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 that in tracts in Lower Bengal where the fever has been most deadly the water-level in the dry months the prevalence and intensity of fever has not yet been traced in Lower Bengal.

Both irrigation and drainage are there new things. The first irrigation work was not begun until 1862, and that by a private company: the Government expended nothing upon works of this class until 1868 or 1869.

The Dancienic Drainage Works, in the Hooghly district, carried out last year, are the first of their kind.

But in N.W. India—i.e. the N.W. Provinces and Punjab—some important facts have been established. In the districts on the upper part of the Ganges Canal, which were, of course, the first and the most copiously irrigated, there has been for many years a terrible increase of fever. By many it was asserted that the fever owed its origin to the canal; that the Mozuffernuggur District, e g., which is now said to be so unhealthy that it is in general avoided by officials, was formerly one of the healthiest and most popular.

This, however, appears to have been clearly disproved. There is abundant proof of the existence of fever long before the canal was heard of. But this also seems to be certain that, wherever irrigation has been excessive, and stagnant pools and swamps have been formed, by carrying the minor distributary channels (as was formerly frequently done in the hurry of construction or from a faulty system) across the natural drainages, there has been a marked increase in the prevalence and virulence of fever.

Wherever the subsoil levels (which are usually termed the 'spring levels' in the N.W. Provinces and Punjab Reports) have been raised by supersaturation of soil from their original depth of twenty-five to forty feet to twelve feet or less, there there has been a terrible increase in the mortality from fever. Though still disputed, this fact is now pretty generally admitted by the best authorities, and in some official 'Resolution' of the N.-W. Provinces Government, it is distinctly laid down as the basis of remedial measures. Sir W. Muir is a hearty friend to irrigation.

How far this 'water-logged' state of the soil in the districts referred to is due to excessive irrigation, and how far to the faulty alignments of distributaries and neglect of drainage above alluded to is not decided.

But misuse of water is often made an excuse for not draining.