The legacy of the 1811-1812 New Madrid, Central United States, earthquakes is one of tremendous enigma. We are left with just enough contemporary information to provide a measure of constraint on the isoseismal contours and therefore magnitudes of the three principal events (Nuttli, 1973; Street, 1982; Johnston, 1996; Hough et al., 2000), yet given the sparse population density and limited documentation of effects, our interpretations will always be plagued by a significant degree of uncertainty. Although the magnitudes of the three principal New Madrid main shocks will likely never be established with precision, all contemporary analyses (see above references) obtain magnitudes upward of 7 for all three events—large enough to produce perceptible ground motions as far away as the Atlantic seaboard.

One enduring and interesting bit of folklore concerning the New Madrid earthquakes of 1811-1812 involves the tale of a volcanic eruption in North Carolina at the time of the first main shock on 16 December 1811. The site of this supposed volcano was approximately 750 km east of the main shock and 40 km northwest of Asheville, North Carolina, at an area known in the early 1800's as “the springs” or “the warm springs” (Figure 1). I will henceforth refer to the location by the name of the town that exists there now: Hot Springs. The tale has merited a brief mention in some modern treatises on the New Madrid sequence. For example, Penick (1981) mentions the 1812 letter by Asheville, North Carolina resident John Clarke Edwards that described the supposed eruption. Penick (1981) goes on to note that the letter was quickly discredited as a hoax.