The spire is cylindrical, not or hardly attenuated towards the base. The peristome is double, with the inner rim projecting distinctly beyond the outer rim. The radial ribs are rather high and thick, and spiral striation is absent. Shells are recorded from soil deposits in disturbed to degraded secondary woodland on limestone bedrock. Shells are known from Kampot Province, Cambodia, and the Ha Tien area of Kien Giang Province, Vietnam.
The spire is cylindrical, not or hardly attenuated towards the base.
Shells are recorded from soil deposits in disturbed to degraded secondary woodland on limestone bedrock.
The peristome is double, with the inner rim projecting distinctly beyond the outer rim.
The radial ribs are rather high and thick, and spiral striation is absent.
An extinction-risk assessment has not been added yet.