SPRING RIVER WATERSHED INVENTORY and ASSESSMENT This Information Is Based on the Spring River Watershed Inventory and Assessment Prepared by Lisa K
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Spring 2021 | Issue No
SPRING 2021 | ISSUE NO. 31 THE CANAL QUARTERLYwww.CanalTrust.org CANAL STEWARDS PROVIDE VITAL SERVICE One of the largest contributions the C&O Stewards perform many types of light Canal Trust makes to the C&O Canal National maintenance tasks, including lopping and Historical Park is the volunteer support pruning, painting, picking up trash, removing we marshal and manage. As the Park's vegetation, raking, and restocking maps and official nonprofit partner, we are focused on trash-free park bags. It's the perfect way for providing volunteer efforts to aid National an individual, couple, or small group to get Park Service (NPS) staff in maintenance and fresh air, exercise, and care for the Park, all beautification projects along the towpath. while social distancing. Every garden mulched and invasive plant pulled by a volunteer is one less chore for an Stewards are able to set their own schedules NPS maintenance worker, freeing him or her in cooperation with the Trust's Canal up for higher-level responsibilities. Stewards Coordinator Becka Lee. Volunteers are required to go through an orientation In late 2020, the Trust added a new volunteer program prior to beginning work at their program to our arsenal, the Canal Stewards site. If you choose to become a Steward, program, which we assumed management you will join the hundreds of dedicated of from NPS staff. Canal Stewards "adopt" volunteers who work to keep the Park clean a section of the canal and maintain it for and safe for its nearly 5 million visitors. For a designated time period. Parking lots, more information, visit www.canaltrust. -
Flood Pulse Effects on Benthic Invertebrate Assemblages in the Hypolacustric Interstitial Zone of Lake Constance
Ann. Limnol. - Int. J. Lim. 48 (2012) 267–277 Available online at: Ó EDP Sciences, 2012 www.limnology-journal.org DOI: 10.1051/limn/2012008 Flood pulse effects on benthic invertebrate assemblages in the hypolacustric interstitial zone of Lake Constance Shannon J. O’Leary1 and Karl M. Wantzen2* 1 School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY 11733, USA 2 CNRS UMR 6371 CITERES/IPAPE, De´partement des Sciences, Universite´Franc¸ois Rabelais, Parc Grandmont, 37200 Tours, France Abstract – In contrast to rivers, the effects of water level fluctuations on the biota are severely understudied in lakes. Lake Constance has a naturally pulsing hydrograph with average amplitudes of 1.4 m between winter drought and summer flood seasons (annual flood pulse (AFP)). Additionally, heavy rainstorms in summer have the potential to create short-term summer flood pulses (SFP). The flood pulse concept for lakes predicts that littoral organisms should be adapted to the regularly occurring AFP, i.e. taking advantage of benefits such as an influx of food sources and low predator pressure, though these organisms will not possess adapta- tions for the SFP. To test this hypothesis, we studied the aquatic invertebrate assemblages colonizing the gravel sediments of Lake Constance, the AFP in spring and a dramatic SFP event consisting of a one meter rise of water level in 24 h. Here, we introduce the term ‘hypolacustric interstitial’ for lakes analog to the hyporheic zone of running water ecosystems. Our results confirm the hypothesis of contrasting effects of a regular AFP and a random SFP indicating that the AFP enhances the productivity and biodiversity of the littoral zone with benthic invertebrates displaying an array of adaptations enabling them to survive. -
Springs of California
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIBECTOB WATER- SUPPLY PAPER 338 SPRINGS OF CALIFORNIA BY GEKALD A. WARING WASHINGTON GOVERNMENT PRINTING OFFICE 1915 CONTENTS. Page. lntroduction by W. C. Mendenhall ... .. ................................... 5 Physical features of California ...... ....... .. .. ... .. ....... .............. 7 Natural divisions ................... ... .. ........................... 7 Coast Ranges ..................................... ....•.......... _._._ 7 11 ~~:~~::!:: :~~e:_-_-_·.-.·.·: ~::::::::::::::::::::::::::::::::::: ::::: ::: 12 Sierra Nevada .................... .................................... 12 Southeastern desert ......................... ............. .. ..... ... 13 Faults ..... ....... ... ................ ·.. : ..... ................ ..... 14 Natural waters ................................ _.......................... 15 Use of terms "mineral water" and ''pure water" ............... : .·...... 15 ,,uneral analysis of water ................................ .. ... ........ 15 Source and amount of substances in water ................. ............. 17 Degree of concentration of natural waters ........................ ..· .... 21 Properties of mineral waters . ................... ...... _. _.. .. _... _....• 22 Temperature of natural waters ... : ....................... _.. _..... .... : . 24 Classification of mineral waters ............ .......... .. .. _. .. _......... _ 25 Therapeutic value of waters .................................... ... ... 26 Analyses -
Immigrants I Through K
I Iager, John, Switzerland, came to the county in 1865, in Newton County 1882 Atlas, patrons, from Missouri Pioneers Volume XVI Iberg, Jacob, Switzerland, 81, in the 1900 Federal Census of Newton CO, MO, Neosho Township Iburg, Herman C., Germany, 54, in the 1910 Federal Census of St. Clair CO, MO, Jackson Township. Also, Herman C. Iburg, Oenhousen [Oeynhausen ?], Germany, born February 23, 1855 [MO death certificate] died October 3, 1910, in St. Clair County, father John Iburg, mother Christina Daniels, informant Mrs. Herman C. Iburg Ihde, William, Petersdorf Cris Templen, Germany, from a 1915 petition for naturalization, McDonald County, Missouri, from Missouri Pioneers Volume XXVIII. Also, William Ihde, Germany, 59, in the 1920 Federal Census of McDonald CO, MO, Cyclone Ikenruth, Adam, Germany, 52, in the 1910 Federal Census of Cedar CO, MO, Linn Township Iker, Joseph, Baden, Germany, 37, in the 1870 Federal Census of Hickory CO, MO, Montgomery Township Iles, Thomas, England, 60, in the 1910 Federal Census of Dade CO, MO, Grant Township. [On son William Carl Iles’ MO death certificate from Dade County father is listed as Thomas Iles born in England and mother Ellen Perr__man[?] ] Imme, Adolph, Germany, 55, in the 1900 Federal Census of Jasper CO, MO, Webb City Immel, John, Germany, born January 28, 1834 [MO death certificate] died August 24, 1917, in Joplin, Jasper County. And, 68, in the 1900 Federal Census of Jasper CO, MO, Joplin Immel, Mrs. Katherine, Germany, born October 7, 1849 [MO death certificate] died June 1, 1933, in Joplin, Jasper County, father Christian Miller, mother Marie Hoffman, husband [deceased] John Immel Inch, Jack, England, 32, born May, 1868, in the 1900 Federal Census of Lawrence CO, MO, Vineyard Township Indermuehle, Gottlieb, Canton Bern, Switzerland, born March 14, 1830 [MO death certificate] died March 4, 1912, in Laclede County, father Christain Indermuehle, informant J. -
Mineral Springs Walking Tour
The Springs Early advertisement for Steamboat’s springs of Steamboat Springs An elk takes a swim in the Heart Spring pool YOUR EXploration OF THE SPRINGS DISCOVER Steamboat’S SPRINGS: can be tailored to your own curiosity level. By starting IRON SPRING at Iron Spring you are within easy walking distance (about one mile) of five mineral springs. For the more SODA SPRING adventuresome—extend your tour with a hike to SULPHUR SPRING the Sulphur Cave or take a plunge in the “soothing SWEETWATER/LAKE SPRING and health-giving” waters of the Old Town Hot Springs. STEAMBOAT SPRING NARCISSUS/TERRACE SPRING Journey in the footsteps of the Yampatika Ute and BLACK SULPHUR SPRING Arapaho tribes and the early pioneers of Steamboat LITHIA SPRING Springs as you discover the city’s mineral springs. No two springs are alike—and each has its own SULPHUR CAVE special mineral content and intriguing allure. HEART SPRING at THE OLD TOWN HOT SPRINGS Use this map for guidance, as the new trail differs from the Please be advised that the waters in these springs are natural one on the blue signs located at each spring. Suitable walking flowing and untreated. Drinking from the springs may cause shoes are advised since parts of the trail are rough and steep. illness or discomfort. After touring the springs, see if you know which is the: For more information about the springs in Steamboat Springs please visit or call: • Hottest spring? • Tread of Pioneers Museum ~ 8th and Oak 970.879.2214 • Lemonade spring? • City of Steamboat Springs ~ 137 10th Street 970.879.2060 • Most odiferous spring? • Bud Werner Memorial Library ~ 12th and Lincoln 970.879.0240 • Yampatika ~ 925 Weiss Drive 970.871.9151 • Most palatable? This document is supported in part by a Preserve America grant administered by • Miraquelle spring? the National Park Service, Department of the Interior. -
Capitol Reef U.S
National Park Service Capitol Reef U.S. Department of the Interior Capitol Reef National Park Spring Canyon Spring Canyon is deep and narrow with towering Wingate cliffs and Navajo domes. It originates on the shoulder of Thousand Lakes Mountain and extends to the Fremont River. The route is marked with rock cairns and signs in some places, but many sections are unmarked and car- rying a topographic map and GPS unit is recommended. It is extremely hot in summer, and the only usually reliable water source is at the spring in Upper Spring Canyon, 1.5 miles (2.41 km) west of the junction with Chimney Rock Canyon. Use caution in narrow canyons particular- ly during the flash flood season (typically July–September). The canyon route is divided into Upper and Lower Spring Canyon sections. It can be accessed midway via Chimney Rock Canyon. The entire canyon is best done as a three- to four-day trip. Upper Spring Canyon is a good two- to three- day trip, while Lower Spring Canyon can be done as an overnight or long day hike. Backcountry permits are required for all overnight trips and can be obtained at the visitor center. Location of Trailheads 1. Upper end of Spring Canyon: Holt Draw, which is a dirt track on the right (north) side of Hwy 24, 0.9 miles (1.44 km) west of the park boundary and 7.2 miles (11.59 km) west of the visitor center. The road is closed to vehicle traf- fic beyond the gate at the forest service boundary near Hwy 24. -
The Legendary Lore of the Holy Wells of England
'? '/-'#'•'/ ' ^7 f CX*->C5CS- '^ OF CP^ 59§70^ l-SSi"-.". -,, 3 ,.. -SJi f, THE LEGENDARY LORE OF THE HOL Y WELLS OF ENGLAND. : THE LEGENDARY LORE ' t\Q OF THE ~ 1 T\ I Holy Wells of England: INCLUDING IRfpers, Xaftes, ^fountains, ant) Springs. COPIOUSLY ILLUSTRATED BY CURIOUS ORIGINAL WOODCUTS. ROBERT CHARLES HOPE, F.S.A., F.R.S.L., PETERHOUSE, CAMBRIDGE; LINCOLN'S INN; MEMBER,OF THE COUNCIL OF THE EAST RIDING OF YORKSHIRE ANTIQUARIAN SOCIETY, AUTHOR OF "a GLOSSARY OF DIALECTAL PLACE-NOMENCLATURE," " AN INVENTORY OF THE CHURCH PLATE IN RUTLAND," "ENGLISH GOLDSMITHS," " THE LEPER IN ENGLAND AND ENGLISH LAZAR-HOUSES ;" EDITOR OF BARNABE GOOGE'S " POPISH KINGDOME." LONDON ELLIOT STOCK, 62, PATERNOSTER ROW, E.C. 1893. PREFACE, THIS collection of traditionary lore connected with the Holy Wells, Rivers, Springs, and Lakes of England is the first systematic attempt made. It has been said there is no book in any language which treats of Holy Wells, except in a most fragmentary and discursive manner. It is hoped, therefore, that this may prove the foundation of an exhaustive work, at some future date, by a more competent hand. The subject is almost inexhaustible, and, at the same time, a most interesting one. There is probably no superstition of bygone days that has held the minds of men more tenaciously than that of well-worship in its broadest sense, "a worship simple and more dignified than a senseless crouching before idols." An honest endeavour has been made to render the work as accurate as possible, and to give the source of each account, where such could be ascertained. -
Short Creek and Shoal Creek in the Spring River Watershed Water Quality Impairment: Total Phosphorus
NEOSHO BASIN TOTAL MAXIMUM DAILY LOAD Waterbody / Assessment Unit: Short Creek and Shoal Creek in the Spring River Watershed Water Quality Impairment: Total Phosphorus 1.0 INTRODUCTION AND PROBLEM IDENTIFICATION Subbasin: Spring Counties: Cherokee HUC8: 11070207 HUC10(12): 08(06) & 09(04) Ecoregion: Ozark Highlands, Springfield Plateau (39a) Drainage Area: Shoal Creek = approximately 10.1 square miles in Kansas Short Creek = approximately 5.94 square miles in Kansas Water Quality Limited Segments Covered Under this TMDL: Station Main Stem Segment Tributary Station SC570 Short Creek (881) Station SC212 Shoal Creek (2) Unnamed Stream (886) 2008, 2010, 2012 & 2014 303(d) Listings: Kansas Stream segments monitored by stations SC212 on Short Creek and SC570 on Shoal Creek, are cited as impaired by Total Phosphorus (TP) for the Neosho Basin. Impaired Use: Special Aquatic Life, Expected Aquatic Life, Contact Recreation and Domestic Water Supply. Water Quality Criteria: Nutrients – Narratives: The introduction of plant nutrient into surface waters designated for domestic water supply use shall be controlled to prevent interference with the production of drinking water (K.A.R. 28-16-28e(c)(3)(D)). The introduction of plant nutrients into streams, lakes, or wetlands from artificial sources shall be controlled to prevent the accelerated succession or replacement of aquatic biota or the production of undesirable quantities or kinds of aquatic life (K.A.R. 28-16- 28e(c)(2)(A)). The introduction of plant nutrients into surface waters designated for primary or secondary contact recreational use shall be controlled to prevent the development of objectionable concentrations of algae or algal by-products or nuisance growths of submersed, floating, or emergent aquatic vegetation (K.A.R. -
Impacts of a Flood Pulsing Hydrology on Plants and Invertebrates in Riparian Wetlands
IMPACTS OF A FLOOD PULSING HYDROLOGY ON PLANTS AND INVERTEBRATES IN RIPARIAN WETLANDS A dissertation submitted to Kent State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy by Maureen K. Drinkard August 2012 Dissertation written by Maureen K. Drinkard B.S., Kent State University, 2003 Ph.D., Kent State University, 2012 Approved by ___Ferenc de Szalay_, Chair, Doctoral Dissertation Committee ___Mark Kershner_______, Members, Doctoral Dissertation Committee _____Oscar Rocha________, ____Mandy Munro-Stasiuk_, Accepted by _____James Blank______, Chair, Department of Biological Sciences ______Raymond Craig___, Dean, College of Arts and Sciences ii TABLE OF CONTENTS LIST OF FIGURES ............................................................................................................... vi LIST OF TABLES ................................................................................................................. vii ACKNOWLEDGEMENTS .................................................................................................... x CHAPTER I. INTRODUCTION ................................................................................................ 1 Dissertation Goals ............................................................................................. 1 Definition of the Flood Pulse Concept .............................................................. 2 Ecological and economic importance ............................................................... 3 Impacts of environmental -
Prevent Soil Erosion on Your Property
How to Use Sandbags Filling Filling sandbags is best done with two people. Fill half full with sand if available or local soil. ������������ ���������� Stacking PREVENT SOIL EROSION Fold top of sandbag down and rest the bag on its top on the stack. Top should be facing upstream. Stamp the bag into place. Complete each layer before starting the next layer. Stagger the layers. Stack no more than three layers high unless they are ON YOUR ROPERTY against a building or stacked pyramid-style. P Sandbag diversion HOMEOWNER S GUIDE TO EROSION CONTROL ��������������� ������������� Sandbags will redirect water away from property but will not A ' �������������� ������������ seal out water. Place sandbags with the folded top toward the upstream or uphill direction. Sandbags are temporary and will deteriorate after several months. DO’S AND DON’TS Do: Don’t: • Contact your local Flood Control Agency or Public Works • Under-estimate the power of debris flows. Authority- Installing these erosion control devices on your property may not be sufficient to thwart extreme flows. • Walk or drive across swiftly flowing water. • Try to direct debris flows away from your property to a • Wait until storms arrive to make a plan. recognized drainage device or to the street. • Try to confine the flows more than is necessary. • Clear a path for debris. • Direct flow to neighbor’s property. • Place protective measures to divert debris, not dam it. • Board up windows facing the flow • Work with your neighbors. Don’t Forget to Plan for Erosion Control ALL YEAR ROUND In an effort to help landowners protect their Preventing runoff during the spring and summer is equally as Soil erosion can happen property, professional NRCS Conservationists important as preventing erosion. -
5.1 Coarse Bed Load Sampling
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1997 The initiation of coarse bed load transport in gravel bed streams Andrew C. Whitaker The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Whitaker, Andrew C., "The initiation of coarse bed load transport in gravel bed streams" (1997). Graduate Student Theses, Dissertations, & Professional Papers. 10498. https://scholarworks.umt.edu/etd/10498 This Dissertation is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter free, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. -
Spring River
NEOSHO RIVER BASIN TOTAL MAXIMUM DAILY LOAD Water Body/Assessment Unit: Spring River Watershed, including Shoal Creek, Short Creek, Shawnee Creek, Turkey Creek and Center Creek Water Quality Impairment: Metals (Lead, Zinc, Copper & Cadmium) 1. INTRODUCTION AND PROBLEM IDENTIFICATION Subbasin: Spring County: Cherokee HUC 8: 11070207 Ecoregion: Ozark Highlands; Springfield Plateau (39a) Drainage Area: Approximately 2830 square miles from Oklahoma Stateline, of which about 520 square miles lie in Kansas and balance is in Missouri. Drainage between Baxter Springs and Crestline is about 1100 square miles. Water Quality Limited Segments on Spring River: 1, 3, 4, 19 Water Quality Limited Segments on Tributaries: 2, 881, 17, 22, 18, 23 Watershed Hierarchy of Main Stem and Tributary Segments Monitored by KDHE Stations (Figure 1) HUC 8 11070207 – Spring River Watershed: Spring River at Baxter Springs Station 213 Spring River (1) Willow Creek (20) Brush Creek (23) Station 212 Shoal Creek (2) Unnamed Trib (886) Spring River (3) Station 569 Shawnee Creek (17) Little Shawnee Creek (22) Station 570 Short Creek (881) Spring River (4) Station 211 Turkey Creek (18) Spring River (19) Station 210 Center Creek Station 568 Spring River nr Crestline (6) 1 Designated Uses of Impaired Streams: Spring River Exceptional State Water, Special Aquatic Life Support, Primary C Recreation, Domestic Water Supply, Food Procurement; Groundwater Recharge, Industrial Water Supply, Irrigation; Livestock Watering. Shoal Creek same; Turkey Creek same, except General Purpose Water instead of Exceptional State Water Expected Aquatic Life Support, Secondary b Recreation & Food Procurement on Shawnee Creek, Little Shawnee Creek, Willow Creek & Brush Creek and Short Creek same, except no Food Procurement 1998 & 2002 303(d) Listings: Neosho River Basin Streams and Biological Impairment Impaired Use: Chronic and Acute Aquatic Life Support Water Quality Standard: Agricultural water supply use.