| Term |
 |
|
| Definition |
 |
|
| Details |
 |
|
| Type |
 |
|
| Onshore |
A movement from sea to land |
Usually used to descibe winds |
Coastal Environment
|
| Backshore |
The beach area, landward of the foreshore above the normal reach of the tides, that provides the primary protection from the hinterland |
|
Coastal Environment |
| Intertidal and Nearshore |
Zone of land between highest and lowest tides |
In low-lying areas i.e mudflats, this can be very extensive and important ecologically |
Coastal Environment |
| Offshore Zone |
A zone that is seaward of the breakpoint |
This may include features such as offshore bars |
Coastal Environment |
| Coast |
The area where landmasses meet the sea |
Often used to encompass the zones on either side of the shoreline |
Coastal Environment |
| Coastline/Shoreline |
A line used in the analysis of shoreline evolution |
It represents the cliff top edge on cliffed coasts, edge of hard defences where these exist, and the backshore/ hinter |
Coastal Environment |
| Coastal Zonation |
The identification of areas of coast often for planning purposes |
The term may refer to zones such as offshore, onshore or to sections of the coast sharing common marine processes. |
Coastal Environment |
| Littoral Zone |
The environmental zone that exists between the highest and lowest levels of the spring tides. |
|
Coastal Environment |
| Beach System |
The inputs, outputs, transfers, processes and stores that interact with each other on the beach |
(blank) |
System |
| Coastal System |
The inputs, outputs, transfers, processes and stores that interact with each other along the coast |
(blank) |
System |
| Littoral Cells |
Offshore littoral zones within which the circulation of sediment through longshore drift and other processes, is relatively self contained. |
11 such zones have been identified for England and Wales |
System |
| Sediment Sinks |
These occur when sediment movements meet and material is lost from marine circulation |
They are often associated with the creation of depositional features |
System |
| Dynamic Equilibrium |
The balance between inputs and outputs in a system |
It is linked to the concept of "steady state" |
System |
| Storm Surge |
A rapid rise in sea level brought about by a combination of factors. |
These factors include; - High sring tides - strong onshore winds - funneling of water into narrow coastal zones - very low atmospheric pressure - esturine rivers at flood level due to prolonged rainfall. |
System |
| Storm Event |
An exceptionally powerful storm with associated geomorphological consequences i.e the creation of a new storm beach |
(blank) |
System |
| Structure |
Geological features |
i.e folding and faulting |
Physical Factor AC |
| Lithology |
Rock Type |
(blank) |
Physical Factor AC |
| Differential Erosion |
The erosion of different geological elements at different rates due to variations. |
i.e lithology or faulting which may lead to features such as headlands and bays. |
Physical Factor AC |
| Fault Zone |
Area of rocks with a high degree of faulting, making it prone to erosion |
(blank) |
Physical Factor AC |
| Jointing |
Fractures in rocks that do not involve faulting |
(blank) |
Physical Factor AC |
| Bedding Plane |
Surface within a rock that is parallel to the surface of deposition |
Often associated with cracks that may lead to erosion |
Physical Factor AC |
| Concordant Features |
Features that occur where geological structures run parallel with the coast |
(blank) |
Physical Factor AC |
| Discordant Features |
Features which occur when structures run at right angles to the coast |
(blank) |
Physical Factor AC |
| Wave Frequency |
The number of waves per minute |
(blank) |
Physical Factor AC |
| Fetch |
The distance that a wave travels before breaking |
(blank) |
Physical Factors AC |
| Dominant Wind |
The wind direction that has the principal impact on marine processes in an area |
(blank) |
Physical Factor AC |
| Prevailing Wind |
The wand that blows most frequently in an area |
It is often the dominant wind |
Physical Factor AC |
| Corrasion |
Erosion caused by pebbles and rock fragments hitting the beach or cliff rocks. |
(blank) |
C Process |
| Abrasion |
Another term for corrasion |
(blank) |
C Process |
| Corrosion |
Erosion brought about by chemical action on rocks |
(blank) |
C Process |
| Hydraulic Action |
Erosion brought about by the pressure of water on cliffs and beaches. |
(blank) |
C Process |
| Wave Refraction |
The "bending" of a wave due to friction as its base touches the seabed |
(blank) |
C Process |
| Longshore Drift |
The movement of material along a beach caused by waves (swash) striking the beach at an angle, and the backwash returning at right angles |
(blank) |
C Process |
| Rip Currents |
Fast flowing backwash that can scour beach channels |
(blank) |
C Process |
| Tides |
The periodic rises and falls of sea level due to the gravitational action of the sun and moon |
(blank) |
C Process |
| Micro-Tidal Environment |
The zone of littoral affected by tidal action |
It has particular relevance to ecological systems |
C Process |
| Swash |
Water moving up a beach after a wave has broken |
(blank) |
C Process |
| Backwash |
The movement of water back down a beach due to gravity |
(blank) |
C Process |
| Sub-aerial Erosion |
Non-marine erosional processes that occur on cliff and beach surfaces |
(blank) |
C Process |
| Rotational Slipping |
Landslipping that occurs on a curved plane |
It is often caused by weak underlying rocks giving way during saturation |
C Process |
| Slumping |
Movement of material down a slope, under gravity, but lubricated by water |
(blank) |
C Process |
| Flow |
The movement of liquid or semi-liquid material downslope e.g on a cliff face |
(blank) |
C Process |
| Landslide |
Movement of dry material downslope (due to gravity) with no lubrication |
(blank) |
C Process |
| Long Term Changes |
Long Term - permanent changes that occur quickly or slowly |
(blank) |
C Process |
| Short Term Changes |
Changes that happen relatively quickly and usually regarded as temporary |
(blank) |
C Process |
| Active Cliffs |
Cliffs undergoing active erosion |
(blank) |
C Landforms |
| Degraded Cliffs |
Non-active cliffs |
(blank) |
C Landforms |
| Wave-cut notch |
An "undercut" or notch at the base of a cliff caused by marine erosion |
(blank) |
C Landforms |
| Wave-cut flatform |
A gently sloping platform (less than 4o) at the base of the cliff, cut by marine action |
(blank) |
C Landfrorms |
| Cliff Profile |
The verticle outline or cross-section of a cliff |
(blank) |
C Landforms |
| Sea Cave |
Hollow cut in a cliff by marine action |
eg. limestone caves Llantwit Major |
C Landforms |
| Sea Arch |
Arch in a cliff cut by marine action |
eg. Durdle Door, Dorset |
C Landform |
| Stack |
Tall remnant of a cliff, left isolated by marine action |
eg. The Needles |
C Landform |
| Stump |
Short remnant of a cliff, left isolated by marine action |
(blank) |
C Landform |
| Geo |
Steep sided inlet cut by marine action |
(blank) |
C Landform |
| Beach |
The deposit of non-cohesive material on the interface between dry land and the sea |
(blank) |
C Landform |
| Beach Cusps |
Small "embayments" found on beaches that channel swash to their centres, thus maintaining their form |
(blank) |
C Landform |
| Beach Profile |
Vertical cross section of a beach |
(blank) |
C Landform |
| Storm Beach |
A line of coarse material deposited on the upper beach during a storm |
(blank) |
C Landform |
| Berm |
Ridge of coarse material on the upper beach deposited by spring tides and storms |
(blank) |
C Landforms |
| Spit |
Long strip of shingle joined to the coast |
This results from marine deposition |
C Landforms |
| Bar |
Offshore deposit of sand or shingle |
(blank) |
C Landform |
| Tombolo |
Island linked to mainland by a depositional feature such as a spit |
(blank) |
C Landform |
| Sea Level Changes |
Can be positive, negative, eustatic, isostatic |
Positive (a sea level rise relative to the land), Negative ( a sea level fall relative to the land), Eustatic ( changes caused by sea volume changes ie. global warming), Isostatic (changes brought about by vertical land movements ie. melting of glaciers) |
C Landform |
| Raised Beach |
Old becah left "high and dry" by falling sea level |
(blank) |
C Landform |
| Fjord |
Glacial valley drowned by sea level rise to form narrow, steep sided inlet |
(blank) |
C Landform |
| Ria |
Steep sided river valley drowned by sea level rise |
e.g Dartmouth |
C Landform |
| Estuaries |
Lower stretches of rivers that are tidal - often drowned by post-glacial sea level rise |
eg. Southhampton Water |
C Landform |