http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AP528224.jpg 2026-04-24T00:08:50Z Revision history for this page on the wiki MediaWiki 1.42.3 http://earthwise-staging.bgs.ac.uk/index.php?title=File:P528224.jpg&diff=17310&oldid=prev 2015-07-11T21:49:01Z

<p>User created page with UploadWizard</p> <p><b>New page</b></p><div>=={{int:filedesc}}==<br /> {{Information<br /> |description={{en|1=Southern face of Kirkhill Quarry [NK 011 528] in 1979 (P528224). The sands and gravels resting on bedrock belong to the Pitscow Sand and Gravel Formation. The conspicuous pale band at their surface is the podzolic Kirkhill Palaeosol Bed. Periglacial sediments of the Swineden Sand Bed and the Camphill Gelifluctate Bed succeed this. The base of the Rottenhill Till Formation is at shoulder level with the figure. It is weathered towards the top (Fernieslack Palaeosol Bed) and is overlain by the pale coloured Corsend Gelifuctate Bed. The overlying Hythie Till Formation has a sharp erosional base. Note, the deformation structure affecting sediments beneath the till (above and to the left of the figure). Approximately 8 m of sediments are exposed. From: Plate 22 in MERRITT, J W, AUTON, C A, CONNELL, E R, HALL, A M, and PEACOCK, J D. 2003. Cainozoic geology and landscape evolution of north-east Scotland. Memoir of the British Geological Survey, Sheets 66E, 67, 76E, 77, 86E, 87W, 87E, 95, 96W, 96E and 97 (Scotland).}}<br /> |date=2015-07-11 22:46:00<br /> |source=British Geological Survey<br /> |author=British Geological Survey<br /> |permission=<br /> |other versions=<br /> }}<br /> <br /> =={{int:license-header}}==<br /> {{subst:Custom license marker added by UW}}<br /> {{BGS}}<br /> <br /> [[Category:Uploaded with UploadWizard]]</div>

Scotfot