waterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterNWEngland ,CumbriaLocationof thefloodingcase studyOxbowlakeformed whena meander iscut off leavinga marshy lakeareaLeveeFlood defenceon banks ofriver can benatural ormanmandeNEEnglandLocationof riverTeesFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseChannelthe bitthe waterflows inDeltafan shapeddepositis atthe mouthof a riverTransportmovementin riversSourceStart ofa riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseSaltationBouncing ofrocks alongthe bed ofthe riverStormDesmondOurfloodingcasestudyMeanderthebend ina riverAttritionRocks aremade smootherand rounder bybashingtogetherAbrasionSand papereffect of therivertransportsedimentMouthEnd ofriverVshapedvalleyIn the uppercourse andshaped byverticalerosionDepositiondroppingstuffPlungepoolforms atthe baseof awaterfallRiverTeesOur casestudyriverErosionwearingaway (withmovement)of the bedand banksEstuaryThenavigablemouth ofa riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterNWEngland ,CumbriaLocationof thefloodingcase studyOxbowlakeformed whena meander iscut off leavinga marshy lakeareaLeveeFlood defenceon banks ofriver can benatural ormanmandeNEEnglandLocationof riverTeesFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseChannelthe bitthe waterflows inDeltafan shapeddepositis atthe mouthof a riverTransportmovementin riversSourceStart ofa riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseSaltationBouncing ofrocks alongthe bed ofthe riverStormDesmondOurfloodingcasestudyMeanderthebend ina riverAttritionRocks aremade smootherand rounder bybashingtogetherAbrasionSand papereffect of therivertransportsedimentMouthEnd ofriverVshapedvalleyIn the uppercourse andshaped byverticalerosionDepositiondroppingstuffPlungepoolforms atthe baseof awaterfallRiverTeesOur casestudyriverErosionwearingaway (withmovement)of the bedand banksEstuaryThenavigablemouth ofa 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. Formed because of a band of hard rock in the course of a river
    waterfall
  2. Erosion using the sheer force of the water
    Hydraulic action
  3. Location of the flooding case study
    NW England , Cumbria
  4. formed when a meander is cut off leaving a marshy lake area
    Ox bow lake
  5. Flood defence on banks of river can be natural or manmande
    Levee
  6. Location of river Tees
    NE England
  7. The area either side of a river that floods especially in the lower course
    Flood plain
  8. the bit the water flows in
    Channel
  9. fan shaped depositis at the mouth of a river
    Delta
  10. movement in rivers
    Transport
  11. Start of a river
    Source
  12. Created when a river erodes round area of harder rocks in the upper course
    Truncated spur
  13. Bouncing of rocks along the bed of the river
    Saltation
  14. Our flooding case study
    Storm Desmond
  15. the bend in a river
    Meander
  16. Rocks are made smoother and rounder by bashing together
    Attrition
  17. Sand paper effect of the river transport sediment
    Abrasion
  18. End of river
    Mouth
  19. In the upper course and shaped by vertical erosion
    V shaped valley
  20. dropping stuff
    Deposition
  21. forms at the base of a waterfall
    Plunge pool
  22. Our case study river
    River Tees
  23. wearing away (with movement) of the bed and banks
    Erosion
  24. The navigable mouth of a river
    Estuary