waterfallFormedbecause of aband of hardrock in thecourse of ariverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseVshapedvalleyIn the uppercourse andshaped byverticalerosionEstuaryThenavigablemouth ofa riverTransportmovementin riversPlungepoolforms atthe baseof awaterfallAbrasionSand papereffect of therivertransportsedimentFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMeanderthebend ina riverStormDesmondOurfloodingcasestudyHydraulicactionErosionusing thesheer forceof the waterAttritionRocks aremade smootherand rounder bybashingtogetherNWEngland ,CumbriaLocationof thefloodingcase studyDepositiondroppingstuffRiverTeesOur casestudyriverErosionwearingaway (withmovement)of the bedand banksDeltafan shapeddepositis atthe mouthof a riverSourceStart ofa riverLeveeFlood defenceon banks ofriver can benatural ormanmandeChannelthe bitthe waterflows inSaltationBouncing ofrocks alongthe bed ofthe riverNEEnglandLocationof riverTeesMouthEnd ofriverwaterfallFormedbecause of aband of hardrock in thecourse of ariverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseVshapedvalleyIn the uppercourse andshaped byverticalerosionEstuaryThenavigablemouth ofa riverTransportmovementin riversPlungepoolforms atthe baseof awaterfallAbrasionSand papereffect of therivertransportsedimentFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMeanderthebend ina riverStormDesmondOurfloodingcasestudyHydraulicactionErosionusing thesheer forceof the waterAttritionRocks aremade smootherand rounder bybashingtogetherNWEngland ,CumbriaLocationof thefloodingcase studyDepositiondroppingstuffRiverTeesOur casestudyriverErosionwearingaway (withmovement)of the bedand banksDeltafan shapeddepositis atthe mouthof a riverSourceStart ofa riverLeveeFlood defenceon banks ofriver can benatural ormanmandeChannelthe bitthe waterflows inSaltationBouncing ofrocks alongthe bed ofthe riverNEEnglandLocationof riverTeesMouthEnd ofriver

River Landforms and processes - Call List

(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.


1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
  1. Formed because of a band of hard rock in the course of a river
    waterfall
  2. Created when a river erodes round area of harder rocks in the upper course
    Truncated spur
  3. In the upper course and shaped by vertical erosion
    V shaped valley
  4. The navigable mouth of a river
    Estuary
  5. movement in rivers
    Transport
  6. forms at the base of a waterfall
    Plunge pool
  7. Sand paper effect of the river transport sediment
    Abrasion
  8. The area either side of a river that floods especially in the lower course
    Flood plain
  9. formed when a meander is cut off leaving a marshy lake area
    Ox bow lake
  10. the bend in a river
    Meander
  11. Our flooding case study
    Storm Desmond
  12. Erosion using the sheer force of the water
    Hydraulic action
  13. Rocks are made smoother and rounder by bashing together
    Attrition
  14. Location of the flooding case study
    NW England , Cumbria
  15. dropping stuff
    Deposition
  16. Our case study river
    River Tees
  17. wearing away (with movement) of the bed and banks
    Erosion
  18. fan shaped depositis at the mouth of a river
    Delta
  19. Start of a river
    Source
  20. Flood defence on banks of river can be natural or manmande
    Levee
  21. the bit the water flows in
    Channel
  22. Bouncing of rocks along the bed of the river
    Saltation
  23. Location of river Tees
    NE England
  24. End of river
    Mouth