Page:Early western travels, 1748-1846 V13.djvu/200

 Rocky creek,[158] opposite to the outlet of which, a ledge of rocks nearly traverses the Arkansa, and presents a considerable obstruction in the navigation at a low stage of water. The current even at this time broke with a considerable noise.

21st.] About six miles above Rocky creek we passed the Charbonniere, so called from the occurrence of coal in its vicinity; we also observed the outlet of Spadrie creek,[159] on the borders of which there {138} are considerable tracts of fertile land, well supplied with springs, and occupied by the Cherokees. The rocks which occasionally border the river, of very inconsiderable elevation, are composed of slaty sandstone, dipping about 25°, sometimes towards the north-west, and at others to the south-east, or in opposite directions, and also exhibiting indications of coal. The Charbonniere rock, in particular, about 50 feet high, presents beds of a slaty sandstone, with a dip of scarcely 20°, and inclined in opposite directions so as to form a basin, in which there are indications of coal. A lofty blue ridge appears to the south, called by the French hunters the Cassetête or Tomahawk mountain,[160] and about eight miles from hence enters the creek of the same name, beyond which we proceeded eight miles of a 12 mile bend, making a journey of about 28 miles in the course of the day, and encamped in view of another lofty