Abstract
The traumatic effects of cyclonic winds on forest vegetation are documented for a regional storm front that was accompanied by a localized tornado. In assessing an ancient thanatocoenosis (death assemblage) that may be the result of blow-downs, it is important to document the regional scatter of trees in order to determine whether or not the traumatic event represents merely violent windstorms or is the result of cyclonic winds. The recognition of such situations in the rock record would allow for a more detailed assessment of prevailing paleoclimate
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