Crossing the karst: speleological observations of Lewis & Clark on the Lower Missouri River.
Ashley, David
Lewis & Clark's pioneering "Voyage of Discovery"
in 1804-06 crossed a significant karst terrane in Missouri, the only
karst encountered on their journey to the Pacific Ocean. Geology and
Speleology were yet to develop as sciences, yet Lewis & Clark made
significant observations of karst, pseudokarst, and paleokarst features.
The expedition's route took the explorers up-section from St.
Charles to Kansas City, crossing notable karst in Ordovician and
Mississippian carbonate rocks, into Pennsylvanian strata that is
primarily clastic sediments with few karst features. The captains and/or
other members of the Corps of Discovery passed the Florissant karst,
visited pseudokarst Tavern Rock Cave, encountered caves in the Gasconade
River drainage, noted a cave near Jefferson City at what is now
Clark's Hill-Norton State Historic Site, and visited numerous
springs. Upriver from Jefferson City, they noted paleokarst features
known today as Bull Rock and Sugar Loaf Rock. They recorded in their
journals the natural arch called Pierced Rock (Roche Percee'). The
party likely saw Rocheport Cave, Wilton Cave, and the spring flowing
from Lewis & Clark Cave in Boone County.
* Vineyard, J.D. Missouri Department of Natural Resources (Retired).