~The Sutlej.~--The Sutlej is the Shatadru of Vedic hymns and the Zaradros of Greek writers. The peasant of the Panjab plains knows it as the Nili or Ghara. After the Indus it is the greatest of Panjab rivers, and for its source we have to go back to the Manasarowar lakes in Tibet. From thence it flows for 200 miles in a north-westerly direction to the British frontier near Shipki. A little beyond the Spiti river brings it the drainage of the large tract of that name in Kangra and of part of Western Tibet. From Shipki it runs for forty miles in deep gorges through Kunawar in the Bashahr State to Chini, a beautiful spot near the Wangtu bridge, where the Hindustan-Tibet road crosses to the left bank. A little below Chini the Baspa flows in from the southeast. The fall between the source and Chini is from 15,000 to 7500 feet. There is magnificent cliff scenery at Rogi in this reach. Forty miles below Chini the capital of Bashahr, Rampur, on the south bank, is only 3300 feet above sea level. There is a second bridge at Rampur, and from about this point the river becomes the boundary of Bashahr and Kulu, the route to which from Simla passes over the Luri bridge (2650 feet) below Narkanda. Beyond Luri the Sutlej runs among low hills through several of the Simla Hill States. It pierces the Siwaliks at the Hoshyarpur border and then turns to the south, maintaining that trend till Rupar and the head-works of the Sirhind canal are reached. For the next hundred miles to the Bias junction the general direction is west. Above the Harike ferry the Sutlej again turns, and flows steadily, though with many windings, to the south-west till it joins the Chenab at the south corner of the Multan district. There are railway bridges at Phillaur, Ferozepur, and Adamwahan. In the plains the Sutlej districts are--on the right bank Hoshyarpur, Jalandhar, Lahore, and Montgomery, and on the left Ambala, Ludhiana and Ferozepur. Below Ferozepur the river divides Montgomery and Multan from Bahawalpur (left bank). The Sutle; has a course of 900 miles, and a large catchment area in the hills. Notwithstanding the heavy toll taken by the Sirhind canal, its floods spread pretty far in Jalandhar and Ludhiana and below the Bias junction many monsoon canals have been dug which inundate a large area in the lowlands of the districts on either bank and of Bahawalpur. The dry bed of the Hakra, which can be traced through Bahawalpur, Bikaner, and Sindh, formerly carried the waters of the Sutlej to the sea.