The spire is rather low-conical; the last half-whorl is not or hardly widened. The outer whorl bears dense, somewhat uneven radial riblets with thin low crests that erode easily and persist better around the umbilicus. The aperture is circular, with a slightly thickened and widened peristome. Shells are recorded from deep soil deposits in moderately disturbed to degraded partly deciduous woodland on limestone bedrock, and organic soil deposits in caves. Shells are recorded from the Kampot and Banteay Meas areas of Kampot Province, Cambodia, and Kien Luong District, Kien Giang Province, Vietnam.
The spire is rather low-conical; the last half-whorl is not or hardly widened.
Shells are recorded from deep soil deposits in moderately disturbed to degraded partly deciduous woodland on limestone bedrock, and organic soil deposits in caves.
The outer whorl bears dense, somewhat uneven radial riblets with thin low crests that erode easily and persist better around the umbilicus.
The aperture is circular, with a slightly thickened and widened peristome.
An extinction-risk assessment has not been added yet.