The general hospitality and frankness of the inhabitants of the mine country could not but make a favourable impression on a stranger. The custom of riding on horseback, in a region which affords great facilities for it, makes every one a horseman and a woodsman, and has generated something of the cavalier air and manners. But nothing impressed me more, in this connexion, than the gallant manner, which I observed here, of putting a lady on horseback. She stands facing you, with the bridle in her right hand, and gives you her left. She then places one of her feet in your left hand, which you stoop to receive, when, by a simultaneous exertion and spring, she is vaulted backwards into the saddle. Whether this be a transmitted Spanish custom, I know not, but I have not observed it in the French, or American settlements west of the Alleghanies.
The earthquakes of 1812, which were so disastrous in South America, are known to have propagated themselves towards the north, and they exerted some striking effects in the lower part of the valley of the Mississippi, sending down into the channel of the latter, large areas of deluvial earth, as was instanced, in a remarkable manner, at New Madrid. Portions of the forest, back of this town, sunk, and gave place to lakes and lagoons. These effects were also witnessed, though in a milder form, in the more solid formations of the mine country. Soon after reaching Potosi, I visited the Mineral Fork, a tributary of the Merrimack, where some of these effects had been witnessed. I descended into the pit and crevices of the Old Mines. These mines were explored in the metalliferous rock. Every thing had an old and ruinous look, for they had been abandoned. Large quantities of the ore had been formerly raised at this mine, which was pursued into a deep fissure of the limestone rock. I descended into this fissure, and found among the rubbish and vein stones, large elongated and orbicular masses of calc spar, the outer surfaces of which bore strong marks of geological abrasion. They broke into rhombs very transparent, and of a honey-yellow colour. Mr. Elliot, the intelligent proprietor of this mine, represented the indications of ore to have been flattering, although every thing was now at a stand. Masses of sulphuret of zinc, in the form of blende, were noticed at this locality. Mr. Elliot invited me to dine, and he filled up the time with interesting local reminiscences. He stated, among other facts, that a copious spring, at these mines, dried up during the remarkable earthquakes of 1812. These earthquakes appear to have discharged their shocks in the direction of the stratification from the southwest to the northeast, but they spent their force west of the Mississippi. Their chief violence was at Natchitoches and New Madrid, at the latter of which they destroyed an immense area of alluvial land. Their effects in the Ohio valley, lying exactly in the direction of their action, were slight. A Mr. Watkins, of Cincinnati, accompanied me on this examination, and rode back with me to Potosi.
On the 9th of August, I had dined with Samuel Perry, Esq., at Mine á Burton, one of the principal inhabitants of the county, and was passing the evening at Mr. Austin's, when Mr. and Mrs. Perry came suddenly in. They had hardly taken seats, when a rabble of persons with bells and horns surrounded the house, and kept up a tumult that would have done honor to one of the wildest festivals of St. Nicholas, headed by Brom Bones himself. This, we were told, was a Chiraviri. And what is a Chiraviri? I am not deep enough read in French local customs to give a satisfactory answer, but the custom is said to be one that the populace may indulge in, whenever a marriage has taken place in the village, which is not in exact accordance with their opinions of its propriety. I was, by this incident, informed of Mr. Perry's recent marriage, and should judge, moreover, that he had exercised both taste and judgment in his selection of a partner. The affair of the Chiraviri is said to have been got up by some spiteful persons.
Towards the middle of the month (12th,) I set out, accompanied by Mr. James B. Austin, on horseback, for Herculaneum, by the way of Hazel Run, a route displaying a more southerly section of the mine country than I had before seen. A ride on horseback over the mine hills, offers one of the most delightful prospects of picturesque sylvan beauty that can be well conceived of. The hills are, with a few exceptions, not precipitous enough to make the ride irksome. They rise in long and gentle swells, resembling those of the sea, in which the vessel is, by an easy motion, alternately at the top of liquid hills, or in the bottom of liquid vales. From these hills the prospect extends over a surface of heath-grass and prairie flowers, with an open growth of oaks, giving the whole country rather the aspect of a park than a wilderness. Occasionally a ridge of pine intervenes, and wherever there is a brook, the waters present the transparency of rock crystal. Sometimes a range of red clay hillocks, putting up rank shrubs and vines of species which were unknown before, indicates an abandoned digging or mine. Farms and farm houses were then few; and every traveller we met on horseback, had more or less the bearing of a country cavalier, with a fine horse, good equipments, perhaps holsters and pistols, sometimes a rifle, and always something of a military air, betokening manliness and independence. Wherever we stopped, and whoever we met on the way, there was evinced a courteous and hospitable disposition.
We did not leave Potosi till afternoon. It was a hot August day, and it was dusk before we entered the deep shady valley of Big River. Some delay arose in waiting for the ferryman to put us across the river, and it was nine o'clock in the evening when we reached Mr. Bryant's, at Hazel Run, where we were cordially received. Our host would not let us leave his house, next morning, till after breakfast. We rode to McCormick's, on the Platten, to dinner, and reached Herculaneum before sunset. The distance by this route from Potosi is forty-five miles, and the road, with the exception of a couple of miles, presented a wholly new section of the country.
The Mississippi was now low, displaying large portions of its margin, and exhibiting heavy deposits of mud and slime, which broke into cakes, as they dried in the sun. I know not whether these exhalations affected me, but I experienced a temporary illness for a few days during this visit. I recollect that we had, during this time, some severe and drenching rain storms, with vivid and copious lightning, and heavy pealing thunder. These drenching and rapid showers convert the brooks and rills of the mine country to perfect torrents, and this explains one cause of the washing away and gullying of roads and streets, so remarkable on the west bank of the Mississippi. My illness induced me to give up returning on horseback; and I set out, on the 18th of the month, in a dearborn, accompanied by Mrs. Austin. On descending the long hill, near Donnell's, beyond the Joachim, the evening was so dark that I became sensible I must have got out of the road. I drove with the more care a few moments, and stopped. Requesting Mrs. Austin to hold the reins, I jumped out and explored the ground. I found myself in an abandoned, badly gullied track, which would have soon capsized the wagon; but leading the horse by the bridle, I slowly regained my position in the direct road and got down the hill, and reached the house without further accident. Next day we drove into Potosi by four o'clock in the afternoon. This was my second visit, and I now accepted a room and quarters for my collection, at their old homestead called Durham Hall.
From this period till the middle of September, I pursued with unremitting assiduity, the enquiry in hand, and by that time had made a cabinet collection, illustrating fully the mineralogy, and, to some extent, the geological structure of the country. I erected a small chemical furnace for assays. Some of the clays of the country were found to stand a high heat, and by tempering them with pulverized granite, consisting largely of feldspar, I obtained crucibles that answered every purpose. Some of the specimens of lead treated in the dry way, yielded from 75 to 82 per cent.
Accident threw in my way, on the 25th of August, a fact which led to the discovery of a primitive tract, on the southern borders of the mine country, the true geological relation of which to the surrounding secondary formations, formed at the outset rather a puzzle. I rode out on horseback on that day, with Mr. Stephen F. Austin, to Miller's, on the