The original narrative, which appeared in the "Annales des Voyages," speaks of this water as flowing from two openings six inches in diameter in a calcareous plain some three miles in extent, and which is raised in almost every direction from ten to twelve feet above the surrounding country. It is formed of the earthy deposits left by the water in cooling. The water rises four inches above the level of the plain. It is clear, and so warm that one cannot keep a hand in it longer than a few minutes. It is surrounded by a thick cloud of smoke. The water, flowing over a horizontal surface, hollows out basins of various shapes, which as they receive the earthy deposits contract again. When they are filled up, the flow of the water again hollows out a new reservoir, which in its turn becomes full. Flowing thus from one to the other, it finally reaches the plain below. The deposit left by the water is as white as the purest stucco close to the opening, a little further it becomes pale yellow, and further still saffron-coloured. At the other spring it is first rose-coloured, and then dark red. These different colours are to be found in the calcareous plain, and are no doubt the work of centuries. Tirthapuri, the residence of a lama, is of great antiquity, and is a favourite rendezvous for the faithful, as a wall more than 400 feet long and four wide, formed of stones upon which prayers are inscribed, sufficiently testifies. Upon the 1st of August the travellers left this place, hoping to reach Lake Manasarowar, and leaving on the right Lake Rawan-rhad, which is supposed to be the source of the largest branch of the Sutlej. Lake Manasarowar lies at the foot of immense sloping prairies, to the south of the gigantic mountains. This is the most venerated of all the sacred places of the Hindus, which is no doubt owing to its distance from Hindustan, the dangers and fatigues of the journey, and the necessity of pilgrims providing themselves with money and provisions. Hindu geographers regard this lake as the source of the Ganges, the Sutlej, and the Kali rivers. Moorcroft had no doubt as to the error of this assertion as regards the Ganges. Desiring to ascertain the truth as to the other rivers, he explored the steep banks of the lake, and found a number of streams which flowed into it, but none flowing out of it. It is possible that before the earthquake which destroyed Srinagar, the lake had an outlet, but Moorcroft found no trace of it. The lake is situated between the Himalayas and the Cailas chain, and is of irregular oblong shape, five leagues long by four wide. The end of the expedition was attained. Moorcroft and Hearsay returned towards India, passed by Kangri, and saw Rawan-rhad; but Moorcroft was too weak, and could not continue the tour; he regained Tirthapuri and Daba, and suffered a great deal in crossing the ghat which separates Hindustan from Thibet.