2004 Edition Twenty Years of Reef Building in New Jersey
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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. -
Physical Geography of Southeast Asia
Physical Geography of Southeast Asia Creating an Annotated Sketch Map of Southeast Asia By Michelle Crane Teacher Consultant for the Texas Alliance for Geographic Education Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 Guiding Question (5 min.) . What processes are responsible for the creation and distribution of the landforms and climates found in Southeast Asia? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 2 Draw a sketch map (10 min.) . This should be a general sketch . do not try to make your map exactly match the book. Just draw the outline of the region . do not add any features at this time. Use a regular pencil first, so you can erase. Once you are done, trace over it with a black colored pencil. Leave a 1” border around your page. Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 3 Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 4 Looking at your outline map, what two landforms do you see that seem to dominate this region? Predict how these two landforms would affect the people who live in this region? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 5 Peninsulas & Islands . Mainland SE Asia consists of . Insular SE Asia consists of two large peninsulas thousands of islands . Malay Peninsula . Label these islands in black: . Indochina Peninsula . Sumatra . Label these peninsulas in . Java brown . Sulawesi (Celebes) . Borneo (Kalimantan) . Luzon Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 6 Draw a line on your map to indicate the division between insular and mainland SE Asia. -
Morphologic Characteristics of the Blow River Delta, Yukon Territory, Canada
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1969 Morphologic Characteristics of the Blow River Delta, Yukon Territory, Canada. James Murl Mccloy Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Mccloy, James Murl, "Morphologic Characteristics of the Blow River Delta, Yukon Territory, Canada." (1969). LSU Historical Dissertations and Theses. 1605. https://digitalcommons.lsu.edu/gradschool_disstheses/1605 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. This dissertation has been microfilmed exactly as received 70-252 McCLOY, James Murl, 1934- MORPHOLOGIC CHARACTERISTICS OF THE BLOW RIVER DELTA, YUKON TERRITORY, CANADA. The Louisiana State University and Agricultural and Mechanical College, Ph.D., 1969 Geography University Microfilms, Inc., Ann Arbor, Michigan Morphologic Characteristics of the Blow River Belta, Yukon Territory, Canada A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography and Anthropology by James Murl McCloy B.A., State College at Los Angeles, 1961 May, 1969 ACKNOWLEDGEMENTS Research culminating in this dissertation was conducted under the auspices of the Arctic Institute of North America. The major portion of the financial support was received from the United States Army under contract no. BA-ARO-D-3I-I2I4.-G832, "Arctic Environmental Studies." Additional financial assistance during part of the writing stage was received in the form of a research assistantship from the Coastal Studies Institute, Louisi ana State University. -
Coastal Wetland Trends in the Narragansett Bay Estuary During the 20Th Century
u.s. Fish and Wildlife Service Co l\Ietland Trends In the Narragansett Bay Estuary During the 20th Century Coastal Wetland Trends in the Narragansett Bay Estuary During the 20th Century November 2004 A National Wetlands Inventory Cooperative Interagency Report Coastal Wetland Trends in the Narragansett Bay Estuary During the 20th Century Ralph W. Tiner1, Irene J. Huber2, Todd Nuerminger2, and Aimée L. Mandeville3 1U.S. Fish & Wildlife Service National Wetlands Inventory Program Northeast Region 300 Westgate Center Drive Hadley, MA 01035 2Natural Resources Assessment Group Department of Plant and Soil Sciences University of Massachusetts Stockbridge Hall Amherst, MA 01003 3Department of Natural Resources Science Environmental Data Center University of Rhode Island 1 Greenhouse Road, Room 105 Kingston, RI 02881 November 2004 National Wetlands Inventory Cooperative Interagency Report between U.S. Fish & Wildlife Service, University of Massachusetts-Amherst, University of Rhode Island, and Rhode Island Department of Environmental Management This report should be cited as: Tiner, R.W., I.J. Huber, T. Nuerminger, and A.L. Mandeville. 2004. Coastal Wetland Trends in the Narragansett Bay Estuary During the 20th Century. U.S. Fish and Wildlife Service, Northeast Region, Hadley, MA. In cooperation with the University of Massachusetts-Amherst and the University of Rhode Island. National Wetlands Inventory Cooperative Interagency Report. 37 pp. plus appendices. Table of Contents Page Introduction 1 Study Area 1 Methods 5 Data Compilation 5 Geospatial Database Construction and GIS Analysis 8 Results 9 Baywide 1996 Status 9 Coastal Wetlands and Waters 9 500-foot Buffer Zone 9 Baywide Trends 1951/2 to 1996 15 Coastal Wetland Trends 15 500-foot Buffer Zone Around Coastal Wetlands 15 Trends for Pilot Study Areas 25 Conclusions 35 Acknowledgments 36 References 37 Appendices A. -
New York State Artificial Reef Plan and Generic Environmental Impact
TABLE OF CONTENTS EXECUTIVE SUMMARY ...................... vi 1. INTRODUCTION .......................1 2. MANAGEMENT ENVIRONMENT ..................4 2.1. HISTORICAL PERSPECTIVE. ..............4 2.2. LOCATION. .....................7 2.3. NATURAL RESOURCES. .................7 2.3.1 Physical Characteristics. ..........7 2.3.2 Living Resources. ............. 11 2.4. HUMAN RESOURCES. ................. 14 2.4.1 Fisheries. ................. 14 2.4.2 Archaeological Resources. ......... 17 2.4.3 Sand and Gravel Mining. .......... 18 2.4.4 Marine Disposal of Waste. ......... 18 2.4.5 Navigation. ................ 18 2.5. ARTIFICIAL REEF RESOURCES. ............ 20 3. GOALS AND OBJECTIVES .................. 26 3.1 GOALS ....................... 26 3.2 OBJECTIVES .................... 26 4. POLICY ......................... 28 4.1 PROGRAM ADMINISTRATION .............. 28 4.1.1 Permits. .................. 29 4.1.2 Materials Donations and Acquisitions. ... 31 4.1.3 Citizen Participation. ........... 33 4.1.4 Liability. ................. 35 4.1.5 Intra/Interagency Coordination. ...... 36 4.1.6 Program Costs and Funding. ......... 38 4.1.7 Research. ................. 40 4.2 DEVELOPMENT GUIDELINES .............. 44 4.2.1 Siting. .................. 44 4.2.2 Materials. ................. 55 4.2.3 Design. .................. 63 4.3 MANAGEMENT .................... 70 4.3.1 Monitoring. ................ 70 4.3.2 Maintenance. ................ 72 4.3.3 Reefs in the Exclusive Economic Zone. ... 74 4.3.4 Special Management Concerns. ........ 76 4.3.41 Estuarine reefs. ........... 76 4.3.42 Mitigation. ............. 77 4.3.43 Fish aggregating devices. ...... 80 i 4.3.44 User group conflicts. ........ 82 4.3.45 Illegal and destructive practices. .. 85 4.4 PLAN REVIEW .................... 88 5. ACTIONS ........................ 89 5.1 ADMINISTRATION .................. 89 5.2 RESEARCH ..................... 89 5.3 DEVELOPMENT .................... 91 5.4 MANAGEMENT .................... 96 6. ENVIRONMENTAL IMPACTS ................. 97 6.1 ECOSYSTEM IMPACTS. -
Richard Sullivan, President
Participating Organizations Alliance for a Living Ocean American Littoral Society Arthur Kill Coalition Clean Ocean Action www.CleanOceanAction.org Asbury Park Fishing Club Bayberry Garden Club Bayshore Regional Watershed Council Bayshore Saltwater Flyrodders Belford Seafood Co-op Main Office Institute of Coastal Education Belmar Fishing Club Beneath The Sea 18 Hartshorne Drive 3419 Pacific Avenue Bergen Save the Watershed Action Network P.O. Box 505, Sandy Hook P.O. Box 1098 Berkeley Shores Homeowners Civic Association Wildwood, NJ 08260-7098 Cape May Environmental Commission Highlands, NJ 07732-0505 Central Jersey Anglers Voice: 732-872-0111 Voice: 609-729-9262 Citizens Conservation Council of Ocean County Fax: 732-872-8041 Fax: 609-729-1091 Clean Air Campaign, NY Ocean Advocacy [email protected] Coalition Against Toxics [email protected] Coalition for Peace & Justice/Unplug Salem Since 1984 Coast Alliance Coastal Jersey Parrot Head Club Communication Workers of America, Local 1034 Concerned Businesses of COA Concerned Citizens of Bensonhurst Concerned Citizens of COA Concerned Citizens of Montauk Eastern Monmouth Chamber of Commerce Fisher’s Island Conservancy Fisheries Defense Fund May 31, 2006 Fishermen’s Dock Cooperative, Pt. Pleasant Friends of Island Beach State Park Friends of Liberty State Park, NJ Friends of the Boardwalk, NY Garden Club of Englewood Edward Bonner Garden Club of Fair Haven Garden Club of Long Beach Island Garden Club of Middletown US Army Corps of Engineers Garden Club of Morristown -
Understanding the Temporal Dynamics of the Wandering Renous River, New Brunswick, Canada
Earth Surface Processes and Landforms EarthTemporal Surf. dynamicsProcess. Landforms of a wandering 30, 1227–1250 river (2005) 1227 Published online 23 June 2005 in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/esp.1196 Understanding the temporal dynamics of the wandering Renous River, New Brunswick, Canada Leif M. Burge1* and Michel F. Lapointe2 1 Department of Geography and Program in Planning, University of Toronto, 100 St. George Street, Toronto, Ontario, M5S 3G3, Canada 2 Department of Geography McGill University, 805 Sherbrooke Street West, Montreal, Quebec, H3A 2K6, Canada *Correspondence to: L. M. Burge, Abstract Department of Geography and Program in Planning, University Wandering rivers are composed of individual anabranches surrounding semi-permanent of Toronto, 100 St. George St., islands, linked by single channel reaches. Wandering rivers are important because they Toronto, M5S 3G3, Canada. provide habitat complexity for aquatic organisms, including salmonids. An anabranch cycle E-mail: [email protected] model was developed from previous literature and field observations to illustrate how anabranches within the wandering pattern change from single to multiple channels and vice versa over a number of decades. The model was used to investigate the temporal dynamics of a wandering river through historical case studies and channel characteristics from field data. The wandering Renous River, New Brunswick, was mapped from aerial photographs (1945, 1965, 1983 and 1999) to determine river pattern statistics and for historical analysis of case studies. Five case studies consisting of a stable single channel, newly formed anabranches, anabranches gaining stability following creation, stable anabranches, and an abandoning anabranch were investigated in detail. -
Appendix E Fish Habitat Utilization Literature Review
Appendix E Fish Habitat Utilization Literature Review East Kitsap Nearshore Assessment Appendix E Appendix E - Fish Habitat Utilization Literature Review Toft et al. (2007) City Shoreline Fish Distribution Study objective: study the abundance and behavior of juvenile salmon and other fishes among various marine shoreline habitat types near the city of Seattle. Focused on 5 types of shorelines - cobble beach - sand beach - riprap extending into the upper intertidal zone - deep riprap extending into the subtidal - edge of overwater structures Also examined stomach contents of juvenile salmon. Fish sampling methods included enclosure nets and snorkel surveys. Riprap often results in greater beach slopes and steep embankments which effectively reduces the intertidal zone. These characteristics in turn, result in habitat loss for juvenile flatfishes. At high intertidal habitats, more crab were encountered at cobble beaches compared to sand beaches and riprap. Demersal fishes (cottids) were found in greater numbers at riprap. Differences in species density between habitat type were more apparent for demersal fishes than for pelagic species. Densities of salmon were significantly different among habitat types. The highest densities occurred at the edge of overwater structures and in deep riprap. Deep riprap creates some structured habitat which seems to attract surfperches and gunnels. Threespine stickleback, tubesnout, and bay pipefish were also more prevalent at deep riprap than at cobble, sand, and high elevation riprap. Beamer et al. (2006) – Habitat and fish use of pocket estuaries in the Whidbey basin and north Skagit county bays, 2004 and 2005 Pocket estuaries are characterized as having more dilute marine water relative to the surrounding estuary. -
Abandoned Channels (Avulsions)
Musselshell BMPs 1 Abandoned Channels (Avulsions) Applicability The following Best Management Practices (“BMPs”) summarize several recommended approaches to managing abandoned channels within the Musselshell River stream corridor. The information is based upon the on- site evaluation of floodplain features and discussions with producers, and is intended for producers and residents who are living or farming in areas where abandoned channel segments exist. Description Perhaps the most dramatic 2011 flood Figure 1. 2011 avulsion, Musselshell River. impact on the Musselshell River was the number of avulsions that occurred over the period of a few weeks. An “avulsion” is the rapid formation of a new river channel across the floodplain that captures the flow of the main channel thread. River avulsions typically occur when rivers find a relatively steep, short flow path across their floodplain. When floodwaters re- enter the river over a steep bank, they form headcuts that migrate upvalley, creating a new channel, causing intense erosion, and sending a sediment slug downswtream. If the new channel completely develops, it can capture the main thread, resulting in a successful avulsion. If floodwaters recede before the new channel is completely formed, or if the floodplain is resistant to erosion, the avulsion may fail. From near Harlowton to Fort Peck Reservoir, 59 avulsions occurred on the Musselshell in the spring of 2011, abandoning a total of 39 miles of channel. The abandoned channel segments range in length from 280 feet to almost three miles. One of the reasons there were so many avulsions on the Figure 2. Upstream-migrating headcuts showing Musselshell River in 2011 is because the floodwaters stayed creation of avulsion path, 2011. -
The Origin and Paleoclimatic Significance of Carbonate Sand Dunes Deposited on the California Channel Islands During the Last Glacial Period
Pages 3–14 in Damiani, C.C. and D.K. Garcelon (eds.). 2009. Proceedings of 3 the 7th California Islands Symposium. Institute for Wildlife Studies, Arcata, CA. THE ORIGIN AND PALEOCLIMATIC SIGNIFICANCE OF CARBONATE SAND DUNES DEPOSITED ON THE CALIFORNIA CHANNEL ISLANDS DURING THE LAST GLACIAL PERIOD DANIEL R. MUHS,1 GARY SKIPP,1 R. RANDALL SCHUMANN,1 DONALD L. JOHNSON,2 JOHN P. MCGEEHIN,3 JOSSH BEANN,1 JOSHUA FREEMAN,1 TIMOTHY A. PEARCE,4 1 AND ZACHARY MUHS ROWLAND 1U.S. Geological Survey, MS 980, Box 25046, Federal Center, Denver, CO 80225; [email protected] 2Department of Geography, University of Illinois, Urbana, IL 61801 3U.S. Geological Survey, MS 926A, National Center, Reston, VA 20192 4Section of Mollusks, Carnegie Museum of Natural History, 4400 Forbes Ave., Pittsburgh, PA 15213 Abstract—Most coastal sand dunes, including those on mainland California, have a mineralogy dominated by silicates (quartz and feldspar), delivered to beach sources from rivers. However, carbonate minerals (aragonite and calcite) from marine invertebrates dominate dunes on many tropical and subtropical islands. The Channel Islands of California are the northernmost localities in North America where carbonate-rich coastal dunes occur. Unlike the mainland, a lack of major river inputs of silicates to the island shelves and beaches keeps the carbonate mineral content high. The resulting distinctive white dunes are extensive on San Miguel, Santa Rosa, San Nicolas, and San Clemente islands. Beaches have limited extent on all four of these islands at present, and some dunes abut rocky shores with no sand sources at all. Thus, the origin of many of the dunes is related to the lowering of sea level to ~120 m below present during the last glacial period (~25,000 to 10,000 years ago), when broad insular shelves were subaerially exposed. -
Dune Nourishment Fact Sheet
StormSmart Coasts StormSmart Properties Fact Sheet 1: Artificial Dunes and Dune Nourishment The coast is a very dynamic environment and coastal shorelines—especially beaches, dunes, and banks—change constantly in response to wind, waves, tides, and other factors such as seasonal variation, sea level rise, and human alterations to the shoreline system. Consequently, many coastal properties are at risk from storm damage, erosion, and flooding. Inappropriate shoreline stabilization methods can actually do more harm than good by exacerbating beach erosion, damaging neighboring properties, impacting marine habitats, and diminishing the capacity of beaches, dunes, and other natural landforms to protect inland areas from storm damage and flooding. StormSmart Properties—part of the Massachusetts Office of Coastal Zone Management’s (CZM) StormSmart Coasts program—provides coastal property owners with important information on a range of shoreline stabilization techniques that can effectively reduce erosion and storm damage while minimizing impacts to shoreline systems. This information is intended to help property owners work with consultants and other design professionals to select the best option for their circumstances. What Are Artificial Dunes and Dune Nourishment? A dune is a hill, mound, or ridge of sediment that No shoreline stabilization option permanently stops has been deposited by wind or waves landward of all erosion or storm damage. The level of protection a coastal beach. In Massachusetts, the sediments provided depends on the option chosen, project design, that form beaches and dunes range from sand to and site-specific conditions such as the exposure to gravel- and cobble-sized material. An artificial dune storms. All options require maintenance, and many is a shoreline protection option where a new mound also require steps to address adverse impacts to of compatible sediment (i.e., sediment of similar the shoreline system, called mitigation. -
River Channel Bars and Dunes- Theory of Kinematic Waves
River Channel Bars and Dunes- Theory of Kinematic Waves GEOLOGICAL SURVEY PROFESSIONAL PAPER 422-L River Channel Bars and Dunes- Theory of Kinematic Waves By WALTER B. LANGBEIN and LUNA B. LEOPOLD PHYSIOGRAPHIC AND HYDRAULIC STUDIES OF RIVERS GEOLOGICAL SURVEY PROFESSIONAL PAPER 422-L UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 20 cents (paper cover) CONTENTS Page Page Abstract_________________________________________ LI Effect of rock spacing on rock movement in an ephemeral Introduction.______________________________________ 1 stream._________________________________________ L9 Flux-concentration relations________________________ 2 Waves in bed form________________________________ 12 Relation of particle speed to spacing a flume experi- General features________________________________ 12 ment______-_____-____-____-_-____________--____. 4 Kinematic properties_._______-._________________ 15 Transport of sand in pipes and flumes_________________ 5 Gravel bars____________________________________ 17 Flux-concentration curve for pipes________________ 6 Summary__________________________________________ 19 Flume transport of sand_________________________ 7 References________________.______________________ 19 ILLUSTRATIONS Page FIGURE 1. Flux-concentration curve for traffic___________________________________________________-_-_-__-___-