Late quaternary geomorphology and geoarchaeology of a segment of the Central Mimbres River Valley, Grant County, New Mexico /
A. D. II 50 A. D. 1300) is believed to be associated with
| Main Author: | |
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| Format: | Thesis eBook |
| Language: | English |
| Published: |
[Place of publication not identified] :
[publisher not identified] ;
1996.
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| Subjects: | |
| Online Access: | Link to OAKTrust copy |
| Summary: | A. D. II 50 A. D. 1300) is believed to be associated with analyzing the soils and sediments in more detail to and duration of soil formation. answered because of the absence of reliable absolute ages at the end of the Classic Mimbres Period could not be capped by a welldeveloped soil (S 1) believed to be of composed of three major depositional units (II, III, and expanding the alluvial history to other segments of the for the deposits. Future research should focus on geomorphic map and generalized geologic cross section of identified along a segment of the central Mimbres River IV) each capped with a soil (S2, S3, and S4 Mimbres River and its side drainages, collecting Mimbres-Mogollon, are buried in the fill of TI. A Pleistocene age. The younger Holocene terrace, TI, is provide more information about depositional environments question of the abandonment of the Mimbres River Valley radiocarbon samples to develop an absolute chronology, respectively). An Animas/Black Mountain Period site (ca. S3, and it is possible other sites, from Cliff/Salado to T2, is composed of one major depositional unit (1) and is the study area were also produced. Unfortunately, the Two terraces, a modem floodplain, and alluvial fans were Valley in Grant County, New Mexico. The oldest terrace, |
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| Item Description: | "Major subject: Geography". Vita. |
| Physical Description: | viii, 99 leaves : illustrations, maps ; 28 cm. Also available online. Issued also on microfiche from Lange Micrographics. |
| Bibliography: | Includes bibliographical references: pages 83-86. |