I determined to land definitively at this point, purposing to visit the mines, after completing my ascent by land to St. Louis. It was now the 23d of July, the whole of which, from the 1st, we had spent in a diligent ascent of the river, by setting pole and cordelle, from the junction of the Ohio—a distance of one hundred and seventy miles. We were still thirty miles above St. Louis.
I have detailed some of the incidents of the journey, in order to denote the difficulties of the ascent with barges prior to the introduction of steam, and also the means which this slowness of motion gave me of becoming acquainted with the physical character of this river and its shores. A large part of the west banks I had traveled on foot, and gleaned several facts in its mineralogy and geology which made it an initial point in my future observations. The metalliferous formation is first noticed at the little chain of rocks. From the Grand Tower, the western shores become precipitous, showing sections and piled-up pinnacles of the series of horizontal sandstones and limestones which characterize the imposing coast. Had I passed it in a steamer, downward bound, as at this day, in forty-eight hours, I should have had none but the vaguest and most general conceptions of its character. But I went to glean facts in its natural history, and I knew these required careful personal inspection of minute as well as general features. There may be a sort of horseback theory of geology; but mineralogy, and the natural sciences generally, must be investigated on foot, hammer or goniometer in hand.