EstuaryThenavigablemouth ofa riverMeanderthebend ina riverSourceStart ofa riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseLeveeFlood defenceon banks ofriver can benatural ormanmandeMouthEnd ofriverCondensationLocationof riverTeesErosionwearingaway (withmovement)of the bedand banksHydraulicactionErosionusing thesheer forceof the waterwaterfallFormedbecause of aband of hardrock in thecourse of ariverDeltafan shapeddepositis atthe mouthof a riverVshapedvalleyIn the uppercourse andshaped byverticalerosionOxbowlakeformed whena meander iscut off leavinga marshy lakeareaTransportmovementin riversDepositiondroppingstuffPlungepoolforms atthe baseof awaterfallChannelthe bitthe waterflows inSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseSpringBouncing ofrocks alongthe bed ofthe riverAbrasionSand papereffect of therivertransportsedimentRiverBrunOur casestudyriverBoggygroundLocationof thefloodingcase studyPrecipitationRocks aremade smootherand rounder bybashingtogetherStormsOurfloodingcasestudyEstuaryThenavigablemouth ofa riverMeanderthebend ina riverSourceStart ofa riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseLeveeFlood defenceon banks ofriver can benatural ormanmandeMouthEnd ofriverCondensationLocationof riverTeesErosionwearingaway (withmovement)of the bedand banksHydraulicactionErosionusing thesheer forceof the waterwaterfallFormedbecause of aband of hardrock in thecourse of ariverDeltafan shapeddepositis atthe mouthof a riverVshapedvalleyIn the uppercourse andshaped byverticalerosionOxbowlakeformed whena meander iscut off leavinga marshy lakeareaTransportmovementin riversDepositiondroppingstuffPlungepoolforms atthe baseof awaterfallChannelthe bitthe waterflows inSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseSpringBouncing ofrocks alongthe bed ofthe riverAbrasionSand papereffect of therivertransportsedimentRiverBrunOur casestudyriverBoggygroundLocationof thefloodingcase studyPrecipitationRocks aremade smootherand rounder bybashingtogetherStormsOurfloodingcasestudy

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