THE country to which the term Hindustan is strictly and properly applied may be roughly described as a rhomboid, bounded on the north-west by the rivers Indus and Satlej, on the south-west by the Indian Ocean, on the south-east by the Narbadda and the Son, and on the north-east by the Himalaya Mountains and the river Ghagra. In the times of the emperors, it comprised the provinces of Sirhind (or Lahore), Rajputana, Gujrat, Malwa, Audh (including Rohilkand, strictly Rohelkhand, the country of the Rohelas, or "Rohillas" of the Histories), Agra, Allahabad, and Dehli: and the political division was into subahs, or divisions, sarkars or districts; dasturs, or sub-divisions; and parganahs, or fiscal unions. The Deccan, Panjab (Punjab), and Kabul, which also formed parts of the Empire in its widest extension at the end of the seventeenth century, are omitted, as far as possible, from notice, because they did not at the time of our narration form part of the territories of the Empire of Hindustan, though included in the territory ruled by the earlier and greater Emperors. Bengal, Bihar, and Orissa also formed, at one time, an integral portion of the Empire, but fell away without playing an important part in the history we are considering, excepting for a very brief period. The division into Provinces will be understood by reference to the map. Most of these had assumed a practical independence during the first quarter of the eighteenth century, though acknowledging a weak feudatory subordination to the Crown of Dehli. The highest point in the plains of Hindustan is probably the plateau on which stands the town of Ajmir, about 230 miles south of Dehli. It is situated on the eastern slope of the Aravalli Mountains, a range of primitive granite, of which Abu, the chief peak, is estimated to be near 5,000 feet above the level of the sea; the plateau of Ajmir itself is some 3,000 feet lower. The country at large is, probably, the upheaved basin of an exhausted sea which once rendered the highlands of the Deccan an island like a larger Ceylon. The general quality of the soil is accordingly sandy and light, though not unproductive; yielding, perhaps, on an average about one thousand lbs. av. of wheat to the acre. The cereals are grown in the winter, which is at least as cold as in the corresponding parts of Africa. Snow never falls, but thin ice is often formed during the night. During the spring heavy dews fall, and strong winds set in from the west. These gradually become heated by the increasing radiation of the earth, as the sun becomes more vertical and the days longer. Towards the end of May the monsoon blows up from the Indian Ocean and from the Bay of Bengal, when a rainfall averaging about twenty inches takes place and lasts during the ensuing quarter. This usually ceases about the end of September, when the weather is at its most sickly point. Constant exhalations of malaria take place till the return of the cold weather.