Summerhill Climate Detectives

Coastal Erosion in North Norfolk: Can anything be done?

Introduction

The East Coast of England has suffered from coastal erosion for hundreds of years. Several villages and important ports from the past are now under the sea.

 Climate change imposes an even greater threat on small seaside villages and towns, with the rate of coastal erosion likely to increase with the rising sea levels and storms predicted for the near future.

 Although the rapid coastal erosion threatens several towns and villages, we focused our study on the North Norfolk village of Happisburgh, home to some of the fastest eroding cliffs in the UK. Happisburgh has been affected by coastal erosion much faster than other locations. Several houses have been demolished due to the receding cliffs, and many more will soon have the same fate.

  Between the ’60s and the '90s, sea defences were built and maintained to slow down erosion. However, these suffered deterioration, and the government did not renovate them.

 This project is set to identify how this erosion is happening, investigate how residents and local businesses have been and will be affected, especially by climate change, and study the feasibility of defending the village.

Our research question is: 

How is the coastal erosion in North Norfolk affecting residents and businesses? What actions are feasible?

Our investigation included several data sources:

Satellite images and aerial photographs

helped us visualise and measure how fast erosion is happening;


Soil samples

helped us understand erosion and Happisburgh vulnerability; 


Interviews

helped us empathise and understand people directly impacted by this problem and helped us understand policies and constraints of the Coastal Management Team at the North Norfolk District Council;


Secondary sources

We looked at sea-level rise predictions from NASA and MetOffice UK to understand how the cliffs will interact with the sea in the future. We studied the coastal erosion risk projection map recently released by the UK government to compare the future scenario considering today's climate and climate change.

Identifying a local environmental problem 

Coastal erosion is not a new problem in the East of England. It has been happening for centuries. Dunwich is a village very close to our school. It now has less than 200 inhabitants, but it was once, during the Middle Ages, the second largest city in the East of England and one of the most important ports in the country. This was possible because sediments brought by the current from other shores in Norfolk and Yorkshire built a natural harbour. The coastal erosion in other places further north benefited the Dunwich location.

But the same phenomenon that brought progress to Dunwich caused its downfall when the harbour entrance was closed with more sediments brought by the current. The city lost its port and rapidly decayed. Eventually, the area itself was eroded and the city lies today under the sea. The sequence of images below show All Saints Church, the last church of the old city of Dunwich that had its last tower claimed by the sea in 1919.


Dunwich's cliffs have not suffered any erosion since around 2000. This happened mainly due to the shingle and the slopes going down to the beach. When we went to Dunwich, the cliffs had vegetation, which is evidence of them not eroding lately. 

Although the erosion in Dunwich is stable at the moment, we found out that there are several areas in the East of England suffering from intense coastal erosion. This video shows satellite views from Covehithe, Hornsea and Happisburgh, home to some of the fastest eroding cliffs in the UK. These videos were taken from the Copernicus browser, Sentinel-2.

We chose to focus our study on Happisburgh because, as seen in the video, the erosion can be seen easily in the satellite images, which allowed us to take measurements. Also, Happisburgh is relatively close to our school, so we could visit it and collect ground data. There are lots of threatened buildings there, including the Church of St. March, a Grade I Listed Building from the 14th century; Happisburgh Manor, a Grade II listed building, park and garden; and Happisburgh Lighthouse and Cottages, a Grade II listed building. 

Happisburgh Lighthouse and Cottages 

St. Mary's Church Rooms, part of Happisburgh Manor 

St. Mary's Church (inside )

St. Mary's Church 

Happisburgh cliffs - no vegetation shows recent erosion, which can also be seen in some areas 

Working with satellite images and data 

We worked with the Copernicus browser to analyse the recession of the cliffs in Happisburgh and the elevation profile in critical areas. We chose to use Sentinel-2, since it "provides high-resolution images in the visible and infrared wavelengths, to monitor vegetation, soil and water cover, inland waterways and coastal areas" (Copernicus Browser), which is what we needed. The Copernicus Browser provided images from 2016 

We also looked at Historical images on Google Earth, since there were images there from 1999. However, when we tried to make measurements on Google Earth, we noticed that the images from different years were not aligned, so the measurements would not be reliable. We compiled the pictures in a video only for illustration purposes. 

In the Copernicus browser, we gathered one image from every year from 2017 to 2025 (the available period in the Copernicus Browser), and drew a line along the coast . 

We measured the recession of the cliffs year by year in 10 different spots (every 100m) and calculated the mean value for every year, which is shown on this histogram . The recession of the cliffs in 2021 were very small, so we did not consider that year. 

When measuring the erosion, we realised that there was a lot of erosion at the Beach Road area, where the most vulnerable houses are. Some measurements were as high as 15 meters in one year.

The graph on Figure 9 shows the cumulative erosion in that area from 2017 to 2024. We can see that the erosion was constant until 2021, it slowed down from 2021 to 2022, before it increased again in 2023. This can also be seen clearly in the aerial pictures we added to the graph.

Still using the Copernicus browser, we also measured the total lost area in Happisburgh due to erosion. This picture shows how much land was lost to the sea in the last 8 years, from 2017 to 2025. The total loss was 30,000 m2, which is equivalent to 4 full-size football fields. 

The cliffs

The cliffs at Happisburgh are composed of clay (lower layer), silt (middle layer), sand (top layer).

We collected samples from the soil and tested their strength and resistance to water.

This video shows how the soil easily crumbles even under light pressure applied with our hands.

Looking at the soils under the microscope, we could see that the clay has the finest particles, followed by the silt, with the sand having the largest particles. The finest particles of the clay give it very low permeability, while the particles of sand, being larger, let water in easily. That means that when it rains, the sand lets the water pass and, when it reaches the clay, the water stops as it cannot penetrate that layer, creating a giant "puddle" which places a huge weight on the clay. This also makes the sand more likely to slide down the cliff, increasing erosion.

When we poured some water over the soil samples, we could see the particles being washed from the piece of soil. This happened with both the clay, the silt and the sand, although the sand was clearly more vulnerable. This shows how fragile the soil is when in contact with water

 The pictures below show samples of clay, silt and sand collected from the cliffs in Happisburgh when dry and when wet, showing some particles easily washed away, and images of the soils observed on a microscope, augmented 4 times, which shows the difference in the particle sizes.

Sand from Happisburgh cliffs

 Silt from Happisburgh cliffs    

 Clay from Happisburgh cliffs 

Although rain plays an important part on the erosion of the cliffs, the main cause of the erosion is the sea hitting and wetting the cliffs during high tides, and storms from the North or North-East, which rise the sea level even more and cause strong waves which crash on the cliffs. 

The sea and the effect of climate change 

In order to understand how the sea affects the erosion in Happisburgh, we investigated the tides. We used the software Poltips, which gives predictions and historical data about astronomical tides.

We isolated the height of the high tides from the past six years to analyse whether they changed considerably from year to year. We plotted box plots for each of the years, which show the minimum, the lower quartile, the median, the upper quartile, and the maximum height of the high tides. We concluded that the high tides do not change significantly.

We wanted to investigate how the high tides hit the cliffs. We used the Copernicus Browser to plot the elevation profile at the Beach Road area (The pictures below shows the area we chose to focus on and the elevation profile along the line shown). We chose that location since it is one of the most vulnerable areas. 

We plotted a graph of the astronomical high tides (from Poltips) during one year and superimposed it on the elevation profile. We also superimposed a photograph we took of the same area to make it easier to see which layer of the cliffs was being hit.

 We researched how storms affect the sea level and discovered that the waves can reach a height of 0.7m to 1.7m higher than the predicted astronomical tide during a storm.

 This picture shows a graph extracted from the National Tide and Sea Level Facility (https://ntslf.org/storm-surges/skew-surges/england-east) showing the top 1% of skew surges at Cromer, which is the closest port to Happisburgh. We added a line on our graph (blue line) showing the height that the waves can reach during a storm. 

From this graph it is clear that every single high tide hits the clay layer of the cliffs and the waves can get as high as the silt layer during a storm. 

As stated in the section about the soil, the clay gets easily washed away when wet. The sea keeps on "carving" this layer and, without the clay, the sand on top of the cliffs has no foundation and, therefore, falls. The photograph on the right illustrates this process. 

Learning the risks storms combined with high tides impose on the cliffs at Happisburgh; we set off to investigate if storms frequently occur during the highest tides of the year. 

The picture below shows a graph of the high tides and named storms from 2019 to 2024. We can see from the graph that the tides reach their highest points in the Spring and Autumn months, while during the summer, the highest high tides are much lower.

 We also noticed that, in the Summer, there were no storms, which were very frequent during the winter. Although the tides in the winter are not the highest, they are also not as low as in the summer, so storms can have a very negative impact on erosion. 

Climate change can bring a greater vulnerability to these cliffs. According to the MetOffice UK and NASA, the sea levels have risen by approximately 20cm since the start of the 20th century, being 10cm since 1993. NASA website (https://climate.nasa.gov/vital-signs/sea-level/?intent=121) has an interactive tool which allows users to see the exact sea levels at a given date since the beginning of the use of satellite data.

The picture to the left shows a graph extracted from the MetOffice website (https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/pdf/research/ukcp/ukcp18-infographic-headline-findings-marine.pdf) showing the prediction of how much the sea levels will rise by 2100 in two scenarios: low greenhouse gases emission and high emissions.


In London, which is the closest city from Happisburgh out of the capital cities in the UK, even in the low-emission scenario, the sea level is expected to rise from a minimum of 29cm to a maximum of 70cm. In the high-emission scenario, this rise will be from 53cm to 115cm. 

We added this information to our graph(from higher up in the site but shown here again). The yellow shaded area shows where the water might reach considering the sea level rise in 75 years. This height is on the sand layer, and this can cause a severe increase in erosion since the particles of the sand are larger and more easily washed away. 

This year, the Environmental Agency in the UK released a new coastal erosion risk projection map. It shows the prediction of land that will be lost to the sea until 2055 and 2105, considering today's climate and the expected climate change. This interactive tool can be found at https://environment.data.gov.uk/shoreline-planning . The figures below show the projections for Happisburgh for 2055 and 2105. The darker area considers today's climate, and the lighter area takes into account climate change, in its worst case scenario. 

Projection for 2055

Projection for 2105


The projections for 2105 show how climate change will greatly affect this community. The listed buildings will still be up in 2105 if the climate stays as it is today, while all except the lighthouse would have to be demolished if the sea level keeps rising at the rate it has lately. Approximately 20 houses are also between today's climate projection and the worst-case scenario projection.

The gif below artistically represents the scary scenario of the amount of land that can be lost to erosion in the next 80 years if we do not manage to control climate change in the near future.

Interview with a resident 

We interviewed Patrice Baldwin, a Happisburgh resident and home owner.

These are the questions we asked her:

1) How long have you been living in Happisburgh?

2) Why have you chosen to move here? Were you aware of the risks by then?

3) Is your house endangered by coastal erosion?

4) How are you affected by the coastal erosion in Happisburgh?

5) How do you feel about the Council's decision not to renovate the sea defences?

6) Can you talk about what you saw on those years regarding coastal erosion? Any particular bad   year? Good year?

7) If you were to describe a perfect scenario for Happisburgh, if there were no restrictions, what       would it be?

8) Are you involved with the Save Happisburgh campaign? If so, can you talk about its aims and   struggles? How are you involved?

9) Are you concerned about climate change?

10) What message would you tell the world about coastal erosion and climate change?

11) Anything else you would like to say?

Patrice moved to Happisburgh in January 1991, so she has been there for 34 years. She moved there because it was beautiful and was not aware of coastal erosion, even though her mum warned her about it.

 She lives one field away from the cliffs and her house is endangered, although not as much as some of the other houses in the Beach Road area. She said Happisburgh is not entitled to sea defences because it depends "on the number of chimneys" and Happisburgh does not have enough.

 She thinks it is unfair that Happisburgh does not get any sea defences, especially since lots of places around it do. She thinks this increase the erosion at Happisburgh. She spoke about how when they get a high tide combined with a storm from the North-East, the erosion is very intense, sometimes taking meters overnight.

 She cited 1953 as a very bad year because of the flood (although she was just a baby then). She also acknowledged 2013, because of the storm surge of December 5th, when a bungalow in Happisburgh was left hanging on the cliff edge.

 She is not part of the "Save Happisburgh" campaign, but sometimes attends the meeting. She sees the campaign as a huge and important effort from residents, but she does not see any changes coming from it, since Happisburgh never seems to qualify for defences. 

She is very concerned about climate change, and believes countries are too late on taking action. She said that if not all countries work together to fight it, no effect will be achieved. In an ideal world, she would like to see sea defences in Happisburgh and not so much bad publicity about the village. 

She also would like people to receive compensation for their houses when they need to be demolished so they can restart their lives somewhere else. She feels powerless, since nothing can be done: The residents cannot even purchase rocks to add to the ones on the beach. 

She said that the village is slowly disappearing, since no young people have come to live there. Lots of houses are being bought and rented as holiday accommodation and no new houses can be built in the area. She cited, for example, that the local primary school had an intake of only 3 new children this current school year.

Interview with a business owner 

We interviewed Chris Lomax, the owner of the Caravan Park in Happisburgh.

These are the questions we asked him:

1) How long have you had the Caravan Park at Happisburgh?

2) We saw that the park used to be next to the cliffs, and it moved to the site where it is now not that long ago. Why did you move it? Was your business affected by the move?

3) Did you invest a lot of money into moving your caravan park? Why do you choose to keep running the park? Have you considered leaving Happisburgh and maybe having a caravan park somewhere else?

4) Was the site of the old caravan park yours? If so, do you still own it? What happened to the site?

5) How do you feel about the Council's decision not to renovate the sea defences?

6) Can you talk about what you saw on those years regarding coastal erosion?

7) If you were to describe a perfect scenario for Happisburgh, if there were no restrictions, what would it be?

8) Are you involved with the Save Happisburgh campaign? If so, can you talk about its aims and struggles? How are you involved?

9) Are you concerned about climate change?

10) What message would you tell the world about coastal erosion and climate change?

11) Anything else you would like to say?

The Caravan Park has been in Chris' family for 60 years. He had to move his caravan park further inland in 2009 because he had lost a great park of his land to the sea and was running with only 2/3 of the caravans he was allowed to.

 He did not get any compensations or incentives to move. On the contrary, he had to buy the new land and get planning permission. This was first denied, so he spent extra money with lawyers and the process for the construction to be approved. He only managed to sell the land of the old caravan park in February 2025 (the day we were interviewing him!). The Council bought it, but he does not know what they plan to do on the land.

He told us he is not too worried about sea defences now that he has moved further inland, since his caravan park is not in danger. However, he feels for the people whose houses are close to the cliffs and thinks they should be compensated somehow. When we asked if he lived in Happisburgh, he said: "Who would want to live here?", making a reference to the houses having to be demolished, the owners having to pay for demolition and residents feeling neglected. 

He is not involved with the "Save Happisburgh" campaign. He said residents are always getting together and organising themselves to try to save the village. He spoke about the Path Finder project, which was getting funds and buying the endangered houses so people could move further inland.

 When we researched about this project, we found out they were the ones who bought all the houses in Beach Road and demolished them in 2012/2013. However, this project does not exist anymore and there is no support for the people who are losing their homes. Just like Patrice, he thinks we are too late in our fight against climate change, and believes that the whole world needs to work together to slow it down, but is very skeptical and thinks this will not happen because governments are selfish and just want votes, which they will get with short-term actions. 

His message to the world: "Wake up! If the coast keeps on eroding this fast, it won't be a problem only for the coastal villages; the sea will flood a lot of land and a lot of people will be affected."

Interview with an engineer from the North Norfolk District Council 

We interviewed Fiona Keenaghan, a coastal engineer from the Coastal Management Team at North Norfolk District Council.

These are the questions we asked her:

1) What is the policy regarding sea defences in North Norfolk?

2) Why doesn't Happisburgh fit in the constraints of the places with sea defences?

3) How do you respond to the house owners when a house needs demolishing because of coastal erosion?

4) Can you talk about the feasibility of installing sea defences? Costs? Environmental effects? Anything else?

5) If the people in a village raise money and build the sea defences privately to save their village, would that be allowed?

6) Are you aware of the "Save Happisburgh" campaign? If so, how does the Council deal with the people from the campaign?

7) If you were to describe a perfect scenario, if there were no money restrictions, would that change the council's decisions?

8) Anything else you would like to add?

Fiona told us the policy for Happisburgh is "Managed Realignment", which means that you move important constructions further inland and let erosion continue naturally, without interference of new sea defences. The Coastal Management Team receives money from the government and the environmental agency each year to protect villages. The council wants to do as much as possible but they get very little money so they only put sea defences where there are many businesses and properties. Since Happisburgh only has 1400 people and very few businesses, it is not eligible to have sea defences. 

When a resident loses a house, they do not get any compensation or support towards relocation; they have to pay for their own house to be demolished. There is a programme from the government called Coastwise that sometimes can help residents with the cost of demotion, but it will end in 2027. She also told us that building sea defences in one location can lead to a worse negative impact further down the current, so this also needs to be considered when analysing where to build sea defences.

Fiona spoke to us about something called coastal catch-up. She said that, when sea defences are removed or fail, the rate of erosion increases until it reaches where the cliffs would be had the defences never been there. According to this, erosion rates should slow down at some point in Happisburgh.

She also told us how Shell UK Ltd and Perenco UK Ltd funded the sandscaping scheme at Bacton, to protect the gas terminal. She said that business and even residents can fund defences, but they need planning for the construction and for the continuation of the schemes, which are all very expensive. She is aware that residents from Happisburgh feel abandoned and she guaranteed that, although they do not necessarily believe it, the sandscaping scheme in Bacton will help Happisburgh, which will get sediments brought from Bacton.

 Conclusions


Coastal erosion in Happisburgh is not linear. Some years nature is kind and the erosion slows down, while in others erosion is very severe. However, through the years, it does not seem to slow down. Happisburgh has a very high rate of erosion and is not entitled sea defences. Climate change will raise sea levels and increase the number of storms, which will further increase erosion rates, since the sea will reach higher layers of the cliffs, which are very vulnerable to the sea and the waves hitting it.

There is no plan for sea defences in Happisburgh, since the population is small and it lands on the "managed realignment" category. Because of coastal catch-up, erosion rates might decrease slightly in the future, but the projections are not promising, especially if climate change is not slowed down. Happisburgh might see his listed buildings being demolished in the next 80 years.

We only have satellite data since 2017, so the study is limited, since we could not get precise data from before that date. However, although not as precise, we could see that the erosion rates were also fast since 1996 through aerial photos and Google Earth, especially after the sea defences failed.

Residents and business owners feel let down, neglected and ignored. Happisburgh is a lively community that is dying. Houses are being demolished, and few people want to live or invest there, reducing the population. Happisburgh might have the same fate as the old Dunwich and become a ghost village or even just a tourist spot before it all erodes into the sea.

Despite all that, the council does not have enough funds to build sea defences for all the towns and villages on the coastline. Also, building sea defences in one place affects the coast further down the current, increasing erosion there and, sometimes, creating an even bigger problem.

Actions

Unfortunately, building sea defences everywhere is not feasible. The only way to slow down erosion in Happisburgh is to slow down climate change. This will only happen if the whole world works together. Happisburgh is just a tiny example of a community suffering from the effects of climate change. It is our responsibility to demand that governments follow the plan they submitted for the Paris Agreement and that countries support each other in meeting the targets. The more people who are conscious of the damage that climate change has done and will do to our world, the louder the voice demanding actions.

We also think that Happisburgh residents need to be supported so they do not feel abandoned. By making their voices reach more people, we want the government to take action so that they feel safe that they will have a place to live once the sea claims their house. The government should allocate resources to help this and other communities rebuild their lives and not feel powerless.

We want to spread the word, so these voices get louder. We are presenting the project to our school during an event with students and families next term. We also plan to present it at local schools, both around our area and in Norfolk. We created a website, so people can access the results of our project anywhere in the world, and we are starting to use the hashtag #HappisburghClimateDetectives to spread the word on social media. We want people to see that Happisburgh is not just a village falling into the sea: it is a rich community which deserves to feel seen and safe.

The Cliff Hangers

Summerhill's Climate Detectives

Catarina

Age: 12

Likes: Gymnastics and dancing

Enjoyed listening to the council's point of view and learning how to make websites.

Ruhan

Age: 15

Likes: Gymnastics and Taylor Swift

Was thrilled to learn about satellites and how every corner of the earth is being observed from space.

Aria

Age: 12

Likes: Baking

Coastal erosion is something bigger than she ever knew.

Vicente

Age: 10

Likes: Football, gymnastics and ducks

Loved the trip to Happisburgh and is already looking forward to next year's project.

Sami

Age: 12

Likes: Drawing and crochet

Learned about a new part of climate change and became aware of what's happening to our world.

Andresa

Our AMAZING teacher who helped us so much!!!

Acknowledgements

We met so many people who were willing to help us during this project! Here is a big thank you to all these people:

  • Patrice Baldwin, who volunteered very quickly to be interviewed and gave us many insights and useful information from the residents' point of view.
  • Chris Lomax, who agreed to be interviewed and received us in his caravan park, being very kind to answer our questions.
  • Katharine Shackcloth, who gave us several slides taken by her deceased father, Jim Hardy, documenting coastal erosion in Happisburgh. These slides are such rich documentation!
  • Fiona Keenaghan, from the Coastal Management Team at the North Norfolk District Council, gave us a different perspective on the problem and was kind, patient, and helpful during the interview.
  • Mike Page, who gave us some high-resolution aerial photographs from Happisburgh over the years. They were very valuable, especially since we did not have satellite images from before 2017.
  • Lisa Eastwood, from the National Oceanography Centre, who, in the name of the Poltips team, provided us with access to Poltips 4, the software we used to study the tides. This was a crucial part of our project, and we could not be more grateful.
  • Augusto Cuginotti helped us and guided us in the creation of the website.
  • Taline Schulbach, for helping us edit Happisburgh aerial photograph to show the projection for 2105.
  • Sarah Peel and Jane Hamilton, who received us at the Dunwich Museum and gave us many insights when we were starting this project.

Bibliography

During this project, we used several sources to investigate our problem and make sense of the data we collected. Here is a list of websites and books we used and found particularly interesting:

  • Costal catch-up: https://publications.naturalengland.org.uk/publication/6478278672252928
  • Coastwise programme: https://www.north-norfolk.gov.uk/tasks/projects/coastwise/coastwise-faqs/
  • Hansard: Debate about coastal communities (20/03/2025): https://hansard.parliament.uk/commons/2025-03-20/debates/8AA0AD7F-CFF4-4EDE-9634-BD48FD9356A2/CoastalCommunities?fbclid=IwZXh0bgNhZW0CMTEAAR3_PJGGs4IoExDRX_uXPNL45wqM5-KnpnWa0bUMScEJW1WUKHEv8TogRHk_aem_OZffm5XtpwDGO0SdPCoDKw
  • Sandscaping scheme: https://www.north-norfolk.gov.uk/tasks/coastal-management/sandscaping-frequently-asked-questions/
  • The 2013 storm surge: https://www.north-norfolk.gov.uk/tasks/projects/coastwise/coastwise-faqs/
  • Shoreline management plans: https://environment.data.gov.uk/shoreline-planning
  • Sea currents: https://marine.copernicus.eu/access-data/myocean-viewer
  • Storm centre: https://weather.metoffice.gov.uk/warnings-and-advice/uk-storm-centre/index
  • Happisburgh landslide observatory: https://www.bgs.ac.uk/geology-projects/landslides/happisburgh-landslide-observatory/
  • National Tidal and Sea level facility: https://ntslf.org/storm-surges/skew-surges/england-east
  • Sea level (NASA): https://climate.nasa.gov/vital-signs/sea-level/?intent=121
  • UKCP18 Marine Climate Change: https://www.metoffice.gov.uk/binaries/content/assets/metofficegovuk/pdf/research/ukcp/ukcp18-infographic-headline-findings-marine.pdf
  • Coastal erosion and Climate Change: https://environment.data.gov.uk/shoreline-planning/help/coastal-erosion-and-climate-change
  • Coastal erosion risk projection maps: https://environment.data.gov.uk/shoreline-planning/unit/SMP6/6.12
  • Timeline of recent coastal erosion issues at Happisburgh: https://happisburgh.org.uk/ccag/timeline/
  • Scientific article about coastal erosion in Happisburgh: https://nora.nerc.ac.uk/id/eprint/214/1/Poulton_FINAL_text_with_images.pdf
  • Coastal risk screening tool: https://coastal.climatecentral.org/
  • BLAXLAND, Juliet. The easternmost sky: adapting to change in the 21st century. Inverness: Sandstone Press, 2021
  • BLAXLAND, Juliet. The easternmost house: a year of life on the edge of England. Dingwall, Rossshire: Sandstone Press, 2019
  • BUNTING, Madeleine. The seaside: England's love affair. London: Granta, 2023
  • DAVIES, John A. and WATERHOUSE, David M. G. Exploring Norfolk's Deep History Coast. Cheltenham: The History Press, 2023
  • TRETT, Mary and HOGGETT, Richard. The Book of Happisburgh. Wellington: Halsgrove, 2011
  • WILLIAMSON, Tom. England's Landscape: East Anglia. London: Collins, 2006

Website made by: Catarina