Statistics for A level Physical Geography: Coasts Part 1

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General Stats

  • This quiz has been taken 107 times
  • The average score is 11 of 42

Answer Stats

HintAnswer% Correct
Energy and matter can enter and leave the systemOpen
54%
Energy and matter cannot enter or leave the systemClosed
51%
The movement of material along a coast by waves approaching the beach at an angleLongshore Drift
51%
Occurs after weathering. Rocks fall to the cliff base and forms screeRockfall
42%
Type of rock formed only under pressure with moderate to fast erosion ratesSedimentary
42%
Layers of rockStrata
41%
Pebbles and sand are consistently thrown at the base of the cliffAbrasion
40%
Dissolved minerals are carried by the seaSolution
40%
Waves force air to be trapped in cracks within the cliff profile. Constant pressure causes the rock to crack and break apartHydraulic Action
36%
Large boulders and pebbles are rolled along the sea bedTraction
36%
As pieces of rock material are transported by waves, rock particles are worn downAttrition
35%
Small stones, pebbles and silt bounce along the sea bedSaltation
35%
Fine materials such as clay and sediment are carried by the seaSuspension
33%
Where inputs = outputsDynamic Equilibrium
32%
Type of rock formed under pressure and heat with slow ersosion ratesMetamorphic
32%
Coast that has been exposed by the sea due to a relative fall in sea levelEmergent
31%
Type of rock formed under pressure with very slow erosion ratesIgneous
31%
Very slow downhill movement of individual particlesSoil creep
28%
The general characteristics of the rocks in a particular areaLithology
26%
The movement of weathered material down a slope as a result of gravityMass Movement
26%
Saturated rock and sediment 'slumps' downwards under rotational movementSlumping
26%
Coast that has been inundated by the seaSubmergent
24%
Gradual breakdown of rock at, or close to the ground surfaceWeathering
23%
When erosional processes are selective and erode weaker areas of cliff quicker than othersDifferential Erosion
22%
The cross sectional shape of a coastlineProfile
22%
Natural breaks in strata caused by gaps in time during rock formationBedding planes
21%
When cliff profiles are composed of alkaline rocks, weak acids in seawater can dissolve themCorrosion
21%
Formed when pressure exceeds the rocks internal strength causing it to fractureFaults
21%
Saturated soil and rock flows downhill under gravityMudflow
19%
A view showing the layout of a landscape from abovePlan
19%
The shape and form of coastal landscapes and their featuresMorphology
18%
Formed under pressure duting tectonic activity, making rocks buckle and crumbleFolds
17%
The angle at which the rock strata liesDips
15%
When top soil thaws in the summer, saturated soil below flows over the subsoil and rockSolifluction
15%
Downward folds in rock strataSynclines
15%
Word meaning 'over time'Temporal
15%
The balance between sediment added to, and removed from the coastal systemSediment Budget
14%
Upward folds in rock strataAnticlines
13%
Physical features of rocks, usually formed through tectonic activityStructure
13%
Cliffs with different layers of rock, possibly formed from different time periodsComposite cliffs
10%
A combination of lithology and structure affecting the rate of processDifferential Denundation
10%
Caused by contraction when sediment dries outJoints
9%

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