Cover-beds (colluvium that may contain admired loess) are usually not regar
ded of use for relative dating. Three examples from the western USA, where
intervening soil forming episodes provide a stratigraphic framework of such
deposits, demonstrate otherwise. The stratigraphic value of cover-bed and
soil sequences was tested on a river terrace chronosequence in southeastern
Utah, on ice-wedge casts in south-central Wyoming, and on till and affilia
ted outwash in northeastern Nevada. There is indication that Mt. St. Helens
-derived cummingtonite can serve as a stratigraphic marker mineral in the a
rea. When relative-dating relief by overlying cover-beds, care must be take
n of erosion hiatuses and of tectonically induced processes out of phase wi
th those driven by climate. Because cover-beds are widespread and cover lar
ge areas, similar approaches are encouraged to test their stratigraphic val
ue elsewhere.