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Alternating garnet-rich (brown), magnetite-rich and hornblende-rich (black) bands in skarn. The skarn is thought to have formed where granite-related fluids interacted with the different lithologies of the metamorphic aureole.
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Although granite is not exposed at Botallack, abundant granite boulders are scattered in the mine waste. Granite is found at shallow depths below the current exposure. The granite in this area is variably megacrystic with large orthoclase crystals in a matrix of quartz, orthoclase, biotite, muscovite and plagioclase.
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Banded skarn with domains rich in garnet (brown) and hornblende (black). The subhorizontal banding appears to follow cleavage in the host rock.
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Boundary between magnetite-hornblende skarn (black, lower part of photo) and garnet skarn (brown, upper part of photo).
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Folded quartz vein in Devonian metabasalt. Although the metabasalt (as a competent rock) doesn't display extensive foliation, the quartz vein has been folded and can be inferred to pre-date the Variscan deformation.
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Folded quartz veins in Devonian slate.
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Small trial adit along the path. Trial adits like this were commonly dug to explore the underground continuity of faults or small mineral exposures at the surface.
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Steeply dipping interbedded slate and metabasite.
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The host rock is a succession of slates and interbedded metabasites. At the Grylls Bunny, this host has been intensely altered to clays and has a very soft and crumbly appearance. Subhorizontal foliation is visible from the weathering. Subvertical veins carry quartz and tourmaline with occasional arsenopyrite and pyrite.
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Tourmaline impregnation in the wall rock around a subvertical quartz vein
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A 20 cm thick band of tourmalinite (black) is exposed between the lower workings of the Gryll's Bunny excavations. The band appears to have followed the tin floor that was the subject of the excavation.
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