On the 2nd we came on to the village of Khojanpur (leaving the town and cantonments of Sagar to our left), a distance of some fourteen miles.  The road for a great part of the way was over the bare back of the sandstone strata, the covering of basalt having been washed off.  The hills, however, are, at this distance from the city and cantonments of Sagar, nicely wooded; and, being constantly intersected by pretty little valleys, the country we came over was picturesque and beautiful.  The soil of all these valleys is rich from the detritus of the basalt that forms or caps the hills; but it is now in a bad state of cultivation, partly from several successive seasons of great calamity, under which the people have been suffering, and partly from over-assessment; and this posture of affairs is continued by that loss of energy, industry, and character, among the farmers and cultivators, which must everywhere result from these two evils.  In India, where the people have learnt so well to govern themselves, from the want of settled government, good or bad government really depends almost altogether upon good or bad settlements of the land revenue.  Where the Government demand is imposed with moderation, and enforced with justice, there will the people be generally found happy and contented, and disposed to perform their duties to each other and to the state; except when they have the misfortune to suffer from drought, blight, and other calamities of season.[l2]

I have mentioned that the basalt in the Sagar district reposes for the most part immediately upon the sandstone of the Vindhya range; and it must have been deposited on the sand, while the latter was yet at the bottom of the ocean, though this range is now, I believe, nowhere less than from fifteen hundred to two thousand feet above the level of the sea.  The marks of the ripple of the sea may be observed in some places where the basalt has been recently washed off, beautifully defined, as if formed only yesterday, and there is no other substance to be seen between the two rocks.

The texture of the sandstone at the surface, where it comes in contact with the basalt, has in some places been altered by it, but in others it seems to have been as little changed as the habitations of the people who were suffocated by the ashes of Vesuvius in the city of Pompeii.  I am satisfied, from long and careful examination, that the greater part of this basalt, which covers the tableland of Central and Southern India, must have been held for some time in suspension in the ocean or lake into which it was first thrown in the shape of ashes, and then gradually deposited.  This alone can account for its frequent appearance of stratification, for the gentle blending of its particles with those of the sand near the surface of the latter; and, above all, for those level steps, or tables, lying one above another horizontally in parallel bars on one range, corresponding exactly with the same parallel lines one above another on