2 edition of Pleistocene molluscan faunas and physiographic history of Pecos Valley in Texas found in the catalog.
Pleistocene molluscan faunas and physiographic history of Pecos Valley in Texas
Dr. A. Byron Leonard
Includes bibliographical references (p. 29) and index.
|Statement||by A. Byron Leonard and John C. Frye.|
|Series||Report of investigations / Bureau of Economic Geology, University of Texas ;, no. 45, Report of investigations (University of Texas. Bureau of Economic Geology) ;, no. 45.|
|Contributions||Frye, John Chapman, 1912-|
|LC Classifications||QE167 .T42 no. 45|
|The Physical Object|
|Pagination||42 p., 4 leaves of plates :|
|Number of Pages||42|
|LC Control Number||62064020|
Texas Memorial Museum. A new larger species of Sthenodectes is based on two well preserved skulls and other material from the late Bridgerian or early Uintan (middle or late Eocene) of the Agua Fria area in Trans-Pecos Texas. It was derived from the Pecos River valley and varies in thickness and particle size from a thin veneer of sandy loam in the southwest to a thick deposit of clay loam in the northeast (Reeves ; Holliday a). The Pleistocene lake deposits underlie, are interbedded with, or are inset against these eolian sediments (fig. ).
PECOS RUINS edited by David Grant Noble Pecos Pueblo was an important focus of Peublo culture for hundreds of years for Europeans arrived in the Southwest. It was a strategic trading center for the Plains Indians, central to the Pueblo Revolt against the Spanish in , and later an important stop for merchants on the Santa Fe : Paperback. Buda Limestone (Early Cretaceous) at surface, covers 2 % of this area. Buda Limestone; Eastern part of Trans-Pecos and High Plains and Western part of Trans-Pecos and North, central, and south Texas including Quaternary for all of west Texas.
The Pecos River has avoided some of the challenges faced by the state’s other waterways. But it has not been spared from the ecological changes brought by . Pecos NHP is 6, acres in size and lies in the Upper Pecos River Valley east of Santa Fe, New Mexico. The park’s predominant vegetation is pinyon-juniper woodland. Other habitats include grassland areas, riparian habitat along the Pecos River and Glorieta Creek, .
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RID. Pleistocene Molluscan Faunas and Physiographic History of Pecos Valley in Texas - Downloadable PDF. Part Number RID - Downloadable PDF. Get this from a library. Pleistocene molluscan faunas and physiographic history of Pecos Valley in Texas.
[A Byron Leonard; John C Frye]. RI Pleistocene Molluscan Faunas and Physiographic History of Pecos Valley in Texas, by A. Leonard and J. Frye. 42 p., 4 figs., 4 plates, ISSN. Late Pleistocene Amphibians and Reptiles of the Clear Creek and Ben Franklin Local Faunas of Texas.
Journal of the Graduate Research Center, SMU, 31(3). Leonard, A.B. and J.C. Frye (). Pleistocene Molluscan Faunas and Physiographic History of Pecos Valley in Texas. Bureau of Economic Geology, Report of Investigations - Number LATE CENOZOIC MOLLUSCAN FAUNAS FROM HIGH PLAINS paleontologic description is limited to the mollusks, the faunal interpretations are synthetic.
Earlier work on the various faunas is summarized under the description of each. The history of this study may be noted here, however. As a member ofCited by: History. The river played a large role in the exploration of Texas by the the latter half of the 19th century, "West of the Pecos" was a reference to the rugged desolation of the Wild Texas storekeeper, bartender, and justice of the peace, Roy Bean, a native of Kentucky, was often described as "The Only Law West of the Pecos", a phrase made popular from the syndicated Mouth: Rio Grande.
New Mexico Geological Society Guidebook, 57PLEISTOCENE VERTEBRATES FROM SOUTHEASTERN NEW MEXICOth Field Conference, Caves and Karst of Southeastern New Mexico,p. PLEISTOCENE VERTEBRATES FROM SOUTHEASTERN NEW MEXICO GARY S.
MORGAN AND SPENCER G. LUCAS New Mexico Museum of Natural History, Mountain File Size: 1MB. Early Tertiary Vertebrate Faunas Big Bend Area Texas-Pecos Texas: Brontotheriidae Paperback – January 1, See all formats and editions Hide other formats and editions.
Price New from Used from Paperback, January 1, "Please retry" Manufacturer: Texas Memorial Museum. PDF | Rivaer gravels in the Pecos Valley just north of Roswell, Chaves County, New Mexico, produced fossil vertebrates identified as Gopherus of. | Find, read and cite all the research you.
The Cenozoic Pecos Alluvium aquifer is located in the upper Pecos River Valley of western Texas (fig. This alluvium aquifer underlies parts of Crane, Ector, Loving, Pecos, Reeves, Upton, Ward, and Winkler Counties and extends north into New Mexico. The Cenozoic Pecos Alluvium occurs in a region with an arid climate characterized by.
from a Pleistocene (Rancholabrean) site in the Pecos River valley of southeastern New Mexico/ southwestern Texas Gary S. Morganand Spencer G. Lucas, New Mexico Museum of Natural History, Mountain Road NW, Albuquerque, NM FIGURE 1—Map of part of southeastern New Mexico and southwestern T exas.
The. Eight faunas from the central and southern Rio Grande Valley are medial Blancan in age ( Ma), including the Pajarito and Belen faunas from the Albuquerque basin, the Arroyo de la Parida LF.
Parks › New Mexico › Pecos › History & Culture Pecos National Historical Park preserves o years of rich cultural history including Pecos Pueblo and Spanish mission ruins, the ruts of the Santa Fe Trail, the Forked Lighting Ranch and the Civil War Battle of Glorieta.
Within caves along the Pecos River in West Texas, you'll find mysterious ancient rock art known. The drawings could be more than 2, years old, and the names of their creators have been lost to. The Pecos Valley Aquifer is a major aquifer found in Far West Texas. Water bearing sediments include alluvial and windblown deposits in the Pecos River Valley.
These sediments fill several structural basins, the largest of which are the Pecos Trough in the west and Monument Draw Trough in the east. Groundwater flow. Texas Tech University, BoxLubbock, TX ABSTRACT-The mammals of the Carrol Creek local fauna, radiocarbon dated at 32, + YBP, were found in a late Pleistocene (Middle Wisconsin, Rancholabrean Land Mammal Age) deposit in Donley Co., Texas.
Thirteen of 17 taxa were at least tentatively identified to species. Neofiber. Strategraphic positions for the Candelaria local fauna (late Uintan), the Porvenir local fauna (early Chadronian), Little Egypt, and Airstrip local faunas (Chadronian) within the Vieja Group are given.
The Porvenir local fauna contains 32 genera in common with Chadronian faunas to the north and six genera in common with the Lapoint fauna. GEOLOGY, PHYSIOGRAPHY, AND GROUNDWATER RESOURCES Within the Basin and Range Province, the Earth's crust (and upper mantle) has been stretched up to % of its original width.
The entire region has been subjected to extension that thinned and cracked the crust as it was pulled apart, creating large faults. By the end of Pliocene time, about Ma, the Pecos fluvial system and its tributaries had buried their valleys and covered the divides that formerly separated them.
The cold, moist climate of the late Pleistocene, 70 to Ky, enabled the Pecos Slope, Pecos Valley, and Llano Estacado into West Texas to. Jules Marcou - Geology of North America; with two reports on the prairies of Arkansas and Texas, the Rocky Mountains of New Mexico, and the Sierra Nevada of California.
- Privately published, Zürich. pp., 7 plts. h.t. with fossils, 3 plts. h.t. with col. maps folding-out. Reduced orig. front cover pasted on endpaper, loose in provisional modern folder, text pages partly browned. Stratigraphic Occurrence and Correlation of Early Tertiary Vertebrate Faunas, Trans-Pecos Texas - Agua Fria-Green Valley Areas * John Andrew Wilson: Journal of Vertebrate Paleontology, Vol.
6, No. 4, (Dec. 24, ), pp. North American Mammal ages: Arikareean age = to mya Whitneyan age = to mya.Pleistocene molluscan faunas in central and southwestern Hokkaido (Morrowan) gastropods from the Magdalena Formation of the Hueco Mountains, Texas.
- Amer. Mus. Novit. ; 46 pp. 60 fig./phot. Orig. issue with libr. ticket taped to blanc corner of title page, otherwise very good. (Bivalvia: Pectinidae) off southeastern Tasmania.PECOS Pecos River, one of the major tributaries of the Rio Grande, rises on the western slope of the Santa Fe mountain range in Mora County, New Mexico (at 35°59' N, °33' W), and runs south through San Miguel, Guadalupe, De Baca, Chaves, and Eddy counties in New Mexico before it enters Texas just east of the th meridian.