Jefferson's Salt Mountain
Where the Story Came FromProbably from, among others, Zebulon Pike. In 1803 (thus before the Lewis & Clark expedition) Pike wrote of a "mountain of salt" in the west and saw "bushels" of salt from it in St. Louis. In English it is possible to use the word "salt" as an adjective in front of the noun "mountain." This might mean a mountain composed of salt, or it might mean a mountain simply in some way associated with salt. In either Spanish or French, the languages by which Anglo-Americans might hear of the wonders of Louisiana, the word for "mountain" must come first, followed by a preposition, followed by the object of the preposition, that is, the word for "salt." Now take the Spanish or French phrase and translate it into English, and you get "mountain of salt"--which phrase connotes to an English-speaker that the mountain is composed of salt. Thus Jefferson believed that the Salt Mountain was a mountain of salt.The man who sorted out this misconception was a gentleman explorer named George Champlin Sibley. In 1811 he set out from his post at Fort Osage, on the Missouri River, to travel the central plains on a two-fold mission. First, he was to make friends and allies among the Indians. Second--and this interest was more personal--he wanted to find Jefferson's Salt Mountain. He thought he had the mystery figured out. ![]()
Sibley wrote to his superior, William Clark, of this site that he called the Rock Saline, It is a level flat of redish colored sand containing about 500 acres longitudinally intersected by a small stream [the Buffalo] which flows into a branch [the Cimarron] of the Arkansas. It is bounded from S.E. to N.N.W. by very lofty hills, whose sides next the saline area are for the most part perpendicular and faced with rugged rocks of gypsum of various kinds intermixed with red clay and some flint. From the bases of these hills issue many springs of salt water. There are also four springs that arise within the flat. . . . The water of the springs in the flat is so strong that salt will not dissolve in it. After a long series of very hot weather this section is nearly all covered with a solid rock of salt from 5 to 12 inches thick, and immediately round the four springs, a kind of hollow cones of salt are formed more than two feet above the general surface; at one of these I hewed out with my tommahawk a block of salt 16 inches in thickness. . . . The quality of the rock salt is unquestionably superior to any that I ever saw. It is beautifully white. . . . herewith are some few specimens of this salt, and also some of gypsum.These salt samples were not the first sent east from Jefferson's Salt Mountain, however. In 1804 Meriwether Lewis, en route west, had interviewed a French trader in St. Louis about a saline "on a considerable southern branch of the Arkansas." Notes of this interview, along with salt samples acquired by Auguste Chouteau, were carried to Jefferson by Pierre Chouteau. Thus Jefferson once held in his hands salt from the mountain that had caused him so much embarrassment. It is unclear whether he ever realized where it came from. He donated the salt samples to the American Philosophical Society.
BibliographyIsern, Thomas D. "George Champlin Sibley, 1811 and 1825-1826," in Joseph A. Stout, Ed., Frontier Adventures: American Exploration in Oklahoma (Oklahoma City: Oklahoma Historical Society, 1976), pp. 19-37.Isern, Thomas D. "Jefferson's Salt Mountain: The Big Salt Plain of the Cimarron River," Chronicles of Oklahoma 58 (Summer 1980): 160-175. Isern, Thomas D., Ed. "Exploration and Diplomacy: George Champlin Sibley's Report to William Clark, 1811," Missouri Historical Review 73 (October 978): 85-102.
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