Plungepoolforms atthe baseof awaterfallBoggygroundLocationof thefloodingcase studyDeltafan shapeddepositis atthe mouthof a riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverSourceStart ofa riverPrecipitationRocks aremade smootherand rounder bybashingtogetherStormsOurfloodingcasestudyLeveeFlood defenceon banks ofriver can benatural ormanmandeAbrasionSand papereffect of therivertransportsedimentHydraulicactionErosionusing thesheer forceof the waterRiverBrunOur casestudyriverVshapedvalleyIn the uppercourse andshaped byverticalerosionTransportmovementin riversDepositiondroppingstuffCondensationLocationof riverTeesSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverMouthEnd ofriverEstuaryThenavigablemouth ofa riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseSpringBouncing ofrocks alongthe bed ofthe riverChannelthe bitthe waterflows inErosionwearingaway (withmovement)of the bedand banksPlungepoolforms atthe baseof awaterfallBoggygroundLocationof thefloodingcase studyDeltafan shapeddepositis atthe mouthof a riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverSourceStart ofa riverPrecipitationRocks aremade smootherand rounder bybashingtogetherStormsOurfloodingcasestudyLeveeFlood defenceon banks ofriver can benatural ormanmandeAbrasionSand papereffect of therivertransportsedimentHydraulicactionErosionusing thesheer forceof the waterRiverBrunOur casestudyriverVshapedvalleyIn the uppercourse andshaped byverticalerosionTransportmovementin riversDepositiondroppingstuffCondensationLocationof riverTeesSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverMouthEnd ofriverEstuaryThenavigablemouth ofa riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseSpringBouncing ofrocks alongthe bed ofthe riverChannelthe bitthe waterflows inErosionwearingaway (withmovement)of the bedand banks

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