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Travel Guide exploring India

YoungBites. Dated: 5/6/2017 9:31:46 AM


PLACES TO VISIT IN RAJASTHAN ( Jal Mahal )


Jal Mahal Jal Mahal (meaning "Water Palace") is a palace located in the middle of the Man Sagar Lake in Jaipur city, the capital of the state of Rajasthan, India. The palace and the lake around it were renovated and enlarged in the 18th century by Maharaja Jai Singh II of Amber. "The Jal Mahal palace has got an eyepopping makeover. Traditional boat-makers from Vrindavan have crafted the Rajput style wooden boats. A gentle splashing of oars on the clear lake waters takes you to Jal Mahal. You move past decorated hallways and chambers on the first floor to climb all the way up to the fragrant Chameli Bagh. Across the lake, you can view the hills, dotted with temples and ancient forts, and on the other side, bustling Jaipur. The most remarkable change is in the lake itself. The drains were diverted, two million tonnes of toxic silt were dredged from the bottom, increasing its depth by over a metre, a water treatment system was developed, local vegetation and fish reintroduced, the surrounding wetlands regenerated and five nesting islands created to attract migratory birds. The lake, situated to the north of Jaipur city lies between Amer, the historic city and Jaipur, the provincial headquarters of Rajasthan state. It has a water spread area of 300 acres (121 ha) and is enclosed by the Aravalli hills on the north, west and eastern sides, while the southern side consists of plains that are intensely inhabited. There is the Nahargarh Fort (Nahargarh meaning home of tigers) in the hills that provides a commanding view of the Man Sagar Lake and the Jal Mahal palace, in addition to a beautiful view of the city of Jaipur. The lake was created by constructing a dam across the Darbhawati River, between Khilagarh hills and the hilly areas of Nahargarh, in the 16th century. The drainage area of the lake is 23.5 square kilometres (9.1 sq mi)contributed by an urban area accounting for 50% and hilly terrain accounting for the balance, being degraded Aravalli hills, which have added to the siltation problem in the lake. A rain fall average of 657.4 millimetres (25.88 in) per year (90% of this rainfall occurs during the months of June to September) in the catchment contributes to the storage in the reservoir. At the outlet end of the dam there is an irrigation system that is supplied with water stored in the reservoir (obligatory water demand for this is reported to be 2,410,000 cubic metres during the five months from November to March). Two large nalas (streams) that also drain the surrounding Nahargarh hills and Jaipur are the Brahmpuri and Nagtalai, which bring in large amounts of untreated sewage, in addition to solid wastes. The hills surrounding the lake area, towards the north east of Jaipur, have quartzite rock formations (with a thin layer of soil cover), which is part of Aravalli hills range. Rock exposures on the surface in some parts of the project area have also been utilised for constructing buildings. From the north east, the Kanak Vrindavan valley, where a temple complex is situated, the hills slope gently towards the lake edge. Within the lake area, the ground area is made up of a thick mantle of soil, blown sand and alluvium. Forest denudation, particularly in the hilly areas, has caused soil erosion, compounded by wind and water action. Due to this, silt built up in the lake resulting in a raising of the bed level of the lake. GEOLOGY AND SOILS The hills surrounding the lake area, towards the north east of Jaipur, have quartzite rock formations (with a thin layer of soil cover), which is part of Aravalli hills range. Rock exposures on the surface in some parts of the project area have also been utilised for constructing buildings. From the north east, the Kanak Vrindavan valley, where a temple complex is situated, the hills slope gently towards the lake edge. Within the lake area, the ground area is made up of a thick mantle of soil, blown sand and alluvium. Forest denudation, particularly in the hilly areas, has caused soil erosion, compounded by wind and water action. Due to this, silt built up in the lake resulting in a raising of the bed level of the lake. In the past, at the location of the lake, there was a natural depression where water used to accumulate. During 1596 AD, when there was a severe famine in this region there was consequent acute shortage of water. The then ruler of Amer was, therefore, motivated to build a dam to store water to overcome the severe hardships caused by the famine to the people inhabiting the region.

 

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