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Scales of preservation and root causes of mantle heterogeneities in the Iapetan Ocean convecting upper mantle NERC grant NE/J00457X/1

Although the terrestrial mantle comprises ~80 vol.% of our planet, its compositional architecture is not well understood despite the importance such knowledge holds for constraining Earth's thermal...

How does the Earth's crust grow at divergent plate bundaries? A unique opportunity in Afar, Ethiopia. [REMOTE SENSING SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

GSNI GeoIndex Groundwater vulnerability screening layer

This map layer represents an assessment of the vulnerability of groundwater within the uppermost aquifer. This classification was initially undertaken to support groundwater assessments undertaken...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [Gravity Sub Report]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [GEODESY SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [ANALOGUE MODELLING SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [STRUCTURAL SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar Ethiopia. [PETROLOGY SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [SEISMOLOGY SUB REPORT] (University of Leeds)

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [MAGNETOTELLURICS SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [Numerical Modelling SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

How does the Earth's crust grow at divergent plate boundaries? A unique opportunity in Afar, Ethiopia. [MAPPING SUB REPORT]

PROJECT DETAILS ONLY - NO DATA. The African continent is slowly splitting apart along the East African rift valley, a 3000 km-long series of deep basins and flanking mountain ranges. This process...

Habitat point records from 1987 OPRU HRE Christchurch Harbour survey

Christchurch Harbour is situated in east Dorset, approximately mid-way between Poole Harbour and the Solent. It was formed during the post glacial marine transgression which drowned the combined...

Habitat point records from 1988 UMBSM Loch Ryan survey

Loch Ryan is situated at the southern entrance to the Firth of Clyde and is the most southerly of the Scottish sea lochs. It is 13.4 km in length and is shallow over its entire area with an average...

Habitat point records from 1981 James south Cornwall sublittoral survey

The principal aim of this survey was to record community and habitat information from the rocky sublittoral along the coast of Cornwall from Land's End to Nare Head (10 km north-east of Falmouth)....

Species point records from 1987 OPRU HRE Christchurch Harbour survey

Christchurch Harbour is situated in east Dorset, approximately mid-way between Poole Harbour and the Solent. It was formed during the post glacial marine transgression which drowned the combined...

Species point records from 1981 James south Cornwall sublittoral survey

The principal aim of this survey was to record community and habitat information from the rocky sublittoral along the coast of Cornwall from Land's End to Nare Head (10 km north-east of Falmouth)....

Species point records from 1988 UMBSM Loch Ryan survey

Loch Ryan is situated at the southern entrance to the Firth of Clyde and is the most southerly of the Scottish sea lochs. It is 13.4 km in length and is shallow over its entire area with an average...

Species point records from 1989 UMBSM Mull sealochs survey

The island of Mull, which is the second largest of the Scottish Inner Hebrides island group, has a deeply indented coastline containing nine sealochs and at least one other large embayment. The...