial Record of Erosion and Fires in the Southern Blue Ridge Mountains, USA David S. Leigh Abstract Bottomland sediments from the southern Blue Ridge Mountains provide a coarse-resolution, multi-millennial stratigraphic record of past regional forest disturbance (soil erosion). This record is represented by 12 separate vertical accre- tion stratigraphic profi les that have been dated by radiocarbon, luminescence, cesium-137, and correlation methods continuously spanning the past 3,000 years of pre-settlement (pre-dating widespread European American settlement) and post- settlement strata. Post-settlement vertical accretion began in the late 1800s, appears to be about an order of magnitude faster than pre-settlement rates, and is attribut- able to widespread deforestation for timber harvest, farming, housing develop- ment, and other erosive activities of people. Natural, climate-driven, or non-anthropic forest disturbance is subtle and diffi cult to recognize in pre-settle- ment deposits. There is no indication that pre-settlement Mississippian and Cherokee agricultural activities accelerated erosion and sedimentation in the region. A continuous 11,244 years before present (BP) vertical accretion record from a meander scar in the Upper Little Tennessee River valley indicates abundant charcoal (prevalent fi res) at the very beginning of the Holocene (11,244–10,900 years BP). In contrast, moderate to very low levels of charcoal are apparent over the remaining Holocene until about 2,400 years BP when charcoal infl ux registers a pronounced increase. These data are consistent with the idea that Native Americans used fi re extensively to manage forests and to expanded agricultural activities during Woodland and later cultural periods over the past 3000 years. -
Conservation Planning in the Mississippi River Alluvial Plain
Conservation Planning in the Mississippi River Alluvial Plain Photo courtesy of Nancy Webb The Nature Conservancy 2002 Conservation Planning in the Mississippi River Alluvial Plain (Ecoregion 42) The Nature Conservancy May, 2002 For questions or comments on this document contact The Nature Conservancy at P.O. Box 4125, Baton Rouge, LA, 70821. (225) 338-1040 ii Preface The information presented herein is the result of four years of conservation planning and represents two iterations of the Mississippi River Alluvial Plain (MSRAP) ecoregional plan as developed by The Nature Conservancy (TNC) and many partners. The bulk of the text describes the process the MSRAP team undertook to: • identify important biological species, communities, and ecological systems, commonly referred to as “conservation targets,” existing in the ecoregion; and • select priority sites, or conservation areas, for biodiversity conservation based on the perceived viability of those targets. It should be noted that a considerable amount of time was spent developing data as few Heritage data, the common building blocks of TNC’s ecoregional plans, were available for the ecoregion. Much of the emphasis on data collection was focused on terrestrial targets. The dearth of aquatics data required that the team rely heavily on the use of coarse filter, abiotic information to identify aquatic systems warranting further investigation. To help fill the gap in aquatics data and better inform MSRAP conservation planning, the Charles Stewart Mott Foundation provided funding to TNC’s Southeast Conservation Science Center and Freshwater Initiative to assess freshwater biodiversity in several southeast ecoregions including the Mississippi Embayment Basin (MEB), of which MSRAP is a part.