Missionary Travels And Researches In South Africa By David Livingstone



 -   The cattle in this country are seldom milked,
on account of the strong prejudice which the Portuguese entertain
against the - Page 631
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The Cattle In This Country Are Seldom Milked, On Account Of The Strong Prejudice Which The Portuguese Entertain Against The Use Of Milk.

They believe that it may be used with safety in the morning, but, if taken after midday, that it

Will cause fever. It seemed to me that there was not much reason for carefully avoiding a few drops in their coffee, after having devoured ten times the amount in the shape of cheese at dinner.

The fort of Pungo Andongo (lat. 9d 42' 14" S., long. 15d 30' E.) is situated in the midst of a group of curious columnar-shaped rocks, each of which is upward of three hundred feet in height. They are composed of conglomerate, made up of a great variety of rounded pieces in a matrix of dark red sandstone. They rest on a thick stratum of this last rock, with very few of the pebbles in its substance. On this a fossil palm has been found, and if of the same age as those on the eastern side of the continent, on which similar palms now lie, there may be coal underneath this, as well as under that at Tete. The asserted existence of petroleum springs at Dande, and near Cambambe, would seem to indicate the presence of this useful mineral, though I am not aware of any one having actually seen a seam of coal tilted up to the surface in Angola, as we have at Tete. The gigantic pillars of Pungo Andongo have been formed by a current of the sea coming from the S.S.E.; for, seen from the top, they appear arranged in that direction, and must have withstood the surges of the ocean at a period of our world's history, when the relations of land and sea were totally different from what they are now, and long before "the morning stars sang together, and all the sons of God shouted for joy to see the abodes prepared which man was soon to fill." The imbedded pieces in the conglomerate are of gneiss, clay shale, mica and sandstone schists, trap, and porphyry, most of which are large enough to give the whole the appearance of being the only remaining vestiges of vast primaeval banks of shingle.

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