Coasts Revision Flashcards
What is a concordant coastline?
How are metamorphic rocks formed? Name some examples
Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means “change in form”.
The original rock (protolith) is subjected to heat (temperatures greater than 150 to 200 °C) and pressure (100 megapascals (1,000 bar) or more), causing profound physical or chemical change.
Quartzite and slate are types of metamorphic rock
What is isostaic sea level change?
Isostatic sea level change is the result of an increase or decrease in the height of the land. When the height of the land increases, the sea level falls and when the height of the land decreases the sea level rises. This could happen from tectonic movements
Isostatic change is a local sea level change whereas eustatic change is a global sea level change
What distinctive landforms are created by mass movement?
Rotational scars, talus scree slopes, terraced cliff profiles
Describe what we mean by a fault in a cliff
Describe the faults in the image below
What is an emergent coastline?
An emergent coastline is a stretch along the coast that has been exposed by the sea by a relative fall in sea levels by either isostasy or eustasy
The emergent coastline may have several specific landforms:
Raised beach
Wave cut platform
What is a sediment cell?
A sediment cell is a largely self-contained stretch of coastline. They are regarded as closed systems as sedimentis not usually transferred from one to the other. In reality, somesediment does get transferred between neighbouring cells. Each sediment major cell typically has many smaller sub-cells.
Name the different inputs into a coastal system
Marine – waves, tides and currents<br></br>Energy – kinetic energy from waves and wind, thermal energy from the sun and potential energy from material on cliffs/slopes and material from processes of weathering, mass movement, erosion and deposition<br></br>Geological – rock type, structure and tectonics. material from marine deposition, weathering and mass movement<br></br>Atmospheric – climate, weather and climate change<br></br>People – urban planning, housing, industry, coastal management/defences, leisure
What are coastal plains?
A coastal plain is flat, low-lying land adjacent to a sea coast
What is a ria?
A ria is a coastal inlet formed by the partial submergence of an unglaciated river valley. It is a drowned river valley that remains open to the sea.
Where is the Haff coastline and what are its distinctive characteristics?
The Haff coastline is the low and regular coastline found in Eastern Germany. It is formed of soft sediments and the sandy strips run parallel to the coast.
The term haff is also used more widely to describe a lowland coast where the long bars and lagoons are parallel to the shore
Explain the influence of dip on cliff profiles
- the dip of a rock layer is the angle of tilt from the horizontal.
- if a rock layer dips towards sea the blocks of rock may slide under the influence of gravity (mass movement)
- if the angle of the dip is landward, weathering and erosion may attack exposed bedding planes and joints, creating an irregular profile
Describe how the differential erosion of alternating and contrasting rocks affects the coastline
- sedimentary rocks are permeable whereas metamorphic rocks are impermeable.
- the presence of water in these rocks can affect weathering and mass movement e.g. Slumping due to saturation
- some rocks such as limestone contain soluble minerals and so are vulnerable to chemical weathering such as carbonation (sea water absorbs co2 which splashes onto limestone and dissolves it)
Explain why estuaries are ideal for the development of salt marshes
- estuaries are low energy environments where tidal conditions bring seawater and sediments in and out and rivers bring fine MUDs and silts and deposit them at the estuary
- the clay particles sick to one another (flocculation) and once deposited are colonised by algae.
- salt marshes can then be found at the edges of estuaries.
Explain the formation of embryo dunes
- sand dunes form where there is a plentiful supply of sand and a large area for it to dry out.
- onshore winds blow sand towards land and obstacles such as vegetation and shingle ridges which trap the sand
- embryo dunes are formed first.