The very thin, somewhat translucent shell is yellowish brown to brown and low-conical. The last whorl is rounded at the periphery in adults but angular in juveniles. The umbilicus is open and very narrow. Shells are recorded from montane to subalpine forest on granodiorite and sandstone soils at 1600–3400 m. It is known from Mount Kinabalu, Sabah, Malaysia.
The very thin, somewhat translucent shell is yellowish brown to brown and low-conical.
Shells are recorded from montane to subalpine forest on granodiorite and sandstone soils at 1600–3400 m.
The last whorl is rounded at the periphery in adults but angular in juveniles.
The umbilicus is open and very narrow.
An extinction-risk assessment has not been added yet.