Krauskopfite, BaSi2O4(OH)2·2H2O,
one of the rarer species at the deposits, is restricted to
a single site above Rush Creek, where it occurs with
macdonaldite in white veinlets up to 5-mm thick (Site 3).
Krauskopfite is opaque to translucent white, and occurs
as cleavage masses and occasional elongated tabular
cleavages on fracture surfaces.
