This specimen exhibits a replacement texture of former Spodumene, a lithium silicate. The original Spodumene crystal form has been nicely preserved by the fine-grained Cookeite, another aluminosilicate of lithium. David London in his book "Pegmatites", sites examples of selective replacement, in which some crystals of the pegmatites are completely replaced yet an adjacent mineral is left completely untouched.
I have not seen this particular replacement before, but is not that unusual. The Bennet pegmatite in Maine and pegmatites in Portugal have very similar examples. In this specimen the Spodumene was altered to Cookeite and Kaolinite. The Kaolinite eventually dissolved out leaving behind the Cookeite cast. A good paper on this process can be read here: Alteration of Spodumene to Cookeite (2007) Clays and Clay Minerals, Bobos, I. et al V55 n3. Although it concerns a Portugal occurrence rather than the Golconda pegmatite, where this specimen was collected. Spodumene does weather easily and has good cleavage, which creates conduits for solutions to penetrate and breakdown the chemistry.
Cookeite
Formula
(Al,Li)3Al2(Si,Al)4O10(OH)8
Crystal System
Monoclinic
Crystal Habit
Micaceous, Pseudo Hexagonal
Cleavage
Perfect, None, None
Luster
Vitreous (Glassy)
Color
white, green, brown, yellowish white, pinkish white
