The Changes downstream in a river valley RIVER STUDIES The Changes downstream in a river valley

The Hydrologic Cycle Infiltration = Groundwater System Runoff = Surface Water System

Satellite view of river drainage, Middle East What is this features?

Upper valley characteristics

Upper valley characteristics

Upper valley characteristics “V”shape valley, vertical erosion dominant

Upper valley characteristics “V”shape valley, vertical erosion dominant Interlocking spurs

Upper valley characteristics “V”shape valley, vertical erosion dominant Interlocking spurs Slumping and landslides - very active hill slopes

Upper valley characteristics “V”shape valley, vertical erosion dominant Narrow, shallow channel, low velocity and discharge Interlocking spurs Slumping and landslides - very active hill slopes

Upper valley characteristics “V”shape valley, vertical erosion dominant Narrow, shallow channel, low velocity and discharge Interlocking spurs Slumping and landslides - very active hill slopes Large bed load derived from upstream and from valley sides

Interlocking spurs, Robinson, Lake District A typical upper course valley with interlocking spurs, steep valley sides and active slope processes

River load in upper course Why are they rounded? Boulders are large and semi-rounded, due to attrition within the load and abrasion with the stream bed and banks

Rapids in the Upper Tees Valley WHAT IS A RAPID?

High Force waterfall, R. Tees WHAT IS A WATERFALL?

High Force waterfall, R. Tees Waterfall creates gorge as it recedes upstream by eroding the base and neck What is this feature called? HOW IS A GORGE FORMED? Plunge pool

Waterfall formation Look at the diagram, How is a waterfall formed?

High Force Waterfall R. Tees

Close-up of potholes How are these formed?

Potholes, human scale!!

Erosion Processes Corrosion - Attrition - Abrasion (Corrasion) - Hydraulic Action - is when the river is loaded with material in suspension and scours away at the river banks. (Sandpaper effect) is the shear force of the river impacting on the sides of the river banks. is substances carried in solution such as acids. They dissolve rocks away over long periods of time. is when bed load collides into each other with the current flow and breaks down into smaller particles.

Middle course, R. Tees HOW DOES THIS DIFFER FROM THE UPPER SECTION?

Middle course, R. Tees WHAT DO YOU THINK THE ARROWS POINT TO? Valley opens out, more gentle slopes, wider valley bottom First signs of meanders River channel wider, deeper, greater velocity and discharge

Meandering Rivers WHAT IS A MEANDER?

Formation of Meanders

Point bar deposits

Point Bar Deposits Point bar deposits grows laterally through time

Meander, R. Lavant, Chichester

Meander, R. Lavant, Chichester WHAT DO THE ARROWS POINT TO? WHICH WAY IS THIS MEANDER MOVING? Floodplain Slip-Off Slope River Cliff Point bar deposits on the inner meander bend where there is low energy

} Cut bank erosion (River Cliff) Point bar deposits Meander loop WHERE IS EROSION TAKING PLACE? Cut bank erosion (River Cliff) F A E B Point bar deposits } Meander loop C D WHERE IS DEPOSTION TAKING PLACE?

Meander on the R. Colorado WHY IS DEPOSITION OCCURING HERE?

How did these meanders form?

REVISION: What River features do you get here?

Migrating meanders, R. Gongola, Nigeria WHY ARE THEY MIGRATING?

What happens to the river when it moves to the middles course Gradient becomes less steep River continues to erode vertically but LATERAL erosion now occurs in MEANDERS What is MEANDER MIGRATION ? Name three effects it have on the valley? What factors effect how much load is being carried?

Transportation What are the four methods of transportation? Traction - is when large particles roll along the river bed Saltation - is when smaller particles bounce and collide in a leapfrog manner across the river bed. Suspension - is when the river holds even smaller particles and carries them in its current. This is when the river appears to be murky. Solution - is when dissolved material is carried.

Lower Course: Severn Valley

Lower Severn Valley Very wide floodplain Well developed meanders with bars in the channel indicating high sediment load Very gentle valley side gradients HOW DOES IT DIFFER FROM THE MIDDLE COURSE?

Flood Plains HOW DO YOU THINK THE TERRACES WERE FORMED? The entire floodplain can become covered with water during floods.

Ox Bow Lake Formation LOOK AT THE DIAGRAM & EXPLAIN THERE FORMATION

Formation of an Oxbow

Ox Bow lake on Mississippi

Levee formation

Levees WHAT DO YOU THING HUMANS MIGHT HAVE DONE TO THIS LEVEE?

Delta Formation WHAT IS A DELTA? DEPOSITON OF MATERIAL BY THE RIVER WHEN IT ENTERS THE SEA WHY DOES IT DROP ITS SEDIMENT

Mississippi Delta from Space

The Nile Delta from space River Nile

Estuary Formation HOW DOES THIS DIFFER FROM A DELTA? The Lower Course of a river valley has been DROWNED by a rise in sea level or a fall in the land level. RAISED VALLEY SIDES USING YOUR ATLAS FIND AN ESTUARY (LOOK AT THE RIVER THAMES)

The Rhone Delta USING YOU ATLAS LOCATE THE RHONE DELTA

The Rhone Delta S. France Look at p39 and identify the KEY FEATURES CAN YOU SEE IN THE SATELLITE PHOTO?

The Rhone Delta WHY HAS A DELTA FORMED HERE? LOOK AT P 39

Summary of valley characteristics

The River Tees TRY AND FIND THE RIVER TEES IN YOUR ATLAS HINT LOOK AT THE MAP

Land Use in Drainage Basin of River Tees WHAT IS THE AREA IN EACH BOX?

Upper Tees COW GREEN RESERVOIR WHAT HUMAN INFLUENCES EXIST IN THE MAPS?

The Upper Tees Cronkley Scar WHAT ARE THE KEY GEOGRAPHCIAL FEATURES YOU CAN SEE IN THE PHOTOGRAPH MOORLAND STEEP VALLEY TURBULENT RIVER CHANNEL SLOPE DEBRIS WHAT LAND USES CAN YOU SEE IN THE PHOTO?

Upper Tees WHAT IS THE NAME OF THE WATERFALL?

The Lower Course Tees FLAT VALLEY FLOOR URBAN SETTLEMENT WIDE MEANDERS HOW HAS THE RIVER AND LAND USE CHANGED?

The Lower Tees TEESMOUTH ESTUARY WHAT LAND USE CAN YOU SEE IN THE PHOTOGRAPH?

The River meets the Sea

River Management WHAT IS THE FUNCTIONOF THE BARRAGE? LOOK AT P42 WHAT DO YOU THINK THE PHOTOS SHOW?

Formation of the Mississippi River Delta More recent delta sediments Modern delta Early delta

Causes of Floods A Flood can occur when a river exceeds its bank full stage and water will subsequently inundate the adjacent surrounding area. Heavy rainfall - long periods of heavy rainfall will lead to an increase in surface runoff and increase in river level. Snow melt and heavy rainfall - water in storage may be freed by Spring melts increasing surface runoff. Deforestation - cutting down of trees leads to a reduction in interception rates and an increase in surface runoff. This may also lead to rapid erosion rates due to a lack of stability in the soil subsurface. Urbanisation - tarmac and concrete surfaces are impermeable and lead to an increase in surface runoff.

Flood Control and Management There are a number of ways managing floods: 1. Afforestation - planting trees increases interception rates and reduces surface runoff. 2. Dams and Reservoirs - these hold back and regulate the flow of river water. Can be used as fresh water supply and generation of HEP. 3. Diversion Channels - overflow channels which take surplus water out of a river in times of flood. 4. Channel Straitening and Dredging - smoothens the channel to increase the speed (velocity) of the river and get water out of the drainage basin as quickly as possible. 5. Artificial Levees - makes river banks higher therefore holding more water. 6. Culverts - semi circular, smooth channels increase velocity and gets water away from urban areas as quickly as possible. 7. Revetments and Channel Walls - strengthen river banks from erosion.