that ye fall not out by the way.'

As he ceased, a gleam of sunshine broke through the twilight, and fell full upon him. In its brightness, the noble aspect did not alter, but grew more familiar to their eyes; and Christopher and Hubert knew at the same moment that he was none other than their brother Gottleib. Both sprang to embrace him, but the way, the travellers, and Gottleib, vanished from them. They looked into each other's faces by the early sunlight which streamed through the closed shutters of their room, and gleamed on the brazen clasps of the Coverdale Bible, still lying between them on the table where they had fallen asleep.

Such is the account of the affair given by themselves; although more, it is believed, to suit the taste and belief of the time they lived in than their own. The two brothers had passed many hours silent and in the dark; and it is not unreasonable to suppose that the visionary world, into which they had unconsciously slipped, presented to both such phenomena—founded on the meditations and recollections in which both had been immersed—as were easily rendered in the exoteric types of romance. The brothers talked long over the vision, and could scarcely satisfy even themselves that it was indeed a dream; but they agreed on its use of wisdom and warning, and disputed no more. The old house was not sold, nor the types divided. It is even affirmed that the bookseller's daughter and the Catholic widow lived there as right friendly sisters-in-law; and after many a broadside and folio page, the press they had worked for so many years at length struck off the tale we have just related—the German brothers supposing that some honest men in England might profit, as they had done, by a look upon Life's Highway.

DUST-SHOWERS AND RED-RAIN.

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Recent scientific investigations in Europe and America have thrown some interesting light on the nature of these very curious phenomena. The results arrived at may be brought familiarly before our readers.

Mr Charles Darwin, in the narrative of his voyage in the Beagle, states that while he was at St Jago, one of the Cape de Verd islands, in January 1832: 'The atmosphere was generally very hazy; this appears chiefly due to an impalpable dust, which is constantly falling, even on vessels far out at sea. The dust,' he goes on to say, 'is of a brown colour, and under the blow-pipe, easily fuses into a black enamel. It is produced, as I believe, from the wear and tear of volcanic rocks, and must come from the coast of Africa.' The same opinion was held by scientific men generally, as well of the dust met with in the North Atlantic, as of that which sometimes falls on the islands and shores of the Mediterranean: Africa was supposed to be the original source of the air-borne particles. Some of the dust, however, having been sent to Ehrenberg of Berlin, that celebrated savant, after a microscopical examination, laid an account of his inquiry before the Akademie der Wissenschaften, in May 1844, in which he shewed that the dust, so far from being inorganic, contained numerous specimens of a species of flint-shelled animalcules, or infusoria, known as polygastrica, and minute portions of terrestrial plants. The investigation led him to certain conclusions: '1. That meteoric dust-rain is of terrestrial origin. 2. That the same is not a rain of volcanic ashes. 3. That it is necessarily a dust carried up to a great height by a strong current of air or whirlwind from a dried-up swamp-region. 4. That the dust neither demonstrably nor necessarily comes from Africa, notwithstanding that the wind may blow from thence as the nearest land when the dust falls, because there are in it no forms whatsoever exclusively native to Africa.' These were remarkable facts, but warranted by the evidence: one, if not more, of the animalcules was proved to be peculiar to America, and that country was naturally inferred to be the quarter from which they had been derived.

The inquiry once begun was followed up; other specimens of dust were submitted to the same critical test, and found generally to contain a much greater number and variety of infusoria than the first—mostly fresh-water forms, but with a few of marine origin; whence the conclusion, that they had been brought from a coast-region; and especially remarkable was the fact, that among all the forms there was not one peculiar to the African continent. One example was known to belong to the Isle of France, the others were chiefly South American. After an examination of six specimens, obtained at different intervals, Ehrenberg discovered that they contained four organisms in common. 'I now consider myself,' he observes, 'justified in the conclusion, that all the Atlantic dust may come only from one and the same source, notwithstanding its extent and annual amount. The constant yellow and reddish colour of the dust, produced by ferruginous matter, its falling with the trade-winds and not with the harmattan, increase the interest of the phenomena.'

It had always been supposed, that the dust which traversed the Mediterranean was borne from the Great Sahara; but in a quantity collected on board the ship Revenge, at Malta, an infusoria peculiar to Chili was met with, which, with other characteristics, proved the dust to be the same as that observed on the Atlantic. Their colour, too, was identical; while the Sahara is a 'dazzling white sand:' hence the dust brought across the Mediterranean by the sirocco was not peculiar to Africa. The conclusion here arrived at was still further verified by another sirocco-storm in May 1846, which extended to Genoa, and bore with it a dust that 'covered the roofs of the city in great abundance.' This, as was clearly ascertained, contained formations identical with those which had been collected off the Cape de Verd; and it was shewn that the dust-showers of the Atlantic, and those of Malta and Genoa, were 'always of a yellow ochre-like colour—not gray, like those of the kamsin, in North Africa.' The peculiar colour of the dust was found to be caused by iron-oxide; and from one-sixth to one-third of the whole proved to consist 'of determinable organic parts.' In the following year, 1847, Ehrenberg had another opportunity of testing his conclusions, in specimens of dust which had fallen in Italy and Sicily in 1802 and 1813; the same result came out on examination; 'several species peculiar to South America, and none peculiar to Africa.'

Thus, omitting the two last-mentioned instances, there had been five marked falls of dust between 1830 and 1846; how many others passed without notice, it would now be impossible to ascertain. The showers sometimes occur at a distance of 800 miles from the coast of Africa, and this region lies between the parallels of 17 and 25 degrees north latitude, and whence, as we have seen, they extend to the northern shores of the Mediterranean. In the dust collected from these various falls, there have been found altogether nineteen species of infusoria; of which eight were polythalamia, seven polygastrica, and two phytolitharia, these chiefly constituting the flint-earth portion of the dust. The iron was composed of the gaillonilla, and 'the carbonic chalk earth corresponded tolerably well to the smaller number of polythalamia.' The uniform character of the specimens obtained at intervals over so long a course of years is especially remarkable.

To turn, now, for a few moments to the second phenomenon indicated in our title. In October 1846, a fearful and furious hurricane visited Lyon and the district between that city and Grenoble, during which occurred a fall of blood-rain. A number of drops were caught and preserved, and when the moisture had evaporated, there was seen