AbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverLeveeFlood defenceon banks ofriver can benatural ormanmandeDeltafan shapeddepositis atthe mouthof a riverMeanderthebend ina riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseBoggygroundLocationof thefloodingcase studyStormsOurfloodingcasestudywaterfallFormedbecause of aband of hardrock in thecourse of ariverSourceStart ofa riverTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksPrecipitationRocks aremade smootherand rounder bybashingtogetherHydraulicactionErosionusing thesheer forceof the waterPlungepoolforms atthe baseof awaterfallRiverBrunOur casestudyriverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaSpringBouncing ofrocks alongthe bed ofthe riverSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseChannelthe bitthe waterflows inDepositiondroppingstuffVshapedvalleyIn the uppercourse andshaped byverticalerosionMouthEnd ofriverCondensationLocationof riverTeesAbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverLeveeFlood defenceon banks ofriver can benatural ormanmandeDeltafan shapeddepositis atthe mouthof a riverMeanderthebend ina riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseBoggygroundLocationof thefloodingcase studyStormsOurfloodingcasestudywaterfallFormedbecause of aband of hardrock in thecourse of ariverSourceStart ofa riverTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksPrecipitationRocks aremade smootherand rounder bybashingtogetherHydraulicactionErosionusing thesheer forceof the waterPlungepoolforms atthe baseof awaterfallRiverBrunOur casestudyriverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaSpringBouncing ofrocks alongthe bed ofthe riverSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseChannelthe bitthe waterflows inDepositiondroppingstuffVshapedvalleyIn the uppercourse andshaped byverticalerosionMouthEnd ofriverCondensationLocationof riverTees

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