3 reasons why our coastlines are important
The littoral zone is….
Area of shoreline from sea to land - the coastal zone in which sediments are moved around between land, beach and sea.
This zone is subdivided into:
The backshore is….
The area between high tide and the land
The foreshore is….
The area between high tide and low tide
The nearshore is….
The area between low tide and point where waves break - ‘breaker zone’
The offshore is….
The area of the sea where deposition, transport and erosion no longer affects the coastline - zone is seawards
3 Inputs which affect the coastline:
3 Processes which affect the coastline:
3 Outputs which affect the coastline:
The 3 different types of coastline is:
High energy coastlines are:
Rocky coasts where waves are powerful for the most of the year - erosion land-forms are found
Low energy coastlines are:
sandy coastlines - constructive waves dominate - deposition landforms are found
Coastal plain coastlines are:
Areas of low,flat relief. Can be susceptible to coastal flooding
Other two ways of classifying coasts more broadly:
-rocky coastlines
- coastal plains
Rocky coastlines:
Coastal plains:
Where does coastal sediment come from:
Unconsolidated is….
A sediment that is loosly arranged or unstratifed (not in layers) or whose particles are not cemented together (soft rock)
Put igneous, sedimentary and metamorphic rock in order from weakest to strongest with an example
4 geological influences on coasts
Lithology can mean any of the following characteristics:
Explain strata
layers of rock
Explain Bedding plane
horiontal cracks
natural breaks in strata, caused by gaps in time during periods of rock formation