| Hint | Answer | % Correct |
|---|---|---|
| Energy and matter cannot enter or leave the system | Closed | 55%
|
| The movement of material along a coast by waves approaching the beach at an angle | Longshore Drift | 55%
|
| Energy and matter can enter and leave the system | Open | 55%
|
| Pebbles and sand are consistently thrown at the base of the cliff | Abrasion | 47%
|
| Dissolved minerals are carried by the sea | Solution | 46%
|
| Layers of rock | Strata | 45%
|
| Large boulders and pebbles are rolled along the sea bed | Traction | 43%
|
| Waves force air to be trapped in cracks within the cliff profile. Constant pressure causes the rock to crack and break apart | Hydraulic Action | 41%
|
| As pieces of rock material are transported by waves, rock particles are worn down | Attrition | 39%
|
| Occurs after weathering. Rocks fall to the cliff base and forms scree | Rockfall | 39%
|
| Small stones, pebbles and silt bounce along the sea bed | Saltation | 39%
|
| Type of rock formed only under pressure with moderate to fast erosion rates | Sedimentary | 39%
|
| Type of rock formed under pressure and heat with slow ersosion rates | Metamorphic | 35%
|
| Where inputs = outputs | Dynamic Equilibrium | 34%
|
| Fine materials such as clay and sediment are carried by the sea | Suspension | 34%
|
| Type of rock formed under pressure with very slow erosion rates | Igneous | 32%
|
| Very slow downhill movement of individual particles | Soil creep | 31%
|
| The movement of weathered material down a slope as a result of gravity | Mass Movement | 29%
|
| Coast that has been exposed by the sea due to a relative fall in sea level | Emergent | 26%
|
| Saturated rock and sediment 'slumps' downwards under rotational movement | Slumping | 25%
|
| Saturated soil and rock flows downhill under gravity | Mudflow | 24%
|
| Gradual breakdown of rock at, or close to the ground surface | Weathering | 24%
|
| The general characteristics of the rocks in a particular area | Lithology | 23%
|
| When erosional processes are selective and erode weaker areas of cliff quicker than others | Differential Erosion | 19%
|
| Coast that has been inundated by the sea | Submergent | 19%
|
| The cross sectional shape of a coastline | Profile | 17%
|
| The balance between sediment added to, and removed from the coastal system | Sediment Budget | 17%
|
| When cliff profiles are composed of alkaline rocks, weak acids in seawater can dissolve them | Corrosion | 16%
|
| Formed when pressure exceeds the rocks internal strength causing it to fracture | Faults | 16%
|
| A view showing the layout of a landscape from above | Plan | 16%
|
| Natural breaks in strata caused by gaps in time during rock formation | Bedding planes | 15%
|
| The shape and form of coastal landscapes and their features | Morphology | 15%
|
| Word meaning 'over time' | Temporal | 13%
|
| Formed under pressure duting tectonic activity, making rocks buckle and crumble | Folds | 12%
|
| When top soil thaws in the summer, saturated soil below flows over the subsoil and rock | Solifluction | 12%
|
| The angle at which the rock strata lies | Dips | 11%
|
| Downward folds in rock strata | Synclines | 10%
|
| Upward folds in rock strata | Anticlines | 8%
|
| Physical features of rocks, usually formed through tectonic activity | Structure | 8%
|
| Cliffs with different layers of rock, possibly formed from different time periods | Composite cliffs | 6%
|
| A combination of lithology and structure affecting the rate of process | Differential Denundation | 6%
|
| Caused by contraction when sediment dries out | Joints | 5%
|