abstract
Aspects of the biology, physico-chemistry and geology of a remote inland nunatak pond are described. The pond is unusually located in that it occurs in a rocky depression forming part of the nunatak. It occurs in the upper part of a Kullen-type sill which forms part of the c 1000 Ma Borgmassivet Suite. Crude layering in the sill suggests that its morphology is highly undulating, and that the depression in which the pond occurs is controlled by this primary structure.