Abstract
Abstract Five trenches across the Bootheel lineament, a possible surface expression of one of the coseismic faults of the great New Madrid earthquakes of 1811 and 1812, indicate that ground failure took place along this 135-km-long feature, probably in 1811 or 1812. The morphology and en echelon pattern of the north-northeast-trending lineament are suggestive of strike-slip displacement on a fault. Three trenches cross portions of the lineament along which liquefied sand was injected. Vertically displaced strata were observed in two of these trenches, but the displacement could be due to collapse caused by the removal of liquefied sand from below. Shear zones exposed in two other trenches do not appear to be directly related to liquefaction and may represent near-surface deformation associated with deeper deformation along potentially seismogenic structures.
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