A Hill is generally considered to be an elevated piece of land less than 600-610meters high, and a Mountain is an elevation of land that is more than 610m high. Some hills are called mountains while some mountains are referred to as hills
Related to the eroded and depositional features of the rivers like ox-bow lake, meander, levees, etc. All types of river patterns including dendritic are part of drainage
The Safed Koh range is drained by River Kabul, which runs in a West to East direction and eventually joins River Indus. The Waziristan hills are drained by small seasonal rivers like Kurram, Tochi, and Gomal.
These rivers run from West to East, and all are the Western tributaries of the River Indus. The Sulaiman range is drained by small hill torrents and small seasonal rivers such as the Bolan and Mula.
These rivers usually lead to small inland lakes, where the water collects and then dries up (for example the lake Damas). The rain falling on Eastern slopes of Sulaiman range runs down the slopes and falls into piedmont plains leading to the formation of alluvial fans.
The Kirthar range on the other hand is drained by the River Hab (seasonal river), which flows in a North to South direction and eventually joins the Arabian Sea.
In the Southern part of the Balochistan Plateau, the River Dasht and River Porali flow from north to South, thus eventually draining into the Arabian Sea. Both are seasonal rivers; they flow only during the rainy season.