Transportmovementin riversPrecipitationRocks aremade smootherand rounder bybashingtogetherFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseRiverBrunOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverDepositiondroppingstuffSourceStart ofa riverMeanderthebend ina riverErosionwearingaway (withmovement)of the bedand banksVshapedvalleyIn the uppercourse andshaped byverticalerosionCondensationLocationof riverTeesOxbowlakeformed whena meander iscut off leavinga marshy lakeareaStormsOurfloodingcasestudyChannelthe bitthe waterflows inLeveeFlood defenceon banks ofriver can benatural ormanmandeEstuaryThenavigablemouth ofa riverAbrasionSand papereffect of therivertransportsedimentSpringBouncing ofrocks alongthe bed ofthe riverBoggygroundLocationof thefloodingcase studyPlungepoolforms atthe baseof awaterfallHydraulicactionErosionusing thesheer forceof the waterMouthEnd ofriverSpurCreated when ariver erodesround area ofharder rocks inthe uppercourseTransportmovementin riversPrecipitationRocks aremade smootherand rounder bybashingtogetherFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseRiverBrunOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverDepositiondroppingstuffSourceStart ofa riverMeanderthebend ina riverErosionwearingaway (withmovement)of the bedand banksVshapedvalleyIn the uppercourse andshaped byverticalerosionCondensationLocationof riverTeesOxbowlakeformed whena meander iscut off leavinga marshy lakeareaStormsOurfloodingcasestudyChannelthe bitthe waterflows inLeveeFlood defenceon banks ofriver can benatural ormanmandeEstuaryThenavigablemouth ofa riverAbrasionSand papereffect of therivertransportsedimentSpringBouncing ofrocks alongthe bed ofthe riverBoggygroundLocationof thefloodingcase studyPlungepoolforms atthe baseof awaterfallHydraulicactionErosionusing thesheer forceof the waterMouthEnd ofriverSpurCreated when ariver erodesround area ofharder rocks inthe uppercourse

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