Staca Fada - view south
Staca Fada - view west
Staca Fada Formation - close up 1
Stac Fada Formation - possible cooling joints? 2
Stac Fada Formation - possible cooling joints? 1
Stac Fada Formation
Bay of Stoer and Stac Fada
Bay of Stoer - north west
A' Clach Thuill south from Airn na Mòine 2
A' Clach Thuill south from Airn na Mòine 1
Gneiss erratic on Bay of Stoer Formation at Sgèir…
Sgèir na Tràghad bedding planes and sea
Sgèir na Tràghad panorama
Gneiss erratic on Bay of Stoer Formation at Sgèir…
Bay of Stoer Formation bedding plane
Sgèir na Tràghad 2
Sgèir na Tràghad 1
Bay of Stoer view NNW panorama x2 vertical exagger…
Bay of Stoer from Clachtoll broch An Dùn
Bay of Stoer NNW panorama
View north to Stac Fada from Clachtoll broch An Dù…
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Staca Fada Formation - close up 2
Stac Fada at the northern end of the Bay of Stoer, north west Scotland, is the type locality for the Stac Fada Formation, recently interpreted as a meteorite impact debris horizon, comparable with suevite from the much younger (Miocene, 15 Ma) Ries meteorite impact event in south Germany. The Stac Fada Formation lies within the Bay of Stoer Formation, mostly fluviatile sandstones and siltstones (Mesoproterozoic, c. 1200 Ma).
The Stac Fada Formation is about 12 metres thick at this location. The photo shows a close-up view of part of the middle section. The red-brown arkosic sand matrix contains darker grey-green chloritised clasts and fragments representing formerly molten debris blasted into the air from the original impact, together with un-melted rock fragments.
The prominent clast in the centre appears to be a somewhat deformed rock fragment which may have been near-molten during its passage through the air following the impact. Rounded edges and fish-tailed ends may indicate ablation by hot gasses whilst in motion.
Small cavities lined with pale pink feldspar crystals, especially on around the margin of the clast are interpreted as elutriation channels where steam and other volatiles escaped as the ejecta deposit cooled.
The coin shown for scale is a UK 5p piece, 1.8 cm in diameter.
The site of the meteorite impact is now correlated with a well-defined, roughly circular, low-gravity anomaly some 50 km to the east, near the village of Lairg, although any impact crater is now buried beneath younger rocks. SEE UPDATE BELOW.
For more details see:
Simms, M. J., 2015. The Stac Fada impact ejecta deposit and the Lairg Gravity Low: evidence for a buried Precambrian impact crater in Scotland?, Proceedings of the Geologists Association, 126 (2015), 742 - 761.
UPDATE June 2019:
Latest research based on detailed field observations, geochemical and geomagnetic work now seems to indicate that the impact site is located in the present day Minch, about 15 - 20 km WNW of Enard Bay. See:
Amor, K. et al, 2019. The Mesoproterozoic Stac Fada proximal ejecta blanket, NW Scotland: constraints on crater location from field observations, anisotropy of magnetic susceptibility, petrography and geochemistry. Journal of the Geological Society 176/4 (2019).
dx.doi.org/10.1144/jgs2018-093
The Stac Fada Formation is about 12 metres thick at this location. The photo shows a close-up view of part of the middle section. The red-brown arkosic sand matrix contains darker grey-green chloritised clasts and fragments representing formerly molten debris blasted into the air from the original impact, together with un-melted rock fragments.
The prominent clast in the centre appears to be a somewhat deformed rock fragment which may have been near-molten during its passage through the air following the impact. Rounded edges and fish-tailed ends may indicate ablation by hot gasses whilst in motion.
Small cavities lined with pale pink feldspar crystals, especially on around the margin of the clast are interpreted as elutriation channels where steam and other volatiles escaped as the ejecta deposit cooled.
The coin shown for scale is a UK 5p piece, 1.8 cm in diameter.
The site of the meteorite impact is now correlated with a well-defined, roughly circular, low-gravity anomaly some 50 km to the east, near the village of Lairg, although any impact crater is now buried beneath younger rocks. SEE UPDATE BELOW.
For more details see:
Simms, M. J., 2015. The Stac Fada impact ejecta deposit and the Lairg Gravity Low: evidence for a buried Precambrian impact crater in Scotland?, Proceedings of the Geologists Association, 126 (2015), 742 - 761.
UPDATE June 2019:
Latest research based on detailed field observations, geochemical and geomagnetic work now seems to indicate that the impact site is located in the present day Minch, about 15 - 20 km WNW of Enard Bay. See:
Amor, K. et al, 2019. The Mesoproterozoic Stac Fada proximal ejecta blanket, NW Scotland: constraints on crater location from field observations, anisotropy of magnetic susceptibility, petrography and geochemistry. Journal of the Geological Society 176/4 (2019).
dx.doi.org/10.1144/jgs2018-093
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