[67] The latitude of this point was ascertained by Major Long, in December, 1819, to be a few minutes below 34° north.—James.

Comment by Ed. On the Kiamesha (Kiamichi) see Nuttall's Journal, in our volume xiii, note 177.

[68] Just east of the ninety-ninth meridian, the Canadian almost touches the thirty-sixth parallel, and then turning southeast passes below the thirty-fifth, turning northeast again near the ninety-sixth meridian. The party is now near the bend to the southeast; the map probably shows them on the nineteenth too far along the southeast course. The stream flowing southeast was doubtless a tributary of the Washita. Gypsum (sulphate of lime) occurs in great abundance along the Canadian, especially between the ninety-ninth and one hundredth meridians. Near the ninety-ninth meridian begins a wooded district known as the Cross Timbers; it varies in width from five to thirty miles, and is four hundred miles in length, extending from the Arkansas to the Brazos.—Ed.

[69] This elegant centaurea has a head of flowers nearly as large as that of the cincus lanceolatus, so commonly naturalized in the East. Some specimens from seeds, brought by Major Long, have flowered in Mrs. Peale's garden, near Germantown. The plant will be easily naturalized, and will be found highly ornamental.—James.

[70] Chapter i in volume iii of the original London edition.—Ed.

[71] Later explorations proved that the divide between the Red and Canadian was well supplied with springs.—Ed.

[72] In places where the absence of crocodiles permits people to enter the river, Humboldt and Bonpland observed, that the immoderate use of baths, while it moderated the pain of the old stings of zanceadores, rendered them more sensible to new. By bathing more than twice a day, the skin is brought into a state of nervous irritability, of which no idea can be formed in Europe. It would seem as if all feeling were carried towards the integuments. Humboldt's Personal Narrative, vol. v. p. 105.—James.

[73] These are the three largest tributaries of the Arkansas from the west. The Ne-sew-ke-tonga is the modern Cimarron; the Negracka is the Salt Fork. The Cimarron is between the other two, in size as well as place; the Canadian is largest and most southerly. All united with the Arkansas between the thirty-fifth and thirty-seventh parallels. The two smaller streams between the Cimarron and Negracka, named Saline Creek and Strong Saline on the map, are now respectively known as Black Bear and Red Rock creeks.—Ed.

[74] Ampelopsis quinquefolia of Michaux.—James.

[75] The name is a corruption of the French aux arcs (with bows), applied to the Indians of Missouri and Arkansas. The hills here meant are known as the Shawnee Hills, from the Indians of that tribe, who later had villages on the Canadian about a hundred and twenty-five miles from Fort Smith.—Ed.