The Xiaoxiang are notable for their high ridge line, providing an unusually consistent straight range of peaks in the region. This is due to the Xiaoxiang's orogenic formation at the edge of the Yangtze Plate. The highest point of the range is Huatou Point (铧头尖) at above sea level. The Xiaoxiang Range was heavily glaciated during the last glacial period leaving many cirques and tarns dotted along the ridgeline today.