Fig. 8. In this photo can be seen a massive, pink, granite facies of the Josephine pluton. Pink K-feldspar crystals are 1 cm long. This granite has exactly the same textures, including myrmekite, as occur in the narrow "dikes" that are observed in Fig. 7, but now this rock is part of a pluton more that one km wide. Is not the myrmekite in both places evidence that K-metasomatism can create granite bodies on a plutonic scale with a uniform composition and massive appearance?