1.b. Coastal landscape systems are influenced by a range of physical factors. Flashcards
Potential influences on coastal landscape systems of:
- winds, including speed, direction and frequency
Wind speed, direction + frequency DETERMINES WAVE ENERGY
Speed-
Faster + stronger winds -> more energy -> higher energy waves -> destructive waves -> higher rates of erosion
Waves with less energy -> deposit more -> building the beach
Direction-
Direction of prevailing wind -> determines direction of LSD -> landforms such as spits and bars can form
Frequency-
more winds -> more aeolian processes -> coastline will be shaped by winds
Fetch= distance wind has travelled over uninterrupted water
Long fetch = more wave energy
Potential influences on coastal landscape systems of:
- waves, including wave formation, development and breaking
Wind speed, direction + frequency DETERMINES WAVE ENERGY
Constructive
- Low energy
- Stronger swash than backwash -> adding sediment to the beach -> net gain
- Lower frequency (6-8 per min)
- Lower and longer waves
versus
Destructive
- High energy
- Stronger backwash than swash -> takes sediment away from beach -> net loss
- Higher frequency (11-14 per min)
- Taller and shorter waves
Different types of breaking waves-
- spilling
- surging
- plunging
-> effects beach profile
Potential influences on coastal landscape systems of:
- tides, including tidal cycles and range
Short term changes in sea level determined by the gravitation pull of the moon -> high tide follows the moon
When the sun + moon are aligned -> strong gravitational pull
-> spring tides with high tidal ranges
When the sun + moon are at right angles to each other -> week gravitational pull
-> neap tides with low ridal ranges
Neap and spring tides -> differing tidal range -> effects rates of erosion of landforms
Evaluation- these are short term changes -> therefore having limited long term effects on the coastline
Potential influences on coastal landscape systems of:
- geology, including lithology and structure
Lithology = the composition of rocks -> including chemical and physical composition
Structure= the properties of rocks -> including joins, cracks + pores
- how reactive minerals in the rock are -> effects rate of chemical weathering
- whether the rocks are clastic or
crystalline:
clastic - sediment particles cemented together
these are sedimentary rocks e.g. sandstone and clay
crystalline- interlocking mineral crystals
these are indigenous e.g. granite and metamorphic rocks e.g. marble
- the amount of joints, cracks + pores -> these weaknesses are exploited by erosion and weathering
sedimentary rocks also may have bedding planes- more vulnerable to erosion
the angle the bedding planes are pointing -> influences cliff profile -> landward + horizontal = steep vs seaward = gentle
how rocks lie on a coastline-
discordant =
alternating bands of hard and soft rock lie PERPENDICULAR to the coastline -> formation of headland + bays
concordant =
alternating bands of hard and soft rock lie PARALLEL to the coastline -> straighter coastline -> coves can form
Potential influences on coastal landscape systems of:
- global pattern of ocean currents.
The global masses of water -> that transfer heat around the planet
Warm ocean currents = low latitudes -> polar regions
Cold ocean currents = polar regions -> low latitudes
Evaluation- has little effect on coastal processes -> however directly impacts air temperature -> therefore sub-aerial processes of weathering + mass movement
rip currents-
help transport sediment
either caused by tidal motion or waves breaking at right angles to the shore
a cellular circular is created when the wave returns to the sea -> this is created by differing wave heights
wave with a larger height breaks on the beach and when it returns back to the sea, dragging back the wave with the lower height
this movement of water can produce cups on the shoreline