The shell is globose. The spire is much elevated. The aperture is obliquely crescent-shaped. The described material came from the limestone areas of Bardai Mountain and Kyankaw Mountain. It is known from two limestone areas, Bardai Mountain and Kyankaw Mountain, in the southern Salween River basin at Hpa-An, Kayin State, Myanmar.
The shell is globose.
The described material came from the limestone areas of Bardai Mountain and Kyankaw Mountain.
The spire is much elevated.
The aperture is obliquely crescent-shaped.
An extinction-risk assessment has not been added yet.