Flows of Largest U.S. Rivers-Length, Discharge, and Ddrainage Area
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Article Title: Soldiers As Farmers: Army Agriculture in the Missouri Valley, 1818-1827
Nebraska History posts materials online for your personal use. Please remember that the contents of Nebraska History are copyrighted by the Nebraska State Historical Society (except for materials credited to other institutions). The NSHS retains its copyrights even to materials it posts on the web. For permission to re-use materials or for photo ordering information, please see: http://www.nebraskahistory.org/magazine/permission.htm Nebraska State Historical Society members receive four issues of Nebraska History and four issues of Nebraska History News annually. For membership information, see: http://nebraskahistory.org/admin/members/index.htm Article Title: Soldiers as Farmers: Army Agriculture in the Missouri Valley, 1818-1827 Full Citation: Roger L Nichols, “Soldiers as Farmers: Army Agriculture in the Missouri Valley, 1818-1827,” Nebraska History 52 (1971): 239-254. URL of article: http://www.nebraskahistory.org/publish/publicat/history/full-text/NH1971Soldier_Farmers.pdf Date: 3/16/2011 Article Summary: During the decade following the War of 1812, the military frontier preceded the settlers’ frontier in the Missouri Valley and soldiers became pioneer farmers. The soldiers of Fort Atkinson in Eastern Nebraska engaged in the first extensive American agricultural activity west of the Missouri River. Cataloging Information: Names: Talbot Chambers, Henry Atkinson, Benjamin O’Fallon, Henry Leavenworth, Ashael Savery, Edmund P Gaines, Lord Selkirk, John Gale, De Witt Clinton, George Croghan Place Names: Fort Atkinson, Nebraska; Fort Osage, -
Missouri River Infolink 1999 Report
Missouri River InfoLINK 1999 Report In cooperation with the US Environmental Protection Agency and the National Biological Information Infrastructure Missouri River InfoLINK 1999 Report US Department of the Interior US Geological Survey Missouri River InfoLINK 1999 Report Missouri River InfoLINK 1999 Report The InfoLINK enhances understanding of the Missouri River through information, partnerships, maps, and science The Missouri River flows 2,341 miles from the Rocky Mountains through the Great Plains to its confluence with the Mississippi River at St! Louis! CONTENTS Its watershed drains one-sixth of the United States! One-third of the meandering river has been channelized! 2The Big Muddy Another third has been impounded by six dams that 3 Beginnings allow the U!S! Army Corps of Engineers to regulate the water flow through the river system! The Missouri 4 Information River system is managed for multiple uses! 6 Partnerships Decisions related to river management affect the lifestyles of Americans from Montana to Missouri! 10 Maps The Missouri River InfoLINK was created for these 12Science stakeholders who represent diverse river interests and need to make informed decisions about its future 16 Bridging the Gap use and management! It is for people who want to understand how the river functions! The InfoLINK seeks to be a center point for common ground, uniting interests through sharing information that facilitates communication among all of the basins citizens! Missouri River InfoLINK 1999 Report Green areas: Native American Tribes Red -
The Missouri Is America's Longest River
The Missouri is America’s Longest River This is Shirley Griffith. And this is Steve Ember with the VOA Special English program, EXPLORATIONS. Today, we tell about another important American river, the Missouri. It is the longest river in the United States. The first American Indians to live along the Missouri River called the river the Mine Sose. It means the muddy river. Even today, the Missouri is called "the Big Muddy" by many people. This is because it carries huge amounts of dirt from the land through which it flows. The dirt makes the river a brown color for much of its length. The Missouri begins in the Rocky Mountains of North America. It is formed by three rivers that come together in what is the north central state of Montana. The three rivers are the Jefferson, Madison, and Gallatin Rivers. They become the Missouri River in the southwestern part of Montana, more than one thousand two hundred meters above sea level. The river is clear and flows rapidly as it begins its travels east and south. It moves more slowly as it flows down to the waters of the Mississippi River, about ten kilometers north of the modern-day city of Saint Louis. The Missouri travels four-thousand kilometers from the high mountains in the north to the low lands of the south. It flows along the borders of seven states: Montana, North Dakota, South Dakota, Iowa, Nebraska, Kansas, and finally Missouri. The first Europeans who reported seeing the river were at the mouth of the Missouri where it empties into the Mississippi. -
Today's Missouri River
DID YOU KNOW? The Missouri River is the longest river in North America. The Missouri is the world’s 15th- TODAY’S longest river. The Missouri has the nickname MISSOURI RIVER “Big Muddy,” because of the large The Missouri River has been an important resource for amount of silt that it carries. people living along or near it for thousands of years. As time went on and the corridor of the Missouri River was developed and populations increased, efforts have been There are approximately 150 fish made to control flows, create storage, and prevent flooding. species in the Missouri River, and As a result, six mainstem dams have been in place for more about 300 species of birds live in the than half a century, with the goal of bringing substantial Missouri River’s region. economic, environmental, and social benefits to the people of North Dakota and nine other states. The Missouri’s aquatic and riparian Since the building of the mainstem dams, it has been habitats also support several species realized that for all of the benefits that were provided, the of mammals, such as mink, river dams have also brought controversy. They have created otter, beaver, muskrat, and raccoon. competition between water users, loss of riparian habitat, impacts to endangered species, stream bank erosion, and delta formation - which are only a few of the complex issues The major dams built on the river related to today’s Missouri River management. were Fort Peck, Garrison, Oahe, Big Bend, Fort Randall, and Gavin’s Point. This educational booklet will outline the many benefits that the Missouri River provides, and also summarize some of the biggest issues that are facing river managers and residents within the basin today. -
A New Corps of Discovery for Missouri River Management Sandra B
Nebraska Law Review Volume 83 | Issue 2 Article 4 2004 A New Corps of Discovery for Missouri River Management Sandra B. Zellmer University of Nebraska Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/nlr Recommended Citation Sandra B. Zellmer, A New Corps of Discovery for Missouri River Management, 83 Neb. L. Rev. (2004) Available at: https://digitalcommons.unl.edu/nlr/vol83/iss2/4 This Article is brought to you for free and open access by the Law, College of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Nebraska Law Review by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Sandra B. Zellmer* A New Corps of Discovery for Missouri River Management TABLE OF CONTENTS I. Introduction .......................................... 306 II. The Jeffersonian Corps of Discovery ................... 310 III. Of Famine and Floods: The Flood Control Act of 1944 ............................................... 312 A. The Impetus for the Flood Control Act ............. 312 B. The Implementation of the Flood Control Act ...... 315 IV. The Environmental Era: All Creatures Great and Sm all ............................................ 319 V. The Clash of the Titans: Engineers, Barges, Birds, and Fish .............................................. 324 A. Track One: The States' Flood Control Act Litigation ......................................... 324 B. Track Two: The Environmental Groups' ESA Litigation ......................................... 326 C. The Minnesota Opinion and 2004 Master M anual ........................................... 329 VI. A New Corps of Discovery: An Organic Act for a Sustainable Management Paradigm ................... 334 A. The Law of the Missouri River ..................... 334 B. A Federal Missouri River Organic Act ............. 337 C. The Basic Organic Act Principles .................. 346 D. Other Options, from Most to Least Drastic ........ -
Class 14: Basic Hydrograph Analysis Class 14: Hydrograph Analysis
Engineering Hydrology Class 14: Basic Hydrograph Analysis Class 14: Hydrograph Analysis Learning Topics and Goals: Objectives 1. Explain how hydrographs relate to hyetographs Hydrograph 2. Create DRO (direct runoff) hydrographs by separating baseflow Description 3. Relate runoff volume to watershed area and create UH (next time) Unit Hydrographs Separating Baseflow DRO Hydrographs Ocean Class 14: Hydrograph Analysis Learning Gross rainfall = depression storage + Objectives evaporation + infiltration Hydrograph + surface runoff Description Unit Hydrographs Separating Baseflow Rainfall excess = (gross rainfall – abstractions) DRO = Direct Runoff = DRO Hydrographs = net rainfall with the primary abstraction being infiltration (i.e., assuming depression storage is small and evaporation can be neglected) Class 14: Hydrograph Hydrograph Defined Analysis Learning • a hydrograph is a plot of the Objectives variation of discharge with Hydrograph Description respect to time (it can also be Unit the variation of stage or other Hydrographs water property with respect to Separating time) Baseflow DRO • determining the amount of Hydrographs infiltration versus the amount of runoff is critical for hydrograph interpretation Class 14: Hydrograph Meteorological Factors Analysis Learning • Rainfall intensity and pattern Objectives • Areal distribution of rainfall Hydrograph • Size and duration of the storm event Description Unit Physiographic Factors Hydrographs Separating • Size and shape of the drainage area Baseflow • Slope of the land surface and channel -
River Dynamics 101 - Fact Sheet River Management Program Vermont Agency of Natural Resources
River Dynamics 101 - Fact Sheet River Management Program Vermont Agency of Natural Resources Overview In the discussion of river, or fluvial systems, and the strategies that may be used in the management of fluvial systems, it is important to have a basic understanding of the fundamental principals of how river systems work. This fact sheet will illustrate how sediment moves in the river, and the general response of the fluvial system when changes are imposed on or occur in the watershed, river channel, and the sediment supply. The Working River The complex river network that is an integral component of Vermont’s landscape is created as water flows from higher to lower elevations. There is an inherent supply of potential energy in the river systems created by the change in elevation between the beginning and ending points of the river or within any discrete stream reach. This potential energy is expressed in a variety of ways as the river moves through and shapes the landscape, developing a complex fluvial network, with a variety of channel and valley forms and associated aquatic and riparian habitats. Excess energy is dissipated in many ways: contact with vegetation along the banks, in turbulence at steps and riffles in the river profiles, in erosion at meander bends, in irregularities, or roughness of the channel bed and banks, and in sediment, ice and debris transport (Kondolf, 2002). Sediment Production, Transport, and Storage in the Working River Sediment production is influenced by many factors, including soil type, vegetation type and coverage, land use, climate, and weathering/erosion rates. -
Missouri River District
Missouri River District Missouri River District January 2017 Missouri River District News 2016 Wrap Up Any churches that didn’t submit a 2016 parsonage report or a 2017 budget please email a copy of both to Kris at missouririv- [email protected] right away. Mission Share payments for 2016 can be made up until January 9, 2017 (see page 2 for more information). Please make January 2017 sure to like our ALL CHURCHES are required to enter Yearend Statistics (Table 1, Facebook page. 2, 3) into Ezra no later than 5:00 p.m. January 31, 2017. Please Click on the above icon do not wait until the end of January to complete this task. Infor- for a direct link. mation can be found on page 3 or by going to the on the Great Plains website at www.greatplainsumc.org, under Administration > Church Council and Leader Resources > Yearend Reports. SPRC Training will also be held in January on Saturday the 21st Hungry? Join Lefler from 9:00-11:00 a.m. at Springfield UMC, 480 Main St, Spring- or Nehawaka for one field, NE. ALL SPRC Chairs need to attend. Pastors and other or all of their upcom- SPRC committee members are welcome to attend as well. ing dinners! CLICK HERE for a link to signup or more information on page 4. —————————————————- February 2017 Lefler Dinners 2017 dates to be District Training on Multi-Media in Worship will take place on Sat- announced. urday, February, 18, 2017 at Omaha Living Faith UMC from 9AM- —————————————————- 4PM. This event is open to both clergy and laity. -
Real-Time Stream Flow Gages in Montana
REAL-TIME STREAM FLOW GAGES IN MONTANA Montana is home to over 264 real-time stream lows and improve water management practices. It gages located throughout the state. These gages can drive the understanding for other sciences and and their networks assist in delivering water data to helps inform citizens on how we can prepare for scientists and the public. While Montana’s demand changes in our water supply. It is imperative to for water continues to grow, water availability maintain as many gages as possible to preserve varies from year-to-year and can change these historical records for current and future dramatically in any given year. Managing supply and generations. demand challenges is an ongoing feature of life. REAL-TIME GAGES Accurate, near real-time, publicly accessible information on stream flows assists both day to day A real-time stream gage is used to report stream decision making and long-term planning, as well as flow (discharge) in cubic feet per second. These emergency planning and notification. This gages measure the stage (height) of the river in feet, information is generated in Montana by multiple and water temperature along with other networks of real-time stream gages operated by the environmental data. U.S. Geological Survey (USGS), the Department of Natural Resources and Conservation (DNRC), and some tribes. Within each network, the operation and maintenance of gages are financially supported by different sources including federal, state, tribal, local, and private funds. Some of the gages are funded by multiple agencies and organizations. The recorded data are essential to make informed water management decisions across the state. -
Chapter 5 Streamflow Data
Part 630 Hydrology National Engineering Handbook Chapter 5 Streamflow Data (210–VI–NEH, Amend. 76, November 2015) Chapter 5 Streamflow Data Part 630 National Engineering Handbook Issued November 2015 The U.S. Department of Agriculture (USDA) prohibits discrimination against its customers, em- ployees, and applicants for employment on the bases of race, color, national origin, age, disabil- ity, sex, gender identity, religion, reprisal, and where applicable, political beliefs, marital status, familial or parental status, sexual orientation, or all or part of an individual’s income is derived from any public assistance program, or protected genetic information in employment or in any program or activity conducted or funded by the Department. (Not all prohibited bases will apply to all programs and/or employment activities.) If you wish to file a Civil Rights program complaint of discrimination, complete the USDA Pro- gram Discrimination Complaint Form (PDF), found online at http://www.ascr.usda.gov/com- plaint_filing_cust.html, or at any USDA office, or call (866) 632-9992 to request the form. You may also write a letter containing all of the information requested in the form. Send your completed complaint form or letter to us by mail at U.S. Department of Agriculture, Director, Office of Adju- dication, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410, by fax (202) 690-7442 or email at [email protected] Individuals who are deaf, hard of hearing or have speech disabilities and you wish to file either an EEO or program complaint please contact USDA through the Federal Relay Service at (800) 877- 8339 or (800) 845-6136 (in Spanish). -
Colorado River Compact, 1922
Colorado River Compact, 1922 The States of Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming, having resolved to enter into a compact under the Act of the Congress of the United States of America approved August 19, 1921 (42 Statutes at Large, page 171), and the Acts of the Legislatures of the said States, have through their Governors appointed as their Commissioners: W.S. Norviel for the State of Arizona, W.F. McClure for the State of California, Delph E. Carpenter for the State of Colorado, J.G. Scrugham for the State of Nevada, Stephen B. Davis, Jr., for the State of New Mexico, R.E. Caldwell for the State of Utah, Frank C. Emerson for the State of Wyoming, who, after negotiations participated in by Herbert Hoover appointed by The President as the representative of the United States of America, have agreed upon the following articles: ARTICLE I The major purposes of this compact are to provide for the equitable division and apportionment of the use of the waters of the Colorado River System; to establish the relative importance of different beneficial uses of water, to promote interstate comity; to remove causes of present and future controversies; and to secure the expeditious agricultural and industrial development of the Colorado River Basin, the storage of its waters, and the protection of life and property from floods. To these ends the Colorado River Basin is divided into two Basins, and an apportionment of the use of part of the water of the Colorado River System is made to each of them with the provision that further equitable apportionments may be made. -
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.