waterfallFormedbecause of aband of hardrock in thecourse of ariverStormsOurfloodingcasestudyPrecipitationRocks aremade smootherand rounder bybashingtogetherSourceStart ofa riverPlungepoolforms atthe baseof awaterfallMeanderthebend ina riverSpringBouncing ofrocks alongthe bed ofthe riverErosionwearingaway (withmovement)of the bedand banksVshapedvalleyIn the uppercourse andshaped byverticalerosionAbrasionSand papereffect of therivertransportsedimentDepositiondroppingstuffLeveeFlood defenceon banks ofriver can benatural ormanmandeTransportmovementin riversSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseOxbowlakeformed whena meander iscut off leavinga marshy lakeareaRiverBrunOur casestudyriverBoggygroundLocationof thefloodingcase studyDeltafan shapeddepositis atthe mouthof a riverCondensationLocationof riverTeesEstuaryThenavigablemouth ofa riverHydraulicactionErosionusing thesheer forceof the waterMouthEnd ofriverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseChannelthe bitthe waterflows inwaterfallFormedbecause of aband of hardrock in thecourse of ariverStormsOurfloodingcasestudyPrecipitationRocks aremade smootherand rounder bybashingtogetherSourceStart ofa riverPlungepoolforms atthe baseof awaterfallMeanderthebend ina riverSpringBouncing ofrocks alongthe bed ofthe riverErosionwearingaway (withmovement)of the bedand banksVshapedvalleyIn the uppercourse andshaped byverticalerosionAbrasionSand papereffect of therivertransportsedimentDepositiondroppingstuffLeveeFlood defenceon banks ofriver can benatural ormanmandeTransportmovementin riversSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseOxbowlakeformed whena meander iscut off leavinga marshy lakeareaRiverBrunOur casestudyriverBoggygroundLocationof thefloodingcase studyDeltafan shapeddepositis atthe mouthof a riverCondensationLocationof riverTeesEstuaryThenavigablemouth ofa riverHydraulicactionErosionusing thesheer forceof the waterMouthEnd ofriverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseChannelthe bitthe waterflows in

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