The Construction and Configuration of Anasazi Pebble-Mulch Gardens in the Northern Rio Grande

1995 ◽  
Vol 60 (3) ◽  
pp. 459-470 ◽  
Author(s):  
Dale R. Lightfoot ◽  
Frank W. Eddy

Rio Grande Anasazi in the fourteenth and fifteenth centuries A.D. mulched hundreds of garden-sized plots with pebbles to increase soil moisture, reduce erosion, extend the growing season, and increase crop yields. This paper reports on the construction and configuration of pebble-mulch gardens in New Mexico, focusing particularly on those in the Galisteo Basin. Surfaces adjacent to these gardens were scraped and pits were excavated to collect gravel, which was placed over garden surfaces in layers 5 to 11 cm thick. Gardens averaged 15 x 23 m in size, although both size and shape were highly variable, and they collectively covered an area of 41,000 m2 Although this unique agricultural strategy has been shown to be effective, construction was limited to sites with natural gravel deposits, pebbled surfaces inhibited the recycling of crop wastes, and such gardens never became as widely used as more traditional field forms.

2016 ◽  
Author(s):  
Travis W. Clow ◽  
◽  
Whitney M. Behr ◽  
Mark Helper ◽  
Peter Gold ◽  
...  

1990 ◽  
Vol 6 (4) ◽  
pp. 657-680 ◽  
Author(s):  
Charles E. Glass

Estimates of the probability of future earthquake activity are difficult to make in areas where historical seismicity may be low or absent, but where young fault scarps attest to recent or ongoing tectonism. Three non-Poisson models, a Weibull model, a Gaussian model and a lognormal model, are used to estimate the earthquake hazard for one such area, the northern Rio Grande Rift. This portion of the Rio Grande Rift displays numerous Holocene faults attesting to ongoing tectonism, but displays essentially no historical seismicity. The earthquake hazard for the Sangre de Cristo fault zone from Taos, New Mexico to Salida, Colorado calculated using these models is remarkably consistent (probability of at least one Mo = 7 earthquake in the next 50 years ∼ 2.5 × 10−3), with increased hazard for the Sangre de Cristo fault in north San Luis Valley (∼5.0×10−3) and near Taos (∼1.0×10−2) due to the long holding times along these segments.


KIVA ◽  
2007 ◽  
Vol 73 (2) ◽  
pp. 117-130 ◽  
Author(s):  
BRADLEY J. VIERRA ◽  
RICHARD I. FORD

Author(s):  
Benjamin J. Drenth ◽  
◽  
V.J.S. Grauch ◽  
Ren A. Thompson ◽  
Brian D. Rodriguez ◽  
...  

2012 ◽  
Vol 77 (3) ◽  
pp. 424-448 ◽  
Author(s):  
B. Sunday Eiselt ◽  
J. Andrew Darling

AbstractEconomic reforms introduced by the Bourbon Monarchy after A.D. 1750 ushered in an Hispanic social formation in the northern Rio Grande identified as Vecino. Aspects of Vecino gendered economy are examined through a detailed analysis of five ceramic assemblages from the Chama and Taos Valleys of New Mexico. Geochemical (NAA) and stylistic clues identify the ethnic identities of producers and their relationships to Vecino consumers. Evidence for ceramic production by Vecino women during the nineteenth century is evaluated on the basis of detailed paste analysis of plain and micaceous ceramics as well as the occurrence of pottery-producing tools and clay-cleaning debris. Analytical results reveal that Jicarilla women dominated the production of micaceous cook ware to supply Vecino kitchens. Implications for understanding Vecino economics and the constitution of female-based systems of economic value are considered.


1985 ◽  
Vol 5 (3) ◽  
pp. 217-233
Author(s):  
Gordon Bronitsky

The Pueblo IV period in the northern Rio Grande valley of New Mexico (AD 1200–1540) was one of increasing climatic and demographic variability. Analysis of certain chipped stone tools from Arroyo Hondo, New Mexico (LA-12) has provided an understanding of some of the means prehistoric populations in the region employed to cope with this variability, focusing on changes in productive strategy. A theoretical model of resource restriction is presented, derived from general ecological studies and recent research into the relationships between population growth and cultural change. Selected lithic data are used to test implications of the model. The results of these tests and their bearing on the general model are then discussed.


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