Part 614 Stream Visual Assessment Protocol Version 2
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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. -
Flood Hazard of Dunedin's Urban Streams
Flood hazard of Dunedin’s urban streams Review of Dunedin City District Plan: Natural Hazards Otago Regional Council Private Bag 1954, Dunedin 9054 70 Stafford Street, Dunedin 9016 Phone 03 474 0827 Fax 03 479 0015 Freephone 0800 474 082 www.orc.govt.nz © Copyright for this publication is held by the Otago Regional Council. This publication may be reproduced in whole or in part, provided the source is fully and clearly acknowledged. ISBN: 978-0-478-37680-7 Published June 2014 Prepared by: Michael Goldsmith, Manager Natural Hazards Jacob Williams, Natural Hazards Analyst Jean-Luc Payan, Investigations Engineer Hank Stocker (GeoSolve Ltd) Cover image: Lower reaches of the Water of Leith, May 1923 Flood hazard of Dunedin’s urban streams i Contents 1. Introduction ..................................................................................................................... 1 1.1 Overview ............................................................................................................... 1 1.2 Scope .................................................................................................................... 1 2. Describing the flood hazard of Dunedin’s urban streams .................................................. 4 2.1 Characteristics of flood events ............................................................................... 4 2.2 Floodplain mapping ............................................................................................... 4 2.3 Other hazards ...................................................................................................... -
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. -
Drainage Patterns
Drainage Patterns Over time, a stream system achieves a particular drainage pattern to its network of stream channels and tributaries as determined by local geologic factors. Drainage patterns or nets are classified on the basis of their form and texture. Their shape or pattern develops in response to the local topography and Figure 1 Aerial photo illustrating subsurface geology. Drainage channels develop where surface dendritic pattern in Gila County, AZ. runoff is enhanced and earth materials provide the least Courtesy USGS resistance to erosion. The texture is governed by soil infiltration, and the volume of water available in a given period of time to enter the surface. If the soil has only a moderate infiltration capacity and a small amount of precipitation strikes the surface over a given period of time, the water will likely soak in rather than evaporate away. If a large amount of water strikes the surface then more water will evaporate, soaks into the surface, or ponds on level ground. On sloping surfaces this excess water will runoff. Fewer drainage channels will develop where the surface is flat and the soil infiltration is high because the water will soak into the surface. The fewer number of channels, the coarser will be the drainage pattern. Dendritic drainage pattern A dendritic drainage pattern is the most common form and looks like the branching pattern of tree roots. It develops in regions underlain by homogeneous material. That is, the subsurface geology has a similar resistance to weathering so there is no apparent control over the direction the tributaries take. -
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 -
Stream Visual Assessment Protocol (SVAP)
National Water and Climate Center Technical Note 99–1 United States Department of Agriculture Natural Resources Conservation Service Stream Visual Assessment Protocol Issued December 1998 Cover photo: Stream in Clayton County, Iowa, exhibiting an impaired riparian zone. The U. S. Department of Agriculture (USDA) prohibits discrimination in its programs on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Cen- ter at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250-9410 or call (202) 720-5964 (voice or TDD). USDA is an equal opportunity provider and employer. (NWCC Technical Note 99–1, Stream Visual Assessment Protocol, December 1998) Preface This document presents an easy-to-use assessment protocol to evaluate the condition of aquatic ecosystems associated with streams. The protocol does not require expertise in aquatic biology or extensive training. Least-im- pacted reference sites are used to provide a standard of comparison. The use of reference sites is variable depending on how the state chooses to implement the protocol. The state may modify the protocol based on a system of stream classification and a series of reference sites. Instructions for modifying the protocol are provided in the technical information sec- tion. Aternatively, a user may use reference sites in a less structured man- ner as a point of reference when applying the protocol. -
River Blackwater – Manor Farm
River Blackwater – Manor Farm An advisory visit carried out by the Wild Trout Trust – January 2012 1 1. Introduction This report is the output of a Wild Trout Trust advisory visit undertaken on a reach of the River Blackwater adjacent to Manor Farm near Plaitford in Hampshire. The request for the visit was made by the landowner, Hillary Harper. Comments in this report are based on observations on the day of the site visit and discussions with Ms. Harper and Ms. Penny Scott, the owner of a section of the right (southern) bank. Throughout the report, normal convention is followed with respect to bank identification i.e. banks are designated Left Bank (LB) or Right Bank (RB) whilst looking downstream. 2. Catchment overview The River Blackwater rises just to the east of Red Lynch on the northern fringes of the New Forest. From here it flows south easterly for approximately 16km before joining the River Test at the upstream end of its tidal range. The Test has an international reputation as one of the finest chalk stream fisheries in the world. The Blackwater, by contrast, is not a chalk stream but rises from a network of small surface fed streams and gutters running over mainly tertiary clays and gravels. The Blackwater has long been recognised as a crucially important spawning tributary to the main River Test and is thought to be the destination of choice for the bulk of the migratory sea trout (Salmo trutta) that enter the system. Unlike the River Test, the Blackwater does not enjoy any high level statutory protection as a Site of Special Scientific Interest (SSSI). -
Stream Buffer Regulations
BOONE COUNTY ZONING REGULATIONS, BOONE COUNTY, MISSOURI Adopted: May 1985 Revised: September, 1991, September 30, 2003, November 3, 2004, April 30, 2009 CHAPTER 26 STREAM BUFFER REGULATIONS 26.1 Title, Purpose and Intent 26.1.1 Title. This chapter shall be known as the "Stream Buffer Regulations of Boone County, Missouri." 26.1.2 Purpose. The County Commission of Boone County, Missouri has determined that these regulations are necessary for the purpose of promoting the health, safety, comfort, and/or general welfare; and conserving the values of property throughout the County; and lessening or avoiding undue impact of stormwater runoff on adjoining properties and the environment. Buffers adjacent to stream systems provide numerous environmental protection and resource management benefits which can include the following: • Restoring and maintaining the chemical, physical and biological integrity of the water resources, • Removing pollutants delivered in urban storm water, • Reducing erosion and controlling sedimentation, • Stabilizing stream banks, • Providing infiltration of storm water runoff, • Maintaining the base flow of streams, • Contributing the organic matter that is a source of food and energy for the aquatic ecosystem, • Providing tree canopy to shade streams and promote desirable aquatic organisms, • Providing riparian wildlife habitat, • Furnishing scenic value and recreational opportunity, • Protecting the public from flooding, property damage and loss, and • Providing sustainable, natural vegetation. 26.1.3 Intent. It is the purpose of this section to establish minimum acceptable standards for the design of stream buffers to protect the streams, wetlands, floodplains and riparian and aquatic ecosystems of the County of Boone, and the implementation of specifications for the establishment, protection and maintenance of vegetation along all stream systems and/or waterbodies within our County's authority . -
Key to the Larval Stages of Aquatic True Flies (Diptera), Based on the Operational Taxa List for Running Waters in Germany
Ann. Limnol. - Int. J. Lim. 2007, 43 (1), 61-74 Key to the larval stages of aquatic true flies (Diptera), based on the operational taxa list for running waters in Germany A. Sundermann1*, S. Lohse1, L.A. Beck2, P. Haase1 1 Senckenberg Research Institute and Natural History Museum, Department of Limnology and Conservation, Clamecystrasse 12, D-63571 Gelnhausen, Germany 2 Philipps-University Marburg, Department of Biology, Zoology, Marburg, Germany The aquatic larvae of the Diptera are often the most abundant and most diverse group of the benthic macroinvertebrate fauna. They are able to survive in and colonise practically all freshwater habitats, and some species can tolerate harsh environmental conditions. They are therefore both a qualitatively and quantitatively important group of biological indicators for assessing fresh- water systems. On the other hand their determination at the species level is very difficult. This is in part due to a lack of taxo- nomic work in the group, but also the absence of comprehensive determination keys, that meet the needs of water managers. As a result, the aquatic larvae of the Diptera often play a subordinate role in water management. In light of the EU Water Framework Directive the present work is a first step in improving the integration of the important group of the Diptera in water management practice: a comprehensive determination key, which is geared at water managers. The key includes 60 taxa, largely at the family and genus level. In contrast to already existing keys the present work tries to differentiate the taxa on the basis of simple and user-friendly characters. -
Stream Erosion and Deposition
Stream Features Regents Earth Science With Ms. Connery LAB 3 - How long is a Day? making time calculations! SUNRISE SUNSET W 10/29 06 :33 17:02 Seasons Greetings! ESRT - What are the major streams of NYS and which way do they flow?? Let’s draw a conceptual model Why are there streams? • Runoff surface water • Infiltration groundwater • Streams are a combination of both What factors determine whether water infiltrates or runs off the land surface to form a stream? Characteristic HIGH LOW HIGH LOW INFILTRATION INFILTRATION RUN-OFF RUN-OFF GROUNDCOVER • VEGETATED X X • PAVED X X SLOPE of the LAND (water speed) • STEEP SLOPE X X • GENTLE SLOPE X X SOIL PERMEABILITY • HIGH PERMEABILITY X X • LOW PERMEABILITY X X SOIL SATURATION • SATURATED or VERY DRY X X • MODERATE SATURATION X X Key points… What are some key erosional and depositional features of running water? Where do we find different size sediments in a stream? What are the ages of a stream and their characteristics? In the stream speed lab you mostly thought about water levels causing different speeds (like during floods & droughts) but there are other reasons for speed change and erosion and deposition! Cut bank (erosion) and point bar (deposition) Point Bar If the speeds are different, what does the stream channel look like on straight-aways and curves? What does the channel, erosion, and deposition look like on a major river? Using the stream table, you should be able to describe headwaters (source) undercutting tributary sediment sorting by channel water speed flood plain -
Nomenclatural Studies Toward a World List of Diptera Genus-Group Names
Nomenclatural studies toward a world list of Diptera genus-group names. Part V Pierre-Justin-Marie Macquart Evenhuis, Neal L.; Pape, Thomas; Pont, Adrian C. DOI: 10.11646/zootaxa.4172.1.1 Publication date: 2016 Document version Publisher's PDF, also known as Version of record Document license: CC BY Citation for published version (APA): Evenhuis, N. L., Pape, T., & Pont, A. C. (2016). Nomenclatural studies toward a world list of Diptera genus- group names. Part V: Pierre-Justin-Marie Macquart. Magnolia Press. Zootaxa Vol. 4172 No. 1 https://doi.org/10.11646/zootaxa.4172.1.1 Download date: 28. sep.. 2021 Zootaxa 4172 (1): 001–211 ISSN 1175-5326 (print edition) http://www.mapress.com/j/zt/ Monograph ZOOTAXA Copyright © 2016 Magnolia Press ISSN 1175-5334 (online edition) http://doi.org/10.11646/zootaxa.4172.1.1 http://zoobank.org/urn:lsid:zoobank.org:pub:22128906-32FA-4A80-85D6-10F114E81A7B ZOOTAXA 4172 Nomenclatural Studies Toward a World List of Diptera Genus-Group Names. Part V: Pierre-Justin-Marie Macquart NEAL L. EVENHUIS1, THOMAS PAPE2 & ADRIAN C. PONT3 1 J. Linsley Gressitt Center for Entomological Research, Bishop Museum, 1525 Bernice Street, Honolulu, Hawaii 96817-2704, USA. E-mail: [email protected] 2 Natural History Museum of Denmark, Universitetsparken 15, 2100 Copenhagen, Denmark. E-mail: [email protected] 3Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, UK. E-mail: [email protected] Magnolia Press Auckland, New Zealand Accepted by D. Whitmore: 15 Aug. 2016; published: 30 Sept. 2016 Licensed under a Creative Commons Attribution License http://creativecommons.org/licenses/by/3.0 NEAL L. -
Appendix 5: Fauna Known to Occur on Fort Drum
Appendix 5: Fauna Known to Occur on Fort Drum LIST OF FAUNA KNOWN TO OCCUR ON FORT DRUM as of January 2017. Federally listed species are noted with FT (Federal Threatened) and FE (Federal Endangered); state listed species are noted with SSC (Species of Special Concern), ST (State Threatened, and SE (State Endangered); introduced species are noted with I (Introduced). INSECT SPECIES Except where otherwise noted all insect and invertebrate taxonomy based on (1) Arnett, R.H. 2000. American Insects: A Handbook of the Insects of North America North of Mexico, 2nd edition, CRC Press, 1024 pp; (2) Marshall, S.A. 2013. Insects: Their Natural History and Diversity, Firefly Books, Buffalo, NY, 732 pp.; (3) Bugguide.net, 2003-2017, http://www.bugguide.net/node/view/15740, Iowa State University. ORDER EPHEMEROPTERA--Mayflies Taxonomy based on (1) Peckarsky, B.L., P.R. Fraissinet, M.A. Penton, and D.J. Conklin Jr. 1990. Freshwater Macroinvertebrates of Northeastern North America. Cornell University Press. 456 pp; (2) Merritt, R.W., K.W. Cummins, and M.B. Berg 2008. An Introduction to the Aquatic Insects of North America, 4th Edition. Kendall Hunt Publishing. 1158 pp. FAMILY LEPTOPHLEBIIDAE—Pronggillled Mayflies FAMILY BAETIDAE—Small Minnow Mayflies Habrophleboides sp. Acentrella sp. Habrophlebia sp. Acerpenna sp. Leptophlebia sp. Baetis sp. Paraleptophlebia sp. Callibaetis sp. Centroptilum sp. FAMILY CAENIDAE—Small Squaregilled Mayflies Diphetor sp. Brachycercus sp. Heterocloeon sp. Caenis sp. Paracloeodes sp. Plauditus sp. FAMILY EPHEMERELLIDAE—Spiny Crawler Procloeon sp. Mayflies Pseudocentroptiloides sp. Caurinella sp. Pseudocloeon sp. Drunela sp. Ephemerella sp. FAMILY METRETOPODIDAE—Cleftfooted Minnow Eurylophella sp. Mayflies Serratella sp.