Print this pagePennsylvanian 
depositional
systems and geomorphic
development of the Pecos River Canyon, Northern New Mexico
Sonja Heuscher,
Stratigraphic, sedimentologic, and field mapping data from the
Pecos River Canyon of northern New Mexico were used to interpret Pennsylvanian
depositional
systems, their relation to Ancestral Rockies tectonics, and
Cenozoic geomorphic processes. The
Pennsylvanian La Pasada and Alamitos formations record subtidal and shallow
water marine sedimentation on the Pecos shelf at the edge of an actively
subsiding tectonic basin. Evidence of
this tectonism is reflected in the abundance of coarse clastic sediment. Paleocurrents show south transport of thick
arkosic conglomerates, mixed bioclastic/siliciclasitic
sediment, and tabular and trough cross-bedded arkosic sandstones and
siltstones. These sediments are
interpreted as deltaic deposits on the subsiding carbonate Pecos shelf, south
of the Ancestral Rocky Mountains.
Subsidence history calculations indicate that ~450 m of tectonic
subsidence occurred at the Pecos shelf throughout the Pennsylvanian. A well-studied stratigraphic section at
Dalton Bluff, 5 km north of the study area, contains 81 m of correlative
strata.
Geologic mapping reveals folding and faulting that is likely
associated with the Laramide Orogeny and Rio Grande Rift respectively. Formation of the Pecos River Canyon has
resulted in rockfall and large landslides on the east side of the canyon. GPR data show that the landslides are at
least 7 m deep. Pedimentation likely
occurred as a result of Pleistocene climate fluctuation and regional
uplift. Alluvial sedimentation,
colluvial creep, and rockfall are processes that continue in the canyon
today. This study enhances our
understanding of
Key words: Alamitos Formation, La Pasada Formation, arkosic conglomerate, Dalton Bluff, Pennsylvanian