SaltationBouncing ofrocks alongthe bed ofthe riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverStormDesmondOurfloodingcasestudyOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMouthEnd ofriverDepositiondroppingstuffTransportmovementin riversNEEnglandLocationof riverTeesEstuaryThenavigablemouth ofa riverRiverTeesOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverHydraulicactionErosionusing thesheer forceof the waterLeveeFlood defenceon banks ofriver can benatural ormanmandeFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseNWEngland ,CumbriaLocationof thefloodingcase studyVshapedvalleyIn the uppercourse andshaped byverticalerosionAbrasionSand papereffect of therivertransportsedimentErosionwearingaway (withmovement)of the bedand banksPlungepoolforms atthe baseof awaterfallSourceStart ofa riverChannelthe bitthe waterflows inAttritionRocks aremade smootherand rounder bybashingtogetherMeanderthebend ina riverSaltationBouncing ofrocks alongthe bed ofthe riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverStormDesmondOurfloodingcasestudyOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMouthEnd ofriverDepositiondroppingstuffTransportmovementin riversNEEnglandLocationof riverTeesEstuaryThenavigablemouth ofa riverRiverTeesOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverHydraulicactionErosionusing thesheer forceof the waterLeveeFlood defenceon banks ofriver can benatural ormanmandeFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseNWEngland ,CumbriaLocationof thefloodingcase studyVshapedvalleyIn the uppercourse andshaped byverticalerosionAbrasionSand papereffect of therivertransportsedimentErosionwearingaway (withmovement)of the bedand banksPlungepoolforms atthe baseof awaterfallSourceStart ofa riverChannelthe bitthe waterflows inAttritionRocks aremade smootherand rounder bybashingtogetherMeanderthebend ina 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.


1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
  1. Bouncing of rocks along the bed of the river
    Saltation
  2. Formed because of a band of hard rock in the course of a river
    waterfall
  3. Our flooding case study
    Storm Desmond
  4. formed when a meander is cut off leaving a marshy lake area
    Ox bow lake
  5. End of river
    Mouth
  6. dropping stuff
    Deposition
  7. movement in rivers
    Transport
  8. Location of river Tees
    NE England
  9. The navigable mouth of a river
    Estuary
  10. Our case study river
    River Tees
  11. fan shaped depositis at the mouth of a river
    Delta
  12. Erosion using the sheer force of the water
    Hydraulic action
  13. Flood defence on banks of river can be natural or manmande
    Levee
  14. The area either side of a river that floods especially in the lower course
    Flood plain
  15. Created when a river erodes round area of harder rocks in the upper course
    Truncated spur
  16. Location of the flooding case study
    NW England , Cumbria
  17. In the upper course and shaped by vertical erosion
    V shaped valley
  18. Sand paper effect of the river transport sediment
    Abrasion
  19. wearing away (with movement) of the bed and banks
    Erosion
  20. forms at the base of a waterfall
    Plunge pool
  21. Start of a river
    Source
  22. the bit the water flows in
    Channel
  23. Rocks are made smoother and rounder by bashing together
    Attrition
  24. the bend in a river
    Meander