“Forty years have rolled away since Asfa Woosen, on whose memory be peace, grandsire to our beloved monarch, saw in a dream that the red men were bringing into his kingdom curious and beautiful commodities from countries beyond the great sea. The astrologers, on being commanded to give an interpretation thereof, predicted with one accord that foreigners from the land of Egypt would come into Abyssinia during His Majesty’s most illustrious reign, and that yet more and wealthier would follow in that of his son, and of his son’s son, who should sit next upon the throne. Praise be unto God that the dream and its interpretation have now been fulfilled! Our eyes, though they be old, have never beheld wonders until this day, and during the reign over Shoa of seven successive kings, no such miracles as these have been wrought in Ethiopia.”
Volume One—Chapter Forty Six.
By the passage of the polar star over the meridian, the magnetic variation at Ankóber was observed, with the aid of a well-regulated chronometer, to be 7 degrees westerly.
The longitude was determined both by a series of lunars, and by the eclipses of Jupiter’s satellites, the mean of upwards of 150 observations having been taken.
Remarks on the Natural History of that Portion of the Adel Country Situated along the Route from the Sea-Coast to the Frontier of Efát.
From Tajúra to Killulloo.
The advanced state of the season was unfavourable for observations in the department of natural history. Both animal and vegetable life were apparently in a state of torpor; the trees and shrubs were in general leafless; and no annual plant whatever was to be seen, even in the immediate vicinity of the watering-places. The few insects that were not in a state of chrysalis, seemed drowsily to procrastinate their existence until food for the new generation should be prepared by nature. Amphibia, Saurii, and Ophidii, which are generally not so dependent on a supply of water, existed in small numbers in their lurking-places, whilst birds and larger animals must at this season have migrated to more favoured countries.
Basaltic and trachytic hills, either isolated or in chains, rise at a distance of about half a mile from the sea-shore, which is winding and shelving. The hills are in general rounded, and marked by broad veins of similar composition, but containing more perfectly crystallised felspar, quartz, and zeolith. They have not the sharp peak, but are broken and cliffy, and have apparently been upheaved at different periods.