abstract
lstind Peak was visited in November 1973 and successfully scaled. Attention was given to the relationship between the Tindeklypa and lstind Formations and to the stratigraphy of the latter. The stratigraphy and lithology are discussed and it is concluded that the lstind Formation is merely an upward continuation of the Tindeklypa Formation and that no angular unconformity exists between these two formations. It was also established that the igneous rocks occurring in the sequence are intrusive sills and not lava flows.