Holderness Flashcards

1
Q

Where is the Holderness Coast and why is it significant?

A

Located on the east coast of England (Yorkshire), it is one of Europe’s fastest eroding coastlines—eroding at to 1.2m per year.

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2
Q

What is the geology of the Holderness Coast?

A

It consists of soft boulder clay (glacial till), which is easily eroded by marine and sub-aerial processes. Chalk is found further north at Flamborough Head.

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3
Q

What are the main coastal processes affecting the Holderness Coast?

A

Hydraulic action, abrasion, and corrosion (marine processes); Weathering and mass movement (slumping common due to saturated clay); Longshore drift moves material southward, leaving some areas starved of sediment.

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4
Q

What erosional landforms are found at the Holderness Coast?

A

Headlands and bays at Flamborough Head; Caves, arches, stacks, and stumps (e.g., Selwicks Bay); Wave-cut platforms.

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5
Q

What depositional landforms are found along the Holderness Coast?

A

Spurn Point: a recurved spit formed by longshore drift; Sandy beaches in low-energy environments (e.g., around Withernsea).

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6
Q

How has human management attempted to protect the Holderness Coast?

A

Hard engineering at Hornsea, Mappleton, and Withernsea (e.g., groynes, sea walls, rock armour); Two rock groynes and revetments installed at Mappleton in 1991; Soft engineering at Spurn Head (previously managed retreat).

Seas walls at Withernsea, Hornsea, and Bridlington

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7
Q

What are the impacts of coastal management at Holderness?

A

Groynes prevent longshore drift, starving areas further south (e.g., increased erosion at Cowden); Spurn Point is at risk of being breached without sediment supply; Conflicts between protecting property and natural processes.

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8
Q

What role does climate change play in the erosion of the Holderness Coast?

A

Rising sea levels increase wave energy and erosion; More frequent storms add to cliff retreat and damage to defences.

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9
Q

What are the main stakeholder conflicts along the Holderness Coast?

A

Local residents want protection for homes; Farmers want land preserved but often can’t afford private defences; Environmentalists support natural processes (e.g., managed retreat); East Riding of Yorkshire Council balances cost, protection, and sustainability; Businesses & tourism want protection for economic stability; Conflicts arise when defences in one area increase erosion elsewhere.

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10
Q

What is sustainable coastal management and how is it applied at Holderness?

A

Focuses on long-term, low-impact strategies that work with natural processes; Example: Managed retreat at Spurn Head—no longer defending spit from erosion; East Riding Coastal Change Fund helps relocate and compensate at-risk residents; Coastal monitoring & adapting strategies over time = adaptive management.

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11
Q

What are the hard engineering strategies used at Holderness?

A

Sea walls (e.g., Hornsea): reflect wave energy but expensive and need maintenance; Groynes (e.g., Hornsea & Mappleton): trap sediment to build up beaches but starve southern areas; Rock armour (riprap): large boulders absorb wave energy (e.g., Withernsea, Mappleton); Revetments: sloping structures that absorb wave energy (used at Mappleton in 1991).

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12
Q

What is Spurn Head and why is it significant?

A

A recurved spit formed by longshore drift transporting sediment south; Protects the Humber Estuary; Home to unique ecosystems and bird habitats; Was defended in the past but now is under managed retreat; It is one of the longest spits in Europe.

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13
Q

What is Flamborough Head and why is it resistant to erosion?

A

Flamborough Head is a headland made of chalk, which is a harder, more resistant rock than glacial till, so it erodes more slowly.

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14
Q

What is the geological structure of the Holderness coastline?

A

The Holderness coast is a discordant coastline, where alternating bands of chalk and glacial till create headlands and bays.

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15
Q

Why are chalk joints and faults significant for erosion?

A

Vertical cracks (joints) and faults in chalk are weak points, making them more susceptible to erosion and weathering.

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16
Q

What makes Bridlington Bay vulnerable to erosion?

A

Bridlington Bay has a narrow beach, offering little protection to the soft cliffs, making them highly vulnerable to erosion.

17
Q

How does erosion at Holderness contribute to the sediment cell?

A

High erosion rates generate large amounts of sediment, which are transported by longshore drift to feed the sediment cell.

18
Q

How much has the Holderness coastline retreated since Roman times?

A

The coastline has retreated up to 5km since Roman times, leading to the loss of settlements.

19
Q

What are the two main rock types along the Holderness coast and how do they differ?

A

Chalk is resistant, forming headlands (e.g., Flamborough Head), while glacial till is easily eroded, forming bays like Holderness Bay.

20
Q

How do sea and weather conditions increase erosion at Holderness?

A

Northeast winds create a powerful fetch, and low-pressure systems funnel water in the North Sea, causing storm surges.

21
Q

What is the direction and impact of longshore drift at Holderness?

A

Longshore drift moves north to south along the Holderness coast. It transports sediment, but groynes can cause sediment starvation downstream.

22
Q

What is significant about the erosion rate and location of the Holderness Coast?

A

Holderness is the fastest eroding coastline in Europe at 1.2 metres per year. It is located on the North Sea coast.

23
Q

What is the geology of the Holderness Coast and how does it affect erosion?

A

The coastline is made of glacial till (boulders, sand, clay), which is easily eroded due to its softness.

24
Q

How do wind and wave energy affect the Holderness Coast?

A

The UK’s main wind comes from the Caribbean, but Holderness is on the leeward (sheltered) side. It has a short fetch and is part of a sediment cell.

25
Q

What is the origin of the sediment at the Holderness Coast?

A

A thousand years ago, an ice sheet in the North Sea deposited boulders, sand, stone, and clay on the coast. As it melted, it left a blanket of glacial till.

26
Q

What is the impact of historical sea level changes on the Holderness Coast?

A

The melting ice sheet led to a static sea level rise. The last ice age ended around 10,000 years ago.

27
Q

What is the historical significance of the Holderness Coast?

A

The Romans built settlements on the coastline 2,000–3,000 years ago. The cliffs are soft, so erosion is fast.

28
Q

What kind of coastline is Holderness and how does sediment move?

A

It is a discordant coastline. The sea appears brown due to suspended sediment. Longshore drift moves sediment south.

29
Q

What hard engineering strategies are used at Mappleton and Withernsea?

A

Groynes are used at Mappleton. South of Mappleton, there is sediment starvation. Sea walls (including recurved walls) are found at Withernsea.

30
Q

What is the environmental cost of sea defences like concrete sea walls?

A

Concrete sea walls were replaced due to sea level rise. Concrete is responsible for 1% of global CO2 emissions. Sea defences stretch over 1 km at Willemstee beach.

31
Q

Where in holderness has groynes?

A

Mappleton and witherensea