The Man of War Gneiss occurs at the southern end of Lizard Point, where it is exposed mainly in off-shore reefs and appears to have intruded the Old Lizard Head Series by lit-par-lit injection of quartz and feldspar. The multiple folding of the gneisses, similar to that of the enclosing rocks, suggests that they are an early, and probably pre-peridotite, intrusion.
References:
- Edmonds, E.A., McKeown, C., and Williams, M. (1975): British Regional Geology - South West England., 4th ed., p. 18
Mineral List:2 entries listed.
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