The Xiaoxiang Range is situated in the rugged mountainous regions of
Southwestern China where the
Hengduan Mountains abut the
Yungui Plateau. Despite lying between the
Dadu and
Yalong Rivers, the Xiaoxiang are not considered part of the
Daxue Mountains. The Xiaoxiang, and all mountains further south bounded by the
Jinsha (upper
Yangtze) River, are more commonly considered a northern extension of the Yungui. The Xiaoxiang Range is separated from the Daxue Mountains by a narrow fault trench through which the
G5 Expressway runs. 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. The Xiaoxiang Range is drained to west by the
Anning River and its tributaries. The Anning separates the Xiaoxiang from the
Miaoniu Mountains to the west. To the north and east, the Xiaoxiang is drained by tributaries of the Dadu River. Across the Dadu to the north lies the
Daxiang Range. To the south and east are poorly defined mountainous regions with no range-like features with the exception of the
Daliang Mountains further east. ==Human activity==