| WHITE-LEAVED OAK SHALE FORMATION | |||||
| Computer Code: | WOA | Status Code: | FORMAL ENTRY | ||
| Preferred Map Code: | WOa | ||||
| Age or Age Range: | [ EM ] | LATE CAMBRIAN | to | [ ] | |
| Lithological Description: |
| Dark grey mudstones. |
| Definition of Lower Boundary: |
| Faulted junction with Hollybush Sandstone. |
| Definition of Upper Boundary: |
| Nowhere exposed; probably conformable junction with Bronsil Shale. |
| Thickness: |
| 150-250m |
| Geographical Limits: |
| Southwest of Raggedstone Hill; west side of Midsummer Hill, both at south end of Malvern Hills; small proving in well at West Malvern. |
| Parent Unit: | Parent Unit Code: |
| NO IMMEDIATE PARENT [HIERARCHY CODE: NO PARENT OF THE NEXT HIGHER RANK IS IDENTIFIED] | NOPAR |
| Previous Name(s): | Previous Code(s): |
| BLACK SHALES OF MALVERN | |
| WHITE-LEAVED OAK SHALES | WLSH |
| Alternative Name(s): |
| none recorded or not applicable |
| Stratotypes: | |
| Type Area | White-leaved Oak village, Hereford-Worcester. |
| Reference(s): |
| Groom, T T, 1902. The Sequence of the Cambrian and Associated Beds of the Malvern Hills. Quarterly Journal of the Geological Survey, Vol.58, p.99. |
| Worssam, B C, Ellison, R A, and Moorlock, B S P. 1989. Geology of the country around Tewkesbury. Memoir of the British Geological Survey, Sheet 216 (England and Wales). |
| 1:50K maps on which the lithostratigraphical unit is found, and map code used: | |
| Map Code | Sheet Name |
| E | 216 |