Erosionwearingaway (withmovement)of the bedand banksSourceStart ofa riverHydraulicactionErosionusing thesheer forceof the waterAbrasionSand papereffect of therivertransportsedimentStormDesmondOurfloodingcasestudyPlungepoolforms atthe baseof awaterfallAttritionRocks aremade smootherand rounder bybashingtogetherNEEnglandLocationof riverTeesDepositiondroppingstuffFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseLeveeFlood defenceon banks ofriver can benatural ormanmandeRiverTeesOur casestudyriverwaterfallFormedbecause of aband of hardrock in thecourse of ariverMouthEnd ofriverVshapedvalleyIn the uppercourse andshaped byverticalerosionSaltationBouncing ofrocks alongthe bed ofthe riverEstuaryThenavigablemouth ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNWEngland ,CumbriaLocationof thefloodingcase studyTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverChannelthe bitthe waterflows inTransportmovementin riversDeltafan shapeddepositis atthe mouthof a riverErosionwearingaway (withmovement)of the bedand banksSourceStart ofa riverHydraulicactionErosionusing thesheer forceof the waterAbrasionSand papereffect of therivertransportsedimentStormDesmondOurfloodingcasestudyPlungepoolforms atthe baseof awaterfallAttritionRocks aremade smootherand rounder bybashingtogetherNEEnglandLocationof riverTeesDepositiondroppingstuffFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseLeveeFlood defenceon banks ofriver can benatural ormanmandeRiverTeesOur casestudyriverwaterfallFormedbecause of aband of hardrock in thecourse of ariverMouthEnd ofriverVshapedvalleyIn the uppercourse andshaped byverticalerosionSaltationBouncing ofrocks alongthe bed ofthe riverEstuaryThenavigablemouth ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNWEngland ,CumbriaLocationof thefloodingcase studyTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverChannelthe bitthe waterflows inTransportmovementin riversDeltafan shapeddepositis atthe mouthof a river

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.


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