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Bulletin of the Geological Society of America, 1990
The Plio-Pleistocene Puye Formation, north-central New Mexico, contains >15 km 3 of volcaniclastic alluvial sediments deposited in response to rift-margin volcanism associated with the later evolution of the Tschicoma volcanic center, northeastern Jemez Mountains.
DAMON B. WARESBACK, B. N. TURBEVILLE
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The Plio-Pleistocene Puye Formation, north-central New Mexico, contains >15 km 3 of volcaniclastic alluvial sediments deposited in response to rift-margin volcanism associated with the later evolution of the Tschicoma volcanic center, northeastern Jemez Mountains.
DAMON B. WARESBACK, B. N. TURBEVILLE
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Biological Invasions, 2021
Salmonid introductions for sport fishing and, more recently, for farming, have had a large impact on freshwater ecosystems in many regions worldwide. In Patagonia, both activities have contributed to the colonization of freshwater systems particularly by species such as Brown Trout (Salmo trutta) and Rainbow Trout (Oncorhynchus mykiss).
Aliro Manosalva +2 more
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Salmonid introductions for sport fishing and, more recently, for farming, have had a large impact on freshwater ecosystems in many regions worldwide. In Patagonia, both activities have contributed to the colonization of freshwater systems particularly by species such as Brown Trout (Salmo trutta) and Rainbow Trout (Oncorhynchus mykiss).
Aliro Manosalva +2 more
exaly +2 more sources
Pedestal rocks in the Pliocene Puye Formation, New Mexico
Sedimentary Geology, 1986Abstract Pedestal rocks generally form in sandstone/shale terrains, with differential erosion producing a sandstone cap on a shale base. A different type of pedestal rock occurs in the late Pliocene Puye Formation in north-central New Mexico. Here, coarse conglomerate forms the base, and large, detrital boulders form the cap rocks.
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Journal of Volcanology and Geothermal Research, 1989
Abstract The Plio-Pleistocene Puye Formation, north-central New Mexico, is a 200-km2 volcanogenic alluvial fan shed eastward from the Tschicoma volcanic center, part of the Jemez Mountains volcanic field. The fan contains > 15km3 of volcaniclastic material derived from closely spaced lava domes in the northeastern portion of the Tschicoma center ...
Stephen Self
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Abstract The Plio-Pleistocene Puye Formation, north-central New Mexico, is a 200-km2 volcanogenic alluvial fan shed eastward from the Tschicoma volcanic center, part of the Jemez Mountains volcanic field. The fan contains > 15km3 of volcaniclastic material derived from closely spaced lava domes in the northeastern portion of the Tschicoma center ...
Stephen Self
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Biologia PesqueraEn la presente investigación se estudió cuali y cuantitativamente el semen del puye (Galaxias maculatus). Para ello se capturaron especímenes adultos (6,24 ± 0,84 cm de longitud estándar) de aguas límnicas del Sur de Chile y luego fueron mantenidos en cautiverio.
Iván Valdebenito +5 more
openaire +2 more sources
QUATERNARY FAULTING ON THE PUYE FAULT ZONE, ESPAÑOLA BASIN, NEW MEXICO
Geological Society of America Abstracts with Programs, 2023Richard W Briggs
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