The shell is yellowish brown to pale greenish brown and moderately low-conical. The shell has a silky lustre above the periphery and is glossy below it. The umbilicus is closed, and the aperture lip is moderately thickened and turned back. Shells are recorded from montane to subalpine forest on sandstone and granodiorite bedrock at 2400–3300 m. It is endemic to Sabah, Malaysia, and known only from Mount Kinabalu.
The shell is yellowish brown to pale greenish brown and moderately low-conical.
Shells are recorded from montane to subalpine forest on sandstone and granodiorite bedrock at 2400–3300 m.
The shell has a silky lustre above the periphery and is glossy below it.
The umbilicus is closed, and the aperture lip is moderately thickened and turned back.
An extinction-risk assessment has not been added yet.