A nunatak is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also called glacial islands, and smaller nunataks rounded by glacial action may be referred to as rognons.
Starr Nunatak, on the coast of Victoria Land, Antarctica
Cântaro Magro, Serra da Estrela, Portugal, formed as a nunatak during the last ice age and now exposed.