e interested should know somewhat of the constituents of this Nile mud, which is brought down from the south to be deposited, it must be borne in mind, upon sand which in the course of cultivation will naturally, as it is mingled with the mud, render it open, porous, and highly suitable for vegetable growth. A rough analysis proves that quite half of the deposit is argillaceous, or clayey earth, one fourth carbonate of lime. These constituents alone should be sufficient to gladden the heart of any farmer or gardener, without counting the iron, carbonate of magnesia, and silica.
So many of our agricultural outposts are only to be reached by long and tedious journeys across ocean and then inland. Egypt is, of course, in Africa, but only a few days' journey from our own shores. The sea transit is short and frequent; and the country, the ancient mysterious land of the Dark Ages, is rapidly being opened out by rail. The climate, in spite of the heat, is one of the finest in the world, and its healthiness is