Outcrops of axinite-bearing veins in the zawns north of Botallack Head. The area is sometimes referred to as Roscommon cliff, which represents only a minor portion of it.
The mineralization of the veins is pretty much the same and therefore, Wheal Cock Zawn has been included here and is not listed as a separate locality. However, only the Stamps and Jowl Zawn is considered as the type locality of Stokesite.
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UK OS Grid Reference: SW363341
Map Reference: 50°8'51"N , 5°41'29"W
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