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Visit the following website  http://techalive.mtu.edu/meec/module01/HydrologicCycleQuiz.htm for an interactive quiz on the key elements of the hydrological cycle. Click http://polaris.umuc.edu/cvu/envm/hydro/hydro.html for an animation of the hydrological cycle.

Identify the features of a drainage basin
• View this animation showing the function of a drainage basin - drains rivers and its tributaries.

• Long profile of a river

Characteristics of the river in the upper, middle and lower course

Describe and explain factors that affect the energy of a river: velocity and volume.
 VelocityWetted perimeterRiver Channel Processes & LandformsView more presentations from maliadamit.    2. Amount of load     3. Roughness of a channel
Rocks that protrude out from the bank can slow the pace of the water as friction slows it down as it passes the obstacles.
 4. Gradient (steepness) of the river     5. Channel shape  Symmetrical River Channel Asymmetrical River Channel Asymmetrical River Channel DiagrammaticallyVolumeClimatic conditionsPermeability of rock

Permeability of rocks is determined by the size of the pores between the rock particles. If the rock has small pores, water cannot easily pass into the rock and this means that the rock is impermeable. However, if the rock has large pores, water can easily pass through and thus the rock is permeable.
 Presence of vegetation Describe how trees affects volume of river?Size of drainage basinAmount and duration of rainfall
Click here for an interactive activity where you can learn how rainfall and type of vegetation affect the volume of water in a river.

Identify the two directions of river erosion.

Describe and explain with the help of diagrams 4 fluvial erosional and 4 fluvial transportational processes of a river.

4 erosional processes

1. View this animation showing the 4 major river erosional processes.
• Corrasion (abrasion)
• Attrition
• Solution (Corrosion)
• Hydraulic Action

4 transportational processes

1. View this animation showing the 4 major river transportational processes

• Explain the conditions that result in river deposition.
•
1. View animation showing how river deposition takes place

Describe and explain using the Hjulstrom Curve, the relationship between particle size and velocity and how the particles are subjected to various river processes.

Describe and explain the formation of erosional landforms such as waterfalls,plunge pools, gorges, v-shaped valleys, inter-locking spurs and potholes with the help of well-labelled/well-annotated diagrams.

The powerpoint slides below include a video explaining how a waterfall is formed.

Describe and explain the formation of erosional landforms such as waterfalls,plunge pools, gorges, v-shaped valleys, inter-locking spurs and potholes with the help of well-labelled/well-annotated diagrams.
Formation of a waterfall by rocks of different resistance.

Formation of waterfall,plunge pool, gorge and rapids.

The Victoria Falls, an example of a waterfall that is formed by faulting. It is one of the 7 natural wonders of the world.

The Niagara Falls, an example of a waterfall that is formed due to alternating layers of resistant and less resistant rocks. It is made up of THREE waterfalls - namely the American Falls, Bridal Veil Falls and the Canadian Horseshoe Falls

To learn more about the formation of Niagara Falls, click here.

Geology of the Falls (cross sectional view)

A paranomic view of the Falls

Katherine Gorge, Australia

Rapids

V-shaped valley

Interlocking Spurs

Pot holes in the riverbed. Guess which process cause these.

Explain the formation of pools & riffles, river cliffs, slip-off slopes and depositional landforms like ox-bow lakes, meander scars, floodplains and deltas with the help of well-labelled/well-annotated diagrams.
 Pools & Riffles, Cross sections of a meander       Formation of a meander to a scar
View an animation showing the sequential formation of meanders, river cliffs, slip off slopes, cutoff, oxbow lake and meander scar.

There are, in fact, many different types of meanders

Formation of river cliff and slip off slope

A steep river cliff caused by river erosion

A gentle slip off slope formed by river deposition. Photo taken in Kachanaburi, Thailand near the Death Railway.

On one section of the railway track

River Cliff and slip off slope

The process of helicoidal flow (a secondary flow that causes deposition on the convex bank and erosion at the concave bank)

Diagram showing formation of ox bow lake

A cut-off

Meander and Ox bow lakes

Another photograph showing meanders, abandoned loops, meander scars (center of the photograph - light green patches)
Shrewsbury is a county town lying on the river Severn in the West Midlands region and is home to around 71 000 inhabitants. It isplaced inside a meander, and was originally a medieval market town. The meander was very helpful for imports and exports as well as travel in the medieval ages.

Since 1990, Shrewsbury has experienced severe flooding problems becuse of its location - in 2005 the defense systems were increased dramatically to hold back the potential flooding. The land is very fertile due to all the layers of sediment and silt that have been forming over many years. Therefore, farming is a possibility on flood plains, around meanders. These crops must be resilient against high discharge in times of flooding.
 The town of Shrewsbury, UK, placed inside a huge meander bend   Formation of a floodplain         Floodplains    The powerpoint slides below include a sequential diagram and an animation of the formation of floodplains and levees. S3 River Features 4 Levees View more presentations from ACS(BR). Visit the following website http://www.ngfl-cymru.org.uk/vtc/meanders_floodplain/eng/Introduction/Plenary.htm for an interactive quiz on the key features of a floodplain and a meander.   Formation of a delta     The Nile Delta (arcuate delta) and the Bird's Foot Delta (Mississippi Delta)       River Channel Management   Dredging
• mainly to deepen/widen the river channel so as to increase its capacity to prevent flooding.
• it also helps to increase the flow of a river by reducing its wetted capacity
Limitations:
• There may be a lack of a suitable site to dispose the dredged material.
• There may also be a lack of a suitable handling site nearby that is large enough to handle the dredging process.
• It can be expensive
 Dredging at Changi        River Straightening   Straightening rivers allows water to flow more rapidly downstream involves the removal of meanders there by reducing the length of the river channel The faster flow allows water to flow away from the area more quickly and wash away      sediments which have accumulated on the river bed  This thus deepens the channel, allowing it to hold more water and minimize flooding. Limitations  expensive result in flooding downstream accumulation of sediments loss of wetlands River Straightening in Chicago which began in 1926 and completed in 1930         Chicago River Today      Bank Protection   artifical levees to increase the capacity of the river to reinforce the banks of the river to minimise erosion to increase the speed of river flow Limitations   expensive to maintain encourage flooding downstream especially in unprotected parts of the river can be breeched especially during prolonged and heavy rainfall or hurricane.Cause major flooding and worsen the situation when the broken concrete, swept by floodwaters hit/kill people and damages buildings give people living behind the levee a false sense of security Artificial levees along the Mississippi       Breeched section of the levee in the 1993 Mississippi Flood         Gabions   less costly stackable along the banks of the river help divert the flow of water from the river banks to the centre of the channel protect the banks from being eroded by the force of running water, thereby reducing                    the amount of sediments that flow into the river Limitations not as effective as artifical levees wire mesh corrode more easily, destablising the structure allows sediment to accumulate behind the structure Gabions along the banks of a river     Close-up of a Gabion    Prolonged erosion by running water destablised a section of the gabion      Vegetation Planting   make use of the roots of vegetation to hold the soil at the banks of a river together to minimise bank erosion to prevent the addition of eroded sediment into the river which slows down the                     speed of a river minimise the occurance of floods more environmentally friendly, aesthetically pleasing, cheap option Limitations only in areas where climate allows the growth of vegetation roots of vegetation may not be strong enough to withstand rivers with high energy                      or when there is a sudden onset of flood caused by hurricane or prolonged heavy                     rain excessive shade can also kill marine plants and aquatic life as it prevents sunlight                     from entering the water additional weight of vegetation can in fact add additional stress to the river bank,              thereby resulting in bank failure Vegetation Removal   On the other hand, there are occasions which call for the removal of all vegetation                   along the banks or river bed. Vegetation clearance is often conducted to improve                        the speed of flow and stabiles the river channel. Limitations The weight of vegetation, especially trees could add stress to the banks and cause                  them to collapse. More over, the vegetation may contribute woody debris to the river which may                     deflect the flow of water and accelerate bank erosion. Accumulation of such debris may also slow down the flow of water and encourage               flooding.
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