Erosionwearingaway (withmovement)of the bedand banksNWEngland ,CumbriaLocationof thefloodingcase studyPlungepoolforms atthe baseof awaterfallChannelthe bitthe waterflows inLeveeFlood defenceon banks ofriver can benatural ormanmandeOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverStormDesmondOurfloodingcasestudySaltationBouncing ofrocks alongthe bed ofthe riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseNEEnglandLocationof riverTeesTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverVshapedvalleyIn the uppercourse andshaped byverticalerosionSourceStart ofa riverMouthEnd ofriverDepositiondroppingstuffRiverTeesOur casestudyriverAbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverTransportmovementin riversDeltafan shapeddepositis atthe mouthof a riverHydraulicactionErosionusing thesheer forceof the waterAttritionRocks aremade smootherand rounder bybashingtogetherErosionwearingaway (withmovement)of the bedand banksNWEngland ,CumbriaLocationof thefloodingcase studyPlungepoolforms atthe baseof awaterfallChannelthe bitthe waterflows inLeveeFlood defenceon banks ofriver can benatural ormanmandeOxbowlakeformed whena meander iscut off leavinga marshy lakeareawaterfallFormedbecause of aband of hardrock in thecourse of ariverStormDesmondOurfloodingcasestudySaltationBouncing ofrocks alongthe bed ofthe riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseNEEnglandLocationof riverTeesTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverVshapedvalleyIn the uppercourse andshaped byverticalerosionSourceStart ofa riverMouthEnd ofriverDepositiondroppingstuffRiverTeesOur casestudyriverAbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverTransportmovementin riversDeltafan shapeddepositis atthe mouthof a riverHydraulicactionErosionusing thesheer forceof the waterAttritionRocks aremade smootherand rounder bybashingtogether

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