butterflies,) flying about in full vigour. The autumn is said to be fine, almost beyond former example.
Near the river Ohio the soil is light, but much broken on the surface by funnel-shaped hollows, not unlike those where the sides of coal-pits have fallen in. These inverted cones are evidently excavated by the infiltration of water, and indicate that the strata abounds with large fissures or caverns.
In travelling over the last forty miles, limestone is the only stratified mineral that I have seen. It lies in a position nearly horizontal, and is literally conglomerated with organic remains. Amongst these, the most remarkable is a species of terebratula, which is very abundant, and varies from the size of a walnut to that of a pin's head. In addition to the concentric striated character, so frequent amongst bivalve shells, it has large radiated grooves; the grooves on one valve opposite to ridges on the other. The superior margin is, of course, a zig-zag line, resembling the base of {103} polyhedral crystals, where the sides of one pyramid are set on the angles of another.
For some days past I have found the expense of travelling to be uniformly three shillings and elevenpence farthing per day.
Limestone, sometimes called Maysville,[63] is a considerable landing place on the Kentucky side of the river Ohio. The houses stand above the level of the highest floods. There is a rope-walk, a glass-house, several stores and taverns, and a bank, in the town.
On the 26th, I left Limestone by the road for Lexington, which is sixty-four miles distant. The roads, hitherto
