PUNCH,
OR THE LONDON CHARIVARI.

VOL. 1.

OCTOBER 16, 1841.

TRADE REPORT.

(FROM OUR OWN REPORTER.)

The market has been in a most extraordinary state all the morning. Our first advices informed us that feathers were getting very heavy, and that lead was a great deal brisker than usual. In the fish-market, flounders were not so flat as they had been, and, to the surprise of every one, were coming round rapidly.

The deliveries of tallow were very numerous, and gave a smoothness to the transactions of the day, which had a visible effect on business. Every species of fats were in high demand, but the glut of mutton gave a temporary check to the general facility of the ordinary operations.

The milk market is in an unsettled state, the late rains having caused an unusual abundance. A large order for skim, for the use of a parish union, gave liveliness to the latter portion of the day, which had been exceedingly gloomy during the whole morning.

We had a long conversation in the afternoon with a gentleman who is up to every move in the poultry-market, and his opinion is, that the flouring system must soon prove the destruction of fair and fowl commerce. We do not wish to be premature, but our informant is a person in whom we place the utmost reliance, and, indeed, there is every reason why we should depend upon so respectable an authority.

Cotton is in a dull state. We saw only one ball in the market, and even that was not in a dealer’s hands, but was being used by a basket-woman, who was darning a stocking. After this, who can be surprised at the stoppage of the factories?

Nothing was done in gloves, and what few sales were effected, seemed to be merely for the purpose of keeping the hand in, with a view to future dealings.

THE GEOLOGY OF SOCIETY.

The study of Geology, in the narrow acceptation of the word, is confined to the investigation of the materials which compose this terrestrial globe;—in its more extended signification, it relates, also, to the examination of the different layers or strata of society, as they are to be met with in the world.

Society is divided into three great strata, called High Life—Middle Life—and Low Life. Each of these strata contains several classes, which have been ranged in the following order, descending from the highest to the lowest—that is, from the drawing-room of St. James’s to the cellar in St. Giles’s.

It will be seen, by a glance at the above table, that the three great divisions of society, namely, High Life, Low Life, and Middle Life, are subdivided, or more properly, sub-classed, into the Superior, Transition, and Metamorphic classes. Lower still than these in the social scale is the Primitive Formation—which may be described as the basis and support of all the other classes. The individuals comprising it may be distinguished by their ragged surface, and shocking bad hats; they effervesce strongly with gin or Irish whiskey. This class comprehends the St. Giles’s Group—(which is the lowest of all the others, and is found only in the great London basin)—and that portion of the Whitechapel group whose individuals wear Bluchers and ride in pleasure ‘wans’ to Richmond on Sundays. In man’s economy the St. Giles’s Group are exceedingly important, being usually employed in the erection of buildings, where their great durability and hod-bearing qualities are conspicuous. Next in order is the Metamorphic class—so called, because of the singular metamorphoses that once a week takes place amongst its individuals; their common every-day appearance, which approaches nearly to that of the St. Giles’s Group, being changed, on Sundays, to a variegated-coloured surface, with bright buttons and a shining “four-and-nine”—goss. This class includes the upper portion of the Whitechapel Group, and the two lower strata of the Clapham Group. The Whitechapel Group is the most elevated layer of the inferior series. The Shabby Genteel stratum occupies a wide extent on the Surrey side of the water—it is part of the Clapham Group, and is found in large quantities in the neighbourhood of Kennington, Vauxhall, and the Old Kent-road. A large vein of it is also to be met with at Mile-end and Chelsea. It is the lowest of the secondary formation. This stratum is characterised by its fossil remains—a great variety of miscellaneous articles—such as watches, rings, and silk waistcoats and snuff-boxes being found firmly imbedded in what are technically termed avuncular depositories. The deposition of these matters has been referred by the curious to various causes; the most general supposition being, a peremptory demand for rent, or the like, on some particular occasion, when they were carried either by the owner, his wife, or daughter, from their original to their present position, and left amongst an accumulation of “popped” articles from various districts. The chief evidence on this point is not derived from the fossils themselves, but from their duplicates, which afford the most satisfactory proof of the period at which they were deposited. Articles which appear originally to have belonged to the neighbourhood of Belgrave-square have been frequently found in