File:GA Image 0441.jpg
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Summary
Figure 7 Plan of Westcombe Park. The two chalk-pits a few yards eastward of the station were first visited. The dip of the Chalk, as indicated by the layers of flint, is,, in this neighbourhood, slight in amount and southerly in direction, and the same remark applies to the dip of the overlying Lower Tertiary Beds. A little Thanet Sand, however, is seen overlying the Chalk in either pit.
| From: A record of excursions made between 1860 and 1890. Edited by Thomas Vincent Holmes , F.G.S. and C. Davies Sherborn, F.G.S. London: Edward Stanford [For the Geologists’ Association], 1891. Source: Cornell University copy on the Internet Archive (Public domain work) |
Licencing
| This image is Copyright Geologists' Association. The images may be reproduced free of charge for any non-commercial use in any format or medium provided they are reproduced accurately and not used in a misleading or derogatory context. Where any images on this site are being republished or copied to others, the source of the material must be identified and the copyright status acknowledged. For all other uses of the images please contact the Geologists' Association archive@geologistsassociation.org.uk |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:05, 3 February 2022 | Error creating thumbnail: File missing | 1,063 × 796 (154 KB) | Scotfot (talk | contribs) | Figure 7 Plan of Westcombe Park. The two chalk-pits a few yards eastward of the station were first visited. The dip of the Chalk, as indicated by the layers of flint, is,, in this neighbourhood, slight in amount and southerly in direction, and the same remark applies to the dip of the overlying Lower Tertiary Beds. A little Thanet Sand, however, is seen overlying the Chalk in either pit. {{Template:GA excursions1860-1890}} = Licencing == {{GA}} |
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