Saltburn to Flamborough head Flashcards
(8 cards)
Location and features of the coastline
High-energy coastline
Spans 60km along the East Yorkshire coast
discordant coastline
facing the North Sea
lying adjacent to the North Yorkshire Moors
What makes it a high energy coastline?
Dominant waves from N-NE have a fetch of around 1500 km, leading to high energy waves - creates longshore drift from North to South
Sediment sources of the coastline
some driven onshore at the end of last glacial till
cliff erosion
limited fluvial sediment due to river management
Cliffs on the coastline
most cliffs are overlain by a layer of weak glacial till
Cliffs at Flamborough head are made of chalk (strong) and are 20-30 m high
Further North, between Robin Hood’s Bay and Saltburn, the cliffs are much higher and have a stepped profile due to weaker geology
Headlands and Bays on the coastline
created due to being a discordant coastline
Robin Hood’s bay created due to weak shales eroding away, leaving only sandstone headlands on either side - Ravenscar to the south and Ness Point to the North
Further South, Filey Bay has been created due to being made of weak Kimmeridge clay with limestone and chalk either side
Flamborough head is formed from chalk with weak clay either side
Wave Cut Platforms on the coastline
Robin Hood’s bay has a wave cut platform which slopes at a typical angle of 1 degrees but ramped sections could be as steep as 15 degrees. the wave cut platform has a width of 500m but extends further into the offshore zone
Landforms on headlands
Wave refraction leads to wave energy being concentrated on the resistant headland
Weaknesses, such as joints or folds, are exploited by erosive action to form caves and arches - Selwick’s bay and Flamborough Head
Green Stacks Pinnacle - stack isolated at the end of a headland
50 Geos have formed along the coastline facing the dominant wave direction
Blowholes have developed where vertical joints have been enlarged
Beaches on the coastline
Found in the sheltered, low-energy environment such as Scarborough and Filey Bay
Lack of spits and drift-aligned features, partly due to high tidal range of around 4 m and a lack of estuarine environments that would provide sediment sinks