| Lake Pichola | |
| Pushpin Map: | India Rajasthan##India |
| Pushpin Map Caption: | Location of Lake Pichola in Rajasthan##Location of Lake Pichola in India |
| Pushpin Map Alt: | Location of Pichola lake within Rajasthan |
| Coords: | 24.572°N 73.679°W |
| Lake Type: | Freshwater Lake |
| Catchment: | 55km2 |
| Length: | 4km (02miles) |
| Width: | 3km (02miles) |
| Area: | 696ha |
| Depth: | 4.32m (14.17feet) |
| Max-Depth: | 8.5m (27.9feet) |
| Islands: | Jag Niwas, the Jag Mandir and Arsi Vilas |
| Cities: | Udaipur |
| Agency: | Arvind Singh Mewar |
Lake Pichola, situated in Udaipur city in the Indian state of Rajasthan, is an artificial fresh water lake, created in the year 1362, named after the nearby Picholi village.[1] [2] It is one of the several contiguous lakes, and developed over the last few centuries in and around the famous Udaipur city. The lakes around Udaipur were primarily created by building dams to meet the drinking water and irrigation needs of the city and its neighbourhood. Two islands, Jag Niwas and Jag Mandir are located within Pichola Lake, and have been developed with several palaces to provide views of the lake.[1] [3]
There are four islands on the lake:
Three of the numerous lakes found in the vicinity of Udaipur which connect with the Pichola lake and the Swaroop Sagar Lake connected by an arched bridge built by Maharana Swaroop Singh (1842-1861) which in turn connects to the Fateh Sagar Lake, the crystal watered lake in the midst of tree lined hills and the smaller Arsi Vilas.[1] [3]
Lake Pichola is approachable by road from Udaipur City. Local buses, Tongas, auto-rickshaws and taxis provide the needed transport. The lake is adjacent to the Bagore Ki Haveli[4] museum, making it a good landmark. Udaipur, in turn, is well connected through the Golden Quadrilateral road network, and it lies equidistant, at 650 kilometres, from Delhi and Mumbai on the National Highway (NH) 8. Jaipur, the capital of Rajasthan is 6 hours by road and a 3.5 hours drive from Ahmedabad to Udaipur. Rajasthan Tourism operates a regular bus service from Delhi. It also falls on the East-West Corridor which starts from Porbandar and ends at Silchar and intersects the Golden Quadrilateral and a part of this is the stretch from Udaipur to Chittor. 24 km from the lake is the Dabok Airport which connects to Delhi and Bombay. Udaipur Railway Station and Maharana Pratap Bus Stand are both 3 km away from the Lake.
Pichola Lake was built by Maharaja of Parmar Rajputs, in 1362 AD. It is a hearsay that lake got its name from nearby village Picholi, during the reign of Maharana Lakha.[5] Later, Maharana Udai Singh, impressed by the charm of this lake with the backdrop of green hills, founded the city of Udaipur on the banks of the lake and also enlarged the Lake by constructing a stone masonry dam in the Badipol region on the shore of the Lake.[1] The lake's surroundings and the several islands within the lake have been developed over the centuries, with palaces, marble temples, family mansions, bathing ghats or chabutaras (a raised platform, normally within a courtyard); some of the famous ones are the Lake Palace (now converted into a heritage hotel) in the middle of the lake also called the Pichola Palace (pictured) or Jag Nivas located on the Jag Island, the Jag Mandir, the Mohan Mandir (in the northeast corner of the lake built by Jagat Singh between 1628 and 1652), the City Palace of Udaipur (Bansi Ghat) from where boats ply to all other parts of the Lake, the Arsi Vilas Island, which is a sanctuary for birds and the Sitamata Game Sanctuary on the western shore of the Lake.[3] [6]
At several locations where the lake narrows, ornamental arch bridges have been built to span the waterway between the banks.[3] [7]
The Sisarma stream, a tributary of the Kotra River, drains a catchment of 55 km2 from the Aravalli Mountains and contributes to the flows in the lake.[8] The average annual rainfall in the lake basin is 635mm. The lake has a surface area of about 696 ha. It is 4km (02miles) long and 3km (02miles) wide, and has depth varying from a minimum of 4.32m (14.17feet) to a maximum of 8.5m (27.9feet). In the heart of the Lake, a palace called the Lake Palace was built, which is now converted into a heritage palace hotel. This palace built in marble in 1746 by Maharana Jagat Singh II, 62nd successor to the royal dynasty of Mewar, spreads across the 1.6ha island and is claimed to be as impressive as the Taj Mahal. At the southern end, a dam was built across the major tributary to facilitate the Banjara tribesman to ford the stream with animals carrying grains. After 1560, Maharana Udai Sing II strengthened the dam (to a height of 15.24 m) when he established the city of Udaipur around the picturesque Lake. Machchala Magra hill, to the south of the city palace complex, is part of the old city wall and the small fort of Eklinggarh and the temple.[3] [6] [9] [10] The fact that the Pichola lake was built by nomadic gypsies testifies that the rulers of Mewar encouraged people to build water harvesting structures.[11]
During drought conditions because of lower rainfall & degradation of the catchment the lake becomes dry (pictured). During the years 1998 to July 2005. the Lakes of Udaipur were reportedly dry.[8]
According to a study carried out by the "Centre of Advanced Study in Geology", Punjab University, the water quality of the lake has a high sodium and Bicarbonate content, which is attributed to the continental weathering due to anthropogenic pressure (tourist influx), intense development activities in the basin area and untreated effluent from municipal and domestic sewage into the Lake. The semi arid conditions of the area, saline and alkaline soils/groundwater conditions and weathering of the silicate rock exposed in the drainage basin are assessed as the reasons for the supply of major ions. The report infers[12] that
The increase in phosphate loading and consequent depletion of silica suggests biological consumption of the latter. The observed chemical data of the Pichola Lake was used to predict the mineral assemblages in the carbonate and aluminosilicate system. It demonstrates that calcite and dolomite are the possible minerals that are in equilibrium with the lake water system and that the lake water chemistry is in the range of stability of kaoliniteThe average of the pollution parameters recorded at random intervals during 2005-2006 as reported by the Rajasthan State Pollution Control Board in 2006 are:[13]
The assessment of quality status determined that water is polluted and needs remedial measures to be implemented to rectify the situation.[13]
Studies conducted by Jheel Sanrakshan Samiti (Udaipur Lake Conservation Society) – JSS - a Non Governmental Organization (NGO) set up in 1992 for Ecological, Limnological and Hydrological Conservation of Udaipur Lake System, has found growth of water hyacinth, the lake bottom is also covered with a thick mat of submerged vegetation, presence of floating micro algae which are detrimental to the public health, and also harbor varieties of harmful organisms. This degree of pollution makes chlorination and treatment by other chemicals ineffective to render the water potable.[8]
Some of the issues identified as causes for deterioration of the Lake environment[14] are:
Steps undertaken to restore the lakes by the NGOs, such as JSS and concerned government organizations are:[8]