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- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Linear features (shown as polylines) represent six classes of geological structural features e.g. faults, folds or landforms e.g. buried channels, glacial drainage channels at the ground or bedrock...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
The following dataset provides climate and cave monitoring data from Cueva de Asiul northern Spain between 2010 and 2014. This data set was initially presented in Smith et al., (2016) Cave...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
The images in this dataset are a sample of Doddington Sandstone from a micro-computed tomography (micro-CT) scan acquired with a voxel resolution of 6.4µm. This dataset is part of a study on the...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
Revised full proposal for scientific drilling (852-CPP2) 'GlaciStore: Understanding Pleistocene glaciation and basin processes and their impact on fluid migration pathways (North Sea)', submitted...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
The images in this dataset are a sample of Doddington Sandstone from a micro-computed tomography (micro-CT) scan acquired with a voxel resolution of 4.2µm. This dataset is part of a study on the...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
To complement the published research that arose from the CASSEM project (see bibliography of outputs) this book presents an overview of the results as multi-authored papers. Carbon Capture and...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 June 2026
A dataset is presented for defining real-time CO2 frost formation in a vertical packed column. ECT could estimate the internal permittivity distribution of the sensing area through boundary...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The survey area between Berwick and Beadnell lies on the North Sea coast just south of the Scottish border. It includes Holy Island and Budle Bay. The area is essentially rural and attracts a...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Loch Cairnbawn is one of the most northerly of Scottish sea lochs, only Lochs Laxford, Dughaill and Inchard lying further north on the west coast. The `Y'-shaped loch system, comprising Lochs a'...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The area covered in this report consists of a coastline which is very deeply dissected by many sea lochs. Three subdivisions are made within the area on the basis of typography. The northernmost of...
- 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
Loch Cairnbawn is one of the most northerly of Scottish sea lochs, only Lochs Laxford, Dughaill and Inchard lying further north on the west coast. The `Y'-shaped loch system, comprising Lochs a'...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
1. This report describes the results of surveys of nearshore sublittoral habitats and communities around the Hebridean islands of Jura and Islay in June and July 1982. 2. Sites were selected to...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
The survey area between Berwick and Beadnell lies on the North Sea coast just south of the Scottish border. It includes Holy Island and Budle Bay. The area is essentially rural and attracts a...
- 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
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,...
