Sarju

Sarju
Kumaoni: सरज्यू, Hindi: सरयू
Sarju River
Aarti at Sarju Ghat, Bageshwar
Location
Country India
StateUttarakhand
regionKumaon
Physical characteristics
Source 
 • locationSarmul, 15 km south of Nanda Kot
 • coordinates30°7′58″N 80°1′56″E / 30.13278°N 80.03222°E / 30.13278; 80.03222
 • elevation3,000 m (9,800 ft)
Mouth 
 • location
Sharda River, Uttarakhand, India
 • coordinates
29°26′38″N 80°14′33″E / 29.44389°N 80.24250°E / 29.44389; 80.24250
 • elevation
429 m (1,407 ft)
Length130 km (81 mi)
Basin features
Tributaries 
 • leftRamganga, Punger
 • rightGomati, Panar, Lahor

The Sarju (Kumaoni: सरज्यू, Hindi: सरयू), also known as Saryu, is a major river draining Central Kumaon region in the Indian state of Uttarakhand. 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. The river forms the South-eastern border between the districts of Pithoragarh and Almora. Temperate and sub-Tropical forests cover the entire Catchment area of the River.

Etymology

According to the Ramayana (Balakanda 24/7-10), the name of this river is derived from 'Sarovar'/Lake (Lake Manasarovar). 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]

Hindu Scriptures

Ved

The name of Sarju /Sarayu river is found in Rigveda (4.30.18) and (5.53.9).

Uta tyā sadya āryā sarayorindra pāratah.

Arņācitrarathāvadhīḥ.

Translation- "O Indra! You have slain at once those two Āryas, Arṇa and Citraratha, (dwelling) on the opposite (bank) of the Sarayu."


mā vo rasānitabhā kubhā krumur mā vaḥ sindhur ni rīramat | mā vaḥ pari ṣṭhāt sarayuḥ purīṣiṇy asme it sumnam astu vaḥ

Translation- Let not the Rasa, the Anitabhā, the Kubhā, or the wide-roving ocean delay you; let not the watery Sarayu oppose you; may the happiness of your (approach) be ours

Ramayana

According to the Ramayana (Balkand 24/7-10), the sarju river originated from Lake Manasarovar , flows through Ayodhya and meets the Ganges River.

Course

The Sarju rises at a place known as Sarmul (or Sarmool), which is located in the extreme north of the Bageshwar district of Uttarakhand. The source of the river is situated at 30°7′58″N 80°1′56″E / 30.13278°N 80.03222°E / 30.13278; 80.03222 on the southern slope of a ridge of the Nanda Kot and is separated on the east from the source of Ramganga and on the west from the sources of Kuphini (the eastern branch of Pindar River) by spurs leading down from the mass culminating at the Nanda Kot peak. It flows initially around 50 km (31 mi) in southwest direction by the Kumaon Himalayas where it receives Kanalgadh stream from the right and Punger river from the left. About 2 km (1.2 mi) further downstream, the river receives Lahor river from the right. Then the river turns towards south and flows through the city of Bageshwar, where it receives Gomati from the right.

The Sarju flows to the lower 65 km in mainly southeastern direction. 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. 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.

Water Quality Characteristics of Sarju during water years 1987 and 1988
ParameterpHAlkalinityHardnessConductivityCalciumMagnesiumSodiumPotassiumChlorideSulphate
Value7.9111.2101.32137.1118.8911.113.501.808.102.41

Tributaries

confluence of Gomati and Sarju at Bageshwar.

Gomati

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

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.

Lahor

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

Panar

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

Ramganga

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

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. ↑ PTI (29 April 2024). "Sacred water from Saryu river to be sent to Sri Lanka for 'Sita Amma' temple consecration". The Hindu. ISSN 0971-751X. Retrieved 29 December 2024.
  5. ↑ Negi, Kumaun: The Land and the People, pg-82
  6. ↑ Conder, India, pg-238
  7. ↑ Rawat, Forest Management in Kumaon Himalaya, pg-18
  8. ↑ Aggarwal, Uttarakhand: Past, Present, and Future, pg-170
  9. ↑ Aggarwal, Uttarakhand: Past, Present, and Future, pg-331
  10. ↑ Negi, Himalayan Rivers, Lakes, and Glaciers, pg-120
  11. ↑ Valmiki Ramayana -Balakanda 24/7-10. Gita press. p. 139.
  12. ↑ Rig Veda 4.30.18.
  13. ↑ Rig Veda 5.53.9.
  14. ↑ Ramayana (Balkanda 24/7-10 ). Gita press. p. 139.
  15. ↑ Walton, Almora: A Gazetteer, pg-283
  16. ↑ Aggarwal, Uttarakhand: Past, Present, and Future, pg-182
  17. ↑ Budhawar, The Call of the Mountains: Uttrakhand Explored, pg-39
  18. ↑ Guneratne, Culture and the Environment in the Himalaya, pg-134
  19. ↑ Aggarwal, Uttarakhand: Past, Present, and Future, pg-182
  20. ↑ Walton, Almora: A Gazetteer, pg-284
  21. ↑ Bhatt, Ecology of the Mountain Waters, pg-48,49
  22. ↑ All values in mg/L except ph and conductivity
  23. ↑ Bhatt, Ecology of the Mountain Waters, pg-97
  24. ↑ Rawat, Forest Management in Kumaon Himalaya, pg-19
  25. ↑ Rawat, Forest Management in Kumaon Himalaya, pg-19
  26. ↑ Aggarwal, Uttarakhand: Past, Present, and Future, pg-183
  27. ↑ Aggarwal, Uttarakhand: Past, Present, and Future, pg-182
  28. ↑ Rawat, Forest Management in Kumaon Himalaya, pg-19
  29. ↑ Rawat, Forest Management in Kumaon Himalaya, pg-19
  30. ↑ Negi, Himalayan Rivers, Lakes, and Glaciers, pg-115
  31. ↑ Rawat, Forest Management in Kumaon Himalaya, pg-18
  32. ↑ Negi, Himalayan Rivers, Lakes, and Glaciers, pg-48

Bibliography