Hydaspes to the ancient Greeks, Bihat to the Mughals, Vitasta to brahmins and Vyeth to historians, the Jehlum is the cradle of civilisation in Kashmir.

Lawrence noted that 'Life in the Srinagar city and elsewhere in Kashmir revolves around the river Jhelum.'

The Jehlum starts out as a leisurely flowing river from the immeasurable depths of Verinag and meanders like an immense silver serpent through the valley.

An engraving in 'Letters from India and Kashmir' by J. Duguid, 1870. The caption in the book reads 'The curves of the Jehlum, the inspiration for the shawl or pine pattern…'

Pir Panjal

During its journey the Jehlum receives tributaries from the Pir Panjal and the mighty Himalayas.

The river then forms a delta as it merges into its personal sea – the Wular Lake – at one time the largest fresh water lake in Asia. From the Wular the Jehum flows out towards Uri where it forms a raging torrent as it leaves the valley.

Ordinary rivers have three well-defined stages – rapid flow through steep hillsides, followed by meandering through plains and finally delta formation as the river reaches the sea.

Over the approximately 200-km course of the Jehlum through the valley, the second stage is followed by the third and then the first stage!

Verinag

ORIGIN OF THE JEHLUM

Numerous nars (mountain streams), arising from the snowfields of the mountainous ring between the Hansraj, Kaukut and Sundar Kanthi peaks, merge to form the Sandrin stream which flows in a north-westerly direction for more than 20 kilometres till it meets the Verinag stream, a 300-yard canal originating in the Verinag Spring.

Near Anantnag the Bringi and Arpath streams merge before joining the Sandrin at Khanabal to form the Jehlum river.

RIGHT BANK TRIBUTARIES

Beyond Anantnag, the Lidder river, formed at Pahalgam by the Aru stream from the Kolahoi Glacier merging with the Chandanwari stream originating in Sheshnag Lake, flows into the Jehlum near Sifan.

Aru

Beyond Srinagar, the Sindh, the largest tributary, recieves the Wangat/Kanaknaz stream originating in Gangabal and other lakes around Harmukh in the Sonamarg valley before meeting the Jehlum at Shadipur.

Harmukh

Wangat

LEFT BANK TRIBUTARIES

At Sangam (literally confluence) the mighty Veshav from Kousarnag via Aharbal flows into the Jehlum after meeting the Rambiara stream.

Kousarnag

Aharbal

Veshav

Rambiara

The Jehlum then recieves the Sasara and Romshi streams near Kakapora before flowing into Srinagar.

This post details the journey of the Jehlum through Srinagar.

THE WULAR LAKE AND BEYOND

The Jehlum then flows lazily in and out of the Wular Lake – which also receives the exquisitely-named Erin and Madhumati streams.

Beyond the Wular Lake the Jehlum receives the Pohru formed by the merging of the Kahmil, Lolab and Mawar streams in North Kashmir and the Ningle and Viji streams before Baramulla.

Beyond Baramulla a number of smaller streams like the Mundhri, Boniyar and Uri streams flow into the torrent before the Jehlum crosses into Pakistan at Aman Setu over the Chakoti stream..

FLOOD SPILL CHANNEL

The Flood Spill Channel constructed in 1904 diverts flood waters from the Jehlum at Shivpora towards the Hokarsar wetlands before merging with the Wular floodplain.

The Doodhganga and Shaliganga streams arising from Sang-e-safed in the central Pir Panjal range, the Sukhnag stream below Tosa Maidan and the Ferozepur stream near Tangmarg, flow into the Flood Spill Channel.

Doodhganga

Shaliganga

Ferozepur

Other notable streams flowing in Kashmir are the Dagwan from Marsar lake flowing through Dachigam National Park and the Arpat Kol near Tral.

Dagwan