In this article, we will explore the topic of Haro River in detail, addressing its different facets and perspectives from a holistic view. Haro River is a topic of great relevance today, which has generated extensive debate and interest in various areas. Over the next few lines, we will analyze the historical background of Haro River, its impact on contemporary society, as well as the possible future implications it could have. We will delve into its deepest aspects, with the aim of offering a comprehensive and enriching vision of Haro River, which allows our readers to obtain a greater understanding and perspective on this very relevant topic.
Haro River | |
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![]() The river in the Bagh Nilaab region | |
Physical characteristics | |
Source | |
• location | Dunga Gali |
• coordinates | 33°54′22″N 73°22′39″E / 33.9060914°N 73.377423°E |
Mouth | |
• coordinates | 33°46′02″N 72°14′36″E / 33.7672704°N 72.243408°E |
Basin features | |
River system | Indus River |
The Haro (Urdu: دریائے ہرو) is a river in Pakistan that flows through Khyber Pakhtunkhwa and parts of Punjab. It is a left tributary of the Indus. Its main valley is in Abbottabad District, in the Hazara Division of Khyber Pakhtunkhwa Province, northern Pakistan. The famous Khanpur Dam has been built on this river at Khanpur in the Haripur District of Hazara Division to provide drinking water to the twin cities, i.e. Islamabad (the capital of Pakistan) and Rawalpindi. The decrease in inflows from Khanpur dam from the Haro River results in a water shortage in the twin cities during the summer season.[1]
The Haro River rises at the southern end of the Dunga Gali range, where it has two branches. The eastern branch of the river is called Dhund, and the western is called Karral. The River Haro enters Rawalpindi District near Bhallan and flows through Attock District.[2]
It is fed by four major tributaries:[3]
Minor tributaries include the following rivulets.
This river joins the Indus near Ghazi Barotha Dam.