Vegetation is mostly absent, only some lichens and mosses.
Landform:
Hill summit, deglaciated during the Holocene; May have been a nunatak in the early Holocene; Frost shattering very abundant; stone circles and stone-banked solifluction lobes present nearby.
Lithology:
Bedrock: Myers bluff formation (shales, fine sandstones and greywacke) – Carboniferous to Jurassic.
Medium/Low ice content.