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- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Data identifying landscape areas (shown as polygons) attributed with geological names and rock type descriptions. The scale of the data is 1:25 000 scale. Onshore coverage is partial and BGS has no...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Data identifying landscape areas (shown as polygons) attributed with geological names. The scale of the data is 1:25 000 scale. Onshore coverage is partial and BGS has no intention to create a...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
The data are transcripts of qualitative community surveys carried out in Amuria (A) and Katakwi (K) districts, north-eastern Uganda, as part of a pilot project looking at causes of borehole/hand...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Data identifying landscape areas (shown as polygons) attributed with geological names and rock type descriptions. The data is presented at 1:50 000 scale. Onshore coverage is provided for England,...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Data identifying landscape areas (shown as polygons) attributed with geological names. The scale of the dataset is 1:250 000, providing a generalised geology. Onshore coverage is provided for all...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
The map shows the localities where samples that form part of the BGS rock collections have been taken. Many of these samples are from surface exposure, and were collected by BGS geologists during...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
The property subsidence assessment dataset provides an understanding of the shrink-swell hazard at both the individual property and/or postcode level for England and Wales. It builds upon the BGS...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
In developing countries, the dominant model for managing rural water supplies is a community-level association or committee. Although a relative paucity of evidence exists to support this model, it...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Dual stable isotope analysis comprising nitrogen-15 and oxygen-18 ratios for groundwater samples collected every 2-3 months over one hydrogeological year from the East Riding of Yorkshire. Isotopic...
- Published by:
- Department for Environment, Food and Rural Affairs
- Last updated:
- 11 June 2018
The December survey of Agriculture provides information and evidence on the condition of the agricultural industry in England.
Source agency: Environment, Food and Rural Affairs
Designation:...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Loch Leven is a relatively small sealoch in Lochaber District of Highland Region on the west coast of Scotland and forms part of the extensive Loch Linnhe system. To the north lies Fort William,...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Fieldwork, using SCUBA techniques, was carried out in June and August 1987, and showed that the muddy sediments of the upper arms of Loch Sween, Argyll, Scotland, were extensively bioturbated by...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Loch Etive is a typical fjord, carved into grantie and metamorphic rocks by glaciers from the Rannoch Moor area. The steeply walled, deep upper basin is followed by a series of shallower basins and...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Cowal peninsula and mainland around the northern Firth of Clyde are deeply indented by six sealochs: Lochs Riddon, Striven, Goil, Long, the Holyloch and the Gareloch. The first two are...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Uist island chain in the Outer Hebrides is formed of Lewisian gneiss and is generaly low-lying with extensive and complex fresh and brackish water systems and a heavily indented eastern...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Loch Etive is a typical fjord, carved into grantie and metamorphic rocks by glaciers from the Rannoch Moor area. The steeply walled, deep upper basin is followed by a series of shallower basins and...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Fieldwork, using SCUBA techniques, was carried out in June and August 1987, and showed that the muddy sediments of the upper arms of Loch Sween, Argyll, Scotland, were extensively bioturbated by...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Uist island chain in the Outer Hebrides is formed of Lewisian gneiss and is generaly low-lying with extensive and complex fresh and brackish water systems and a heavily indented eastern...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Loch Leven is a relatively small sealoch in Lochaber District of Highland Region on the west coast of Scotland and forms part of the extensive Loch Linnhe system. To the north lies Fort William,...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Cowal peninsula and mainland around the northern Firth of Clyde are deeply indented by six sealochs: Lochs Riddon, Striven, Goil, Long, the Holyloch and the Gareloch. The first two are...
