The Chuska Valley is a geographical region located in the northwestern portion of the U.S. state of New Mexico. Although identified as a "valley" in archaeological literature, the region encompasses the eastern slope of the Chuska Mountains, situated in their rain shadow.[1] Sitting atop the Colorado Plateau in the Four Corners region of the desert Southwest, it is near both Chacra Mesa and Chaco Canyon, which are noted for their Chacoan Anasazi ruins. The Chaco Slope is differentiated from the neighboring Gobernador Slope, Chaco Core, and Chaco Plateau by distinct surface water drainage patterns and geological formations. These regions were first labelled by archaeologist Gwinn Vivian.[2]
![](http://upload.wikimedia.org/wikipedia/commons/thumb/c/cc/ISS-64_Chuska_Mountains%2C_New_Mexico.jpg/300px-ISS-64_Chuska_Mountains%2C_New_Mexico.jpg)
Citations
editFagan, B (2005), Chaco Canyon: Archaeologists Explore the Lives of an Ancient Society, Oxford University Press, ISBN 0-19-517043-1
References
edit- ^ Vierra, Bradley J; Graves, William M (2014). "Movement, persistence and identity in the Southern Chuska Valley". Bridging the basin: Land use and social history in the southern Chuska Valley. Vol. 4. Statistical Research, Inc. OCLC 880909621. Archived from the original on 2023-07-28.
Most of the [Chuska] valley is situated along the eastern slope of the Chuska Mountains, within their rain shadow.
- ^ Fagan 2005, pp. 45–46.
36°12′N 108°42′W / 36.2°N 108.7°W