The Pajarito Plateau of northern New Mexico contains a rich and diverse record of late Quaternary landscape changes in a variety of geomorphic settings that include gently-sloping mesa tops, steep canyon walls, and canyon bottoms. A broad range of investigations during the past decade, motivated by environmental and seismic hazard concerns, have resulted in examination of the characteristics, stratigraphy, and age of sediments and soils at numerous locations throughout the Plateau. Geochronologic control is provided by >140 radiocarbon dates supplemented by soil characterization and tephrochronology. In this paper we first summarize some of the results of recent and ongoing work on late Quaternary deposits on the Pajarito Plateau, illustrat...
Due to the character of the original source materials and the nature of batch digitization, quality ...
AbstractThe Pajarito fault forms the western margin of the Rio Grande rift in north-central New Mexi...
The Cenozoic history of crustal deformation, surface uplift, and erosion of the central Colorado Pla...
In northeastern Arizona, on the Colorado Plateau, landscapes associated with weakly cemented sandsto...
Presented here is the first comprehensive late Quaternary alluvial stratigraphic record from desert ...
The causal mechanisms for the onset and patterns of post-Miocene erosion of the western Great Plains...
Soils in the arid to semi-arid piedmont landscapes of central New Mexico were examined in order to e...
In order to evaluate potential effects of tectonics and climate change on the behaviour of the axial...
There is little doubt that climate is an important parameter affecting the shape of the Earth`s surf...
The East Potrillo Mountains are located just north of the U.S.-Mexico border in southwestern Dona An...
Apatite thermochronology is, in principle, uniquely suited to document the Cenozoic erosion of the C...
Stratigraphic records in Middle Park in north-central Colorado provide evidence for the late Quatern...
Predictions of how ecosystems may respond to future climatic changes must be based on an understandi...
Relationships between river incision, aggradation, and widening are investigated in a ∼5 km reach of...
Tectonic geomorphology of the Toroweap Fault, western Grand Canyon, Arizona: implications for transg...
Due to the character of the original source materials and the nature of batch digitization, quality ...
AbstractThe Pajarito fault forms the western margin of the Rio Grande rift in north-central New Mexi...
The Cenozoic history of crustal deformation, surface uplift, and erosion of the central Colorado Pla...
In northeastern Arizona, on the Colorado Plateau, landscapes associated with weakly cemented sandsto...
Presented here is the first comprehensive late Quaternary alluvial stratigraphic record from desert ...
The causal mechanisms for the onset and patterns of post-Miocene erosion of the western Great Plains...
Soils in the arid to semi-arid piedmont landscapes of central New Mexico were examined in order to e...
In order to evaluate potential effects of tectonics and climate change on the behaviour of the axial...
There is little doubt that climate is an important parameter affecting the shape of the Earth`s surf...
The East Potrillo Mountains are located just north of the U.S.-Mexico border in southwestern Dona An...
Apatite thermochronology is, in principle, uniquely suited to document the Cenozoic erosion of the C...
Stratigraphic records in Middle Park in north-central Colorado provide evidence for the late Quatern...
Predictions of how ecosystems may respond to future climatic changes must be based on an understandi...
Relationships between river incision, aggradation, and widening are investigated in a ∼5 km reach of...
Tectonic geomorphology of the Toroweap Fault, western Grand Canyon, Arizona: implications for transg...
Due to the character of the original source materials and the nature of batch digitization, quality ...
AbstractThe Pajarito fault forms the western margin of the Rio Grande rift in north-central New Mexi...
The Cenozoic history of crustal deformation, surface uplift, and erosion of the central Colorado Pla...