# data[].attributes.body
Mass movement
Boulder clay=unconsolidated
weak and little resistance to erosion
Fetch- win wand waves across north sea
No beaches(terminal groyne syndorme?) to provide extra protection and absorb wave energy leading to destructive waves.

# data[].attributes.body
the coast has boulder clay which is very unconsolidated and easily eroded
high energy waves due to the long fetch are able to erode the cliff
this area could be an area where terminal groyne syndrome affects it which would starve the area of sediment increasing erosion rates
there could be chemical weathering of the chalk (oxidisation) as well as biological weathering from the grass on the top of the cliff

# data[].attributes.body
-mass movement- rotational slumping
-heavy rain fall = ground saturated + slumps under own weight
-boulder clay, soft rock = easily eroded.
-could have groynes further up coast = terminal groyne syndrome.
- strong wave power: long fetch, shape of coast line, lake of beach.

# data[].attributes.body
-The cliffs at the Holderness coast are made up of bolder clay which is unconsolidated, this means that the rate of erosion is increased.
-There is a lack of defences in the figure this means that the cliff face is more vulnerable to erosion
-Unconsolidated material becomes saturated meaning it slumps due to its increased weight
-Destructive waves mean that the cliff faces more erosion

# data[].attributes.body
-Weak geology (boulder clay) which is unconsolidated and easily eroded.
-Human activity (e.g. camping) can destabilise the cliff further by creating weak points.
-A long fetch across the north sea and the Atlantic creates powerful waves that quickly erode the base of the cliff.
-Biological weathering at the top of the cliff

# data[].attributes.body
Geology - main rocks here are chalk and Boulder clay. Boulder clay easily eroded while chalk more resistant
Waves - destructive waves attack foot of the cliffs
Weather - Winter storms mean stronger  waves + higher sea levels so Boulder clay becomes more saturated and leads to slumping and other forms of mass movement
Human - groynes north of mappleton trap sediment while starving areas south of mappleton leading to erosion (long term groyne syndrome)

# data[].attributes.body
- weak boulder clay (less resistant)
- lack of protection to the exposed coastline
- caravan sites above the cliff increases pressure and unstability of cliff (human acitivty)
- holderness coast waves have a large fetch and therefore more destructive leading to more coastal recession with the weak sedimented cliff face

# data[].attributes.body
- Made up of softer rock, Boulder clay - weak and less resistant
- The tide comes very close to the edge of the cliff therefore, there is no protection against the cliff meaning the destructive waves will hit the cliff with full power, no friction to reduce the energy of the waves
- Groynes are at Mappleton and Hornsea mean that terminal groyne syndrome occurs and starves the sediment.
- Mass movement looks like it has occurred as the cliff is seaward dipping hence the material sliding forward.

# data[].attributes.body
Coast made of less resistant rock- boulder clay
Lack of coastal defence's
Possibly terminal groyne syndrome

# data[].attributes.body
The geology of the rocks there mean it is vulnerable to erosion, Boulder clay is unconsolidated and there full easy to break down.
Due to groynes at Hornsea and Mappleton, Aldborough experiences TGS and is starved of sediment meaning it’s it’s exposed to waves. A lack of beach material means there is no friction to prevent this.
Steep cliffs

# data[].attributes.body
- made of boulder clay which is structurally weak and can be exploited by powerful destructive waves due to it being less resistant.
-no beaches infront of the coastline which are able to absorb any of the wave energy meaning that waves are very destructive due to sediment starvation
- lack of hard engineering strategies to protect the coastline such as groynes or sea walls
-The unconsolidated sediment become saturated with water making it heavy and slumps.
- waves approaching the Holderness coast are powerful due to their fetch and the wind.