Format:GIS polygon data (ESRI, MapInfo, others available by request)
£0.3 per km2 Subject to number of users, licence fee and data preparation fee.
Uses:Local-level to regional-level use
The BGS geological indicators of flooding dataset is a digital map based on the BGS Digital Geological Map of Great Britain at 1:50 000 scale (BGS Geology 50k). Coverage includes England, Wales and Scotland. It characterises superficial deposits on BGS Geology 50k in terms of their likely susceptibility to flooding, either from coastal inundation or fluvial (inland) water flow.
Geological maps show where all the floodplains and coastal plains in Britain are located and therefore the main areas at greatest risk of flooding; the BGS has produced the geological indicators of flooding dataset from this information. The map shows areas vulnerable to two main types of flooding; inland (river floodplains) and coastal/estuarine.
BGS geological indicators of flooding data should be regarded as complementary to, and not a replacement for, existing flood risk maps such as those provided by the Environment Agency.
Inland flood plains are flattish areas near to the river where mud, sand and gravel were deposited by previous floods. These materials are commonly known as ‘alluvium’ on geological maps, but they can also include lake deposits and river terraces.
On coastal plains, a range of marine deposits, for example tidal flats, define areas where the sea has formerly occupied the land.
The map is based on observation of the types of geological deposit present and does not take into account any human influences such as house building or flood-protection schemes. It also doesn’t take into account low-lying areas where flooding could occur but where there are no materials indicating flooding in the geological past.
The majority of these coastal and fluvial superficial deposits are considered ‘young’ in geological terms, most having been formed within the last few tens of thousands of years. Typically they have been laid down by processes of erosion and deposition and they have produced subtle topographical features, resulting in low-lying landforms we call floodplains and coastal plains.
The mapping of floodplains and coastal plain landforms, in conjunction with characterisation of deposits that underlie them, allows us to determine the extent of the coastal and inland flooding that created them. Observations made during recent major inland and coastal flooding events have demonstrated that the current floodplains and coastal plains continue to play a role in controlling where and how flooding occurs.
On this basis, the floodplains and coastal plains constituting areas of greatest susceptibility from flooding can be both visualised and defined by superficial deposits as depicted on geological maps.
Zone 1 deposits: include river alluvium and lacustrine (lake) alluvium.
Zone 2 deposits: younger river terraces or ‘floodplain terrace’ (raised level areas adjacent to or within floodplains, which represent the level of the floodplain prior to the most recent episode of floodplain formation).
Zone 2 deposits: are perceived to be susceptible to flooding in more extreme events such as very heavy and prolonged periods of rainfall and/or extreme high tides, with high wind speeds and storm surges. They are the areas where secondary flooding may occur. Older and higher river terraces have been excluded as they tend to lie outside the geologically defined floodplain and relate to older generations of floodplains extending back over hundreds of thousands of years in some cases.
Areas at risk from coastal inundation are similarly characterised by a range of estuarine or marine deposits that include, for example, tidal flats and low-lying raised beaches.
The two types of flooding, fluvial and coastal, are each separated into two zones as below:
Fluvial Zone 1 & Zone 2
Flooding from rivers where the capacity of the river channel is exceeded and water overflows. This is identified as fluvial in the BGS geological indicators of flooding, and is subdivided into higher (zone 1) and lower (zone 2) susceptibility categories.
Coastal Zone 1 & Zone 2
Flooding from the sea as a result of high tides and storm surges is identified as coastal flooding in BGS geological indicators of flooding. This is similarly subdivided into higher (zone 1) and lower (zone 2) susceptibility categories.
Both classifications are also subject to an element of pluvial flooding from land as a result of an episode of heavy intense rainfall. We do not have a specific category to identify this type of event.
BGS pluvial flooding research, with the Centre for Ecology and Hydrology (CEH), is ongoing.
BGS geological indicators of flooding does not currently identify the presence of permanent standing bodies of ‘water’ such as lakes or canals.