The Sipra from Pipalda, the little Sind[[41]] from Dewas, and other minor streams passing Ujjain, all unite with the Chambal in different stages before he breaks through the plateau.
The Kali Sind, from Bagri, and its petty branch, the Sodwia, from Raghugarh; the Niwaz (or Jamniri), from Morsukri and Magarda; the Parbati, from the pass of Amlakhera, with its more eastern arm from Daulatpur, uniting at Pharhar, are all points in the crest of the Vindhya range, whence they pursue their course through the plateau, rolling over precipices,[[42]] till engulfed in the Chambal at the ferries of Nunera and Pali. All these unite on the right bank.
On the left bank his flood is increased by the Banas, fed by the perennial streams from the Aravalli, and the Berach from the lakes of Udaipur; and after watering Mewar, the southern frontier of Jaipur, and the highlands of Karauli, the river turns south to unite at the holy Sangam,[[43]] Rameswar. Minor streams contribute (unworthy, however, of separate notice), and after a thousand involutions he reaches the Jumna, at the holy Triveni,[[44]] or ‘triple-allied’ stream, between Etawa and Kalpi.
The course of the Chambal, not reckoning the minor sinuosities, is upwards of five hundred miles;[[45]] and along its banks specimens of nearly every race now existing in India may be found: Sondis, Chandarawats, Sesodias, Haras, Gaur, Jadon, Sakarwal, Gujar, Jat,[[46]] Tuar, Chauhan, Bhadauria, Kachhwaha, Sengar, Bundela; each in associations of various magnitudes, from the substantive state of the little republic communes between the Chambal and Kuwari[[47]] [17].
The Western Desert.
The Luni River.
The Luni, from its sources, the sacred lakes of Pushkar and Ajmer, and the more remote arm from Parbatsar to its embouchure in the great western salt marsh, the Rann, has a course of more than three hundred miles.
In the term Eirinon of the historians of Alexander, we have the corruption of the word Ran or Rann,[[50]] still used to describe that extensive fen formed by the deposits of the Luni, and the equally saturated saline streams from the southern desert of Dhat. It is one hundred and fifty miles in length; and where broadest, from Bhuj to Baliari, about seventy:[[51]] in which direction the caravans cross, having as a place of halt an insulated oasis in this mediterranean salt marsh. In the dry season, nothing meets the eye but an extensive and glaring sheet of salt, spread over its insidious surface, full of dangerous quicksands: and in the rains it is a dirty saline solution, up to the camels’ girths in many places. The little oasis, the Khari Kaba, furnishes pasture for this useful animal and rest for the traveller pursuing his journey to either bank.
The Mirage.
Such phenomena are common to the desert, more particularly where these extensive saline depositions exist, but varying from certain causes. In most cases, this powerfully magnifying and reflecting medium is a vertical stratum; at first dense and opaque, it gradually attenuates with increased temperature, till the maximum of heat, which it can no longer resist, drives it off in an ethereal vapour. This optical deception, well known to the Rajputs, is called sikot, or ‘winter castles,’ because chiefly visible in the cold season: hence, possibly, originated the equally illusory and delightful ‘Chateau en Espagne,’ so well known in the west.[[54]]