Deltafan shapeddepositis atthe mouthof a riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseRiverTeesOur casestudyriverMouthEnd ofriverAttritionRocks aremade smootherand rounder bybashingtogetherMeanderthebend ina riverAbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNWEngland ,CumbriaLocationof thefloodingcase studyTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercoursewaterfallFormedbecause of aband of hardrock in thecourse of ariverVshapedvalleyIn the uppercourse andshaped byverticalerosionNEEnglandLocationof riverTeesLeveeFlood defenceon banks ofriver can benatural ormanmandeChannelthe bitthe waterflows inStormDesmondOurfloodingcasestudyTransportmovementin riversSourceStart ofa riverHydraulicactionErosionusing thesheer forceof the waterSaltationBouncing ofrocks alongthe bed ofthe riverDepositiondroppingstuffPlungepoolforms atthe baseof awaterfallErosionwearingaway (withmovement)of the bedand banksDeltafan shapeddepositis atthe mouthof a riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseRiverTeesOur casestudyriverMouthEnd ofriverAttritionRocks aremade smootherand rounder bybashingtogetherMeanderthebend ina riverAbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNWEngland ,CumbriaLocationof thefloodingcase studyTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercoursewaterfallFormedbecause of aband of hardrock in thecourse of ariverVshapedvalleyIn the uppercourse andshaped byverticalerosionNEEnglandLocationof riverTeesLeveeFlood defenceon banks ofriver can benatural ormanmandeChannelthe bitthe waterflows inStormDesmondOurfloodingcasestudyTransportmovementin riversSourceStart ofa riverHydraulicactionErosionusing thesheer forceof the waterSaltationBouncing ofrocks alongthe bed ofthe riverDepositiondroppingstuffPlungepoolforms atthe baseof awaterfallErosionwearingaway (withmovement)of the bedand banks

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