Filter by
364
results found
- Published by:
- Office for National Statistics
- Last updated:
- 24 November 2024
A best fit lookup between lower layer super output areas as at December 2001 and lower layer super output areas and local authority districts as at December 2011 in England and Wales. This product...
- Published by:
- Office for National Statistics
- Last updated:
- 24 November 2024
This is a best fit lookup file between middle layer super output areas as at December 2001 and middle layer super output areas and local authority districts as at December 2011 in England and...
- Published by:
- Environment Agency
- Last updated:
- 08 May 2026
PLEASE NOTE: This dataset has been retired. It has been superseded by https://environment.data.gov.uk/dataset/1786c0a7-5ace-457d-bcc9-ef114269e18f
Saltmarsh Change Summary:
The Saltmarsh Change...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Exe estuary is situated in southeast Devon and opens into the western side of Lyme Bay in the English Channel. The estuary is approximately 10km in length and between 1 and 2 km in width at the...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Exe estuary is situated in southeast Devon and opens into the western side of Lyme Bay in the English Channel. The estuary is approximately 10km in length and between 1 and 2 km in width at the...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The inner Solway is an area of predominantly sedimentary substrata, with large expanses of mobile sediment and constantly migrating river channels from the Rivers Esk and Eden which enter the Firth...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The inner Solway is an area of predominantly sedimentary substrata, with large expanses of mobile sediment and constantly migrating river channels from the Rivers Esk and Eden which enter the Firth...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The inner Solway is an area of predominantly sedimentary substrata, with large expanses of mobile sediment and constantly migrating river channels from the Rivers Esk and Eden which enter the Firth...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The inner Solway is an area of predominantly sedimentary substrata, with large expanses of mobile sediment and constantly migrating river channels from the Rivers Esk and Eden which enter the Firth...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
This information details the method of calculating dilatancy from pore volumometry measurements. In the velocity step tests, an initial shear enhanced compaction phase drastically reduces the...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
This survey was undertaken as part of a general study of the Menai Strait, commisioned by NCC, required to assist in decisions related to its designation as one of Britain's Marine Nature Reserves....
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
This survey was undertaken as part of a general study of the Menai Strait, commisioned by NCC, required to assist in decisions related to its designation as one of Britain's Marine Nature Reserves....
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Dart Estuary is situated on the south coast of Devon and opens into Start Bay. The estuary itself runs through a steep sided channel from Totnes, some 18 km to the north, to Dartmouth and...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Loch Linnhe forms the submerged western end of the Great Glen Fault which divides the highlands in two between Inverness and Fort William. With Lochs Etive, Creran, a'Choire, Leven and Eil...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The Dart Estuary is situated on the south coast of Devon and opens into Start Bay. The estuary itself runs through a steep sided channel from Totnes, some 18 km to the north, to Dartmouth and...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Loch Linnhe forms the submerged western end of the Great Glen Fault which divides the highlands in two between Inverness and Fort William. With Lochs Etive, Creran, a'Choire, Leven and Eil...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
This dataset contains raw (clean but not interpreted) triaxial compressive strength data of tests conductive at elevated pressure and temperature as outlined in "Vannucchi, P., Clarke, A., de...
- Published by:
- North Sea Transition Authority
- Last updated:
- 24 June 2026
The
North Sea Transition Authority (NSTA) launched the 32nd Offshore Licensing
Round on 11th July 2019. This included 16 blocks covering 15
Carboniferous and Bunter Fields that have reached CoP in...
- Published by:
- Environment Agency
- Last updated:
- 06 May 2026
NCEA Saltmarsh Network Analysis Ready dataset, comprised of spatial layers used in ecological monitoring and reporting, Natural Capital Ecosystem Assessments, and for coastal flood and erosion risk...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Data produced from NERC Grant NE/J008745/1. Grant Abstract: Iron sulfides are widespread in the environment, where they regulate and control the global geochemical iron and sulfur cycles. However,...
