From Rivers to Lakes: Engineering Pittsburgh's Three Rivers
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Vegetation Survey of Monongahela River Phase 2 - 2001 VEGETATION SURVEY of the MONONGAHELA RIVER
Vegetation Survey of Monongahela River Phase 2 - 2001 VEGETATION SURVEY OF THE MONONGAHELA RIVER Prepared by: Dr. Susan Kalisz Department of Biological Sciences, University of Pittsburgh 3 Rivers - 2nd Nature Studio for Creative Inquiry Carnegie Mellon University 3R2N Woody Vegetation Survey Phase 2 - 2001 For more information on the 3 Rivers – 2nd Nature Project, see http:// 3r2n.cfa.cmu.edu If you believe that eeeccooll ooggii ccaall ll yy hheeaall tthhyy rrii vveerrss aarree 22 nndd NNaattuurree and would like to participate in a river dialogue about water quality, recreational use and biodiversity in the 3 Rivers Region, contact: Tim Collins, Research Fellow Director 3 Rivers - 2nd Nature Project STUDIO for Creative Inquiry 412-268-3673 fax 268-2829 [email protected] CCooppyyrrii gghhtt ©© 2002 –– SSttuuddii oo ffoorr CCrreeaattii vvee II nnqquuii rryy,, CCaarrnneeggii ee MMeell ll oonn All rights reserved Published by the STUDIO for Creative Inquiry, Rm 111, College of Fine Arts, Carnegie Mellon University Pittsburgh PA 15213 412-268-3454 fax 268-2829 http:// www.cmu.edu/studio First Edition, First Printing 2 CCoo--AAuutthhoorrss Tim Collins, Editor Reiko Goto, C0-Director, 3R2N Priya Krishna, GIS (Geographical Information System) PPaarrttnneerrss ii nn tthhii ss PPrroojj eecctt 3 Rivers Wet Weather Incorporated (3RWW) Allegheny County Health Department (ACHD) Allegheny County Sanitary Authority (ALCOSAN) 3 RRii vveerrss -- 2nndd NNaattuurree AAddvvii ssoorrss Reviewing this Project John Arway Chief Environmental Services, PA Fish and Boat Commission Wilder Bancroft Environmental Quality Manager, Allegheny County Health Dept. Bob Bingham Professor Art, Co-Director, STUDIO for Creative Inquiry, CMU Don Berman Environmental Consultant, Jacqui Bonomo V.P. -
The Trail Through Shadow of Ljcaut C"P. from a Phoiogrnph Made by the Author in September, 1909
The Trail through Shadow of lJcaUt C"p. From a phoiogrnph made by the Author in September, 1909. The Wilderness Trail Or The Ventures and Adventures of the Pennsyl vania Traders on the Allegheny Path With Some New Annals of the Old West, and the Records of Some Strong Men and Some Bad Ones By Charles A. Hanna Author of .. The Scotch-Irish" With Eighty Maps alld Illustratiuns In Two Volumes Volume One G. P. Plltnam's Sons New York and London ltDe 1T1111c~erbocllec lIlreo6 1911 CHAPTER XII THE OHIO MINGOES OF THE WHITE RIVER, AND THE WENDATS IERRE JOSEPH DE CELORON, Commandant at Detroit in 1743, P wrote in the month of June of that year to Bcauharnois, the Governor-General of Canada at Quebec, respecting some Indians" who had seated themselves of late years at the White River." These Indians, he reported, were Senecas, Onondagas, and others of the Five Iroquois villages. At their urgent request, Celoron permitted some residents of Detroit to carry goods thither, and had recently sent Sicur Navarre to the post, to make a report thereupon. Navarre's account was trans nUtted to Quebec with this letter. Celoron's letter has been printed in the New York Colonial Doc1tments, but the accompanying report of Sieur Navarre has not heretofore been published. Following is a portion of that report: "Memoir of an inspection made by me, Navarre,l of the trading post where the Frenchman called Saguin carries on trade; of the different nations who are there established, and of the trade which can be de veloped there. -
The Principal Indian Towns of Western Pennsylvania C
The Principal Indian Towns of Western Pennsylvania C. Hale Sipe One cannot travel far in Western Pennsylvania with- out passing the sites of Indian towns, Delaware, Shawnee and Seneca mostly, or being reminded of the Pennsylvania Indians by the beautiful names they gave to the mountains, streams and valleys where they roamed. In a future paper the writer will set forth the meaning of the names which the Indians gave to the mountains, valleys and streams of Western Pennsylvania; but the present paper is con- fined to a brief description of the principal Indian towns in the western part of the state. The writer has arranged these Indian towns in alphabetical order, as follows: Allaquippa's Town* This town, named for the Seneca, Queen Allaquippa, stood at the mouth of Chartier's Creek, where McKees Rocks now stands. In the Pennsylvania, Colonial Records, this stream is sometimes called "Allaquippa's River". The name "Allaquippa" means, as nearly as can be determined, "a hat", being likely a corruption of "alloquepi". This In- dian "Queen", who was visited by such noted characters as Conrad Weiser, Celoron and George Washington, had var- ious residences in the vicinity of the "Forks of the Ohio". In fact, there is good reason for thinking that at one time she lived right at the "Forks". When Washington met her while returning from his mission to the French, she was living where McKeesport now stands, having moved up from the Ohio to get farther away from the French. After Washington's surrender at Fort Necessity, July 4th, 1754, she and the other Indian inhabitants of the Ohio Val- ley friendly to the English, were taken to Aughwick, now Shirleysburg, where they were fed by the Colonial Author- ities of Pennsylvania. -
Geomorphic Classification of Rivers
9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations. -
Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution
Graduate Theses, Dissertations, and Problem Reports 2020 Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift West Virginia University, [email protected] Follow this and additional works at: https://researchrepository.wvu.edu/etd Part of the Geomorphology Commons Recommended Citation Swift, Mark D., "Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution" (2020). Graduate Theses, Dissertations, and Problem Reports. 7542. https://researchrepository.wvu.edu/etd/7542 This Thesis is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift Thesis Submitted to the Eberly College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Master of Arts in Geography Jamison Conley, Ph.D., Co-Chair J. Steven Kite, Ph.D., Co-Chair Nicolas Zegre, Ph.D. Department of Geology and Geography Morgantown, West Virginia 2020 Keywords: landscape evolution, knickzone, southwest Pennsylvania Copyright 2020 Mark D. -
History of Navigation on the Yellowstone River
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1950 History of navigation on the Yellowstone River John Gordon MacDonald 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 MacDonald, John Gordon, "History of navigation on the Yellowstone River" (1950). Graduate Student Theses, Dissertations, & Professional Papers. 2565. https://scholarworks.umt.edu/etd/2565 This Thesis 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]. HISTORY of NAVIGATION ON THE YELLOWoTGriE RIVER by John G, ^acUonald______ Ë.À., Jamestown College, 1937 Presented in partial fulfillment of the requirement for the degree of Mas ter of Arts. Montana State University 1950 Approved: Q cxajJL 0. Chaiinmaban of Board of Examiners auaue ocnool UMI Number: EP36086 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT Ois8<irtatk>n PuUishing UMI EP36086 Published by ProQuest LLC (2012). Copyright in the Dissertation held by the Author. Microform Edition © ProQuest LLC. -
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. -
Is Hydrology Kinematic?
HYDROLOGICAL PROCESSES Hydrol. Process. 16, 667–716 (2002) DOI: 10.1002/hyp.306 Is hydrology kinematic? V. P. Singh* Department of Civil and Environmental Engineering, Louisiana State University, Baton Rouge, LA 70803-6405, USA Abstract: A wide range of phenomena, natural as well as man-made, in physical, chemical and biological hydrology exhibit characteristics similar to those of kinematic waves. The question we ask is: can these phenomena be described using the theory of kinematic waves? Since the range of phenomena is wide, another question we ask is: how prevalent are kinematic waves? If they are widely pervasive, does that mean hydrology is kinematic or close to it? This paper addresses these issues, which are perceived to be fundamental to advancing the state-of-the-art of water science and engineering. Copyright 2002 John Wiley & Sons, Ltd. KEY WORDS biological hydrology; chemical hydrology; physical hydrology; kinematic wave theory; kinematics; flux laws INTRODUCTION There is a wide range of natural and man-made physical, chemical and biological flow phenomena that exhibit wave characteristics. The term ‘wave’ implies a disturbance travelling upstream, downstream or remaining stationary. We can visualize a water wave propagating where the water itself stays very much where it was before the wave was produced. We witness other waves which travel as well, such as heat waves, pressure waves, sound waves, etc. There is obviously the motion of matter, but there can also be the motion of form and other properties of the matter. The flow phenomena, according to the nature of particles composing them, can be distinguished into two categories: (1) flows of discrete noncoherent particles and (2) flows of continuous coherent particles. -
THE FORT PITT BLOCK HOUSE Prepared by Kelly Linn - January 2008
THE FORT PITT BLOCK HOUSE Prepared by Kelly Linn - January 2008 The Block House is just one small defensive redoubt and the only surviving structure of Fort Pitt - a key British fortification during the French and Indian War in North America (or the Seven Years War as it is known in Europe). Constructed as the second largest British fort on the colonial frontier, Fort Pitt measured about 18 acres. Crown Point in New York was the largest covering 3.5 square miles. Both of these installations date to the same military era. Fort Pitt was constructed at the Forks of the Ohio (now the Point at Pittsburgh, Pennsylvania) between 1759 and 1761. It was a classic star-shaped fort with 5 bastions projecting from the corners. The Music Bastion and the Grenadiers Bastion were on the east, or land side, of the Point, the Flag and Monongahela Bastions fronted the Monongahela River and the Ohio Bastion overlooked the Allegheny River floodplain. Only the eastern walls were faced with brick to repel cannon fire; the remaining walls of the fort were earthen ramparts covered with sod. The walls of the fort averaged a height of 15 feet above the Monongahela terrace upon which it was constructed. In January 1762 - only a few months after the fort was completed - flood waters from the Allegheny and Monongahela Rivers crested at nearly 40 feet inflicting heavy damage to the fort. Repairs were made, but in March 1763, another flood cresting at 41 feet, destroyed the Ohio Bastion entirely and heavily damaged the Monongahela Bastion a second time. -
Upper Mon River Trail
Upper Monongahela River Water Trail Map and Guide Water trails are recreational waterways on a lake, river, or ocean between specific locations, containing access points and day-use and/or camping sites for the boating public. Water trails emphasize low-impact use and promote stewardship of the resources. Explore this unique West Virginia and Pennsylvania water trail. For your safety and enjoyment: Always wear a life jacket. Obtain proper instruction in boating skills. Know fishing and boating regulations. Be prepared for river hazards. Carry proper equipment. THE MONONGAHELA RIVER The Monongahela River, locally know as “the Mon,” forms at the confluence of the Tygart and West Fork Rivers in Fairmont West Virginia. It flows north 129 miles to Pittsburgh, Pennsylvania, where it joins the Allegheny River to form the Ohio River. The upper section, which is described in this brochure, extends 68 miles from Fairmont to Maxwell Lock and Dam in Pennsylvania. The Monongahela River formed some 20 million years ago. When pioneers first saw the Mon, there were many places where they could walk across it. The Native American named the river “Monongahela,” which is said to mean “river with crumbling or falling banks.” The Mon is a hard-working river. It moves a large amount of water, sediment, and freight. The average flow at Point Marion is 4,300 cubic feet per second. The elevation on the Upper Mon ranges from 891 feet in Fairmont to 763 feet in the Maxwell Pool. PLANNING A TRIP Trips on the Mon may be solitary and silent, or they may provide encounters with motor boats and water skiers or towboats moving barges of coal or limestone. -
Louisiana Folk Boats by Malcolm Comeaux Malcolm Comeaux Received His Ph.D
Louisiana Folk Boats by Malcolm Comeaux Malcolm Comeaux received his Ph.D. in Folk boats are those small craft made by their users or by local boat geographyfrom Louisiana State University in 1969. He is currently a professor ofgeogra builders who learned their construction techniques from an older gen phy at Arizona State University in Tempe. eration. Hundreds of folk boats are built each year without blueprints He has conducted extensive field research or plans in backyards and small boatyards scattered throughout south on the development offishing systems in in land waters, particularly in the Mississippi Louisiana, where this tradition remains an important part of every- River System and in the Atchafalaya Swamp day life. It is not a folk tradition that depends upon sales to tourists; ofLouisiana. rather it survives simply because many require small boats for their livelihood. Boats are found throughout the state, although in north Louisiana there was never a strong folk boat tradition, for the area was settled by Anglo southerners who had little need for boats. In south Louisiana, however, where there was always a close relationship between man and water, boat traditions survive because the craft are needed to exploit marine environments. Coastal regions, as well as lakes, bayous and swamps, are rich in resources, producing fish, crawfish, frogs, fur Plank pirogue used in Atchafalaya Basin. bearing animals, Spanish moss, crabs, shrimp, alligators, and the like. Photo courtesy Louisiana Office of Tourism To harvest these resources, boats are needed- not just any boats, but 22 ones designed to fit various ecological conditions and accomplish Building a Lafitte skiff in the backyard of a south Louisiana home. -
River Engineering John Fenton
River Engineering John Fenton Institute of Hydraulic Engineering and Water Resources Management Vienna University of Technology, Karlsplatz 13/222, 1040 Vienna, Austria URL: http://johndfenton.com/ URL: mailto:[email protected] 1. Introduction 1.1 The nature of what we will and will not do – illuminated by some aphorisms and some people “There is nothing so practical as a good theory” – stated in 1951 by Kurt Lewin (D-USA, 1890-1947): this is essentially the guiding principle behind these lectures. We want to solve practical problems, both in professional practice and research, and to do this it is a big help to have a theoretical understanding and a framework. “The purpose of computing is insight, not numbers” – the motto of a 1973 book on numerical methods for practical use by the mathematician Richard Hamming (USA, 1915-1998). That statement has excited the opinions of many people (search any three of the words in the Internet!). However, numbers are often important in engineering, whether for design, control, or other aspects of the practical world. A characteristic of many engineers, however, is that they are often blinded by the numbers, and do not seek the physical understanding that can be a valuable addition to the numbers. In this course we are not going to deal with many numbers. Instead we will deal with the methods by which numbers could be obtained in practice, and will try to obtain insight into those methods. Hence we might paraphrase simply: "The purpose of this course is insight into the behaviour of rivers; with that insight, numbers can be often be obtained more simply and reliably".