It departs from Talas range and spreads out to south-west to the right bank of Angren (river).

The highest elevations of the Chatkal Range are located in its north-east part.

[1] [2] Northern slopes are steep and short, while southern ones are gentle.

The range is composed by primarily of limestone, granite, and schist.

[3] The axial line of the range is composed of limestone of Lower Carboniferous and Upper Devonian.