Page:John Uri Lloyd - Etidorhpa.djvu/113

From Wikisource
Jump to navigation Jump to search
This page needs to be proofread.

in both directions, its extremes dissolving in a bed of forest. A great black bluff, far up the stream, rose like a mountain, upon the left side of the river; bottom lands were about us, and hills appeared across the river in the far distance—towards the Tennessee River. With regret I finally drew my eyes from the vision, and we resumed the journey. We followed the left bank of the river to the base of the black bluff,—"Biswell's Hill," a squatter called it,—and then skirted the side of that hill, passing along precipitous stone bluffs and among stunted cedars. Above us towered cliff over cliff, almost perpendicularly; below us rolled the river.

I was deeply impressed by the changing beauties of this strange Kentucky scenery, but marveled at the fact that while I became light-hearted and enthusiastic, my guide grew correspondingly despondent and gloomy. From time to time he lapsed into thoughtful silence, and once I caught his eye directed toward me in a manner that I inferred to imply either pity or envy. We passed Biswell's Bluff, and left the Cumberland River at its upper extremity, where another small creek empties into the river. Thence, after ascending the creek some distance, we struck across the country, finding it undulating and fertile, with here and there a small clearing. During this journey we either camped out at night, or stopped with a resident, when one was to be found in that sparsely settled country. Sometimes there were exasperating intervals between our meals; but we did not suffer, for we carried with us supplies of food, such as cheese and crackers, purchased in Smithland, for emergencies. We thus proceeded a considerable distance into Livingston County, Kentucky.

I observed remarkable sinks in the earth, sometimes cone-shaped, again precipitous. These cavities were occasionally of considerable size and depth, and they were more numerous in the uplands than in the bottoms. They were somewhat like the familiar "sink-holes" of New York State, but monstrous in comparison. The first that attracted my attention was near the Cumberland River, just before we reached Biswell's Hill. It was about forty feet deep and thirty in diameter, with precipitous stone sides, shrubbery growing therein in exceptional spots where loose earth had collected on shelves of stone that cropped out