stripes
A ring of four prominent phonolite plugs rising 150-250 m together with a ridge, also of phonolite, are separated by talus slopes but probably coalesce at depth. The phonolite is highly porphyritic with phenocrysts of alkali feldspar, nepheline and aegirine-augite/aegirine in a groundmass of the same minerals, apatite and magnetite.
DARTON, N.H. and O'HARRA, C.C. 1907. Devils Tower Folio: Wyoming. Geologic Atlas of the United States: 150.
HILL, D.J., IZETT, G.A. and NAESER, C.W. 1975. Early Tertiary fission track ages of sphene from Devils Tower and Missouri Buttes, Black Hills, northeastern Wyoming. Abstracts with Programs, Geological Society of America, 7: 613-4.
MCDOWELL, F.W. 1971. K-Ar ages of igneous rocks from the western United States. Isochron/West, New Mexico Bureau of Mines and Mineral Resources, 2: 1-16