Topic Page: Floodplains
|
|
- Lesley Shields
- 5 years ago
- Views:
Transcription
1 Topic Page: Floodplains Definition: f loodplain from The Penguin English Dictionary a low-lying area beside a river that is composed of sedimentary deposits and is subject to periodic flooding. Summary Article: Floodplain from Encyclopedia of Geography Image from: The setting sun glints off the Amazon River and... in Encyclopedia of Geography channel. A floodplain is one of the ubiquitous fluvial features found along major rivers. It is a wide, flat plain of alluvium on either side of a river extending to the base of a valley that is seasonally inundated. Inundation may originate from overbank flow due to the high amount of rainfall or spillage from dams (see Amazon and White Volta photos). Geomorphologically, actively inundated areas are the composite fringing floodplains of rivers located near the main A floodplain is a complex assemblage of landforms (Figure 1) including channel features such as bars; channel edge features such as banks, benches, knickpoints, and levees; and features such as old channels (oxbow lakes), old levees, back swamps, and crevasse splays. The existence, development, and spatial structure of a floodplain and its features are, in effect, a record of the past history of the river and its current activities. Floodplains have natural qualities that provide sites for agricultural production, urban expansion, industrial location, recreational activities, and conservation of nature and sites of cultural and historic value (see Nile and Mississippi photos). Floodplain Development Along the longitudinal river profile, tectonic interventions contribute to the formation of floodplains, creating different channel densities and patterns that influence hydraulic connections between lotic and lentic water bodies. Tectonic deformation of a river course leads to raised and subsided blocks displaying different hydrologic patterns (see A and B in Figure 2). Uplift blocks develop large and small lakes, whereas subsided blocks display complex anastomosing drainage patterns with a lot of irregular interconnected lakes. Base level and climate changes to some extent influence floodplain development. The base level at the coast or valley mouth controls the upstream extent of horizontal and vertical channel migration, creating a landmass that can contain seasonal overbank flow and sediment deposition. Floodplain development is stabilized if there is a final standstill of the base level. The scientists Wolman and Leopold proposed in 1957 a model of floodplain formation based on geomorphologic reasoning and observation of streams. A floodplain is constructed entirely of horizontal layers of fine-grained sediments interrupted by coarse-grained channel deposit. It is dominated by braids and meanders migrating back and forth over the valley floor, leaving behind a sandy bar deposit.
2 The setting sun glints off the Amazon River and numerous lakes in its floodplain in this astronaut photograph from August 19, Source: NASA. Landsat 7 image showing floodplain of a section of the White Volta River in Ghana Source: Author.
3 Figure 1 Floodplain and its related features Source: Retrieved from Redrawn by J. M. Insaidoo. Satellite image showing land use in the floodplains of the Nile River (A) and the Mississippi River (B) Source: Author. According to Nevidimova, floodplains are formed due to the simultaneous horizontal and vertical displacement of the river channel. A displaced river in a horizontal plane leaves behind a low surface that gets inundated during high waters but changes with time.
4 Types of Floodplains Geomorphologically, two types of floodplains can be distinguished, namely, hydrological flood-plains and topographic floodplains (Figure 3). A hydrological floodplain is the land adjacent to the base flow channel residing below the bankfull elevation, which is inundated once every year. Not every stream has such a floodplain. A topographic floodplain is the land adjacent to the channel, including the hydrologic floodplain and other land up to an elevation base reached by a flood peak of a given frequency. Figure 2 A sketch showing different floodplain water networks in uplifted block (A) and sunken block (B) sectors nodal points (1 and 2) Source: Based on Paira, A. R., & Drago, E. C. (2007). Origin, evolution and types of floodplain water bodies, the middle Parana River: Limnology of a subtropical wetland (pp ). Berlin, Germany: Springer. Redrawn by J. M. Insaidoo.
5 Figure 3 Hydrologic and topographic floodplains. The hydrologic floodplain is defined by bankfull elevation. The topographic floodplain includes the hydrologic floodplain and other lands up to a defined elevation. Source: Federal Interagency Stream Restoration Working Group. (1998, October). Stream corridor restoration: Principles, processes, and practices. Retrieved December 3, 2009, from Figure 4 Event hydrograph of water height in a river for the period from August 29, 2005, to September 5, 2005 Deposit s and Flow Over Floodplains Source: Author. Floodplain dynamics are determined by the amount of sediment deposited during the period of flooding and the amount of material removed during the time between floods. Water flow and sediment transport are complicated and difficult to evaluate due to variability in floodplain width and surface topography. Understanding the flow and deposition of sediments involves theoretical approaches and numerical modeling. These approaches are based on experiments carried out in flumes rather than on field approaches, largely due to the unpredictability and difficulty in collecting samples and making observations during flood events. The sedimentation on floodplains consists of millimeter-thick to decimeter-thick strata sets, produced by discrete overbank flooding events. The grain size and internal structures are difficult to specify as they depend on local flow conditions and sediment availability. Many floodplain deposits have varying quantities of fine to very fine sand, silt, and clay. Floodplain deposits closest to the main channel are comparable with the main channel deposits but decrease in grain size with distance from the main channel. Met hods of Floodplain Delineat ion Several methods have been developed to help delineate floodplains. These methods include remote sensing techniques and modeling within the GIS (geographic information system) platform using applicable algorithms. The hydraulic techniques use backwater modeling, based on losses along floodplain reaches. Backwater modeling uses hydrographs of complete events rather than the peak flow rate. Examples of the model include HEC-RAS, TELEMAC, SOBEK, and LISFLOOD-FP.
6 Information required for these models includes the peak flow rate or event hydrograph (Figure 4), topography, and field data on channel and floodplain characteristics. Uses of Floodplains Floodplain resources provide a wide range of benefits to the surrounding communities. Communities use resources found on floodplains for the improvement of their livelihood, for example, firewood, tree stumps for shelter construction, and wood for fencing. Subsurface-waterlevel fluctuations of floodplains have potential effects on sustenance of stream flows, groundwater recharge, availability of water for livestock, and availability of water for dry-season irrigation. Floodplain use for crop cultivation during the season and off-season exposes the land to environmental hazards, altering its hydrodynamics and affecting the flora and fauna. The increasing use of agro-chemicals has the potential of polluting water bodies, changing the species composition, and entering the food chain. The human occupation of floodplains of major rivers such as the Nile, Mississippi, Ganges, Rhine, and Amazon has led to substantial impacts. Figure 5 Cycle of land use on floodplains of the White Volta River Source: Nyarko, B. K. (2007). Floodplain wetland-river flow synergy in the White Volta river basin, Ghana (Ecological and Development Series No. 53). Bonn, Germany: Hausdruckerei der Universitat Bonn. Qualitative characterization of the observed cycle of land use activities on floodplains (Figure 5) and parameters such as the magnitude, frequency, areal extent, spatial distribution, and predictability of floods within a floodplain help avert land degradation to some extent. See also Coastal Erosion and Deposition, Floods, Rivers Further Readings Anderson, M. G., Walling, D. E., & Bates, P. D. (Eds.). (1994). Floodplain processes. New York: Wiley. Bridge, J. S. (2005). Rivers and floodplains: Forms, processes and sedimentary records. Oxford, UK: Blackwell. Nevidimova, O. Quantitative regularities in floodplain formation. Geophysical Research 11 :, Paira, A. R., & Drago, E. C. (2007).. Origin, evolution, and types of floodplain water bodies. In M. H.
7 Iriondo, J. C. Paggi, & M. J. Parma (Eds.), The Middle Paraná River: Limnology of a subtropical wetland (pp ). Berlin, Germany: Springer. Nyarko, Benjamin Kofi APA Chicago Harvard MLA Nyarko, B. K., & Nyarko. (2010). Floodplain. In B. Warf (Ed.), Encyclopedia of geography. Thousand Oaks, CA: Sage Publications. Retrieved from Copyright 2010 by SAGE Publications, Inc. Copyright 2010 by SAGE Publications, Inc.
8 APA Nyarko, B. K., & Nyarko. (2010). Floodplain. In B. Warf (Ed.), Encyclopedia of geography. Thousand Oaks, CA: Sage Publications. Retrieved from Chicago Nyarko, Benjamin Kofi, and Nyarko. "Floodplain." In Encyclopedia of Geography, edited by Barney Warf. Sage Publications, Harvard Nyarko, B.K. and Nyarko. (2010). Floodplain. In B. Warf (Ed.), Encyclopedia of geography. [Online]. Thousand Oaks: Sage Publications. Available from: [Accessed 19 August 2018]. MLA Nyarko, Benjamin Kofi, and Nyarko. "Floodplain." Encyclopedia of Geography, edited by Barney Warf, Sage Publications, 1st edition, Credo Reference,. Accessed 19 Aug
Opportunities to Improve Ecological Functions of Floodplains and Reduce Flood Risk along Major Rivers in the Puget Sound Basin
Opportunities to Improve Ecological Functions of Floodplains and Reduce Flood Risk along Major Rivers in the Puget Sound Basin Christopher Konrad, US Geological Survey Tim Beechie, NOAA Fisheries Managing
More information3/3/2013. The hydro cycle water returns from the sea. All "toilet to tap." Introduction to Environmental Geology, 5e
Introduction to Environmental Geology, 5e Running Water: summary in haiku form Edward A. Keller Chapter 9 Rivers and Flooding Lecture Presentation prepared by X. Mara Chen, Salisbury University The hydro
More informationFigure 1. Which part of the river is labelled in Figure 1? a) Mouth b) Source c) Lower course d) channel
Rivers 1. Study Figure 1 showing the long profile of a river Figure 1 A Which part of the river is labelled in Figure 1? a) Mouth b) Source c) Lower course d) channel (1 mark) 2. Complete the sentences
More informationGEOL 1121 Earth Processes and Environments
GEOL 1121 Earth Processes and Environments Wondwosen Seyoum Department of Geology University of Georgia e-mail: seyoum@uga.edu G/G Bldg., Rm. No. 122 Seyoum, 2015 Chapter 6 Streams and Flooding Seyoum,
More information4.17 Spain. Catalonia
4.17 Spain Catalonia In Spain, inundation studies are the responsibility of the respective Hydrographic Confederations of each river basin (River Basin Authorities). The actual status of inundation studies
More informationGLG362/GLG598 Geomorphology K. Whipple October, 2009 I. Characteristics of Alluvial Channels
I. Characteristics of Alluvial Channels Self-formed morphology set by entrainment, transport, and deposition They move unconsolidated sedimentary materials present in the valley fill flood plain/bank flow
More informationEarth Science Chapter 6 Section 2 Review
Name: Class: Date: Earth Science Chapter 6 Section Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Most streams carry the largest part of their
More informationStream Geomorphology. Leslie A. Morrissey UVM July 25, 2012
Stream Geomorphology Leslie A. Morrissey UVM July 25, 2012 What Functions do Healthy Streams Provide? Flood mitigation Water supply Water quality Sediment storage and transport Habitat Recreation Transportation
More informationEnvironmental Geology Chapter 9 Rivers and Flooding
Environmental Geology Chapter 9 Rivers and Flooding Flooding in Pakistan 2010-1600 killed/20000 affected The hydrologic cycle is powered by the Sun The cycle includes evaporation, precipitation, infiltration,
More informationPHYSICAL GEOGRAPHY. By Brett Lucas
PHYSICAL GEOGRAPHY By Brett Lucas FLUVIAL PROCESSES Fluvial Processes The Impact of Fluvial Processes on the Landscape Streams and Stream Systems Stream Channels Structural Relationships The Shaping and
More informationWhy Geomorphology for Fish Passage
Channel Morphology - Stream Crossing Interactions An Overview Michael Love Michael Love & Associates mlove@h2odesigns.com (707) 476-8938 Why Geomorphology for Fish Passage 1. Understand the Scale of the
More information3.3 CLIMATE, GEOLOGY, TOPOGRAPHY, AND SOILS CLIMATE GEOLOGY TOPOGRAPHY
3.3 CLIMATE, GEOLOGY, TOPOGRAPHY, AND SOILS This section describes the climate, geology, topography, and soil resource characteristics of the Yolo Bypass Wildlife Area (Wildlife Area). Agricultural soil
More informationES 105 Surface Processes I. Hydrologic cycle A. Distribution % in oceans 2. >3% surface water a. +99% surface water in glaciers b.
ES 105 Surface Processes I. Hydrologic cycle A. Distribution 1. +97% in oceans 2. >3% surface water a. +99% surface water in glaciers b. >1/3% liquid, fresh water in streams and lakes~1/10,000 of water
More informationWatershed concepts for community environmental planning
Purpose and Objectives Watershed concepts for community environmental planning Dale Bruns, Wilkes University USDA Rural GIS Consortium May 2007 Provide background on basic concepts in watershed, stream,
More informationTopic 1: Physical Features: Natural topography, Drainage system
Topic 1: Physical Features: Natural topography, Drainage system 1 (a) Study Fig. 1, a physical map of Bangladesh. 2008 (i) Name the two rivers marked A and B. [2] (ii) Name the area marked C. [1] (iii)
More informationNATURAL RIVER. Karima Attia Nile Research Institute
NATURAL RIVER CHARACTERISTICS Karima Attia Nile Research Institute NATURAL RIVER DEFINITION NATURAL RIVER DEFINITION Is natural stream of water that flows in channels with ih more or less defined banks.
More informationWATER ON AND UNDER GROUND. Objectives. The Hydrologic Cycle
WATER ON AND UNDER GROUND Objectives Define and describe the hydrologic cycle. Identify the basic characteristics of streams. Define drainage basin. Describe how floods occur and what factors may make
More informationFLUVIAL LANDFORMS. Floodplains
FLUVIAL LANDFORMS Floodplains fairly flat & continuous surface occupying much of a valley bottom normally underlain by unconsolidated sediments subject to periodic flooding (usually once every year or
More informationIntroduction to the Hydrogeomorphic (HGM) Classification System
Introduction to the Hydrogeomorphic (HGM) Classification System Objectives The Student Will be Able to: Define the 7 HGM Classes List the 3 Parameters That Define HGM Classes List the Major Water Budget
More informationSTREAM SYSTEMS and FLOODS
STREAM SYSTEMS and FLOODS The Hydrologic Cycle Precipitation Evaporation Infiltration Runoff Transpiration Earth s Water and the Hydrologic Cycle The Hydrologic Cycle The Hydrologic Cycle Oceans not filling
More informationPrecipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle. Runoff Transpiration
STREAM SYSTEMS and FLOODS The Hydrologic Cycle Precipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle Runoff Transpiration The Hydrologic Cycle The Hydrologic Cycle Oceans not filling
More informationStreams. Water. Hydrologic Cycle. Geol 104: Streams
Streams Why study streams? Running water is the most important geologic agent in erosion, transportation and deposition of sediments. Water The unique physical and chemical properties of water make it
More informationWhat do you need for a Marathon?
What do you need for a Marathon? Water and a snack? What about just a normal day? 1 flush = 3.5 gallons 1 flush = 3.5 gallons 10 minute shower = 20 gal 1 flush = 3.5 gallons 10 minute shower = 20 gal Jeans
More informationRunning Water Earth - Chapter 16 Stan Hatfield Southwestern Illinois College
Running Water Earth - Chapter 16 Stan Hatfield Southwestern Illinois College Hydrologic Cycle The hydrologic cycle is a summary of the circulation of Earth s water supply. Processes involved in the hydrologic
More informationYear 6. Geography. Revision
Year 6 Geography Revision November 2017 Rivers and World knowledge How the water cycle works and the meaning of the terms evaporation, condensation, precipitation, transpiration, surface run-off, groundwater
More informationRiver Morphology. EAD 511 River management
River Morphology EAD 511 River management Introduction FLUVIAL GEOMORPHOLOGY Webster's New World Dictionary defines fluvial as: of, found in, or produced by a river or rivers. The same reference defines
More informationCAUSES FOR CHANGE IN STREAM-CHANNEL MORPHOLOGY
CAUSES FOR CHANGE IN STREAM-CHANNEL MORPHOLOGY Chad A. Whaley, Department of Earth Sciences, University of South Alabama, MobileAL, 36688. E-MAIL: caw408@jaguar1.usouthal.edu The ultimate goal of this
More informationFluvial Systems Lab Environmental Geology Lab Dr. Johnson
Fluvial Systems Lab Environmental Geology Lab Dr. Johnson *Introductory sections of this lab were adapted from Pidwirny, M. (2006). "Streamflow and Fluvial Processes". Fundamentals of Physical Geography,
More informationFinal Exam. Running Water Erosion and Deposition. Willamette Discharge. Running Water
Final Exam Running Water Erosion and Deposition Earth Science Chapter 5 Pages 120-135 Scheduled for 8 AM, March 21, 2006 Bring A scantron form A calculator Your 3 x 5 paper card of formulas Review questions
More informationFresh Water: Streams, Lakes Groundwater & Wetlands
Fresh Water:, Lakes Groundwater & Wetlands Oct 27 Glaciers and Ice Ages Chp 13 Nov 3 Deserts and Wind and EXAM #3 Slope hydrologic cycle P = precip I = precip intercepted by veg ET = evapotranspiration
More informationHow Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin?
How Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin? Bruce Rhoads Department of Geography University of Illinois at Urbana-Champaign
More informationDiego Burgos. Geology 394. Advisors: Dr. Prestegaard. Phillip Goodling
Sediment Transport into an Urban Tributary Junction Diego Burgos Geology 394 Advisors: Dr. Prestegaard Phillip Goodling 1 Abstract Tributary junctions are an important component of stream morphology and
More informationStreams. Stream Water Flow
CHAPTER 14 OUTLINE Streams: Transport to the Oceans Does not contain complete lecture notes. To be used to help organize lecture notes and home/test studies. Streams Streams are the major geological agents
More informationAppendix D. Sediment Texture and Other Soil Data
5 6 7 8 Appendix D. Sediment Texture and Other Soil Data This appendix describes the sediment texture of the aquifer system in the Restoration Area. The contents of this appendix describe the: Importance
More informationSurface Water and Stream Development
Surface Water and Stream Development Surface Water The moment a raindrop falls to earth it begins its return to the sea. Once water reaches Earth s surface it may evaporate back into the atmosphere, soak
More informationDo you think sediment transport is a concern?
STREAM RESTORATION FRAMEWORK AND SEDIMENT TRANSPORT BASICS Pete Klingeman 1 What is Your Restoration Project Like? k? Do you think sediment transport is a concern? East Fork Lewis River, WA Tidal creek,
More informationM14/3/GEOGR/SP2/ENG/TZ0/XX/Q GEOGRAPHY STANDARD LEVEL PAPER 2. Monday 19 May 2014 (morning) 1 hour 20 minutes INSTRUCTIONS TO CANDIDATES
M14/3/GEOGR/SP2/ENG/TZ0/XX/Q 22145203 GEOGRAPHY STANDARD LEVEL PAPER 2 Monday 19 May 2014 (morning) 1 hour 20 minutes INSTRUCTIONS TO CANDIDATES Do not open this examination paper until instructed to do
More informationAPPENDIX E. GEOMORPHOLOGICAL MONTORING REPORT Prepared by Steve Vrooman, Keystone Restoration Ecology September 2013
APPENDIX E GEOMORPHOLOGICAL MONTORING REPORT Prepared by Steve Vrooman, Keystone Restoration Ecology September 2 Introduction Keystone Restoration Ecology (KRE) conducted geomorphological monitoring in
More informationOBJECTIVES. Fluvial Geomorphology? STREAM CLASSIFICATION & RIVER ASSESSMENT
STREAM CLASSIFICATION & RIVER ASSESSMENT Greg Babbit Graduate Research Assistant Dept. Forestry, Wildlife & Fisheries Seneca Creek, Monongahela National Forest, West Virginia OBJECTIVES Introduce basic
More informationLandscape Development
Landscape Development Slopes Dominate Natural Landscapes Created by the interplay of tectonic and igneous activity and gradation Deformation and uplift Volcanic activity Agents of gradation Mass wasting
More informationAvoiding Geohazards in the Mid-Atlantic Highlands by Using Natural Stream Principles
Avoiding Geohazards in the Mid-Atlantic Highlands by Using Natural Stream Principles J. Steven Kite, WVU Neal Carte, WVDOT Will Harman, Michael Baker Corp. Donald D. Gray, WVU Photo: W. Gillespie North
More informationLab 7: Sedimentary Structures
Name: Lab 7: Sedimentary Structures Sedimentary rocks account for a negligibly small fraction of Earth s mass, yet they are commonly encountered because the processes that form them are ubiquitous in the
More informationGeography Exams. RAG rate The Challenge of Natural Hazards
Geography Exams You will sit three papers, Paper 1 will last 1 hour 30 minutes and will examine your understanding of The Challenge of Natural Hazards, The Living World and Physical Landscapes in the UK.
More information11/12/2014. Running Water. Introduction. Water on Earth. The Hydrologic Cycle. Fluid Flow
Introduction Mercury, Venus, Earth and Mars share a similar history, but Earth is the only terrestrial planet with abundant water! Mercury is too small and hot Venus has a runaway green house effect so
More informationStewards Pooi Kei College TEACHING SCHEDULE ( ) Form: S4 Subject : Geography No. of periods per cycle: 9 Teacher: Mr. Eric Chau Year/Month
Form: S4 Subject : Geography No. of periods per cycle: 9 Teacher: Mr. Eric Chau Year/Month 2009 September October November Topics / Subjects to be covered skills (if any) Remarks Cycle 1 What is tropical
More informationNew GCSE Geography AQA
Learning Checklist Half Term 1 26 th September 3 rd October 10 th October 17 th October 1.1.1 Tectonic Hazards Plate tectonics theory. Global distribution of earthquakes and volcanic eruptions and their
More informationPaper presented in the Annual Meeting of Association of American Geographers, Las Vegas, USA, March 2009 ABSTRACT
Paper presented in the Annual Meeting of Association of American Geographers, Las Vegas, USA, March 2009 ABSTRACT CHANGING GEOMORPHOLOGY OF THE KOSI RIVER SYSTEM IN THE INDIAN SUBCONTINENT Nupur Bose,
More informationDiagnostic Geomorphic Methods for Understanding Future Behavior of Lake Superior Streams What Have We Learned in Two Decades?
Diagnostic Geomorphic Methods for Understanding Future Behavior of Lake Superior Streams What Have We Learned in Two Decades? Faith Fitzpatrick USGS WI Water Science Center, Middleton, WI fafitzpa@usgs.gov
More informationUGRC 144 Science and Technology in Our Lives/Geohazards
UGRC 144 Science and Technology in Our Lives/Geohazards Flood and Flood Hazards Dr. Patrick Asamoah Sakyi Department of Earth Science, UG, Legon College of Education School of Continuing and Distance Education
More informationADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN
ADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN Conor Shea - Hydrologist U.S. Fish and Wildlife Service Conservation Partnerships Program Arcata, CA Learning Objectives Examine
More informationLab 13: Fluvial Processes and Landforms
Name: Lab 13: Fluvial Processes and Landforms Geomorphology is the study of Earth s surface and of the processes acting to shape it. Streams, for example, are significant continental land-shaping agents.
More informationFUTURE MEANDER BEND MIGRATION AND FLOODPLAIN DEVELOPMENT PATTERNS NEAR RIVER MILES 241 TO 235, SACRAMENTO RIVER
FUTURE MEANDER BEND MIGRATION AND FLOODPLAIN DEVELOPMENT PATTERNS NEAR RIVER MILES 241 TO 235, SACRAMENTO RIVER Eric W. Larsen University of California, Davis With the assistance of Evan Girvetz REPORT
More informationLecture Outlines PowerPoint. Chapter 5 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 5 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
More informationVermont Stream Geomorphic Assessment. Appendix E. River Corridor Delineation Process. VT Agency of Natural Resources. April, E0 - April, 2004
Vermont Stream Geomorphic Assessment Appendix E River Corridor Delineation Process Vermont Agency of Natural Resources - E0 - River Corridor Delineation Process Purpose A stream and river corridor delineation
More informationTechnical Memorandum No Sediment Model
Pajaro River Watershed Study in association with Technical Memorandum No. 1.2.9 Sediment Model Task: Development of Sediment Model To: PRWFPA Staff Working Group Prepared by: Gregory Morris and Elsie Parrilla
More informationLab 12 Coastal Geology
Lab 12 Coastal Geology I. Fluvial Systems Hydrologic Cycle Runoff that flows into rivers = precipitation (rain and snowmelt) [infiltration (loss to groundwater) + evaporation (loss to atmosphere) + transpiration
More informationChapter 10. Running Water aka Rivers. BFRB Pages
Chapter 10 Running Water aka Rivers BFRB Pages 101-116 Stream Erosion and Transportation Running water is all precipitation (rain, snow, etc) that falls on Earth and is pulled downhill by gravity. Running
More informationConceptual Model of Stream Flow Processes for the Russian River Watershed. Chris Farrar
Conceptual Model of Stream Flow Processes for the Russian River Watershed Chris Farrar Several features of creeks affect the interactions between surface and groundwater. This conceptual model uses the
More informationRiparian Assessment. Steps in the right direction... Drainage Basin/Watershed: Start by Thinking Big. Riparian Assessment vs.
Riparian Assessment vs. Monitoring Riparian Assessment What is a healthy stream? Determine stream/riparian health Determine change or trend, especially in response to mgmt Classification = designation
More informationExtra Credit Assignment (Chapters 4, 5, 6, and 10)
GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Extra Credit Assignment (Chapters 4, 5, 6, and 10) For this assignment you will require: a calculator and metric ruler. Chapter 4 Objectives:
More informationDomino Effect of River Training in Large Sand-Bed Braiding Rivers
6 th International Conference on Structural Engineering and Construction Management 2015, Kandy, Sri Lanka, 11 th -13 th December 2015 SECM/15/176 Domino Effect of River Training in Large Sand-Bed Braiding
More informationSediment and nutrient transport and storage along the urban stream corridor
Sediment and nutrient transport and storage along the urban stream corridor Greg Noe, Cliff Hupp, Ed Schenk, Jackie Batson, Nancy Rybicki, Allen Gellis What is the role of floodplains everywhere? Noe 2013,
More informationFlow regime, floodplain inundation and floodplain waterbody connectivity at Congaree National Park
Flow regime, floodplain inundation and floodplain waterbody connectivity at Congaree National Park John Kupfer Dept. of Geography Univ. of South Carolina Kimberly Meitzen Duke University Nature Conservancy
More informationAn analysis on the relationship between land subsidence and floods at the Kujukuri Plain in Chiba Prefecture, Japan
doi:10.5194/piahs-372-163-2015 Author(s) 2015. CC Attribution 3.0 License. An analysis on the relationship between land subsidence and floods at the Kujukuri Plain in Chiba Prefecture, Japan Y. Ito 1,
More informationAquifer an underground zone or layer of sand, gravel, or porous rock that is saturated with water.
Aggradation raising of the streambed by deposition that occurs when the energy of the water flowing through a stream reach is insufficient to transport sediment conveyed from upstream. Alluvium a general
More informationCR AAO Bridge. Dead River Flood & Natural Channel Design. Mitch Koetje Water Resources Division UP District
CR AAO Bridge Dead River Flood & Natural Channel Design Mitch Koetje Water Resources Division UP District Old County Road AAO Bridge Map courtesy of Marquette County Silver Lake Basin McClure Basin
More informationGY 111 Lecture Note Series Sedimentary Environments 2: Rivers and Deltas
GY 111 Lecture Notes D. Haywick (2008-09) 1 GY 111 Lecture Note Series Sedimentary Environments 2: Rivers and Deltas Lecture Goals A) Rivers and Deltas (types) B) Water Flow and sedimentation in river/deltas
More informationLecture 19: Fluvial Facies
GEOL 440 Sedimentology and stratigraphy: processes, environments and deposits Lecture 19: Fluvial Facies Aims Examine controls on alluvial channel pattern List the types of channel pattern Examine meandering
More informationLaboratory Exercise #3 The Hydrologic Cycle and Running Water Processes
Laboratory Exercise #3 The Hydrologic Cycle and Running Water Processes page - 1 Section A - The Hydrologic Cycle Figure 1 illustrates the hydrologic cycle which quantifies how water is cycled throughout
More informationFOREST RESEARCH INSTITUTE, DEHRADUN
PROJECT REPORT DRAINAGE AND REPLENISHMENT STUDY OF MINED AREA OF GANGA SHYAMPUR RIVER HARIDWAR Submitted to UTTARAKHAND FOREST DEVELOPMENT CORPORATION (UFDC) 73, Nehru Road, Deharadun Prepared&Submitted
More informationUpper Drac River restoration project
Upper Drac River restoration project Restoration of a braided river bed incised in clay substratum through sediment reloading and bed widening SHF Conference, Nantes, 6 & 7 october 2014 Small scale morphological
More informationRivers T. Perron
1 Rivers T. Perron 12.001 After our discussions of large-scale topography, how we represent topography in maps, and how topography interacts with geologic structures, you should be frothing at the mouth
More informationA MULTI-CRITERIA APPROACH SUPPORTING THE INVESTIGATION OF A FLOODPLAIN POTENTIALLY CONTAMINATED BY PESTICIDES
A MULTI-CRITERIA APPROACH SUPPORTING THE INVESTIGATION OF A FLOODPLAIN POTENTIALLY CONTAMINATED BY PESTICIDES L ZILIANI, B GROPPELLI, S CECCON, F COLOMBO (RAMBOLL ENVIRON) D BOCCHIOLA, M C RULLI, G RAVAZZANI,
More informationInfluence of the Major Drainages to the Mississippi River and Implications for System Level Management
Influence of the Major Drainages to the Mississippi River and Implications for System Level Management Brian M. Vosburg Geologist Louisiana Coastal Protection and Restoration Authority brian.vosburg@la.gov
More informationTerm Knowledge Using and applying Grade Criteria Autumn 1 Assessment window October Natural hazards pose major risks to people and property.
Assessment Schedule Year 9 2015/6 Term Knowledge Using and applying Grade Criteria Autumn 1 Assessment window October 2015 3.1.1.2 Tectonic Natural hazards pose major risks to people and property. Definition
More informationCaspian Rapid Sea Level Changing Impact on Estuaries Morphodynamic Deformation
2013, TextRoad Publication ISSN 2090-4304 Journal of Basic and Applied Scientific Research www.textroad.com Caspian Rapid Sea Level Changing Impact on Estuaries Morphodynamic Deformation Naser Ebadati
More informationMISSISSIPPI RIVER DELTA OVERVIEW
MISSISSIPPI RIVER DELTA OVERVIEW Science and Engineering Special Team Conference Louisiana State University October 9, 2012 Introduction Basics of the Mississippi Delta Natural and Human-Induced Land Loss
More informationErosion and Deposition
CHAPTER 3 LESSON 2 Erosion and Deposition Landforms Shaped by Water and Wind Key Concepts What are the stages of stream development? How do water erosion and deposition change Earth s surface? How do wind
More informationWhat landforms make up Australia?!
What landforms make up Australia? The tectonic forces of folding, faulting and volcanic activity have created many of Australia's major landforms. Other forces that work on the surface of Australia, and
More informationRIVERS, GROUNDWATER, AND GLACIERS
RIVERS, GROUNDWATER, AND GLACIERS Delta A fan-shaped deposit that forms when a river flows into a quiet or large body of water, such as a lake, an ocean, or an inland sea. Alluvial Fan A sloping triangle
More informationEvaluation of Meandering Characteristics Using RS & GIS of Manu River
Journal of Water Resource and Protection, 2012, 4, 163-171 doi:10.4236/jwarp.2012.43019 Published Online March 2012 (http://www.scirp.org/journal/jwarp) Evaluation of Meandering Characteristics Using RS
More informationWhy Stabilizing the Stream As-Is is Not Enough
Why Stabilizing the Stream As-Is is Not Enough Several examples of alternatives to the County s design approach have been suggested. A common theme of these proposals is a less comprehensive effort focusing
More informationOverview of fluvial and geotechnical processes for TMDL assessment
Overview of fluvial and geotechnical processes for TMDL assessment Christian F Lenhart, Assistant Prof, MSU Research Assoc., U of M Biosystems Engineering Fluvial processes in a glaciated landscape Martin
More informationThe last three sections of the main body of this report consist of:
Threatened and Endangered Species Geological Hazards Floodplains Cultural Resources Hazardous Materials A Cost Analysis section that provides comparative conceptual-level costs follows the Environmental
More informationFour Mile Run Levee Corridor Stream Restoration
Four Mile Run Levee Corridor Stream Restoration 30% Design Summary U.S. Army Corps of Engineers, Baltimore District Presentation Outline Four Mile Run 1.) Historic Perspective 2.) Existing Conditions 3.)
More informationSTREAM RESTORATION AWRA Summer Specialty Conference, GIS and Water Resources IX
STREAM RESTORATION 2016 AWRA Summer Specialty Conference, GIS and Water Resources IX Innovative Use of 2D Hydraulic Modeling in Stream Restoration Design Presented by: Li Gao, PE and Robert Scrafford,
More informationUpper Truckee River Restoration Lake Tahoe, California Presented by Brendan Belby Sacramento, California
Upper Truckee River Restoration Lake Tahoe, California Presented by Brendan Belby Sacramento, California Mike Rudd (Project Manager), Charley Miller & Chad Krofta Declines in Tahoe s Water Clarity The
More informationA floodplain is the flat land immediately surrounding a stream channel and innundated at 5mes of high flow.
A floodplain is the flat land immediately surrounding a stream channel and innundated at 5mes of high flow. Aggrada5on occurs when deposi5on is greater than erosion. Aggrada&on of the Rivière des Ha! Ha!
More informationRunning Water: The Geology of Streams and Floods Running Water Chapter 14
Geology 800 Today Running Water: The Geology of Streams and Floods Running Water Chapter 14 Next Class Oceans and Coasts 15 Stream Flow Streams Ribbons of water that flow down channels. Runoff Water in
More informationDefining the Limit of Regulated Areas. C.1 Defining the River or Stream Flood Hazard 138. C.2 Defining the River or Stream Erosion Hazard 139
C.1 Defining the River or Stream Flood Hazard 138 C.2 Defining the River or Stream Erosion Hazard 139 C.3 Defining Watercourses 141 C.4 Defining the Lake Ontario Shoreline Flood, Erosion and Dynamic Beach
More informationWetland & Floodplain Functional Assessments and Mapping To Protect and Restore Riverine Systems in Vermont. Mike Kline and Laura Lapierre Vermont DEC
Wetland & Floodplain Functional Assessments and Mapping To Protect and Restore Riverine Systems in Vermont Mike Kline and Laura Lapierre Vermont DEC NWI+ Hydro-Geomorphic Characterization of Wetlands and
More informationRivers and Landslides
Rivers and Landslides Path of desire or path of least resistance? Desire Path: A term in landscape architecture used to describe a path that isn t designed but rather is worn casually away by people finding
More informationQuick Response Report #126 Hurricane Floyd Flood Mapping Integrating Landsat 7 TM Satellite Imagery and DEM Data
Quick Response Report #126 Hurricane Floyd Flood Mapping Integrating Landsat 7 TM Satellite Imagery and DEM Data Jeffrey D. Colby Yong Wang Karen Mulcahy Department of Geography East Carolina University
More informationHydrologic Analysis for Ecosystem Restoration
Hydrologic Analysis for Ecosystem Restoration Davis, California Objectives: To provide participants with: 1) an understanding of the issues in restoration studies; 2) an overview of Corps policies and
More informationGeomorphology Geology 450/750 Spring Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26
Geomorphology Geology 450/750 Spring 2004 Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26 This exercise is intended to give you experience using field data you collected
More informationmountain rivers fixed channel boundaries (bedrock banks and bed) high transport capacity low storage input output
mountain rivers fixed channel boundaries (bedrock banks and bed) high transport capacity low storage input output strong interaction between streams & hillslopes Sediment Budgets for Mountain Rivers Little
More informationLectures Hydrology & Fluvial Geomorphology. Gauley River Images. Ancients' (= Biblical) Model of Water (Hydrologic) Cycle
Lectures 11-13 13 Hydrology & Fluvial Geomorphology Gauley River Images http://www.youtube.com/watch?v=eulmuyegtz4&feature=related Ancients' (= Biblical) Model of Water (Hydrologic) Cycle Stream Water
More information!"#$%&&'()*+#$%(,-./0*)%(!
8:30 Sign in Hoosic River Revival Coalition!"#$%&&'()*+#$%(,-./0*)%(! 12-#30+4/#"5-(60 9:00 Welcome and Introductions 9:15 Goals for Today s Program: A Description of the Planning Process 9:30 First Session:
More informationIntroduction Fluvial Processes in Small Southeastern Watersheds
Introduction Fluvial Processes in Small Southeastern Watersheds L. Allan James Scott A. Lecce Lisa Davis Southeastern Geographer, Volume 50, Number 4, Winter 2010, pp. 393-396 (Article) Published by The
More informationSection 5. Low-Gradient Streams. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 4 Surface Processes Section 5 Low-Gradient Streams What Do You See? Learning Outcomes In this section, you will Use models and real-time streamflow data to understand the characteristics of lowgradient
More information