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Clynelish Quarry Sandstone

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Image
Logs of the Fascally Sandstone and Clynelish Quarry Sandstone members on the south bank of River Brora (H4 and 5 in Fig. 2). The sections, approximately 300 m apart and located more or less along strike of the Helmsdale Fault, can be correlated by a fine-grained marker bed. Notice the change in style of the sandstones from amalgamated, non-graded, structureless beds at Fascally to structureless, top-graded beds at Cawcrask.
Published: 18 September 2020
Fig. 5. Logs of the Fascally Sandstone and Clynelish Quarry Sandstone members on the south bank of River Brora (H4 and 5 in Fig. 2 ). The sections, approximately 300 m apart and located more or less along strike of the Helmsdale Fault, can be correlated by a fine-grained marker bed. Notice
Image
Log and interpreted photomosaic of the Clynelish Quarry Sandstone in the Braamberry Quarry (Fig. 2). The sandstone beds are structureless with wavy amalgamation surfaces marked by diffuse zones of clay chips and shell debris.
Published: 18 September 2020
Fig. 4. Log and interpreted photomosaic of the Clynelish Quarry Sandstone in the Braamberry Quarry ( Fig. 2 ). The sandstone beds are structureless with wavy amalgamation surfaces marked by diffuse zones of clay chips and shell debris.
Image
Interpreted photomosaic of the Clynelish Quarry Sandstone at Fascally (H5 in Fig. 2). Individual beds, outlined with black lines, are wedge-shaped or have distinct snouts. Bed boundaries are wavy with amplitudes up to about 160 cm (lower part of exposed section central part of photograph) and inclinations up to about 25°.
Published: 18 September 2020
Fig. 7. Interpreted photomosaic of the Clynelish Quarry Sandstone at Fascally (H5 in Fig. 2 ). Individual beds, outlined with black lines, are wedge-shaped or have distinct snouts. Bed boundaries are wavy with amplitudes up to about 160 cm (lower part of exposed section central part
Journal Article
Published: 18 September 2020
Scottish Journal of Geology (2020) 56 (2): 159–174.
...Fig. 5. Logs of the Fascally Sandstone and Clynelish Quarry Sandstone members on the south bank of River Brora (H4 and 5 in Fig. 2 ). The sections, approximately 300 m apart and located more or less along strike of the Helmsdale Fault, can be correlated by a fine-grained marker bed. Notice...
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Image
Interpretation of the depositional environment of the Clynelish Quarry Sandstone Member. The Sandstone comprises subaqueous delta-scale clinoforms and lobes prograding away from the Helmsdale Fault during onset of rifting. 1 indicates the position of Strathsteven, 2 of Braamberry and Clynelish quarries and Fascally, and 3 of Cawcrask.
Published: 18 September 2020
Fig. 17. Interpretation of the depositional environment of the Clynelish Quarry Sandstone Member. The Sandstone comprises subaqueous delta-scale clinoforms and lobes prograding away from the Helmsdale Fault during onset of rifting. 1 indicates the position of Strathsteven, 2 of Braamberry
Image
Interpreted photomosaic of the Fascally Sandstone and Clynelish Quarry Sandstone at Cawcrask (H4 in Fig. 2). Bed boundaries, outlined with black lines, show a marked relief. Load structures and sand intrusion at the marker bed level can be observed in the SSW part of the outcrop.
Published: 18 September 2020
Fig. 6. Interpreted photomosaic of the Fascally Sandstone and Clynelish Quarry Sandstone at Cawcrask (H4 in Fig. 2 ). Bed boundaries, outlined with black lines, show a marked relief. Load structures and sand intrusion at the marker bed level can be observed in the SSW part of the outcrop.
Image
Diagram showing the progradational–aggradational–retrogradational evolution of the clinoform-bedded succession of the Clynelish Quarry Sandstone Member exposed at Strathsteven as a function of the ratio between sediment supply and creation of new accommodation space.
Published: 18 September 2020
Fig. 16. Diagram showing the progradational–aggradational–retrogradational evolution of the clinoform-bedded succession of the Clynelish Quarry Sandstone Member exposed at Strathsteven as a function of the ratio between sediment supply and creation of new accommodation space.
Image
Clynelish Sandstone Quarry, near Brora, around 1914 (reproduced with permission of British Geological Survey; Image No. 000-000-032-206-C). Stone from this quarry was used to build London Bridge and Dunrobin Castle.
Published: 01 April 2008
Fig. 9. Clynelish Sandstone Quarry, near Brora, around 1914 (reproduced with permission of British Geological Survey; Image No. 000-000-032-206-C). Stone from this quarry was used to build London Bridge and Dunrobin Castle.
Journal Article
Published: 01 April 2008
Scottish Journal of Geology (2008) 44 (1): 65–73.
...Fig. 9. Clynelish Sandstone Quarry, near Brora, around 1914 (reproduced with permission of British Geological Survey; Image No. 000-000-032-206-C). Stone from this quarry was used to build London Bridge and Dunrobin Castle. ...
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Journal Article
Published: 07 November 2013
Quarterly Journal of Engineering Geology and Hydrogeology (2013) 46 (4): 405–420.
...), Saltwick Formation, Ravenscar Group, Middle Jurassic. ( f ) Grinshill Quarry (Grinshill Stone), Sherwood Sandstone Group, Triassic. ( g ) Corsehill Quarry, (Coreshill Stone) Sherwood Sandstone Group, Triassic. ( h ) Hillhouse Edge Quarry (Huddersfield White Rock), Millstone Grit Group, Carboniferous...
FIGURES
Journal Article
Published: 01 October 2001
Journal of Foraminiferal Research (2001) 31 (4): 324–349.
... interval immediately overlying the concretional level, and the event is dated to the uppermost Callovian Quenstedtoceras lamberti Subzone ( Stephen and Davies, 1998 ). The regressive phase of cycle B4 comprises the Clynelish Quarry Sandstone of tide-influenced upper shoreface origin, and the Brora...
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Journal Article
Journal: Palynology
Published: 01 January 2005
Palynology (2005) 29 (1): 87–142.
... Formation) to the Fascally Sandstone Member (Brora Arenaceous Formation) and all the intercalated lithostratigraphic units, and six samples from the Balintore Formation (Text-Figure 3 ). The Clynelish Quarry Sandstone and the Brora Sandstone members of the Brora Arenaceous Formation were not sampled due...
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Series: Geological Society, London, Geology of Series
Published: 20 August 2024
DOI: 10.1144/GOS5-2023-8
EISBN: 9781786206893
...–Lamberti Zone has been identified (Page in Wright and Cox 2001 ). The Fascally Sandstone Member, composed of bioturbated sandstones with common ammonites, belongs to the uppermost Callovian Lamberti Zone. The uppermost Clynelish Quarry Sandstone Member is a well-sorted cross-bedded sandstone. Previously...
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Book Chapter

Series: Geological Society, London, Geology of Series
Published: 01 January 2002
DOI: 10.1144/GOS4P.11
EISBN: 9781862393905
...), but the scattered nature of present outcrop makes detailed interpretation of the stratigraphy speculative. At the base of the Formation the Fascally Sandstone is bioturbated and contains moulds of bivalves in thin-bedded muddy sandstones with calcareous concretions. The succeeding Clynelish Quarry Sandstone...
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Series: Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2003.207.01.06
EISBN: 9781862394896
... the sandstones quarried were of Devonian age, the foreshore hosts sediments of Upper Jurassic (Kimmeridgian) age ( Waterston 1951 ) and are covered by mid-tide. In breaks from work, and tide permitting, Miller explored this new shoreline and soon discovered for himself the palaeontologicalriches in close...
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