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Updated: May 31, 2025
Malcolmson and Captain Moresby, that Ehrenberg has rather under-rated the influence of corals, in some places at least, on the formation of the tertiary deposits of the Red Sea. There are, in this space, reefs, which, if I had known nothing of those in other parts of the Red Sea, I should unhesitatingly have considered as barrier-reefs; and, after deliberation, I have come to the same conclusion.
Every traveller describes the Harmatan, and most travellers transcribe the errors touching the infusoria and their coats which Ehrenberg found at sea in the impalpable powder near the Cape Verde islands. The dry cold blast is purely local, not cosmical.
Indians and deserts and Ehrenberg did not exist for me any more. My girlhood seemed to have returned, and I enjoyed everything with the keenest zest. My old friend Charley Bailey, who had married for his second wife a most accomplished young San Francisco girl, lived next door to us. General and Mrs. Kautz entertained so hospitably, and were so beloved by all. Together Mrs.
From the appearance of the pale-coloured, fine-grained beds, I was inclined to believe that they corresponded with the upper beds of the S. Cruz; but Professor Ehrenberg, who has examined some of the specimens, informs me that the included microscopical organisms are wholly different, being fresh and brackish-water forms.
So rapidly did he disappear that Ehrenberg could scarcely accompany him down the steps. "Oh, Caroline," said the happy father when he returned, "who could have imagined that the little cherry tree I planted in the flower-garden the day you were born would ever produce such good fruit?" "It was the providence of God," exclaimed the mother, clasping her hands.
Having just lately received my books, I also inclose a pamphlet from Ehrenberg, which he desired me to leave with you, and also the books Professor Silliman has had the kindness to lend me. . . I have made many observations which I wish to publish, but I can find no time to write them for you now.
Among the scientific instructions for the voyage drawn up by a committee of the Royal Society, however, there is a remarkable letter from Von Humboldt to Lord Minto, then First Lord of the Admiralty, in which, among other things, he dwells upon the significance of the researches into the microscopic composition of rocks, and the discovery of the great share which microscopic organisms take in the formation of the crust of the earth at the present day, made by Ehrenberg in the years 1836-39.
Professor Ehrenberg finds that this dust consists in great part of infusoria with siliceous shields, and of the siliceous tissue of plants. I must take this opportunity of acknowledging the great kindness with which this illustrious naturalist has examined many of my specimens. The infusoria, with the exception of two marine species, are all inhabitants of fresh-water.
The most ancient forms recently made known by Ehrenberg are exceedingly like those which now exist: no one has ever pretended that the difference between any ancient and any modern Foraminifera is of more than generic value, nor are the oldest Foraminifera either simpler, more embryonic, or less differentiated, than the existing forms.
True, there was rumor of riot and lawlessness among the miners at Castle Dome and the customary shooting scrape at Ehrenberg and La Paz, but these were river towns, far behind him now as he looked back over the desert trail and aloft into the star-studded, cloudless sky. Nothing could be more placid, nothing less prophetic of peril or ambush than this exquisite summer night.
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