The Almost-Built Canal: Linking Lake Superior to the Mississippi
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Lesson 4: Sediment Deposition and River Structures
LESSON 4: SEDIMENT DEPOSITION AND RIVER STRUCTURES ESSENTIAL QUESTION: What combination of factors both natural and manmade is necessary for healthy river restoration and how does this enhance the sustainability of natural and human communities? GUIDING QUESTION: As rivers age and slow they deposit sediment and form sediment structures, how are sediments and sediment structures important to the river ecosystem? OVERVIEW: The focus of this lesson is the deposition and erosional effects of slow-moving water in low gradient areas. These “mature rivers” with decreasing gradient result in the settling and deposition of sediments and the formation sediment structures. The river’s fast-flowing zone, the thalweg, causes erosion of the river banks forming cliffs called cut-banks. On slower inside turns, sediment is deposited as point-bars. Where the gradient is particularly level, the river will branch into many separate channels that weave in and out, leaving gravel bar islands. Where two meanders meet, the river will straighten, leaving oxbow lakes in the former meander bends. TIME: One class period MATERIALS: . Lesson 4- Sediment Deposition and River Structures.pptx . Lesson 4a- Sediment Deposition and River Structures.pdf . StreamTable.pptx . StreamTable.pdf . Mass Wasting and Flash Floods.pptx . Mass Wasting and Flash Floods.pdf . Stream Table . Sand . Reflection Journal Pages (printable handout) . Vocabulary Notes (printable handout) PROCEDURE: 1. Review Essential Question and introduce Guiding Question. 2. Hand out first Reflection Journal page and have students take a minute to consider and respond to the questions then discuss responses and questions generated. 3. Handout and go over the Vocabulary Notes. Students will define the vocabulary words as they watch the PowerPoint Lesson. -
The Arkansas River Flood of June 3-5, 1921
DEPARTMENT OF THE INTERIOR ALBERT B. FALL, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE 0ns SMITH, Director Water-Supply Paper 4$7 THE ARKANSAS RIVER FLOOD OF JUNE 3-5, 1921 BY ROBERT FOLLANS^EE AND EDWARD E. JON^S WASHINGTON GOVERNMENT PRINTING OFFICE 1922 i> CONTENTS. .Page. Introduction________________ ___ 5 Acknowledgments ___ __________ 6 Summary of flood losses-__________ _ 6 Progress of flood crest through Arkansas Valley _____________ 8 Topography of Arkansas basin_______________ _________ 9 Cause of flood______________1___________ ______ 11 Principal areas of intense rainfall____ ___ _ 15 Effect of reservoirs on the flood__________________________ 16 Flood flows_______________________________________ 19 Method of determination________________ ______ _ 19 The flood between Canon City and Pueblo_________________ 23 The flood at Pueblo________________________________ 23 General features_____________________________ 23 Arrival of tributary flood crests _______________ 25 Maximum discharge__________________________ 26 Total discharge_____________________________ 27 The flood below Pueblo_____________________________ 30 General features _________ _______________ 30 Tributary streams_____________________________ 31 Fountain Creek____________________________ 31 St. Charles River___________________________ 33 Chico Creek_______________________________ 34 Previous floods i____________________________________ 35 Flood of Indian legend_____________________________ 35 Floods of authentic record__________________________ 36 Maximum discharges -
The Welland Ship Canal and the Men Who Died to Build It
The Welland Ship Canal and the men who died to build it Friday, August 28, 2015 Lock 1 of the Welland Canal is shown with its gates closed in June 1924, in this photo taken by J. A. McDonald, courtesy of the Welland Ship Canal album, Brock University Archives. The Welland Canal Fallen Workers Memorial is expected to be completed in 2017 and will be located along the canal close to Lock 3. This series of columns complements the work of the task force in bringing the monument to reality, and brings to life the men who were a part of the construction. This memorial will honour the memory of the 137 men who lost their lives in the construction of this major national infrastructure project. The Welland Ship Canal — also known as the fourth and most current Welland Canal — was a major Canadian infrastructure project. With a view to modernizing and making more efficient the previous canal, the construction work, which began in 1913 and would continue until 1935, would have a lasting impact on the local community. This project cut right through the geography of the region and its economic impact would be felt nationally. At its peak, the work engaged 4,000 workers with many thousands more having been employed at different times over the course of the two decades of construction. As we have read in these pages, this great national project was also one of tragedy. A staggering 137 men lost their lives as a result of accidents that occurred during the construction. This number is shockingly high. -
Stream Restoration, a Natural Channel Design
Stream Restoration Prep8AICI by the North Carolina Stream Restonltlon Institute and North Carolina Sea Grant INC STATE UNIVERSITY I North Carolina State University and North Carolina A&T State University commit themselves to positive action to secure equal opportunity regardless of race, color, creed, national origin, religion, sex, age or disability. In addition, the two Universities welcome all persons without regard to sexual orientation. Contents Introduction to Fluvial Processes 1 Stream Assessment and Survey Procedures 2 Rosgen Stream-Classification Systems/ Channel Assessment and Validation Procedures 3 Bankfull Verification and Gage Station Analyses 4 Priority Options for Restoring Incised Streams 5 Reference Reach Survey 6 Design Procedures 7 Structures 8 Vegetation Stabilization and Riparian-Buffer Re-establishment 9 Erosion and Sediment-Control Plan 10 Flood Studies 11 Restoration Evaluation and Monitoring 12 References and Resources 13 Appendices Preface Streams and rivers serve many purposes, including water supply, The authors would like to thank the following people for reviewing wildlife habitat, energy generation, transportation and recreation. the document: A stream is a dynamic, complex system that includes not only Micky Clemmons the active channel but also the floodplain and the vegetation Rockie English, Ph.D. along its edges. A natural stream system remains stable while Chris Estes transporting a wide range of flows and sediment produced in its Angela Jessup, P.E. watershed, maintaining a state of "dynamic equilibrium." When Joseph Mickey changes to the channel, floodplain, vegetation, flow or sediment David Penrose supply significantly affect this equilibrium, the stream may Todd St. John become unstable and start adjusting toward a new equilibrium state. -
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. -
Barge Canal” Is No Longer an Accurate Description of the New York State Canals Marine Activity on New York’S Canals
The Story of the Afterword Today, the name “Barge Canal” is no longer an accurate description of the New York State Canals marine activity on New York’s canals. Trains and trucks have taken over the transport of most cargo that once moved on barges along the canals, but the canals remain a viable waterway for navigation. Now, pleasure boats, tour Historical and Commercial Information boats, cruise ships, canoes and kayaks comprise the majority of vessels that ply the waters of the legendary Erie and the Champlain, Oswego and Cayuga- Seneca canals, which now constitute the 524-mile New York State Canal ROY G. FINCH System. State Engineer and Surveyor While the barges now are few, this network of inland waterways is a popular tourism destination each year for thousands of pleasure boaters as well as visitors by land, who follow the historic trade route that made New York the “Empire State.” Across the canal corridor, dozens of historic sites, museums and community festivals in charming port towns and bustling cities invite visitors to step back in time and re-live the early canal days when “hoggees” guided mule-drawn packet boats along the narrow towpaths. Today, many of the towpaths have been transformed into Canalway Trail segments, extending over 220 miles for the enjoyment of outdoor enthusiasts from near and far who walk, bike and hike through scenic and historic canal areas. In 1992, legislation was enacted in New York State which changed the name of the Barge Canal to the “New York State Canal System” and transferred responsibility for operation and maintenance of the Canal System from the New York State Department of Transportation to the New York State Canal Corporation, a newly created subsidiary of the New York State Thruway Authority. -
17 Major Drainage Basins
HUC 8 HYDROLOGIC UNIT NAME CLINTON 04120101 Chautauqua-Conneaut FRANKLIN 04150409 CHAMPLAIN MASSENA FORT COVINGTON MOOERS ST LAWRENCE CLINTON 04120102 Cattaraugus BOMBAY WESTVILLE CONSTABLE CHATEAUGAY NYS Counties & BURKE LOUISVILLE 04120103 Buffalo-Eighteenmile BRASHER 04150308 CHAZY ALTONA ELLENBURG BANGOR WADDINGTON NORFOLK MOIRA 04120104 Niagara ESSEX MALONE DEC Regions JEFFERSON 6 04150307 BEEKMANTOWN MADRID 05010001 Upper Allegheny LAWRENCE BELLMONT STOCKHOLM DANNEMORA BRANDON DICKINSON PLATTSBURGH LEWIS OGDENSBURG CITY LISBON 05010002 Conewango 5 PLATTSBURGH CITY HAMILTON POTSDAM SCHUYLER FALLS SARANAC 05010004 French WARREN OSWEGATCHIE DUANE OSWEGO 04150306 PERU 04130001 Oak Orchard-Twelvemile CANTON PARISHVILLE ORLEANS WASHINGTON NIAGARA DE PEYSTER ONEIDA MORRISTOWN HOPKINTON WAVERLY PIERREPONT FRANKLIN 04140101 Irondequoit-Ninemile AUSABLE MONROE WAYNE BLACK BROOK FULTON SARATOGA DEKALB HERKIMER BRIGHTON GENESEE SANTA CLARA CHESTERFIELD 04140102 Salmon-Sandy ONONDAGA NYS Major 04150406 MACOMB 04150304 HAMMOND ONTARIO MADISON MONTGOMERY RUSSELL 04150102 Chaumont-Perch ERIE SENECA CAYUGA SCHENECTADY HERMON WILLSBORO ST ARMAND WILMINGTON JAY WYOMING GOUVERNEUR RENSSELAER ALEXANDRIA CLARE LIVINGSTON YATES 04130002 Upper Genesee OTSEGO ROSSIE COLTON CORTLAND ALBANY ORLEANS 04150301 04150404 SCHOHARIE ALEXANDRIA LEWIS 7 EDWARDS 04150408 CHENANGO FOWLER ESSEX 04130003 Lower Genesee 8 TOMPKINS CLAYTON SCHUYLER 9 4 THERESA 04150302 TUPPER LAKE HARRIETSTOWN NORTH ELBA CHAUTAUQUA CATTARAUGUS PIERCEFIELD 02050104 Tioga ALLEGANY STEUBEN -
2018 FIFA WORLD CUP RUSSIA'n' WATERWAYS
- The 2018 FIFA World Cup will be the 21st FIFA World Cup, a quadrennial international football tournament contested by the men's national teams of the member associations of FIFA. It is scheduled to take place in Russia from 14 June to 15 July 2018,[2] 2018 FIFA WORLD CUP RUSSIA’n’WATERWAYS after the country was awarded the hosting rights on 2 December 2010. This will be the rst World Cup held in Europe since 2006; all but one of the stadium venues are in European Russia, west of the Ural Mountains to keep travel time manageable. - The nal tournament will involve 32 national teams, which include 31 teams determined through qualifying competitions and Routes from the Five Seas 14 June - 15 July 2018 the automatically quali ed host team. A total of 64 matches will be played in 12 venues located in 11 cities. The nal will take place on 15 July in Moscow at the Luzhniki Stadium. - The general visa policy of Russia will not apply to the World Cup participants and fans, who will be able to visit Russia without a visa right before and during the competition regardless of their citizenship [https://en.wikipedia.org/wiki/2018_FIFA_World_Cup]. IDWWS SECTION: Rybinsk – Moscow (433 km) Barents Sea WATERWAYS: Volga River, Rybinskoye, Ughlichskoye, Ivan’kovskoye Reservoirs, Moscow Electronic Navigation Charts for Russian Inland Waterways (RIWW) Canal, Ikshinskoye, Pestovskoye, Klyaz’minskoye Reservoirs, Moskva River 600 MOSCOW Luzhniki Arena Stadium (81.000), Spartak Arena Stadium (45.000) White Sea Finland Belomorsk [White Sea] Belomorsk – Petrozavodsk (402 km) Historic towns: Rybinsk, Ughlich, Kimry, Dubna, Dmitrov Baltic Sea Lock 13,2 White Sea – Baltic Canal, Onega Lake Small rivers: Medveditsa, Dubna, Yukhot’, Nerl’, Kimrka, 3 Helsinki 8 4,0 Shosha, Mologa, Sutka 400 402 Arkhangel’sk Towns: Seghezha, Medvezh’yegorsk, Povenets Lock 12,2 Vyborg Lakes: Vygozero, Segozero, Volozero (>60.000 lakes) 4 19 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 30 1 2 3 6 7 10 14 15 4,0 MOSCOW, Group stage 1/8 1/4 1/2 3 1 Estonia Petrozavodsk IDWWS SECTION: [Baltic Sea] St. -
History of Snake River Canyon Indicated by Revised Stratigraphy of Snake River Group Near Hagerman and King Hill, Idaho
History of Snake River Canyon Indicated by Revised Stratigraphy of Snake River Group Near Hagerman and King Hill, Idaho GEOLOGICAL SURVEY PROFESSIONAL PAPER 644-F History of Snake River Canyon Indicated by Revised Stratigraphy of Snake River Group Near Hagerman and King Hill, Idaho By HAROLD E. MALDE With a section on PALEOMAGNETISM By ALLAN COX SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 644-F Lavaflows and river deposits contemporaneous with entrenchment of the Snake River canyon indicate drainage changes that provide a basis for improved understanding of the late Pleistocene history UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, Acting Director Library of Congress catalog-card No. 72-171031 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 40 cents (paper cover) Stock Number 2401-1128 CONTENTS Page page Abstract ___________________________________________ Fl Late Pleistocene history of Snake River_ _ F9 Introduction.______________________________________ 2 Predecessors of Sand Springs Basalt. 13 Acknowledgments --..______-__-____--__-_---__-_____ 2 Wendell Grade Basalt-________ 14 Age of the McKinney and Wendell Grade Basalts. _____ 2 McKinney Basalt. ____---__---__ 16 Correlation of lava previously called Bancroft Springs Bonneville Flood.________________ 18 Basalt_________________________________________ Conclusion___________________________ 19 Equivalence of pillow lava near Bliss to McKinney Paleomagnetism, by Allan Cox_________ 19 Basalt.._________________________ References cited._____________________ 20 ILLUSTRATIONS Page FIGURE 1. Index map of Idaho showing area discussed.______________________________________________________ F2 2. Chart showing stratigraphy of Snake River Group..____________________________._____--___-_-_-_-. -
Distances Between United States Ports 2019 (13Th) Edition
Distances Between United States Ports 2019 (13th) Edition T OF EN CO M M T M R E A R P C E E D U N A I C T I E R D E S M T A ATES OF U.S. Department of Commerce Wilbur L. Ross, Jr., Secretary of Commerce National Oceanic and Atmospheric Administration (NOAA) RDML Timothy Gallaudet., Ph.D., USN Ret., Assistant Secretary of Commerce for Oceans and Atmosphere and Acting Under Secretary of Commerce for Oceans and Atmosphere National Ocean Service Nicole R. LeBoeuf, Deputy Assistant Administrator for Ocean Services and Coastal Zone Management Cover image courtesy of Megan Greenaway—Great Salt Pond, Block Island, RI III Preface Distances Between United States Ports is published by the Office of Coast Survey, National Ocean Service (NOS), National Oceanic and Atmospheric Administration (NOAA), pursuant to the Act of 6 August 1947 (33 U.S.C. 883a and b), and the Act of 22 October 1968 (44 U.S.C. 1310). Distances Between United States Ports contains distances from a port of the United States to other ports in the United States, and from a port in the Great Lakes in the United States to Canadian ports in the Great Lakes and St. Lawrence River. Distances Between Ports, Publication 151, is published by National Geospatial-Intelligence Agency (NGA) and distributed by NOS. NGA Pub. 151 is international in scope and lists distances from foreign port to foreign port and from foreign port to major U.S. ports. The two publications, Distances Between United States Ports and Distances Between Ports, complement each other. -
Thematic Report January 2020
THEMATIC REPORT RIVER-SEA TRANSPORT IN EUROPE PUBLISHED IN JANUARY 2020 Thematic report Published in RIVER-SEA TRANSPORT January 2020 Please find all our data at: www.inland-navigation-market.org TABLE OF CONTENTS 00 EXECUTIVE SUMMARY (P.4) METHODOLOGY AND SCOPE OF THE REPORT (P.9) 01 Definitions, terminology and scope of the report (p.10) Methodology and data reporting at EU level (p.11) RIVER-SEA TRANSPORT IN EUROPE: THE CASE OF SEAGOING SHIPS NAVIGATING ON INLAND WATERWAYS (P.15) 02 Overview of river-sea transport in Europe performed by sea- going ships (p.16) Legal and economic aspects related to river-sea transport performed by seagoing ships (p.21) River-sea goods transport in main European Union countries (p.26) • River-sea transport in the United Kingdom (p.26) • River-sea transport in Sweden (p.36) • River-sea transport in Romania (p.41) • River-sea transport in the Netherlands (p.49) • River-sea transport in Belgium (p.55) • River-sea transport in Finland (p.60) • River-sea-transport in Germany (p.67) • River-sea transport in France (p.76) • River-sea transport in Portugal (p.86) River-sea transport outside the European Union (p.87) • River-sea transport in Russia (p.87) • River-sea transport in Ukraine (p.88) RIVER-SEA TRANSPORT IN EUROPE: THE CASE OF INLAND VESSELS NAVIGATING “AT SEA” (P.91) 03 Introduction and general classification rules (p.92) Inland vessels at sea: estuary traffic in Belgium (p.95) Inland vessels put at sea in France (p.98) Inland vessels “at sea”: opportunities for the future? (p.102) 4 CCNR THEMATIC REPORT - RIVER-SEA TRANSPORT EXECUTIVE SUMMARY The Central Commission for the Navigation of the Rhine (CCNR), in partnership with the European Commission, publishes annual and biannual reports dealing with the European inland navigation market. -
Community Analysis of Pitcher Plant Bogs of the Little River Canyon National Preserve, Alabama
COMMUNITY ANALYSIS OF PITCHER PLANT BOGS OF THE LITTLE RIVER CANYON NATIONAL PRESERVE, ALABAMA Robert Carter, Terry Boyer, Heather McCoy, and Andrew J. Londo1 Abstract—Pitcher plant bogs of the Little River Canyon National Preserve in northern Alabama contain the federally endan- gered green pitcher plant [Sarracenia oreophila (Kearney) Wherry]. Multivariate analysis of the bog vegetation and envi- ronmental variables revealed three communities with unique species compositions and soil characteristics. The significant soil characteristics were percent A-horizon sand and A-horizon depth. A blackgum (Nyssa sylvatica Marsh.)-yellow poplar (Liriodendron tulipifera L.)-azalea [Rhododendron canescens (Michx.) Sweet] type was found on sites bisected by ephemeral streams with a closed canopy. A scarlet oak (Quercus coccinea Muenchh.) -flowering dogwood (Cornus florida L.) -sweet goldenrod [Solidago speciosa Nutt. var. erecta (Pursh) MacM.] type was found on upland sites close to the canyon rim and along perennial streams sites. A smooth yellow false foxglove [Aureolaria flava (L.) Farw.]-pale-spike lobelia (Lobelia spicata Lam.)- violet lespedeza [Lespedeza violacea (L.) Pers.] type was found on relatively flat sites away from the canyon rim. INTRODUCTION PROCEDURES Populations of the federally-endangered green pitcher plant are In the summer of 2003, a 10 x 30 m plot was placed in each found in scattered moist upland bogs in northern Alabama, of the 8 bogs. Plots were located near the center of the bogs northern Georgia, and western North Carolina. According to and away from roads and power lines. Tree, sapling, seedling, green pitcher plant habitat descriptions, populations are typi- and herbaceous strata were sampled following the Carolina cally found on moist upland and sandy riverbank sites.