GEOGRAPHY Grade 12 GEOMORPHOLOGY 03 JULY 2014
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The Upper James River
Waterproof The Upper James River The James River originates at the only class I or II rapids making it ideal will need to plan a river trip. This guide A Paddle Guide to the Upper confluence of the Jackson and Cowpasture for canoe or kayak trips at normal water includes locations of boat landings, rivers in Botetourt County and forms levels. The white water section below campsites, major rapids, and unique Virginia’s longest and most famous river. Glasgow includes a class III section for historic points of interests along the way. The upper section of the James River those interested in more technical water. This is a great resource for planning day is very scenic with stunning Blue Ridge trips as well as multi-day canoe camping mountain views. Dam releases on the This paddle guide covers the upper 64 expeditions. Jackson River flow releases ensure the miles section from the start of the James upper James River is typically run able river to the Cushaw Dam, just below all season. The first 60 miles contain Snowden. It includes everything a paddler Using This Map George Washington and Rapids (See River Safety panel for class system) Jefferson National Forrest* 30 Mile markers— numbered from start of the James Park* River counting down stream Landmark These maps have been orientated so that the river always flows from the bottom of the map to the top of the map. This allows paddlers to easily orient themselves in the river in terms of river right and left while paddling downstream. Bridge 1km Distance gauge 0 1mi North indicator Canal Boat launch Small boat launch Commercial campground River flow River Informal camping Appalachian Trail Hiking Trail *All land along river bank is private property unless noted otherwise. -
Developing a Form-Process Framework to Describe the Functioning of Semi-Arid Alluvial Fans in the Baviaanskloof Valley, South Africa
DEVELOPING A FORM-PROCESS FRAMEWORK TO DESCRIBE THE FUNCTIONING OF SEMI-ARID ALLUVIAL FANS IN THE BAVIAANSKLOOF VALLEY, SOUTH AFRICA A thesis submitted in the fulfilment of the requirements of the degree of MASTERS OF SCIENCE of RHODES UNIVERSITY By KERRY LEIGH BOBBINS December 2011 i Abstract The Baviaanskloof catchment is a semi - arid catchment located in the Cape Fold Mountains of South Africa. Little is known about the functioning of the complicated Baviaanskloof fluvial system, in particular the role of alluvial fans. This thesis will contribute to field of geomorphology and, more specifically, the field of fan morphometry, by producing a standalone fan framework outlining methods to investigate the influence of fan external and internal control variables. In this thesis, the framework is applied in the Baviaanskloof Valley alongside a case study and used to develop fan restoration guidelines. The framework incorporates external and internal fan control variables at a valley-wide and local fan scale. External control variables include accommodation space, base-level change, and drainage basin inputs. Internal control variables include fan style, morphometry and fan channels. The application of the framework required the creation of a spatial plan of fans and basins in the valley to measure morphometry data. Outcomes of the applied framework include; an understanding of base-level change on fans, relationships between fan basin characteristics and the fan surface and insight into fan channel processes. Results of the applied framework are investigated further using bivariate (correlation matrix) and multivariate (principle component analysis and regression analysis) analysis techniques. Significant relationships identified are: drainage basin area versus fan area, fan area and fan slope and drainage basin ruggedness and basin size. -
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. -
An On-Line River Categorisation Tool
UNDERSTAND YOUR RIVER – AN ON-LINE RIVER ATEGORISATION OOL C T Figure 2. The successful River Restoration workshop that JBA ran in May 2012 brought to sharp relief that there is a vast gap in data, information and material availability relating to our understanding of River types natural processes in rivers and on floodplains. This means that many attempts at river restoration and naturalisation remain based around a limited overall understanding utilising a narrow set of Step-pool Description approaches developed largely for un-reactive low gradient heavily modified river channels. Step-pool river reaches are often composed of large boulder groups, forming steps separated by pools. The pools contain finer sediment. The channel is JBA are developing a website detailing the findings of the workshop and providing information and often stable and the channel gradient is steep. Typical features guidance on the character and functioning of rivers in the UK synthesised from academic research Typical features found in this river system include step-pools and rapids. Flow regime (Figure 1) and field experience (Figure 2). Common flow types include chutes and turbulent flow interspersed with pools. Figure 1. Braided Description Braided river reaches are rare in the UK. They occur in areas of high gradients with high bedload. The channel is characterised by a number of threads, which can be highly dynamic particularly during larger floods. Typical features Typical features found in this river system include rapids, riffles, pools and cut-off channels. Flow regime Common flow types include chutes. Rapid Wandering Description A wandering channel type has the characteristics of a braided and active single-thread system , with a smaller bed material size, a shallower slope and wider valley floor. -
Drainage Basin Morphology in the Central Coast Range of Oregon
AN ABSTRACT OF THE THESIS OF WENDY ADAMS NIEM for the degree of MASTER OF SCIENCE in GEOGRAPHY presented on July 21, 1976 Title: DRAINAGE BASIN MORPHOLOGY IN THE CENTRAL COAST RANGE OF OREGON Abstract approved: Redacted for privacy Dr. James F. Lahey / The four major streams of the central Coast Range of Oregon are: the westward-flowing Siletz and Yaquina Rivers and the eastward-flowing Luckiamute and Marys Rivers. These fifth- and sixth-order streams conform to the laws of drain- age composition of R. E. Horton. The drainage densities and texture ratios calculated for these streams indicate coarse to medium texture compa- rable to basins in the Carboniferous sandstones of the Appalachian Plateau in Pennsylvania. Little variation in the values of these parameters occurs between basins on igneous rook and basins on sedimentary rock. The length of overland flow ranges from approximately i mile to i mile. Two thousand eight hundred twenty-five to 6,140 square feet are necessary to support one foot of channel in the central Coast Range. Maximum elevation in the area is 4,097 feet at Marys Peak which is the highest point in the Oregon Coast Range. The average elevation of summits in the thesis area is ap- proximately 1500 feet. The calculated relief ratios for the Siletz, Yaquina, Marys, and Luckiamute Rivers are compara- ble to relief ratios of streams on the Gulf and Atlantic coastal plains and on the Appalachian Piedmont. Coast Range streams respond quickly to increased rain- fall, and runoff is rapid. The Siletz has the largest an- nual discharge and the highest sustained discharge during the dry summer months. -
Horizons River and Channel Morphology Report Version3
River and channel morphology: Technical Report prepared for Horizons Regional Council Measuring and monitoring channel morphology Dr. Ian Fuller Geography Programme School of People, Environment & Planning March 2007 River and channel morphology: Technical Report prepared for Horizons Regional Council Measuring and monitoring channel morphology Author: Dr. Ian Fuller Geography Programme School of People, Environment & Planning Reviewed By: Graeme Smart Fluvial Scientist NIWA Cover Photo: Tapuaeroa River, East Cape March 2007 Report 2007/EXT/773 FOREWORD As part of a review of the Fluvial Research Programme, Horizons Regional Council have engaged experts in the field of fluvial geomorphology to produce a report answering several key questions related to channel morphology and linkages with instream habitat diversity in Rivers of the Manawatu-Wanganui Region. This report is aimed at introducing concepts of the importance of morphological diversity in the Region’s rivers to the planning framework (to be used in the development of Horizons second generation Regional Plan – the One Plan). This expert advice has been used in the development of permitted activity baselines for activities in the beds of rivers and lakes which may influence the channel morphology and to address the cumulative impacts of these activities over time and space. Monitoring recommendations within this report provide guidance for the management of cumulative reductions in channel morphological diversity over time. Regional implementation of the monitoring of channel morphology is planned for introduction in the 2007/08 financial year through the newly reviewed Fluvial Research Programme. The monitoring will be conducted in line with recommendations from this report. Kate McArthur Environmental Scientist – Water Quality Horizons Regional Council ii CONTENTS Foreword i Contents 3 1. -
Assessing Sediment Connectivity at the Hillslope, Channel and Catchment Scale
ASSESSING SEDIMENT CONNECTIVITY AT THE HILLSLOPE, CHANNEL AND CATCHMENT SCALE Report to the Water Research Commission by BW van der Waal & KM Rowntree Catchment Research Group, Department of Geography, Rhodes University WRC Report No 2260/1/15 ISBN 978-1-4312-0715-2 November 2015 Obtainable from Water Research Commission Private Bag X03 Gezina, 0031 [email protected] or download from www.wrc.org.za DISCLAIMER This report has been reviewed by the Water Research Commission (WRC) and approved for publication. Approval does not signify that the contents necessarily reflect the views and policies of the WRC nor does mention of trade names or commercial products constitute endorsement or recommendation for use. © Water Research Commission Executive Summary Chapter 1. Introduction: context and motivation Connectivity is being embraced increasingly by hydrologists, geomorphologists and ecologists as a concept that allows integration of landscape structure and function at a number of time and space scales. Connectivity allows the free flow of energy and materials through the system and, as a result, mutual adjustment between system components. It is counterbalanced by storage sites, which allow material to be retained in the system. Ecologists, hydrologists and geomorphologists have all embraced the idea of connectivity as described in the literature review. The research was conducted in the catchment of Thina River (Tertiary catchment 34), lying in the headwaters of the Mzimvubu catchment, located in the former homeland of the Transkei where subsistence farming has been practiced for many years. A subcatchment of the Thina, the Vuvu, was investigated in detail. Two changes to connectivity are evident in the research area. -
Morphometric Analysis and Change Detection Analysis of Vrishabhavathi River Basin Using Remote Sensing and GIS
IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) e-ISSN: 2278-1684,p-ISSN: 2320-334X, Volume 17, Issue 6 Ser. III (Nov. – Dec. 2020), PP 45-55 www.iosrjournals.org Morphometric Analysis and Change Detection Analysis of Vrishabhavathi River basin using Remote sensing and GIS Bipin Anand1, Charan SN2,Girija H3,Jithin P Sajeevan4 1,2,3Department of Civil, SJC institute of technology ,Chikballapur. India 4Research Scientist, LRDC,Bengaluru, India Abstract: Remote Sensing(RS) and Geographical Information System (GIS) has become an effective tool in delineation of drainage pattern and water resources management and its planning.In the present study, morphometric analysis of the Vrishabhavathi river basin has been carried by using earth observation data and GIS techniques. The morphometric analysis was performed using ArcGIS to understand the nature, landscape development and hydrologic responses of Vrishabhavathi watershed. The drainage network shows that the terrain exhibits dendritic drainage pattern.The CARTOSAT and LISS(III) (SRTM) data is used for the morphometric analysis of the watershed to derive linear, relief, and aerial aspects.Spatial analysis is performed using ENVI for change detection studies in the basin to understand the effect of urbanization. Strahler’s stream ordering techniques and analysis were followed for advanced analysis.From the analysis, it can be concluded that remote sensing techniques and GIS tools prove to be a competent tool in morphometric analysis. These studies are very useful for sustainable urban planning and also for land, water, and soil resource management in the watershed area. Keywords: GIS,Spatial Analysis, Remote Sensing, Morphometric Analysis, Vrishabhavathi Watershed ----------------------------------------------------------------------------------------------------------------------------- ---------- Date of Submission: 01-12-2020 Date of Acceptance: 15-12-2020 ----------------------------------------------------------------------------------------------------------------------------- ---------- I. -
H3.1 Open-Water Lotic (Rivers and Streams)
PAGE .............................................................. 428 ▼ H3.1 OPEN-WATER LOTIC (RIVERS AND STREAMS) The open-water habitat in rivers and streams is the tion to the morphology of the channel. Rivers and body of water flowing through the channel. The char- streams in Nova Scotia are not deep enough to create acteristics of the water can vary considerably in rela- layering in the water column. H3.1 Open-water Lotic (Rivers and Streams) Plate H3.1.1: Drysdale Falls, Colchester County (sub-Unit 521a). An open-water stream habitat with a waterfall and associated cliff habitat (H5.3). The forest is a spruce, hemlock, pine association (H6.2.6). Photo: R. Merrick Habitats Natural History of Nova Scotia, Volume I © Nova Scotia Museum of Natural History .............................................................. PAGE 429 ▼ FORMATION In fast-moving streams, there is very little pri- mary production in the open-water habitat, due to The dominant feature of all lotic environments is the the velocity and turbulence of the current. continuous movement of water and currents, which Populations of consumer organisms (mainly cuts the channel, molds the character of the stream particulate feeders) are low. Riffle areas provide and influences the chemical and organic composi- valuable habitat for juvenile trout and salmon. Pools tion of the water.1 Water running off the land follows are important resting areas for several fish species, courses of least resistance and develops these as including Atlantic Salmon. The quality of these ar- distinct channels by erosion. Young or rejuvenated eas can be adversely affected when shade trees are streams, with a high velocity, erode more than they removed from the banks. -
Fluvial Processes
The work of rivers Fluvial Processes Three basic processes at work Erosion, Transportation Deposition Weathering does not play a significant role in rivers The effectiveness of these processes depends on the River’s Energy level, it’s overall shape and it’s depth (Deep rivers more powerful than shallow, young rivers more powerful than old age) A River’s Course The area drained by a river = Drainage Basin A drop of rain falling anywhere in this area will eventually find its way into the river. Drainage basins are separated from each other by watersheds What is at X? Definitions River Source __________________________________ Drainage Basin ________________________________ Confluence ___________________________________ Tributary _____________________________________ Watershed ____________________________________ Estuary _______________________________________ River Mouth ___________________________________ Long (real) and Graded (ideal) Profile Drainage Patterns The shape made by a river and it’s tributaries (note, not distributaries) on the landscape Three main patterns Dendritic (tree like) patterns Trellis (right angles) patterns Radial (like radius of a circle) patterns The drainage pattern of a river depends on relief, rock types and river size Dendritic (tree like) Patterns Dendritic Patterns Trellis (right angled) Patterns Radial Patterns (out from a central point) 2007 Leaving Cert Hons Factors affecting fluvial (river) processes – P107 River Volume River Speed/Velocity Slope Width and Depth of a Channel -
Payette River Maps MAIN, MIDDLE FORK, NORTH FORK, SOUTH FORK North Fork
U.S. Department of the Interior Bureau of Land Management Four Rivers Field Office Payette River Maps MAIN, MIDDLE FORK, NORTH FORK, SOUTH FORK North Fork N Experts Only o r NORTH t h F SCALE: o r k 0 1.0 2.0 miles P a y e t t e Staircase R te to McCall et Section ay k P tairase Advanced or le F IV idd Dog 12 M llll ll Bronco 17 ll Leg Canyon III Billy ll lll III+ 13 Section ll R lll lll Oxbow III MAN Advanced Deadwood River Tight & 1 Garden III llll Right Hard Hat III 21 Whitewater 101 II ll a III Valley 8 IIII rprise 7 2 itte as III BANKS ll Rapi IIII III IIII Trashcan III Whitewater 102 II IV Section III III aaar 11 IIII IIII III S-Turn III Beginner + Swirley IIIII ll Go Left or You’re Fired III lll Pine Flats II 9 IIII ll Canyon The Grease III e Pie ll ll Kaleidoscope III Garden Valley 10 Intermediate aaar Ranger Station Lunch Counter II ll Gateway IV lIl 25’ Waterfall So ut ll ll ll ll i as Prtae lll h Bennett’s Rock III For Main Payette k Payette Swirley Banks to Beehive Bend Canyon Series Killer Surf Wave II ll Intermediate II-III Mike’s Hole III lIl 3 Mixmaster III lIl Adios My Friend III e lIl tt ye Pa n ai M 4 5 Main Payette R Beehive Bend to Boat Ramp Beginner + Class II lI with one Class III Rapid Class II lI Class II 6 lI Climax III lIl to Horseshoe Bend and Boise R North Fork N Experts Only o r NORTH t h F SCALE: o r k 0 1.0 2.0 miles P a y e t t e Staircase R te to McCall et Section ay k P tairase Advanced or le F IV idd Dog 12 M llll ll Bronco 17 ll Leg Canyon III Billy ll lll III+ 13 Section ll R lll lll Oxbow -
Grade 12 Geography Geomorphology Revised Learner Notes
GRADE 12 SECONDARY SCHOOL IMPROVEMENT PROGRAMME (SSIP) 2019 GEOGRAPHY REVISED LEARNER NOTES SESSIONS 6 –9 GEOMORPHOLOGY 1 TABLE OF CONTENTS SESSION TOPIC PAGE 6 Drainage Basins in South Africa 7 Fluvial processes River Capture and drainage basin and river 8 management 9 Geomorphology consolidation ACTION VERBS IN ASSESSMENTS VERB MEANING SUGGESTED RESPONSE Account to answer for - explain the cause of - so as to Full sentences explain why Analyse to separate, examine and interpret critically Full sentences Full sentences Annotate to add explanatory notes to a sketch, map or Add labels to drawing drawings Appraise to form an opinion how successful/effective Full sentences something is Argue to put forward reasons in support of or against Full sentences a proposition Assess to carefully consider before making a judgment Full sentences Categorise to place things into groups based on their One-word characteristics answers/phrases Classify to divide into groups or types so that things One-word answers with similar characteristics are in the same /phrases group - to arrange according to type or sort Comment to write generally about Full sentences Compare to point out or show both similarities and Full sentences differences Construct to draw a shape A diagram is required Contrast to stress the differences, dissimilarities, or Full sentences unlikeness of things, qualities, events or problems Create to develop a new or original idea Full sentences Criticise to make comments showing that something is Full sentences bad or wrong Decide to consider