The Long Profile Characteristics. Why does a river meander in its middle and lower course?

Similar documents
River Processes. A) Write definitions for the terms erosion, transportation & deposition.

NATURE OF RIVERS B-1. Channel Function... ALLUVIAL FEATURES. ... to successfully carry sediment and water from the watershed. ...dissipate energy.

What is weathering and how does it change Earth s surface? Answer the question using

(3) Sediment Movement Classes of sediment transported

ES 105 Surface Processes I. Hydrologic cycle A. Distribution % in oceans 2. >3% surface water a. +99% surface water in glaciers b.

PHYSICAL GEOGRAPHY. By Brett Lucas

River Processes. Learning Objective: Discover how a river erodes, transports and deposits material

Physical landscapes River landscapes in the UK

1. The map below shows a meandering river. A A' is the location of a cross section. The arrows show the direction of the river flow.

Stream Geomorphology. Leslie A. Morrissey UVM July 25, 2012

Topic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p ) Workbook Chapter 4, 5 WEATHERING

Streams. Water. Hydrologic Cycle. Geol 104: Streams

River/Stream Erosion Notes

Page 1. Name:

Figure 1. Which part of the river is labelled in Figure 1? a) Mouth b) Source c) Lower course d) channel

River Sediments. Sediment Types Are Not Randomly Distributed in a River s Sediment

(3) Sediment Movement Classes of sediment transported

27. Running Water I (p ; )

Erosion Surface Water. moving, transporting, and depositing sediment.

MEANDER CURVE (MODIFIED FOR ADEED)

GEOL 652. Poudre River Fieldtrip

Mark Scheme (Results) Summer 2007

Morphology and Sedimentology of Panther Creek, Montgomery County Preserve

Surface Water and Stream Development

Landscape Development

Aquifer an underground zone or layer of sand, gravel, or porous rock that is saturated with water.

What are the different ways rocks can be weathered?

Rivers. Regents Earth Science Weathering & Erosion

Chapter 11. Rivers: Shaping our landscape

Streams. Stream Water Flow

Geography Notes for Plonk Meeting

WEATHERING, EROSION & DEPOSITION STUDY GUIDE

Paper One Living with the Physical Environment. SECTION C Physical Landscapes in UK

Weathering, Erosion, Deposition, and Landscape Development

Erosion and Deposition

If a Woodchuck Could Chuck Wood

Chapter 10. Running Water aka Rivers. BFRB Pages

Final Exam. Running Water Erosion and Deposition. Willamette Discharge. Running Water

Stream Classification

RIVERS, GROUNDWATER, AND GLACIERS

Step 5: Channel Bed and Planform Changes

Name: Which rock layers appear to be most resistant to weathering? A) A, C, and E B) B and D

QU: Where does sand do jail time? AIM: To explain the sediment cell concept as a system and what human and natural factors create/upset a dynamic

Weathering, Erosion, Deposition

EROSION AND DEPOSITION

FLUVIAL PROCESSES 13 MARCH 2014

4. The map below shows a meandering stream. Points A, B, C, and D represent locations along the stream bottom.

What factors affect the angle of a slope?

Name. 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different soil horizons, A, B, C, and D, are shown.

Channel Pattern. Channel Pattern, Meanders, and Confluences. Description of Channel Pattern. Bridge (2003)

NATURAL RIVER. Karima Attia Nile Research Institute

Chapter 2. Denudation: Rivers and Ice

Running Water Earth - Chapter 16 Stan Hatfield Southwestern Illinois College

GLG362/GLG598 Geomorphology K. Whipple October, 2009 I. Characteristics of Alluvial Channels

GY 111 Lecture Note Series Sedimentary Environments 2: Rivers and Deltas

GEOL 1121 Earth Processes and Environments

Year 6. Geography. Revision

11/12/2014. Running Water. Introduction. Water on Earth. The Hydrologic Cycle. Fluid Flow

Tom Ballestero University of New Hampshire. 1 May 2013

Earth Science Chapter 6 Section 2 Review

Fluvial Geomorphology

Chapter 3 Erosion and Deposition. The Big Question:

Summary. Streams and Drainage Systems

1. Base your answer to the following question on the map below, which shows the generalized bedrock of a part of western New York State.

GOING WITH THE FLOW (1 Hour)

Fluvial Systems Lab Environmental Geology Lab Dr. Johnson

STREAM SYSTEMS and FLOODS

Precipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle. Runoff Transpiration

Lecture 10: River Channels

Essential Questions. What is erosion? What is mass wasting?

The Hydrologic Cycle STREAM SYSTEMS. Earth s Water and the Hydrologic Cycle. The Hydrologic Cycle. Hydrologic Cycle

Flowing Streams. Adapted from: Field Exercise: Stream Flow Dynamics & Sedimentation by Daniel J. Bisaccio and Donald L. Woodrow.

Name: KEY OBJECTIVES HYDROLOGY:

EROSION, DEPOSITION AND SEDIMENTARY ROCKS. Reading: Earth Science Tarbuck and Lutgens Chapter 5: pages Chapter 3: pages 52-54, 61-69

Earth Science Chapter 9. Day 6 - Finish Capillary Action Lab - Quiz over Notes - Review Worksheets over Sections 9.2 and 9.3

Section 5. Low-Gradient Streams. What Do You See? Think About It. Investigate. Learning Outcomes

Running Water and the Development of Landforms

Figure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant?

True or False: The Earth s surface has stayed the same for thousands of years

Geomorphology Geology 450/750 Spring Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26

ADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN

Unit 3 Review - Surface Processes

Water flowing in the stream can move sediments along the stream channel because of an exchange of energy from the

10/27/2014. Surface Processes. Surface Processes. Surface Processes. Surface Processes. Surface Processes

SESSION 6: FLUVIAL LANDFORMS

Changes in Rivers and their Valleys.

Lectures Hydrology & Fluvial Geomorphology. Gauley River Images. Ancients' (= Biblical) Model of Water (Hydrologic) Cycle

GY 111: Physical Geology

mountain rivers fixed channel boundaries (bedrock banks and bed) high transport capacity low storage input output

Teacher s Pack Key Stage 3 GEOGRAPHY

3/3/2013. The hydro cycle water returns from the sea. All "toilet to tap." Introduction to Environmental Geology, 5e

Surface Processes. Water Cycle. Evaporation Transpiration Condenstation Precipitation Infiltration Runoff

Surface Water Short Study Guide

River Morphology. EAD 511 River management

Geo 302D: Age of Dinosaurs. LAB 2: Sedimentary rocks and processes

Environmental Geology Chapter 9 Rivers and Flooding

Why Stabilizing the Stream As-Is is Not Enough

SCOPE OF PRESENTATION STREAM DYNAMICS, CHANNEL RESTORATION PLANS, & SEDIMENT TRANSPORT ANALYSES IN RELATION TO RESTORATION PLANS

PolyMet NorthMet Project

6.1 Water. The Water Cycle

Transcription:

QU: How are Meanders formed? AIM: To describe and explain meander formation and identify the difference between GCSE and A/S knowledge and expectations. ST: Get the key rivers terms from the pictures. 1 4 2 3 A*/B 5 6 1 Ext: Some have links to others, can you explain the links? 1

The Long Profile Characteristics. Why does a river meander in its middle and lower course? Transition of potential (gravitational) to Kinetic energy. Due to decreasing gradient. The river is closer to its graded profile so no longer works at vertical erosion but any surplus energy is put into lateral erosion. Hence the meandering and widening of the valley. 2

Erosion occurs on the outside of a meander whereas deposition happens on the inside of the meander. A* Velocity is greatest on the outside of the meander. Therefore there is more energy that can erode the banks. On the inside of the bend velocity is slower so the river has less energy. As a result it cannot carry sediment so deposits it on the inside of the bend. A/S Over to you. GCSE Structured, short answers. Describe and explain the formation of a meander. (7) 3

Today 4

In groups you are going to be allocated a stage of meander formation. You will have 5 mins to prepare a short presentation on what happens in your stage. You will present it with the aid of drawings on upturned tables. Success criteria: You use appropriate terminology. Diagrams Everyone chips in You deal with my killer questions. 5

Group 1 Straight river What is helicoidal flow? How is it created and how does it start the meander process? Group 2 Meandering starts What is the Thalweg? Why is it significant in further developing the meander? Group 3 Why are meanders asymmetric in cross section? Why is this a self accenuating process? What features are created across a meander? Group 4 The meander in cross section Bedload across a meander. Bedload across a meander is often sorted. What does this mean and how does it happen? Group 5 What are the last stages of a meander? What is an Ox bow lake? The meander matures 6

It all starts with our friends, the pool and riffle sequence... Riffles are shallow and due to increased friction create turbulance and helicoidal flow. As Helicoidal flow leaves the riffle section and enters a pool it has more energy to erode and will favour one side of the other of the channel. Once favouring one side of the river it will deepen this side and remain shallow on the other. This creates different velocities either side of the river. Erosion will happen one side (deeper more efficient) deposition the other (shallow less efficient). The meander process has begun. 7

lateral erosion lateral erosion deposition deposition deposition lateral erosion The thalweg denotes where greatest velocity is in a river. On a meander this is always on the outside of the bend where the water is deeper and more efficent as a result. This encourages erosion on the outside of the bend. The meander deepens and moves laterally as a result. 8

Well so what if the channel becomes asymmetric? Fastest flow. Why? Why does the inside of the meander have a smaller particles than the outside of bend. Erosion A B Deposition A B The deeper part will have a larger hydraulic radius therefore more energy to erode and increase velocity. This will lead to greater lateral erosion on this side which will lead to a positive feedback loop where the outside of the meander ( faster and more efficient ) grows larger. On the inside, the water has a greater hydraulic radius as more water is in touch with the bank / bed leading to reduction in velocity and ( as Hjulstrom says ) deposition will occur. This is a self accentuating process. (Process continues once started and is irreversable) The meander moves laterally across the floodplain from this process. 9

Due to having a higher settling velocity larger bedload settles on the bed on the outside of the meander. It is able to resist greater energy of the river whereas smaller bedload cannot resist and gets transported to the inside of the next meander downstream where in the lower velocities it is deposited. smallest material larger material Often a river beach shows evidence of sorting where the coarsest material is deposited first with the finest particles last due to settling velocities being reached in order of size. Therefore bedload is 'Sorted by size' 10

11

12

Tasks: ( using these slides and man climbing a tree book pp. 25 26 ) 1) Describe how a meander first starts to form. Make reference to pools and riffles, helicoidal flow, the meandering thalweg, hydraulic radius changes and include at least a 2 step ( sequential ) diagram like fig. 5. 2) Draw a cross section of an asymmetric meander bend. Add annotations including slip off slope, river cliff. Where is hydraulic radius greatest and why? Based on this, explain where erosion and deposition are occurring. Ox Bow lakes: 3) What is an oxbow lake? 4) Draw a set of sequential diagrams to explain how a meander forms an ox bow lake 1) Describe this landform (4) 2) Explain how this landform is created ( 7 ) 13

Meander animation Overdo the answer to these. Rip it to shreds!! 14

What shape is the river cross section at a b, c d, e f? More importantly can you say why? 15

Attachments Meander animation