Sarju

Coordinates: 29°26′38″N 80°14′33″E / 29.44389°N 80.24250°E / 29.44389; 80.24250
Source: Wikipedia, the free encyclopedia.

Sarju
Hindi: सरयू
Sarju River
Sarju River
Location
Country India
StateUttarakhand
regionKumaon
Physical characteristics
Source 
 • locationSarmul, 15 km south of Nanda Kot[1]
 • coordinates30°7′58″N 80°1′56″E / 30.13278°N 80.03222°E / 30.13278; 80.03222
 • elevation3,000 m (9,800 ft)
Gomati
, Panar, Lahor

The Sarju (

Kumaon region[4] in the Indian state of Uttarakhand.[5] Originating from Sarmul, Sarju flows through the cities of Kapkot, Bageshwar and Seraghat before joining Mahakali at Pancheshwar. The Sarju is the largest tributary of the Sharda River.[6] The river forms the South-eastern border between the districts of Pithoragarh and Almora.[7][8] Temperate and sub-Tropical forests cover the entire Catchment area of the River.[9]

Etymology

The name is a noun derived from the Sanskrit root सृ sṛ "to flow". saráyu- as a masculine noun means "air, wind". In the feminine it is the name of the river.[citation needed]

Course

The Sarju rises at a place known as Sarmul (or Sarmool), which is located in the extreme north of the

Gomati from the right.[12][13]

The Sarju flows to the lower 65 km in mainly southeastern direction.[14] Much of the drainage of Gangolihat region of Pithoragarh district flows into the river via Bhadrapatigad stream, which flows into it from the left. Similarly, several streams join it from right draining much of the Chaugarkha region situated in Almora district; notable ones being Gatgadh, Jalairgadh, Bhaurgadh, Alaknadi and Saniaungadh.[15] About 55 km (34 mi) downstream from its confluence with Gomati in Bageshwar, it receives the Panar river from the right. A small river Jaingan gets merge into Sarju river at Seraghat in Almora-Pithoragarh border. About five Km further downstream, at 20 km (12 mi) above its mouth, Ramganga meets the left side on the Sarju at Rameshwar, situated at an elevation of 1,500 ft (460 m). Finally Sarju reaches at Pancheshwar at the Nepalese border to Sharda River after travelling a total of 130 km (81 mi).

Geology

Sarju transfers a sedimental load of 498.4 kg/sec during the peak of raining season.[16]

Water Quality Characteristics of Sarju during water years 1987 and 1988[17][18]
Parameter pH Alkalinity
Hardness
Conductivity Calcium Magnesium Sodium Potassium Chloride
Sulphate
Value 7.9 111.2 101.32 137.11 18.89 11.11 3.50 1.80 8.10 2.41

Tributaries

Gomati and Sarju at Bageshwar
.

Gomati

Gomati river originates in the higher reaches of Bhatkot and merges into Sarju at Bageshwar.[19] It flows through the Katyur Valley which constitutes a major Agricultural zone of Kumaon.[20]

Kuloor

The Kuloor river rises above the Bhadrkali Temple near

Sani-Udiyar
, and flows through Rawatsera, Bans Patan and Ganai Gangoli, before joining the Sarju at Seraghat.

Punger

Punger river rises near village Sangar and joins Sarju from the left at Sartana.[21]

Lahor

Lahor is a small river that joins Sarju from the right.[22]

Panar

Panar originates on the northern slopes of the Mornaula Range, south-east of Almora.[23] Panar joins Sarju near Rameshwar.[24]

Ramganga

Ramganga East is the largest tributary of Sarju. It originates from the Namik Glacier in Pithoragarh district of Uttarakhand and flows towards Southeast.[25][26] The river is fed by numerous small and big rivers and finally joins river Sarju at Rameshwar.[27]

Gallery

  • Camping on saryu river
    Camping on saryu river
  • Saryu river at Bageshwar
    Saryu river at Bageshwar
  • Close-up view of Sarju water flowing
    Close-up view of Sarju water flowing
  • Saryu river at Bageshwar
    Saryu river at Bageshwar
  • Suspension Bridge over Saryu river at Bageshwar
    Suspension Bridge over Saryu river at Bageshwar

References

Notes

  1. ^ Sati, Uttaranchal: Dilemma of Plenties and Scarcities, pg-79
  2. ^ Sharda River is known as Kali Ganga in mountainous regions of Kumaon
  3. ^ Sati, Uttaranchal: Dilemma of Plenties and Scarcities, pg-79
  4. ^ Negi, Kumaun: The Land and the People, pg-82
  5. ^ Conder, India, pg-238
  6. ^ Rawat, Forest Management in Kumaon Himalaya, pg-18
  7. ^ Aggarwal, Uttarakhand: Past, Present, and Future, pg-170
  8. ^ Aggarwal, Uttarakhand: Past, Present, and Future, pg-331
  9. ^ Negi, Himalayan Rivers, Lakes, and Glaciers, pg-120
  10. ^ Walton, Almora: A Gazetteer, pg-283
  11. ^ Aggarwal, Uttarakhand: Past, Present, and Future, pg-182
  12. ^ Budhawar, The Call of the Mountains: Uttrakhand Explored, pg-39
  13. ^ Guneratne, Culture and the Environment in the Himalaya, pg-134
  14. ^ Aggarwal, Uttarakhand: Past, Present, and Future, pg-182
  15. ^ Walton, Almora: A Gazetteer, pg-284
  16. ^ Bhatt, Ecology of the Mountain Waters, pg-48,49
  17. ^ All values in mg/L except ph and conductivity
  18. ^ Bhatt, Ecology of the Mountain Waters, pg-97
  19. ^ Rawat, Forest Management in Kumaon Himalaya, pg-19
  20. ^ Rawat, Forest Management in Kumaon Himalaya, pg-19
  21. ^ Aggarwal, Uttarakhand: Past, Present, and Future, pg-183
  22. ^ Aggarwal, Uttarakhand: Past, Present, and Future, pg-182
  23. ^ Rawat, Forest Management in Kumaon Himalaya, pg-19
  24. ^ Rawat, Forest Management in Kumaon Himalaya, pg-19
  25. ^ Negi, Himalayan Rivers, Lakes, and Glaciers, pg-115
  26. ^ Rawat, Forest Management in Kumaon Himalaya, pg-18
  27. ^ Negi, Himalayan Rivers, Lakes, and Glaciers, pg-48

Bibliography

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