10 Undergraduate Research I (Posters)
Thursday, 4 April 2013
8:00 AM - 12:00 PM
Classroom 108
A PENNSYLVANIAN AGE FOR THE FOUNTAIN FORMATION CONSTRAINED BY LITHOLOGIC COMPARISON OF OVERLYING EOLIAN UNITS
Paper number: 10-8
Program: Theme Sessions
Time: 8:00 AM – 12:00 PM
Authors
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D.E. SweetTexas Tech University, Lubbock, TX
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Aaron J. WattersTexas Tech University, Lubbock, TX
Abstract
Near Loveland, Colorado, eolian and fluvial strata intercalate in the upper 50 m of the Fountain Formation before giving way into the predominately eolian Ingleside Formation. This gradational transition from largely fluvial/alluvial to predominantly eolian is also observed to the south at the Manitou Springs locality. Sandstone mineralogy and grain size distributions of the Ingleside Formation mimic the Manitou Springs eolian unit, whereas similar data from the Lyons Formation does not. Therefore, at Manitou Springs, we suggest that the eolian unit atop the Fountain Formation lithologically is best characterized as Ingleside Formation. Barring a significant southerly time transgression for the Ingleside Formation, this proposed change in nomenclature further suggests age control from the north can be used to constrain a minimum age for the Fountain Formation. Thus, an entirely Pennsylvanian age for the Fountain Formation is proposed.