No More Floods! Build the Missouri River Development Project by Anthony Defranco
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Flooding the Missouri Valley the Politics of Dam Site Selection and Design
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Great Plains Quarterly Great Plains Studies, Center for Summer 1997 Flooding The Missouri Valley The Politics Of Dam Site Selection And Design Robert Kelley Schneiders Texas Tech University Follow this and additional works at: https://digitalcommons.unl.edu/greatplainsquarterly Part of the Other International and Area Studies Commons Schneiders, Robert Kelley, "Flooding The Missouri Valley The Politics Of Dam Site Selection And Design" (1997). Great Plains Quarterly. 1954. https://digitalcommons.unl.edu/greatplainsquarterly/1954 This Article is brought to you for free and open access by the Great Plains Studies, Center for at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Great Plains Quarterly by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. FLOODING THE MISSOURI VALLEY THE POLITICS OF DAM SITE SELECTION AND DESIGN ROBERT KELLEY SCHNEIDERS In December 1944 the United States Con Dakota is 160 feet high and 10,700 feet long. gress passed a Rivers and Harbors Bill that The reservoir behind it stretches 140 miles authorized the construction of the Pick-Sloan north-northwest along the Missouri Valley. plan for Missouri River development. From Oahe Dam, near Pierre, South Dakota, sur 1946 to 1966, the United States Army Corps passes even Fort Randall Dam at 242 feet high of Engineers, with the assistance of private and 9300 feet long.! Oahe's reservoir stretches contractors, implemented much of that plan 250 miles upstream. The completion of Gar in the Missouri River Valley. In that twenty rison Dam in North Dakota, and Oahe, Big year period, five of the world's largest earthen Bend, Fort Randall, and Gavin's Point dams dams were built across the main-stem of the in South Dakota resulted in the innundation Missouri River in North and South Dakota. -
Missouri River Floodplain from River Mile (RM) 670 South of Decatur, Nebraska to RM 0 at St
Hydrogeomorphic Evaluation of Ecosystem Restoration Options For The Missouri River Floodplain From River Mile (RM) 670 South of Decatur, Nebraska to RM 0 at St. Louis, Missouri Prepared For: U. S. Fish and Wildlife Service Region 3 Minneapolis, Minnesota Greenbrier Wetland Services Report 15-02 Mickey E. Heitmeyer Joseph L. Bartletti Josh D. Eash December 2015 HYDROGEOMORPHIC EVALUATION OF ECOSYSTEM RESTORATION OPTIONS FOR THE MISSOURI RIVER FLOODPLAIN FROM RIVER MILE (RM) 670 SOUTH OF DECATUR, NEBRASKA TO RM 0 AT ST. LOUIS, MISSOURI Prepared For: U. S. Fish and Wildlife Service Region 3 Refuges and Wildlife Minneapolis, Minnesota By: Mickey E. Heitmeyer Greenbrier Wetland Services Advance, MO 63730 Joseph L. Bartletti Prairie Engineers of Illinois, P.C. Springfield, IL 62703 And Josh D. Eash U.S. Fish and Wildlife Service, Region 3 Water Resources Branch Bloomington, MN 55437 Greenbrier Wetland Services Report No. 15-02 December 2015 Mickey E. Heitmeyer, PhD Greenbrier Wetland Services Route 2, Box 2735 Advance, MO 63730 www.GreenbrierWetland.com Publication No. 15-02 Suggested citation: Heitmeyer, M. E., J. L. Bartletti, and J. D. Eash. 2015. Hydrogeomorphic evaluation of ecosystem restoration options for the Missouri River Flood- plain from River Mile (RM) 670 south of Decatur, Nebraska to RM 0 at St. Louis, Missouri. Prepared for U. S. Fish and Wildlife Service Region 3, Min- neapolis, MN. Greenbrier Wetland Services Report 15-02, Blue Heron Conservation Design and Print- ing LLC, Bloomfield, MO. Photo credits: USACE; http://statehistoricalsocietyofmissouri.org/; Karen Kyle; USFWS http://digitalmedia.fws.gov/cdm/; Cary Aloia This publication printed on recycled paper by ii Contents EXECUTIVE SUMMARY .................................................................................... -
Missouri River Valley in North Eastern Nebraska
Water-Supply Paper No. 2 15 f A, Economic Geology, 96 n I B, Descriptive Geology, 118 owm] M, General Hydrographic Investigations, 25 [ 0, Underground Waters, 71 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR GEOLOGY AND WATER RESOURCES OF A PORTION OF THE MISSOURI RIVER VALLEY IN NORTH EASTERN NEBRASKA BY GK E. WASHINGTON GOVERNMENT PRINTING OFFICE 1908 CONTENTS. Page. Introduction___________________ Topography ___________________ Descriptive geology _____ Stratigraphy ____________ Structure__________________ Description of the rocks____ Cretaceous system ___ Dakota sandstone __ Benton group______ 10 Graueros shale_ 11 Greenhorn limestone 11 Carlile shale_ 12 Niobrara formation 13 Pierre shale_______ 15 Tertiary system________ 18 Arikaree formation- 18 Pliocene deposits_ 19 Quaternary system_____ 20 Glacial drift_______ 20 Loess ________. 20 Alluvium______. 21 Dune sand_________ 22 Economic geology______________ 22 Mineral resources__________ 22 Brick clay ____________ 22 Sand and gravel_______ 22 Building stone_________ 22 Cement rock________ 23 Coal ____________. 2-i Peat __________________ 2-1 Volcanic ash___________ 24 Water resources- __________ 25 General statement _____ 25 Surface waters ________ 25 Streams___________ 25 Springs _______. 20 Underground waters _ 27 Shallow wells _____ 27 Artesian wells_____ 28 Artesian conditions ___________________ 28. Chemical composition of artesian water- 28 Pressure _______________ _ 29 Temperature of artesian water________ 30 Construction and care of -
Bighorn River Basin, Wyoming
Environmental and Recreational Water Use Analysis for the Wind – Bighorn River Basin, Wyoming Wind – Bighorn River Basin Plan Update Prepared for: Wyoming Water Development Commission 6920 Yellowstone Rd Cheyenne, Wyoming 82009 Prepared by: Western EcoSystems Technology, Inc. 415 W. 17th St., Suite 200 Cheyenne, Wyoming 82001 September 7, 2017 Draft Pre-Decisional Document - Privileged and Confidential - Not For Distribution Wind – Bighorn River Basin Plan Update EXECUTIVE SUMMARY In 2010, the Wyoming Water Development Commission (WWDC) requested a study to develop more robust and consistent methods for defining environmental and recreational (E&R) water uses for the River Basin Planning program. The study outlined that recreational and environmental uses needed to be identified and mapped, in a way that would assess their interactions with traditional water uses throughout the state of Wyoming. Harvey Economics completed the study in 2012, with a report and handbook being produced to identify a consistent viewpoint and accounting process for E&R water demands and to help guide river basin planning efforts in moving forward. The methods developed in the handbook were implemented on the Wind-Bighorn River Basin (Basin), and the results of the Basin plan update are provided in this report. In addition to the handbook guidelines, Western Ecosystems Technology, Inc. coordinated with the WWDC to further the analysis through the development of three models: 1) protection, 2) environmental, and 3) recreation. The Basin is located in central and northwestern Wyoming. Approximately 80% of Yellowstone National Park (YNP) is included in the Basin. Elevations in the Basin are variable as the Wind River and Bighorn Mountains funnel water from alpine areas to lower river corridors. -
Earth Sciences: Two-Ice-Lobe Model for Kansan Glaciation James S
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Transactions of the Nebraska Academy of Sciences Nebraska Academy of Sciences and Affiliated Societies 1982 Earth Sciences: Two-Ice-Lobe Model For Kansan Glaciation James S. Aber Emporia State University Follow this and additional works at: http://digitalcommons.unl.edu/tnas Aber, James S., "Earth Sciences: Two-Ice-Lobe Model For Kansan Glaciation" (1982). Transactions of the Nebraska Academy of Sciences and Affiliated Societies. 490. http://digitalcommons.unl.edu/tnas/490 This Article is brought to you for free and open access by the Nebraska Academy of Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Transactions of the Nebraska Academy of Sciences and Affiliated Societies by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1982. Transactions a/the Nebraska Academy a/Sciences, X:25-29. EARTH SCIENCES TWO-ICE-LOBE MODEL FOR KANSAN GLACIATION James S. Aber Geoscience Department Emporia State University Emporia, Kansas 66801 The Kansan glaciation should be representative of Early Pleisto western source area, the so-called Keewatin Center, in the cene glaciations in the Kansas-Nebraska-Iowa-Missouri region. It is region west of Hudson Bay. Frye and Leonard (1952: 11) often assumed the Kansan ice-sheet advanced as a single, broad lobe supported this concept on the basis of distribution of the coming from somewhere in Canada. This simple view contrasts with the known complexities of the younger Wisconsin glaciation, and indeed Sioux Quartzite, a common erratic derived mainly from east there is much evidence that the Kansan glaciation was equally complex. -
Sauger Population Ecology in Three Missouri River Mainstem Reservoirs Brian D
South Dakota State University Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange Electronic Theses and Dissertations 2006 Sauger Population Ecology in Three Missouri River Mainstem Reservoirs Brian D. S. Graeb South Dakota State University Follow this and additional works at: https://openprairie.sdstate.edu/etd Part of the Natural Resources and Conservation Commons Recommended Citation Graeb, Brian D. S., "Sauger Population Ecology in Three Missouri River Mainstem Reservoirs" (2006). Electronic Theses and Dissertations. 438. https://openprairie.sdstate.edu/etd/438 This Dissertation - Open Access is brought to you for free and open access by Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange. For more information, please contact [email protected]. Sauger Population Ecology in Three Missouri River Mainstem Reservoirs By Brian D. S. Graeb A dissertation submitted in partial fulfillment of the requirements for the degree Doctor of Philosophy Major in Biological Sciences South Dakota State University 2006 11 Sauger Population Ecology in Three Missouri River Mainstem Reservoirs This dissertation is approved as a credible and independent investigation by a candidate for the Doctor of Philosophy degree and is acceptable for meeting the dissertation requirements for this degree. Acceptance of this dissertation does not imply that the conclusions reached by the candidate are necessarily the conclusions of the major department. David W. Willis Date Dissertation Advisor Charles G. Scalet Date Head, Department of Wildlife and Fisheries Sciences iii Acknowledgements I would like to especially thank my wife, Stephanie for her support and guidance in all aspects of my life during my long tenure as a graduate student, and my advisor, Dr. -
Boysen Reservoir and Powerplant
Upper Missouri River Basin Water Year 2015 Summary of Actual Operations Water Year 2016 Annual Operating Plans U.S. Department of Interior Bureau of Reclamation Great Plains Region TABLE OF CONTENTS SUMMARIES OF OPERATION FOR WATER YEAR 2015 FOR RESERVOIRS IN MONTANA, WYOMING, AND THE DAKOTAS INTRODUCTION RESERVOIRS UNDER THE RESPONSIBILITY OF THE MONTANA AREA OFFICE SUMMARY OF HYDROLOGIC CONDITIONS AND FLOOD CONTROL OPERATIONS DURING WY 2015 ........................................................................................................................ 1 FLOOD BENEFITS ...................................................................................................................... 13 UNIT OPERATIONAL SUMMARIES FOR WY 2015 .............................................................. 15 Clark Canyon Reservoir ............................................................................................................ 15 Canyon Ferry Lake and Powerplant .......................................................................................... 21 Helena Valley Reservoir ........................................................................................................... 32 Sun River Project ...................................................................................................................... 34 Gibson Reservoir ................................................................................................................... 34 Pishkun Reservoir ................................................................................................................ -
Missouri River
Missouri River Planning: Recognizing and Incorporating Sediment Management Committee on Missouri River Recovery and Associated Sediment Management Issues; National Research Council ISBN: 0-309-16204-1, 182 pages, 6 x 9, (2010) This free PDF was downloaded from: http://www.nap.edu/catalog/13019.html Visit the National Academies Press online, the authoritative source for all books from the National Academy of Sciences, the National Academy of Engineering, the Institute of Medicine, and the National Research Council: • Download hundreds of free books in PDF • Read thousands of books online, free • Sign up to be notified when new books are published • Purchase printed books • Purchase PDFs • Explore with our innovative research tools Thank you for downloading this free PDF. If you have comments, questions or just want more information about the books published by the National Academies Press, you may contact our customer service department toll-free at 888-624-8373, visit us online, or send an email to [email protected]. This free book plus thousands more books are available at http://www.nap.edu. Copyright © National Academy of Sciences. Permission is granted for this material to be shared for noncommercial, educational purposes, provided that this notice appears on the reproduced materials, the Web address of the online, full authoritative version is retained, and copies are not altered. To disseminate otherwise or to republish requires written permission from the National Academies Press. Missouri River Planning: Recognizing and Incorporating Sediment Management http://www.nap.edu/catalog/13019.html PREPUBLICATION COPY Missouri River Planning: Recognizing and Incorporating Sediment Management Committee on Missouri River Recovery and Associated Sediment Management Issues Water Science and Technology Board Division of Earth and Life Studies THE NATIONAL ACADEMIES PRESS Washington, D.C. -
Fur Trade on the Missouri
Missouri River Missouri National Recreational River Territory. The second expedition was no more successful, ending at a Ponca village where trader Trade, Tribes, and Transition Antoine Lecuyer took “not less than two wives… and wasted a great deal of the goods of the on the Missouri company.” The company’s third expedition under James MacKay and John Evans successfully The fur trade, America’s first fashion-driven reached the Mandan villages eight years before industry, stimulated Euro-American exploration of Lewis & Clark’s better-known American the Missouri River Valley expedition. several decades before Lewis & Clark. Beaver One of the earliest trappers and traders in the was most important, the Yankton area was Pierre Dorion, Sr., who married dense undercoat being used into the Yankton tribe around 1785 and was a short- to make felt hats. The term member of the Lewis and Clark Expedition in entire world used furs, from 1804. He served as liaison and translator for the wolf to muskrat, for warm clothing in this era council near Calumet Bluff. before synthetic insulating materials. In these early days, independent traders and small Trade was nothing new to the Plains Tribes; the parties were at risk of being relieved of their goods various cultures that occupied this land at different by tribes that chose raiding over trading. Later, times had exchanged produce, dried meat, tools, and large companies built impressive posts that not only weapons for thousands of years. By the mid 1700s, offered protection, but projected an image of the Ihanktonwan Nakota (Yankton Sioux) hosted a permanence that led to long-term trade partnerships. -
Wind River Canyon ©WYDOT/Rick Carpenter )|
Wind River Canyon ©WYDOT/Rick Carpenter )| Aê CORRIDOR 8 Aå Shoshoni to Lovell A÷ US 20/WYO 789 )| Aû A¹ A¹ PARK MONTANA )| Aå Aã Shoshoni ?Æ +» )y A÷ Thermopolis Aì Burlington WASHAKIE Byron )| Cowley )y B I G )q H O R N )y HOT Aý ?Ä )v Lovell FREMONT +» SPRINGS STATE SIGNIFICANT CORRIDOR )y A÷ ?Ë N A÷ Basin Worland* Aî )v Greybull )y A÷ )v )r 0 5 10 MILES )v o ?Å BLM BIA NPS Designated Bike Route Intercity Bus Route Primary Airport p General Aviation Greyhound Stations Local Service Urban Area )q 03 CORRIDOR 8 CORRIDOR 8 00157 GOALS CORRIDOR CHARACTERISTICS Connects agricultural communities to Billings, Safety Wind River Canyon the major regional center System Preservation Bighorn Lake and Bighorn Canyon Irrigation and stormwater runoff Economic Recreation Area Sustainability Wildlife/vehicle crashes are problematic Hot Springs State Park, Boysen State Park Environment throughout & Reservoir PRIMARY INVESTMENT TYPE: SAFETY The primary investment need on this corridor is to reduce the number and severity of vehicle crashes, especially in the Wind River Canyon and north of Thermopolis as well as between Greybull and Basin. The possible correction of horizontal and vertical curves should be further investigated in the future corridor plan. Regular maintenance and pavement resurfacing should be included to prevent deterioration of roadway surfaces. Plans should include the rehabilitation and replacement of deficient bridges. CORRIDOR CHARACTERISTICS Corridor Description State Significant Corridor (SSC) 8, from Shoshoni to Lovell, is 157 miles long and passes through the counties of Fremont, Hot Springs, Washakie, and Big Horn. It follows US 20, also called WYO 789, from Shoshoni to Worland. -
Drainage Patterns and Glaciations in Eastern Nebraska William J
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in the Earth and Atmospheric Sciences Earth and Atmospheric Sciences, Department of 1985 Drainage Patterns and Glaciations in Eastern Nebraska William J. Wayne University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Wayne, William J., "Drainage Patterns and Glaciations in Eastern Nebraska" (1985). Papers in the Earth and Atmospheric Sciences. 562. https://digitalcommons.unl.edu/geosciencefacpub/562 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. ... Institute for Tertiary-Quaternary Studies-TER-QUA Symposium Series, 1: 111-117. (Lq Rs) Drainage Patterns and Glaciations in Eastern Nebraska William J. Wayne Department of Geology University of Nebraska-Lincoln Lincoln, Nebraska 68588-0340 Most of the stream courses of eastern Nebraska came into exis fluviatile sediments across Nebraska and the adjacent states tence during the recession of an ice margin. Their patterns include changed many times during that period, but the alluvial many drainage anomalies that suggest both the manner and the times of surface continued to slope eastward, and the drainage lines ice disappearance. Rivers coming from the west flow down the regional slope of the High Plains. Along and east of the "Kansan" glacial border followed that slope. 0 most streams are subparallel, trend S300 _40 E, and probablY mark At the time the first of the Early Pleistocene continental pauses of an actively retreating ice margin. -
The Mandan and Hidatsa Establish Missouri Valley Villages
The North Dakota Studies Newspaper Issue One Native Peoples, First Encounter, Fur Trade 1780-1850 THE MANDAN AND HIDATSA ESTABLISH MISSOURI VALLEY VILLAGES The Mandan and Hidatsa Villages through oral tradition, began with The Year of 1730 Charred Body who lived in the Sky. He heard the bellowing of buffalo, and looking through a Over hundreds of years the Mandan people made hole in the heavens, discovered their way from the eastern woodlands of the the earth below. Liking what he Ohio River Valley to the valley of the Missouri saw, he descended to earth in the River. Divided into five bands, the Nuptadi, form of an arrow. He erected 13 the Mananar, the Nuitadi, the Istope, and the earthlodges and brought down 13 Awikaxa, the Mandan have established nine large young couples who founded the well-fortified villages along the banks of the original families. Sacred arrows Knife, Heart, and Missouri rivers. Some reports have the power to protect the tell us that the Mandan reached their present sites people from evil. as early as the year 900. Not long after the Awatixa arrived Numbering in the neighborhood of 9,000, the on the Missouri, the Awaxawi, Mandan are a Siouan-speaking people who Siouan-speaking eastern neighbors, owe their origins to First Creator and Lone left for the Missouri Valley. The Man. These two powerful spirits, the Mandan Awaxawi origin account begins believe, created the Missouri River Valley and the with the creation of the earth Hidatsa village. animals, plants, and people who live there. First by Lone Man and First Creator Creator made the hills, woods, springs, buffalo, who competed with each other deer, and antelope on the south side of the to see who could make the best Valley.