DL: The River Wye Flashcards

1
Q

Describe the course of the River Wye

A
  • (Source) Plynlimon, Rhayader, Builth Wells, Hay-on-Wye, Hereford, Ross-on-Wye, Symonds Yat, Monmouth, Tintern, Chepstow (mouth)
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2
Q

Where is the source of the River Wye?

A
  • Plynlimon - Plynlimon Hills in Cambrian Mountains
  • 690m above sea level
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3
Q

Describe the geology at the source (Plynlimon)

A
  • Gritstone, mudstone and shales - sedimentary rock which is easy for the river to erode vertically
  • Thin soils
  • Impermeable surfaces leads to more surface runoff
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4
Q

Describe the climate at the source (Plynlimon)

A
  • 2650mm rainfall a year
  • Heavy rainfall due to relief rainfall = surface runoff
  • Cold temps due to altitude = freeze thaw weathering
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5
Q

How does the climate and geology work together at the source?

A
  • More rain means more erosion creating V-shaped valleys
  • Mass movement on the valley sides contributes material to the river
  • More sediment in the river means more abrasion
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6
Q

Describe what happens at Rhayader

A
  • 219m above sea level
  • Rapids form here due to alternation bands of less and more resistant rock
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7
Q

Describe what happens at Bulith Wells

A
  • 130m above sea level
  • Valley begins to widen as the Wye begin to migrate across the floodplain and form meanders
  • Lateral erosion is more important
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8
Q

Describe what happens at Hay-on-Wye

A
  • 97m above sea level
  • River enters its middle course, meanders move across a wider floodplain and creates an ox-bow lake as they migrate
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9
Q

Describe the geology at the middle course (Hay-on-Wye)

A
  • Sandstone, more easily eroded allowing the river to erode laterally (side by side)
  • Horse-shoe bend is an oxbow lake
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10
Q

Describe what happens at Hereford

A
  • Biggest settlement on the River Wye
  • Downstream of Hereford the floodplain starts getting wider as the valley floor is flatter
  • The river Lugg joins the Wye as a tributary, bringing more discharge
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11
Q

Describe what happens at Ross-on-Wye

A
  • As the floodplain as developed at Ross-on-Wye, levees have formed. Over time the levees become vegetated
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12
Q

Describe what happens at Symonds Yat

A
  • The meanders of the Wye are deeply incised forming a gorge as the river is unable to erode more resistant outcrops of limestone
  • Important tourist feature
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13
Q
A

At Chepstow the Wye and Severn have their confluence. At this point both the Severn and Wye are tidal and suspended sediment can be seen in the rivers.​

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14
Q
A
  • In the past, humans have altered the Wye’s course and drainage basin in ways that have exaggerated flooding
  • Deforestation, poor soil management and building on the floodplain have changed the landscape through which the Wye flows
  • People have responded in the past using hard defences to prevent floodwater from reaching properties
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15
Q

Natural flood management

A
  • Increasing infiltration Into the soils - better soil management techniques
  • Slowing the flow of water - creating features which obstruct flow across the river channel or floodplain
  • Storing water upstream - water can be stored within the upstream catchment and released slowly
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16
Q

Trackery improvement

A
17
Q

In channel water retention

A

*

18
Q

Infield water retention

A
  • Allows strips of land upstream along the river to flood, resorting the natural flood plain
  • Allow surface flow to collect and soak away
    *
19
Q

Afforestation

A
  • New trees are planted or seeds are sown in an area where there were no trees, creating a new forest
  • More infiltration
20
Q

Soil improvment

A
  • Aerate soils to increase infiltration rates
21
Q

Overwinter cover

A