This sounds good for the Cowan tenements in the south.
"The Bald Hill pegmatite swarm is considered mineralised in its entirety, with anomalous Li2O and Ta2O5 values occurring throughout, resulting from the crystallisation of spodumene and tantalite as significant phases within the pegmatite mineralogy. The pegmatites vary in width and are generally comprised of quartz-albite-muscovite-spodumene in varying amounts. Late-stage albitisation in the central part of the main outcrop area has resulted in fine-grained, banded, sugary pegmatites with visible fine-grained, disseminated tantalite.
The Bald Hill pegmatite is known to form part of a much larger pegmatite swarm within the local area and has not been sufficiently closed off by current drilling; remaining open to the south."
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Cowan Tenements, page-60
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