Watersheds and the Streams That Flow Through Them
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THOUSAND MILE SONG Also by David Rothenberg
THOUSAND MILE SONG Also by David Rothenberg Is It Painful to Think? Hand’s End Sudden Music Blue Cliff Record Always the Mountains Why Birds Sing THOUSAND MILE SONG Whale Music In a Sea of Sound DAVID ROTHENBERG A Member of the Perseus Books Group New York Copyright © 2008 by David Rothenberg Published by Basic Books, A Member of the Perseus Books Group All rights reserved. Printed in the United States of America. No part of this book may be reproduced in any manner whatsoever without written permission except in the case of brief quotations embodied in critical articles and reviews. For information, address Basic Books, 387 Park Avenue South, New York, NY 10016–8810. Books published by Basic Books are available at special discounts for bulk purchases in the United States by corporations, institutions, and other organizations. For more information, please contact the Special Markets Department at the Perseus Books Group, 2300 Chestnut Street, Suite 200, Philadelphia, PA 19103, or call (800) 255–1514, or e-mail [email protected]. Designed by Linda Mark Set in 12 pt Granjon by The Perseus Books Group Library of Congress Cataloging-in-Publication Data Rothenberg, David, 1962- Thousand mile song: whale music in a sea of sound / David Rothenberg. p. cm. Includes bibliographical references and index. ISBN 978-0-465-07128-9 (alk. paper) 1. Whales—Behavior. 2. Whale sounds. I. Title. QL737.C4R63 2008 599.5’1594—dc22 2007048161 10 9 8 7 6 5 4 3 2 1 CONTENTS 1 WE DIDN’T KNOW, WE DIDN’T KNOW: Whale Song Hits the Charts 1 2GONNA GROW -
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. -
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. -
Music Preferences: a Gateway to Where? by Delia Regan
Music Preferences: A Gateway to Where? Delia Regan Anna Maria College Author’s Note Delia Regan (‘21), Music Therapy Honor Student, Anna Maria College This thesis was prepared for HON 490-01 Seniors Honors Seminar under the instruction of Professor Travis Maruska, Associate Professor of Humanities, Anna Maria College. Correspondence concerning this article should be addressed by electronic mail. Contact: [email protected], [email protected] 1 Abstract This paper discusses the impact of peer pressure on shared music preferences which was conducted through a survey and group interviews. The information on the development of music preferences provides the reader with background on how the music preference process begins. Peer pressure is also discussed from early childhood into adulthood. The solidification of music preferences happens around the same age as college-aged individuals, which overlaps with a decrease in the impact of peer pressure. The research focuses on college-aged individuals who completed a survey on their music preferences in individual and group settings, and then were put into groups to determine if a social setting would influence their responses to the same questions. Overall, a distinct relationship between peer pressure and music preference could not be made. Keywords: College-Aged, Group Cohesion, Music, Music Preference, Peer Pressure, Social Consequence 2 Music Preferences What does music taste say about a person? Music is usually a part of daily life, whether people are aware of it or not. It can help people express themselves, regulate their emotions, and, when used clinically, can help a person regain the ability to walk. Music is powerful, but what draws people to it? Studies have been done to try and determine why people are attracted to music, and they have created multiple theories trying to answer this question. -
Mitchell Creek Watershed Hydrologic Study 12/18/2007 Page 1
Mitchell Creek Watershed Hydrologic Study Dave Fongers Hydrologic Studies Unit Land and Water Management Division Michigan Department of Environmental Quality September 19, 2007 Table of Contents Summary......................................................................................................................... 1 Watershed Description .................................................................................................... 2 Hydrologic Analysis......................................................................................................... 8 General ........................................................................................................................ 8 Mitchell Creek Results.................................................................................................. 9 Tributary 1 Results ..................................................................................................... 11 Tributary 2 Results ..................................................................................................... 15 Recommendations ..................................................................................................... 18 Stormwater Management .............................................................................................. 19 Water Quality ............................................................................................................. 20 Stream Channel Protection ....................................................................................... -
Stream Visual Assessment Manual
U.S. Fish & Wildlife Service Stream Visual Assessment Manual Cane River, credit USFWS/Gary Peeples U.S. Fish & Wildlife Service Conasauga River, credit USFWS Table of Contents Introduction ..............................................................................................................................1 What is a Stream? .............................................................................................................1 What Makes a Stream “Healthy”? .................................................................................1 Pollution Types and How Pollutants are Harmful ........................................................1 What is a “Reach”? ...........................................................................................................1 Using This Protocol..................................................................................................................2 Reach Identification ..........................................................................................................2 Context for Use of this Guide .................................................................................................2 Assessment ........................................................................................................................3 Scoring Details ..................................................................................................................4 Channel Conditions ...........................................................................................................4 -
C. Natural Stream Processes
Natural Stream Processes Guide No. 03 Streams in their natural state are dy- agency officials, and others to start a recycle nutrients from natural pollution namic ecosystems that perform many thoughtful inquiry into the true source sources, such as leaf fall, to purifying beneficial functions. Natural streams of local stream management problems. the water. The natural stream tends and their flood plains convey water The material contained in this guide to maintain itself through the flushing and sediment, temporarily store excess makes evident that the source of many flows of annual floods that clear the flood water, filter and entrap sediment stream problems is in the watershed, channel of accumulated sediments, and pollutants in overbank areas, far from the main stream channel. debris, and encroaching vegetation. recharge and discharge groundwater, Landowners, local officials, and oth- Extreme floods may severely disrupt naturally purify instream flows, and ers concerned with streams need to the stream on occasion, but the natural provide supportive habitat for diverse work together across property lines balance of the stream ecosystem is plant and animal species. The stream and jurisdictional boundaries to find restored rapidly when it is in a state of corridors wherein these beneficial func- suitable solutions to stream problems dynamic equilibrium. tions occur give definition to the land and to implement practices to protect, and offer “riverscapes” with aesthetic restore and maintain healthy stream qualities that are attractive to people. ecosystems. CHANNEL FORMING Human activities that impact stream AND RECONDITIONING ecosystems can and often do cause STREAMS ARE problems by impairing stream functions PROCESSES and beneficial uses of the resource. -
Chapter 11 – Glossary of Terms
CHAPTER 11 GLOSSARY OF TERMS WORD DEFINITION SOURCE Active Channel The channel that contains the discharge Leopold where channel maintenance is most effective, sediment are actively transported and deposited, and that are capable of containing most flows. Active channels are located within the area bounded by bankfull stages. Active Flood plain Low lying areas built by watercourse Collaborative, sediment depositions between top of bank Leopold that are adjacent to a watercourse and that have been constructed by the present river in the present climate. These areas are susceptible to frequent inundation during moderate and higher flows when the active channel’s capacity is exceeded. Active floodplains are most prominent along low- gradient, meandering reaches and are often absent or undistinguishable along steeper sloped stream channels. Active Recreation Includes sports fields, recreation centers, tot San Jose lots, play equipment, multi-use courts, etc. Riparian Should not be located within riparian area. Corridor Policy USER MANUAL: GUIDELINES + STANDARDS FOR LAND USE NEAR STREAMS 11.1 GLOSSARY OF TERMS GLOSSARY OF TERMS WORD DEFINITION SOURCE Bankfull stage Bankfull stage is the point at which the flow Water just begins to enter the active floodplain. Resources Accurate measurements have been Protection conducted on gaged streams, however, in Collaborative, absence of historical hydrological records Leopold there are a number of field indicators that can be used to identify bankfull stages with a great deal of accuracy: • An abrupt change in the slope of the stream channel, usually from a vertical plane to a horizontal plane on top of the floodplain. • The bankfull stage is usually marked by a change in vegetation such as the change from gravel bars to forbs, herbs, or grasses. -
Song & Music in the Movement
Transcript: Song & Music in the Movement A Conversation with Candie Carawan, Charles Cobb, Bettie Mae Fikes, Worth Long, Charles Neblett, and Hollis Watkins, September 19 – 20, 2017. Tuesday, September 19, 2017 Song_2017.09.19_01TASCAM Charlie Cobb: [00:41] So the recorders are on and the levels are okay. Okay. This is a fairly simple process here and informal. What I want to get, as you all know, is conversation about music and the Movement. And what I'm going to do—I'm not giving elaborate introductions. I'm going to go around the table and name who's here for the record, for the recorded record. Beyond that, I will depend on each one of you in your first, in this first round of comments to introduce yourselves however you wish. To the extent that I feel it necessary, I will prod you if I feel you've left something out that I think is important, which is one of the prerogatives of the moderator. [Laughs] Other than that, it's pretty loose going around the table—and this will be the order in which we'll also speak—Chuck Neblett, Hollis Watkins, Worth Long, Candie Carawan, Bettie Mae Fikes. I could say things like, from Carbondale, Illinois and Mississippi and Worth Long: Atlanta. Cobb: Durham, North Carolina. Tennessee and Alabama, I'm not gonna do all of that. You all can give whatever geographical description of yourself within the context of discussing the music. What I do want in this first round is, since all of you are important voices in terms of music and culture in the Movement—to talk about how you made your way to the Freedom Singers and freedom singing. -
Michigan's Copper Country" Lets You Experience the Require the Efforts of Many People with Different Excitement of the Discovery and Development of the Backgrounds
Michigan’s Copper Country Ellis W. Courter Contribution to Michigan Geology 92 01 Table of Contents Preface .................................................................................................................. 2 The Keweenaw Peninsula ........................................................................................... 3 The Primitive Miners ................................................................................................. 6 Europeans Come to the Copper Country ....................................................................... 12 The Legend of the Ontonagon Copper Boulder ............................................................... 18 The Copper Rush .................................................................................................... 22 The Pioneer Mining Companies................................................................................... 33 The Portage Lake District ......................................................................................... 44 Civil War Times ...................................................................................................... 51 The Beginning of the Calumet and Hecla ...................................................................... 59 Along the Way to Maturity......................................................................................... 68 Down the South Range ............................................................................................. 80 West of the Ontonagon............................................................................................ -
Streams and Running Water Streams Are Part of the Hydrologic Cycle (Figure 10.1)
Streams and Running Water Streams are part of the hydrologic cycle (Figure 10.1) Stream: body of running water that is confined in a channel and moves downhill under the influence of gravity. Cross-section of a typical stream (Figure 10.2) 1) Channel Flow 2) Sheet Flow Drainage Basin: area of a stream and its’ tributaries. Tributary: small stream flowing into a large one. Divide: ridge seperating drainage basins. Drainage Patterns 1) Dendritic: resembles tree branches > occurs on uniformly resistant rock 2) Radial: streams diverge outward from a central point > occurs on conic shapes, like volcanoes 3) Rectangular: steams have sharp bends ¾ due to presence of faulting, river follows the fault 4) Trellis: Parallel main streams with right angle tributaries > occurs on valley and ridge geomorphologies Factors Affecting Stream Erosion and Deposition 1) Velocity = distance/time Fast = 5km/hr or 3mi/hr Flood = 25 km/hr or 15 mi/hr Figure 10.6: Fastest in the middle of the channel a) Gradient: downhill slope of the bed of the stream ¾ very high near the mountains ¾ 50-200 feet/ mile in highlands, 0.5 ft/mile in floodplain b) Channel Shape and Roughness (Friction) > Figure 10.9 ¾ Lots of fine particles – low roughness, faster river ¾ Lots of big particles – high roughness, slower river (more friction) High Velocity = erosion (upstream) Low Velocity = deposition (downstream) Figure 10.7 > Hjulstrom Diagram What do these lines represent? Salt and clay are hard to erode, and typically stay suspended 2) Discharge: amount of flow Q = width x depth -
Terminology and Definitions Associated with Revegetation
TECHNICAL NOTES U.S. DEPARTMENT OF AGRICULTURE NATURAL RESOURCES CONSERVATION SERVICE PLANT MATERIALS - 9 SPOKANE, WASHINGTON FEBRUARY, 2005 TERMINOLOGY AND DEFINITIONS ASSOCIATED WITH REVEGETATION This Technical Note is a compilation of several old Technical Notes. Technical Note #9 is subdivided into the following Sections: Section 9.1 Ecological Definitions Section 9.2 A Technical Glossary of Stream & River Stabilization, Restoration, and Bioengineering Terms Section 9.3 Glossary of Terminology commonly used in Mining & Reclamation Technology SECTION 9.1 Ecological Definitions (S.M. Lambert, 1994; revised/updated M.E. Stannard, 2005) ECOSYSTEM A biological community together with the physical, social and chemical environment with which it interacts. ECOREGIONS Regions that have broad ecological similarities with respect to soil, relief, and dominant vegetation. Ecoregions are less commonly used by NRCS in its day-to-day terminology. NRCS uses Major Land Resource Areas and Conservation Resource Areas. MAJOR LAND RESOURCE AREAS (MLRA) Geographically associated land resource units, usually encompassing several thousand acres. They are characterized by particular patterns of soils, geology, climate, water resources, and land use. A unit may be one continuous area or several separate nearby areas. CONSERVATION RESOURCE AREAS (CRA) A geographical area where resource concerns, problems, or treatment needs are similar. It is considered a subdivision of an existing Major Land Resource Area (MLRA) map delineation or polygon. Landscape conditions, soil, climate, human considerations, and other natural resource information are used to determine the geographic boundaries of a Common Resource Area. USDA NRCS OCTOBER 2005 ECOTYPE The individuals of a species that are adapted to a particular environment BIOTYPE Synonymous with Ecotype INTRODUCED SPECIES Does not naturally occur in an area defined by soil, relief, and climate.