The petrology and stratification of the late Pleistocene and Recent mesa deposits in the Mesa Verde area are described. These deposits are believed to have been formed by eolian deposition. Measurements of present-day dust accumulation are reported. The age relationships of the strata are discussed on the basis of measurements of the radioactivity of organic carbon and carbonate precipitates and with reference to the early Mesa Verde culture.
Our of the dust of time
comes a nation's heritage.
Eugene W. Ingle