Cannibalism, Warfare, and Drought in the Mesa Verde Region during the Twelfth Century A.D.

2000 ◽  
Vol 65 (1) ◽  
pp. 145-178 ◽  
Author(s):  
Brian R. Billman ◽  
Patricia M. Lambert ◽  
Banks L. Leonard

AbstractThe existence of cannibalism has emerged as one of the most controversial issues in the archaeology of the American Southwest. In this paper, we examine this issue by presenting the results of our investigation at 5MT10010, a small early Pueblo III habitation site in southwestern Colorado. Battered, broken bones from seven individuals were discovered in two adjacent pithouses at 5MT10010. Mixed and incomplete remains of four adults and an adolescent were recovered from the floor and ventilator shaft of one pithouse; the remains of two subadults were found on the floor and in various subfeatures of the second. Cut marks and percussion scars implicate humans in the disarticulation and reduction of these bodies. Evidence of heat exposure on some bone fragments and laboratory analyses of a human coprolite recovered from one of the pithouses support the interpretation that people prepared and consumed human body parts. The discovery of disarticulated human remains at 5MT10010 is one of a number of similar finds in the northern Southwest. Analysis of cases from the Mesa Verde region indicates a sharp increase in cannibalism around A.D. 1150, a time of drought and the collapse of the Chaco system. The causes, consequences, and nature of this apparent outbreak of cannibalism are examined in light of 5MT10010 and other recent finds.

2002 ◽  
Vol 67 (1) ◽  
pp. 137-144 ◽  
Author(s):  
Robert J. Speakman ◽  
Hector Neff

For decades archaeologists have struggled with the problem of accurately determining organic and mineral-based paints in pottery from the American Southwest. Using Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry (LA-ICP-MS), we have developed a simple and cost-effective method that permits classification of painted surfaces into mineral and organic-based categories. By applying this method to Mesa Verde and Mancos Black-on-white pottery from the Mesa Verde Region, we were able to distinguish easily between mineral and organic-based paints. Preliminary data also suggest that multiple sub-groups of mineral-based paints exist within these ceramic types, indicating that multiple recipes for manufacturing paint may have been employed by prehistoric potters from this region.


2010 ◽  
Vol 75 (3) ◽  
pp. 497-525 ◽  
Author(s):  
Kristin A. Kuckelman

Archaeologists in the Mesa Verde region of the American Southwest have long sought the catalysts of the complete depopulation of the region by Pueblo farmers in the late thirteenth century. Ten years of excavations by the Crow Canyon Archaeological Center at Sand Canyon Pueblo, a large village that was occupied from approximately A.D. 1250 to 1280, yielded abundant data regarding the depopulation of the village and shed new light on causes of this intriguing regional emigration. Comparative analyses of faunal and archaeobotanical remains from middens vs. abandonment assemblages reveal a shift from farming to hunting and gathering that coincided with the onset of the Great Drought about A.D. 1276. Osteological and taphonomic analyses of human remains found in abandonment contexts reveal details of an attack during which many residents were killed and that ended the occupation of the village. These findings from Sand Canyon Pueblo suggest that climate-induced food stress and consequent violent conflict contributed to the depopulation of the Mesa Verde region in the late A.D. 1200s.


1997 ◽  
Vol 62 (4) ◽  
pp. 664-681 ◽  
Author(s):  
Richard H. Wilshusen ◽  
Melissa J. Churchill ◽  
James M. Potter

More than 20 examples of probable prehistoric water basins with minimum storage capacities of 10,000–25,000 gallons of water are known in the Mesa Verde region of the American Southwest. The temporal placement of these artificially constructed basins, their exact uses, and their importance as public architecture have been poorly understood. We summarize the general literature on these features, give a detailed account of the excavation results of a dam and basin that we tested and dated, and then synthesize all available data from the gray literature on prehistoric water basins in our area. We argue that water basins and reservoirs in the northern Southwest typically stored domestic water for particular communities and that the first evidence of these public features is probably associated with Chaco-era communities. These features represent early experiments with large-scale water conservation and suggest a long-term commitment to locales by specific communities. Their locations along the canyon edges foreshadow shifts in settlement and increased water conservation strategies that become more pronounced in the later Great Pueblo-period villages-the last villages in this area before the migration of Puebloan people to the south after A.D. 1280.


2018 ◽  
Vol 204 ◽  
pp. 07020
Author(s):  
Didin Mujahidin ◽  
Poppy Puspitasari ◽  
Djoko Kustono

Bone implants are a tool used as a support of body parts, and bone support in cases of fractures. Scaffold, plate, bone screw, and some other tools can be used in combination to support and fill the connection between broken bones before the tissue grows. The most commonly used implant materials are Titanium, Stainless steel and ceramics, which are very common in the use of medical devices. Biocompatible materials are taken into consideration when planning a medical device. This research intended to know the durability of duralumin material as the latest implant material, as the development and breakthrough in health world. The research methodology used in this study was the optimization in Ansys software 18.1. The implants were designed, the material strength was determined and then given imposition with 6 variations (450 N, 550 N, 650 N, 750 N, 850 N and 950 N). The optimization was a method that identified mat erial strength including Equivalent Stress, Shear Stress and Total Deformation of duralumin material as implant materials with loading variations. Based on the results of the research, the duralumin material had a equivalent stress of 475,700 Pa which was higher than 950000 Pa for ZnO-Al2O3 implants, while the duralumin shear stress of 1084500 Pa was higher than 313720 Pa for ZnO-Al2O3 implants. When compared with titanium implants, the highest equivalent stress of 150000 Pa duralumin material had a higher compression stress than titanium. The highest shear stress of titanium 4358.1 Pa means an implant with a higher shear duralumin material of titanium. Whereas if it was compared to stainless steel with voltage press 564000000 Pa, then the duralumin’s pressure was getting lower. Material hardness affects resistance to wear and tear. Duralumin material hardness was lower than Titanium and ZnO-Al2O3, so total Duralumin deformation (elasticity) was higher than Titanium and ZnO-Al2O3.


2019 ◽  
Vol 85 (1) ◽  
pp. 152-170 ◽  
Author(s):  
James L. Moore ◽  
Eric Blinman ◽  
M. Steven Shackley

Arakawa and colleagues (2011) use temporal changes in obsidian source patterns to link the late thirteenth-century abandonment of the Mesa Verde region to Ortman's (2010, 2012) model of Tewa migration to the northern Rio Grande. They employ Anthony's (1990) concept of reverse migration, inferring that an increase in Mesa Verde–region obsidian from a specific Jemez Mountain source reflects the scouting of an eventual migration path. Weaknesses of this inference are that only obsidian data from the Mesa Verde region were used in its development and that the model does not consider the complexities of previously documented patterns of settlement and stone raw material use in the northern Rio Grande. By examining source data from parts of northwestern and north-central New Mexico, we find that the patterning seen in the Mesa Verde obsidian data is widespread both geographically and temporally. The patterns are more indicative of a change in acquisition within a down-the-line exchange system than a reverse migration stream. Population trends on the southern Pajarito Plateau, the probable source of the acquisition change, suggest ancestral Keres rather than Tewa involvement in thirteenth-century obsidian distribution.


KIVA ◽  
2013 ◽  
Vol 78 (3) ◽  
pp. 279-312 ◽  
Author(s):  
Fumiyasu Arakawa
Keyword(s):  

KIVA ◽  
2011 ◽  
Vol 77 (1) ◽  
pp. 11-31
Author(s):  
JEANNETTE L. MOBLEY-TANAKA
Keyword(s):  

Sign in / Sign up

Export Citation Format

Share Document