Crystals of pascoite, which occur in granular crusts, are minute and lath-like with oblique terminations.
The mineral is dark red-orange to yellow-orange in color and dirty yellow when partially dehydrated.
It occurs as efflorescences in mine tunnels or as a product leached out of surficial vanadium oxides by ground water.
Pascoite has been found in association with carnotite.

Pascoite melts readily to form a deep red liquid.

Pascoite is a member of the eponymous pascoite group.
The magnesium analogue of pascoite is magnesiopascoite.
Crystals of pascoite, which occur in granular crusts, are minute and lath-like with oblique terminations. The mineral is dark red-orange to yellow-orange in color and dirty yellow when partially dehydrated. It occurs as efflorescences in mine tunnels or as a product leached out of surficial vanadium oxides by ground water. Pascoite has been found in association with carnotite.
Pascoite melts readily to form a deep red liquid.
Pascoite is a member of the eponymous pascoite group. The magnesium analogue of pascoite is magnesiopascoite.
Pascoite