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The Great Glen hosts the most prominent fault in the British Isles, the Great Glen Fault. It originated towards the end of the Caledonian Orogeny (around 430-390 million years ago), and cuts diagonally across the Highlands from Fort William to Inverness.
- North Anatolian Fault
The North Anatolian fault stretches across northern Turkey...
- Cwm Idwal
100 Great Geosite Cwm Idwal . For more information about...
- Outer Isles
The great earthquakes that occur on these thrust faults...
- Hartland Quay
Hartland Quay - The Geological Society of London - The Great...
- Vale of Eden
The Vale of Eden is part of the Pennine Fault System that...
- Lulworth Cove
Lulworth Cove - The Geological Society of London - The Great...
- Cairngorms
Cairngorms - The Geological Society of London - The Great...
- Giant's Causeway
This dormant phase was interrupted in north Antrim by the...
- North Anatolian Fault
Map of the Great Glen Fault and other late Caledonian strike-slip faults in Scotland and northwestern Ireland. The Great Glen Fault is a strike-slip fault that runs through the Great Glen in Scotland. Occasional moderate tremors have been recorded over the past 150 years.
Large-scale digital mapping of the Philippine fault zone based on aerial photograph interpretation. The 1,200-km-long Philippine fault zone (PFZ) is a major tectonic feature that transects the whole Philippine archipelago from northwestern Luzon to southeastern Mindanao.
Below are just a couple of many potential links: USGS - The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines. USGS - Remembering Mount Pinatubo 25 Years On. News and updates for members of the public and policy makers interested in how the geosciences interact with society.
Sep 30, 2013 · The Philippine fault is a ~1250-km-long, left-lateral strike-slip fault extending NNW parallel to the Philippine archipelago. This fault has been very active in the past 200 years with...
Aug 12, 2024 · A popular conceptual tectonic model envisages the Great Glen Fault to be part of a sinistral strike-slip system active during the mid-Silurian through early Devonian with c. 700 km of displacement.
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Sep 13, 2024 · A popular conceptual tectonic model envisages the Great Glen Fault to be part of a sinistral strike-slip system active during the mid-Silurian to early Devonian with c. 700 km of displacement. Here we use sedimentological, geochemical and detrital zircon age data to show that restoring 250–300 km of displacement suffices to fulfil key ...