Lewis and Clark began to see products derived from the Fort Union Formation on the Missouri River as far downstream as Blair, in Washington County, Nebraska, on August 4, 1804. It looked to them like pumice stone, so that's what they called it. (Playing by ear, as usual, Clark spelled it "Pumey Stone," and "Pumies Stone.")
Clinker, near Decker, Montana, in the southern end of the Fort Union Formation, far from the Missouri River.
But what was Clark's "pumice stone," really? How was it formed, and how did it get so far away from its place of origin?
The lignite in the Fort Union Formation ignites easily. Prairie fires may set the coal beds afire, but the coal also will combust spontaneously. Sometimes the materials adjacent to the burning coal beds become so hot that they actually froth and, when cooled, resemble the bubbly and cratered volcanic rock called pumice. Some of it is extremely light because it has so much void space in it (and some of the bubbles contain trapped air) that, if washed away into a river, it can float great distances. Most of the burned coal, however, is clinker, a baked shale, and resembles fragments of brick, as in the photograph above.
The rocks Clark observed had originated more than 450 miles upstream in the Fort Union Formation. Having been washed into the Missouri, or fallen from the riverbank, they had floated downriver, far from their place of origin.
The Corps of Discovery's entrance into the neighborhood of the Fort Union Formation was signalled—to us, today—by their observation of some "Stone Cole" in a bank near their campsite of October 20, 1804, a few miles south of today's Mandan, North Dakota.1 They continued to remark on its most conspicuous elements, mainly clinker, varicolored sandstone, and mudstone. The clinker, or burnt coal beds, create conspicuous brick-red stripe across the faces of many bluffs and buttes where the Fort Union Formation is exposed. The clinker is the product of burning of the coal beds; Lewis and Clark commonly called this the burnt earth, or said that it had "burnt appearances." Clinker is sometimes called "scoria." In North Dakota, crushed scoria is frequently used in place of gravel for surfacing country roads.
1. In the eighteenth century the terms stone-coal, pit-coal, and earth-coal were common names for mineral coal, while the word coal alone denoted charcoal, or charred wood. Thus, when Clark mentions that an Indian informant drew a map with a piece of "coal," we may assume he meant charcoal. See John Entick's New Spelling Dictionary, first published in London in 1764, and reprinted numerous times in the United States (Early American Imprints, First Series, No. 37375). Furthermore, Biblical references to coal are necessarily to charcoal, since mineral coal has never been found in Palestine.
Funded in part by a grant from the Montana Committee for the Humanities.
Lewis's Pumice Specimen
A specimen of pumice believed to have been sent to President Jefferson
Photo courtesy of the Academy of Natural Sciences, Philadelphia
Richard M. McCourt, Curator
Among the numerous papers and collections shipped back east from Fort Mandan on the keelboat in April of 1805 was a mineralogical collection of sixty-eight specimens. Lewis's list of the collection's contents is among the "Fort Mandan Miscellany,"1 but only seven of the existing specimens remain, and only one of those, a "Petrified Jawbone of a fish" found by Sergeant Gass on the Missouri River in August of 1804, still has the original label attached. The provenance of the rest cannot be verified.
Three of the sixty-eight descriptions in Lewis's list are of interest in the present context. Number twenty-four was "Carbonated wood found on the Std. side of the Riv near fort mandane 60 feet above high water mark in the Bank Strata 6 Inch thick." Number sixty-four was "Specimen of Carbonated wood with the loose Sand of the sand-Bars of the Missouri & Mississippi, it appears in considerable quantaties in many places." The whereabouts of those specimens are currently unknown.
The third is number sixty-two. Lewis's annotation in the list reads:
Specimen of the pummice stone found amongst the piles of drift wood on the Missouri, sometimes found as low down as the mouth of the osage river. I can hear of no burning mountain in the neighborhood of the Missouri or its Branches, but the bluffs of the river are now on fire at Several places, particularly that part named in our chart of the MissouriThe Burning Bluffs.2 the plains in many places, throughout this great extent of open country, exhibit abundant proofs of having been once on fire . Witness the Specimens of Lava and Pummicestone found in the Hills near fort mandon. . . .
Unfortunately, the association between that description and the specimen pictured above is only anecdotal.
Clearly, Lewis confused cold coal clinker with pumice. But the riddles of the earth's crust, and of the fire at the core, were yet to be solved by geologists—who in the decade of the Expedition had not even agreed upon the name of their science.