AbrasionSand papereffect of therivertransportsedimentDepositiondroppingstuffMeanderthebend ina riverEstuaryThenavigablemouth ofa riverStormDesmondOurfloodingcasestudyHydraulicactionErosionusing thesheer forceof the waterChannelthe bitthe waterflows inMouthEnd ofriverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaVshapedvalleyIn the uppercourse andshaped byverticalerosionSaltationBouncing ofrocks alongthe bed ofthe riverNEEnglandLocationof riverTeesAttritionRocks aremade smootherand rounder bybashingtogetherSourceStart ofa riverNWEngland ,CumbriaLocationof thefloodingcase studyTransportmovementin riversPlungepoolforms atthe baseof awaterfallRiverTeesOur casestudyriverwaterfallFormedbecause of aband of hardrock in thecourse of ariverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseErosionwearingaway (withmovement)of the bedand banksDeltafan shapeddepositis atthe mouthof a riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseLeveeFlood defenceon banks ofriver can benatural ormanmandeAbrasionSand papereffect of therivertransportsedimentDepositiondroppingstuffMeanderthebend ina riverEstuaryThenavigablemouth ofa riverStormDesmondOurfloodingcasestudyHydraulicactionErosionusing thesheer forceof the waterChannelthe bitthe waterflows inMouthEnd ofriverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaVshapedvalleyIn the uppercourse andshaped byverticalerosionSaltationBouncing ofrocks alongthe bed ofthe riverNEEnglandLocationof riverTeesAttritionRocks aremade smootherand rounder bybashingtogetherSourceStart ofa riverNWEngland ,CumbriaLocationof thefloodingcase studyTransportmovementin riversPlungepoolforms atthe baseof awaterfallRiverTeesOur casestudyriverwaterfallFormedbecause of aband of hardrock in thecourse of ariverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseErosionwearingaway (withmovement)of the bedand banksDeltafan shapeddepositis atthe mouthof a riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseLeveeFlood defenceon banks ofriver can benatural ormanmande

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