Haro is the name of a river and its valley in the Abbottabad District, northern Pakistan, identified with the Rigvedic Arjikiya.

It is fed by four major tributaries, the Lora Haro, rising in the Muree Hills around Lora, the Stora Haro, rising in the Nahiagali Hills, the Neelan, rising in the Nara Hills, the Kunhad, draining the area of Siribang and Dubran. Minor tributaries include rivulets of Jab, Hally' Desera and Najafpur.


Soan River is a river in Punjab, Pakistan.

History
The oldest evidence of human life (8,000 to 6,000 years ago) in Pakistan was found in the Soan River valley of Pothohar Plateau region of Punjab. This human activity, called Soan Culture, discovered in the form of pebble tools scattered long the river. In Peshawar Valley of ancient Gandhara, there is evidence of existence of Stone Age men found at Sanghao near Mardan. Stone tools and burnt bones dated 7,000 years were found near caves. Cave dwellers of middle Stone Age used quartz flakes tools.

Soan Culture
The Soan Culture is an extinct human culture, found along the Soan River valley in the Pothohar region of the Punjab. The oldest evidence of human life in South Asia was found in the Soan River valley. Along the river, in the Rawalpindi Division hundreds of man made tools can be found. These tools have been dated to 500,000 to 300,000 years ago.

On Adiyala and Khasala about 16 km (10 miles) from Rawalpindi terrace on the bend of the river hundreds of edged pebble tools were discovered. At Chauntrahand axes and cleavers were found. Due to the peculiarity of the tools to the valley archaeologists named this human activity the Soan Culture.

No human skeletons of this age have yet been found. In the Soan River Gorge many fossil bearing rocks are exposed on the surface. The 14 million year old fossils of gazelle, rhinoceros, crocodile, giraffe and rodents have been found there. Some of these fossils are in display at the Natural History Museum of Islamabad.


The Hispar River forms from the melt water of the Hispar Glacier - a 49 kilometer-long glacier in the Northern Areas of Pakistan's Karakoram Mountains. The Hispar Glacier and river both flow northwest, passing through Hispar, Hopar and Nagar (Nagir) villages until the confluence with the Hunza River in the Hunza Valley. Road conditions are spectacular at best, treacherous at worst. In August 2006, a bridge below Hispar village was condemned, and the Hunza River washed the road away at the confluence, eliminating all vehicular access to the entire valley for some months.


Gujjar Nallah is a stream in Karachi, Sindh, Pakistan. It passes through the city from northwest to the center and merges with Lyari River before draining into the Arabian Sea.


The Indus River Delta occurs where the Indus River flows into the Arabian Sea in Sindh. The delta covers an area of about 16,000 square miles (41,440 km²), and is approximately 130 miles across where it meets the sea. Unlike many other deltas, the Indus River Delta consists of clay and other infertile soils, and is very swampy. The delta receives between 10 and 20 inches of rainfall in a normal year.

Pakistan's fifth largest city, Hyderabad, lies about 130 miles north of the mouths of the Indus. Towns are found throughout the delta, but there are no large cities on the delta south of Hyderabad. Karachi, Pakistan's largest city, lies west of the delta on the coast of the Arabian Sea.

Average temperatures for the delta region in July range from 70 - 85 °F, and 50 - 70 °F in January. The Indus River Delta is an important region for migrating water birds, and is an area rich in freshwater fauna. Fish found in the delta include the Hilsa, Indus baril, Indus garua (a catfish), the giant snakehead, golden mahaseer and the Rita catfish.


The Kunar River (Kunar Rud) is about 480 km long, located in eastern Afghanistan and north-western Pakistan. The Kunar river system is fed from melting glaciers and snow of the Hindu Kush mountains. The Lutkho River joins the Mastuj River just north of the important regional centre of Chitral in Pakistan and is then called the Chitral River, before flowing south into the upper Kunar Valley in Afghanistan, where it is referred to as the Kunar River.

The Kunar River empties into the Kabul River just to the east of the city of Jalalabad in Afghanistan. The combined rivers then flow eastwards into Pakistan, joining the Indus River at the city of Attock.

Before the political division of Afghanistan and Pakistan divided the Kunar/Chitral Valley, it formed an important trade route, being the easiest way to travel from the Pamir Mountains' passes to the plains of the Indian subcontinent.

Peche river is located in Afghanistan. Peche river system is fed from glaciers and snow. It includes the Kunar River, which rises in Nuristan province of Afghanistan, and the main Kunar River, which rises in the eastern Pamir Mountains before flowing through Chitral in Pakistan into the upper Kunar Valley in Afghanistan.


Rupal River rises from the melt water of Rupal Glacier in the south of the Nanga Parbat peak and flows northeast through the Rupal Valley and Tarashing.


Neelum is a river in Azad Kashmir, Pakistan.


The Shyok River is a river flowing through Ladakh and the disputed Northern Areas of Pakistan (Ghangche District). Shyok river (a tributary of the Indus) originates from the Rimo glacier, one of the tounges of Siachin glacier and and becomes very wide at the confluence with the Nubra river (a tributary of Shyok, originating from Siachin Glacier). The alignment of the Shyok river is very unusual, originating from the Rimo glacier it flows in a SE direction and at joining the Pangong range it takes a NW turn and flows parallel to its previous path. The Shyok flowing in a wide valley suddenly enters a narrow gorge after Chalunka and then joins the Indus at Skardu (Pakistan). The Nubra river originating from the Siachin glacier also behaves like the Shyok, before Tirit the SE flowing river takes a NW turn on meeting the river Shyok. The similarity in the courses of these two important rivers probably indicates a series of palaeo fault lines trending NW-SE in delimiting the upper courses of the rivers. The importance of the Indus and the Shyok rivers is in the deposition of a huge thickness of Quaternary sediments a treasure trove for geology researchers.


The Sohan is a river of the Punjab, northern Pakistan, forming the northern border of the Bannu District (at ca. 33.02° 71.73 E° ). It has been identified with the Sushoma of the Rigveda.

The name "Sohan" derives from this river. I.e: Sohan mikkilinenineni...etc...

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