Sacred Earthen Architecture in the Northern Southwest: The Bluff Great House Berm

2002 ◽  
Vol 67 (4) ◽  
pp. 677-695 ◽  
Author(s):  
Catherine M. Cameron

This article reports on the excavation of a “berm”—an earthen mound that surrounds the Bluff Great House in southeastern Utah. Comparisons are made to Chacoan-era (A.D. 850–1150) great house mounds in Chaco Canyon and to other berms and mounds at great houses throughout the Chacoan region. Great house mounds in Chaco Canyon and berms outside Chaco Canyon are assumed to have been ritual architecture, and continuity in the use of mounded earth and trash as a sacred place of deposit is traced through time from the Pueblo 1 period to modern Pueblos. The Bluff berm does not seem to have been constructed as the result of ceremonial gatherings (as has been suggested for the great house mounds in Chaco Canyon), but there is intriguing evidence that it continued to be used into the post-Chacoan era (A.D. 1150–1300), perhaps as a result of a restructuring or revival of Chacoan ideas in the northern San Juan region. Examination of the spatial distribution of berms suggests that they are most common at great houses south and west of Chaco Canyon; the northern San Juan region, where Bluff is located, has far fewer such features, possibly because the revival of Chacoan ideas in this region was short-lived.

2007 ◽  
Vol 32 (4) ◽  
pp. 339-352 ◽  
Author(s):  
Catherine M. Cameron ◽  
Phil R. Geib

1944 ◽  
Vol 9 (4) ◽  
pp. 381-385 ◽  
Author(s):  
Frank C. Hibben ◽  
Herbert W. Dick

One of the activities of the University of New Mexico's 1939 field school at Chaco Canyon was a reconnaissance excavation in the vicinity of Largo Canyon, to the northeast of the Chaco, proper. This was a continuation of the survey and excavations of the past four seasons, as a part of the project for outlining chronologically and geographically the culture known as Gallina. The extent of the Gallina manifestation to the east and south has already been fairly accurately delineated, but its western and northwestern boundaries are unknown. Since the San Juan and Mesa Verde centers lie to the northwest, it was deemed imperative that the cultural connections in that direction be determined. Typical Gallina unit houses are common on the headwaters of the Largo and in the Llegua Canyon area which heads in the same region. The extremely rugged area lying between this district and the San Juan and Mesa Verde region, however, is not only difficult of access, but is practically unknown archaeologically.


1988 ◽  
Vol 53 (3) ◽  
pp. 582-592 ◽  
Author(s):  
Stephen A. Hall

Pollen analysis of woodrat (Neotoma) middens indicates that the local vegetation at Chaco Canyon and the regional vegetation of the San Juan Basin, northwestern New Mexico, have been shrub grassland since at least 10,600 years ago. Plant macrofossils in the same woodrat middens indicate that pinyon pine trees were present in the canyon during much of the Holocene, but low percentages of their pollen grains in both the middens and in adjacent alluvium suggest the trees were few, occurring as small stands or isolated individuals along canyon escarpments. The vegetation at Chaco Canyon during Anasazi times was an arid shrub grassland with a sparse escarpment population of pinyon and juniper. A climate-caused regional increase in pinyon at higher elevation sites occurred approximately at the time of Puebloan abandonment.


2020 ◽  
Vol 85 (2) ◽  
pp. 331-346
Author(s):  
Christopher H. Guiterman ◽  
Christopher H. Baisan ◽  
Nathan B. English ◽  
Jay Quade ◽  
Jeffrey S. Dean ◽  
...  

The iconic Plaza Tree of Pueblo Bonito is widely believed to have been a majestic pine standing in the west courtyard of the monumental great house during the peak of the Chaco Phenomenon (AD 850–1140). The ponderosa pine (Pinus ponderosa) log was discovered in 1924, and since then, it has been included in “birth” and “life” narratives of Pueblo Bonito, although these ideas have not been rigorously tested. We evaluate three potential growth origins of the tree (JPB-99): Pueblo Bonito, Chaco Canyon, or a distant mountain range. Based on converging lines of evidence—documentary records, strontium isotopes (87Sr/86Sr), and tree-ring provenance testing—we present a new origin for the Plaza Tree. It did not grow in Pueblo Bonito or even nearby in Chaco Canyon. Rather, JPB-99 originated from the Chuska Mountains, over 50 km west of Chaco Canyon. The tree was likely carried to Pueblo Bonito sometime between AD 1100 and 1130, although why it was left in the west courtyard, what it meant, and how it might have been used remain mysteries. The origin of the Plaza Tree of Pueblo Bonito underscores deep cultural and material ties between the Chaco Canyon great houses and the Chuska landscape.


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