The shell is obliquely ovate, white and translucent. The shell surface has transverse ridges and becomes nearly smooth, with few ridges near the opening. The opening is nearly quadrangular, with one strong parietal lamella and sometimes a small second lamella adjoining it at a right angle. It has been found in limestone karsts of Kayin State, southeastern Myanmar. The Bardai Mountain material includes animals collected alive. The confirmed live-animal material comes from Bardai Mountain, Hpa-an Township, Kayin State, southeastern Myanmar.
The shell is obliquely ovate, white and translucent.
It has been found in limestone karsts of Kayin State, southeastern Myanmar. The Bardai Mountain material includes animals collected alive.
The shell surface has transverse ridges and becomes nearly smooth, with few ridges near the opening.
The opening is nearly quadrangular, with one strong parietal lamella and sometimes a small second lamella adjoining it at a right angle.
An extinction-risk assessment has not been added yet.