SaltationBouncing ofrocks alongthe bed ofthe riverNEEnglandLocationof riverTeesOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverMeanderthebend ina riverNWEngland ,CumbriaLocationof thefloodingcase studyAbrasionSand papereffect of therivertransportsedimentDepositiondroppingstuffTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseStormDesmondOurfloodingcasestudySourceStart ofa riverPlungepoolforms atthe baseof awaterfallAttritionRocks aremade smootherand rounder bybashingtogetherRiverTeesOur casestudyriverTransportmovementin riversMouthEnd ofriverHydraulicactionErosionusing thesheer forceof the waterChannelthe bitthe waterflows inFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseErosionwearingaway (withmovement)of the bedand banksEstuaryThenavigablemouth ofa riverVshapedvalleyIn the uppercourse andshaped byverticalerosionLeveeFlood defenceon banks ofriver can benatural ormanmandeDeltafan shapeddepositis atthe mouthof a riverSaltationBouncing ofrocks alongthe bed ofthe riverNEEnglandLocationof riverTeesOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverMeanderthebend ina riverNWEngland ,CumbriaLocationof thefloodingcase studyAbrasionSand papereffect of therivertransportsedimentDepositiondroppingstuffTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseStormDesmondOurfloodingcasestudySourceStart ofa riverPlungepoolforms atthe baseof awaterfallAttritionRocks aremade smootherand rounder bybashingtogetherRiverTeesOur casestudyriverTransportmovementin riversMouthEnd ofriverHydraulicactionErosionusing thesheer forceof the waterChannelthe bitthe waterflows inFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseErosionwearingaway (withmovement)of the bedand banksEstuaryThenavigablemouth ofa riverVshapedvalleyIn the uppercourse andshaped byverticalerosionLeveeFlood defenceon banks ofriver can benatural ormanmandeDeltafan shapeddepositis atthe mouthof a river

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