15
results found
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Fjords in two areas of south-west Norway were surveyed to compare the benthic communities present with those found in Scottish sealochs. The results will assist in the evaluation of the nature...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Fjords in two areas of south-west Norway were surveyed to compare the benthic communities present with those found in Scottish sealochs. The results will assist in the evaluation of the nature...
- Published by:
- Marine Environmental Data & Information Network
- Last updated:
- 10 July 2024
Abundance and species composition were determined for phytoplankton in 361
water samples collected at 12 sites: five transects from 488N to 508S in the
Atlantic Ocean, the Benguela upwelling, the...
- Published by:
- Marine Environmental Data & Information Network
- Last updated:
- 01 December 2024
Abundance and species composition were determined for phytoplankton in 361
water samples collected at 12 sites: five transects from 488N to 508S in the
Atlantic Ocean, the Benguela upwelling, the...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
This is a map of the coastal physiographic type 'Sealoch'. The polygons represent sealochs, glacially-formed inlets (fjords, fjards) of western Scotland and Ireland, including the voes of Shetland....
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 February 2026
Geochemical data: %C, %OC, %IC, %N Physical Property data: Wet and dry bulk density, water content, porosity. Sediment cores extracted from Offshore Region: Loch Sunart NM 70277 63360, 56.705259,...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 February 2026
Geochemical data for the upper 300cm of giant piston core MD04-2832. Core MD04-2832 was collected from the middle basin of Loch Sunart a fjord on the west coast of Scotland from the research vessel...
- Published by:
- Greater London Authority
- Last updated:
- 25 February 2026
The GLA strongly believes that Government needs to do more to unlock the power of data, helping organisations to make better decisions and operate more efficiently. Greater sharing of information...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 25 February 2026
SCCS is the largest Carbon Capture and Storage (CCS) research group in the UK. Our internationally renowned researchers provide connected strength across the full CCS chain. With our unique...
- Published by:
- Greater London Authority
- Last updated:
- 12 February 2021
**Welcome to the City Data Strategy for London**.
This document is built around the following vision:
_We want London to have the most dynamic and productive City Data Market in the world. In...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Six lochs were surveyed by UMBSM/NCC during a visit to Harris and Lewis in 1988 (Howson 1989). Six more were subsequently surveyed in August 1990: Loch Stocknish, East and West Loch Tarbert and...
- Published by:
- Joint Nature Conservation Committee
- Last updated:
- 17 May 2018
Six lochs were surveyed by UMBSM/NCC during a visit to Harris and Lewis in 1988 (Howson 1989). Six more were subsequently surveyed in August 1990: Loch Stocknish, East and West Loch Tarbert and...
- Published by:
- British Geological Survey (BGS)
- Last updated:
- 15 March 2024
This report is a contribution to the Strategic Environmental Assessment (SEA7) conducted by the Department of Trade and Industry (now Department of Energy and Climate Change). The coastal and...
- 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
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...