DepositiondroppingstuffOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseRiverBrunOur casestudyriverTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseSourceStart ofa riverVshapedvalleyIn the uppercourse andshaped byverticalerosionStormsOurfloodingcasestudyEstuaryThenavigablemouth ofa riverChannelthe bitthe waterflows inMeanderthebend ina riverBoggygroundLocationof thefloodingcase studyPrecipitationRocks aremade smootherand rounder bybashingtogetherLeveeFlood defenceon banks ofriver can benatural ormanmandeAbrasionSand papereffect of therivertransportsedimentHydraulicactionErosionusing thesheer forceof the waterPlungepoolforms atthe baseof awaterfallSpringBouncing ofrocks alongthe bed ofthe riverDeltafan shapeddepositis atthe mouthof a riverCondensationLocationof riverTeesMouthEnd ofriverDepositiondroppingstuffOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseRiverBrunOur casestudyriverTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseSourceStart ofa riverVshapedvalleyIn the uppercourse andshaped byverticalerosionStormsOurfloodingcasestudyEstuaryThenavigablemouth ofa riverChannelthe bitthe waterflows inMeanderthebend ina riverBoggygroundLocationof thefloodingcase studyPrecipitationRocks aremade smootherand rounder bybashingtogetherLeveeFlood defenceon banks ofriver can benatural ormanmandeAbrasionSand papereffect of therivertransportsedimentHydraulicactionErosionusing thesheer forceof the waterPlungepoolforms atthe baseof awaterfallSpringBouncing ofrocks alongthe bed ofthe riverDeltafan shapeddepositis atthe mouthof a riverCondensationLocationof 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.


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