RiverTeesOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverMouthEnd ofriverPlungepoolforms atthe baseof awaterfallStormDesmondOurfloodingcasestudyDepositiondroppingstuffErosionwearingaway (withmovement)of the bedand banksFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNEEnglandLocationof riverTeesChannelthe bitthe waterflows inSaltationBouncing ofrocks alongthe bed ofthe riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseAbrasionSand papereffect of therivertransportsedimentVshapedvalleyIn the uppercourse andshaped byverticalerosionLeveeFlood defenceon banks ofriver can benatural ormanmandeMeanderthebend ina riverNWEngland ,CumbriaLocationof thefloodingcase studyAttritionRocks aremade smootherand rounder bybashingtogetherSourceStart ofa riverEstuaryThenavigablemouth ofa riverTransportmovementin riversRiverTeesOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverMouthEnd ofriverPlungepoolforms atthe baseof awaterfallStormDesmondOurfloodingcasestudyDepositiondroppingstuffErosionwearingaway (withmovement)of the bedand banksFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNEEnglandLocationof riverTeesChannelthe bitthe waterflows inSaltationBouncing ofrocks alongthe bed ofthe riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseAbrasionSand papereffect of therivertransportsedimentVshapedvalleyIn the uppercourse andshaped byverticalerosionLeveeFlood defenceon banks ofriver can benatural ormanmandeMeanderthebend ina riverNWEngland ,CumbriaLocationof thefloodingcase studyAttritionRocks aremade smootherand rounder bybashingtogetherSourceStart ofa riverEstuaryThenavigablemouth ofa riverTransportmovementin rivers

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