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Irrigation canals from the Calchaqui valley (province of Salta, Argentina)

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Abstract

The archaeological site of Las Pailas, located in the north of the Calchaquí valley (province of Salta, Argentina), is one of the largest agricultural areas developed in the region during the Late Period (900-1430 CE) and the Inca Period (1430-1530 CE). The site consists of a residential area and an extensive area of cultivated land criss-crossed by a dense network of canals, both with and without stone lining, used for irrigation of the fields. This paper presents the results of the topographic contour and architectural mapping of the lined canals, located in a sector of the archaeological site. The canals have stone lining on their walls and ceilings, and most of them are below ground surface, covered by a layer of sediment. Larger and smaller canals distributed water from river intakes to cultivated fields. This required the development of a technical knowledge that included the control of slopes, the management of water flow velocities and discharge values, and the covering of pipes to avoid sediment accumulation and clogging. The analysis of the density of the canals suggests that the irrigation of the fields was a task of great importance for pre-Hispanic peasants.

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... The cultivated area follows the slope of the site, in a NE-SW direction, with altitude differences ranging from 2960 to 3380 m asl at the highest point. The entire surface is crossed by an irrigation network that distributes water throughout the fields (Páez and López, 2019). Parts of the canals are dug in the ground, without lining, while others have rocks on the sides and rooves to protect them from sedimentation and eventual clogging. ...
... Parts of the canals are dug in the ground, without lining, while others have rocks on the sides and rooves to protect them from sedimentation and eventual clogging. The network is composed of water intakes, including primary canals, approximately 1 m wide, and drainage canals, mostly ranging between 0.12 m and 0.23 m, which enter the fields irrigating the planted surface (Páez and Giovannetti, 2014;Páez and López, 2019). ...
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Documentary research combined with field study has made possible the reconstruction of the sociopolitical organization of the Late Prehispanic Chimu and Chimu-Inca polities of the North Coast of Peru. Many aspects of the management of the large-scale irrigation networks of the region are integrated into that organization. Rights to the water of a particular canal-and to the lands it watered-can be shown to have been vested in socio-political groups which occupied different hierarchical positions according the size of the canal. Maintenance, repair, and distribution of the water were carried out by these groups; there was no centralized state bureacracy to oversee hydraulic affairs. Understanding the organization of the canal system permits a series of hypotheses for the reconstruction of ancient territorial units and the organization of settlement patterns within them.
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In the Lake Titicaca Basin of the Andes, narratives of agricultural change have focused exclusively on a single innovation: raised fields. In this article, I examine macrobotanical remains and other archaeological datasets to elucidate a wider range of past farming practices that contributed to processes of agricultural change on the Taraco Peninsula, Bolivia, during the Formative Period (1500 B.C.E.-C.E. 500). This analysis reveals strong continuities in crop selection through time, with farmers gradually diversifying a basic set of cultigens-quinoa and tubers-but never abandoning them. Patterns in wild plant species indicate continuity in agropastoral land use up to the Late Formative Period (second century C.E.) when the unintended consequences of long-term tilling and camelid grazing transformed the botanical landscape into one that required a new set of practices to remove weeds and replenish nutrients to the soils. Examining how these practices and the farmers enacting them articulated with broader processes of demographic, environmental, and sociopolitical change reveals dynamic, multivariate courses of agricultural change even before the inclusion of raised fields.
Article
On the Calchaquí valley the setting of population in conglomerate sites was in IX-X A.D. After this, the population was concentrated on this main valley. The distribution of the greater sites suggests that population articulated spaces on the subsidiary basins for managing the accessibility to important agriculture areas and ways of interregional connection. To evaluate this proposal it is necessary among other aspects to deepen in the environmental features, resources areas, reminds of productive substructure of de secondary basins of the Calchaquí valley. From the point that basic production involves at least one space of local production and another larger and not necessarily continuous we analyze the river Molinos basin. The basin permanent flow and the soil formation make it the major of the Central Calchaquí River. Also to west it is a connection to Puna, to east to Calchaquí Valley and to its way to orient. For agricultural and livestock societies fertile soil it is of main importance. This area is scarce in this resources. Cartographic, satellite and aerial photography analysis allow to identify and measure productive spaces and productive substructure in Molinos River basin.
Article
Based on microfossil and soil data, we discuss a different methodological approach to agricultural and domestic archaeological studies, taking two Formative sites in the north-west Argentinian high valleys (province of Catamarca) as case studies, independently of traditional datasets and historical analogies. As a result of our investigations we not only recognised the vegetal species cultivated in ancient fields (dated to c. AD 800) but also distinguished some of the agricultural practices, such as crop rotation and alternation, use of animal fertilisers and irrigation resources, as well as the abandonment of the site. From this perspective, corral episodes could also be distinguished. In residential enclosures, we obtained results concerning activity areas, the definition of floors and the identification of reoccupations.
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Agricultural terraces in the Colca Valley of southern Peru facilitate the irrigation necessary for agriculture in this semiarid environment. Terrace expansion and contraction, in turn, are closely related to the availability of water. In the short term, households abandon terraces because of constraints in the system of water distribution. In the longer term, periodic droughts trigger water conservation practices which curtail expansion and lead to terrace abandonment. Cyclical patterns of terrace contraction and expansion suggest that repeated observations of land use over time are necessary for an understanding of agricultural intensification and deintensification. -from Author
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Theory linking labor inputs of irrigation agriculture to social organization is briefly reviewed. Labor input is distinguished into five tasks: construction, maintenance, allocation, conflict resolution, and organization of ritual. A sample of world communities is canvassed in search of structural variation. A rationale for studying these phenomena in a local, rather than a society-wide, context is presented. Types of ties of the locality with the larger system are explored. Several propositions about pervasive external linkages with local phenomena are presented. Millon's results, showing no relationship between size of irrigation system and centralization, are challenged. It is found that often irrigation management roles are embedded in other socially powerful roles rather than forming part of a specialized bureaucracy. Conditions for role embeddedness are explored.
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A research methodology for the study of prehistoric irrigation canals is suggested which uses detailed excavation and survey techniques to generate data suitable for analysis by the principles of open channel hydraulics. The results indicate that these principles were empirically understood, even when the question of transporting water down steep slopes is considered, and that prehistoric canal discharge was a function of the farmer's perception of the hydrology of the agricultural system. -Author
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During the last 20 years, research on the agricultural alternatives developed in the Central Andes and Mesoamerica has burgeoned, especially in the Maya area. Descriptions of ancient irrigation, raised fields, terracing, sunken fields, and other systems show that there was a wide range of complex systems in operation in many areas during various time periods. They were practised on various levels of complexity requiring corporate organisation of varying types.-J.Sheail
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Excavation of Aztec-period agricultural features at the sites of Capilco and Cuexcomate in Morelos, Mexico, provides new data on the construction, function, and significance of agricultural terraces in Late Postclassic central Mexico. Stratigraphic and chemical analyses of alluvial deposits associated with cross-channel terraces (“check-dams”) reveal that these features served an agricultural function. Terrace walls were built gradually in small increments, and associated sediments were created by alluvial deposition of eroding topsoil. These findings, together with demographic and social data from nearby excavated houses, suggest that Late Postclassic agricultural intensification was a household-level response to population pressure.
Article
The effect of climatic change on human and natural populations is most readily discernible in geographic locations where climate is a significant factor in limiting the range of activities. Today, as in the past, severe minimum temperatures at high altitudes limit the range of production of various crops in the Peruvian Andes. Periodic climatic cooling, as evidenced by the deposits from two recent glaciations, lowered the upper elevation limit of maize and significantly reduced the area available for its cultivation in the northern Mantaro River Valley. Paleoethnobotanical data from the same area suggest that during the most recent period of climatic cooling, less maize was produced compared to the warmer time periods that bracket this event. During the cooler phase, climatic constraints on maize production could have exacerbated already existing social tensions, perhaps leading to an increased establishment of more defensive settlements. This study shows how climate can affect human actions. This does not mean that climate dictated the major social and political changes seen in the archaeological record; but including environmental constraints and climatic change in discussions about the past can, given appropriate data, provide a more complete picture of cultural change.
Article
Similar forms of subsistence and social organization have emerged in different parts of the world in response to similar ecological, technological, and demographic factors. For example, moldboard plow agriculture evolved in many places as the result of high population density, availability of large domesticable animals, presence of wet and heavy soils, and such staples as wheat, barley, rye, and buckwheat, which required extensive land preparation and “considerable surface area to produce the food calories necessary to feed a family” (Pryor 1985:732). Wolf long ago (1957) noted that the colonial experience had helped to promote the development of closed, corporate communities in rural societies of Mesoamerica and Indonesia.
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The absolute chronology of the agricultural soil from organic matter has always been difficult to measure due to several reasons. In our work on the Prehispanic agriculture in the Calchaqui Valley – Argentina, however, an absolute chronology is necessary to distinguish the Inca prevalence of the previous agricultural structure. Instead of looking for a new dating methodology, we have used the 14C method trying to eliminate the error sources typical of soils. Thus, we have dated new types of agricultural structures, with the assumption that they would have worked as archaeological “seals”. In the present paper we show that the dating of the beginning of the use of the Prehispanic agricultural systems has been successful.
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This paper examines the hydraulic properties (i.e. velocity and discharge) of the main late prehistoric canals of the Moche Valley. Velocities, estimated from excavated canal sections using the Manning flow equation, are compared to tables of maximum permissible velocities and reveal that canals were constructed to transport water efficiently, but that on gradients steeper than 1:100 the Chimu and Inca engineers were unable to transport large discharges without severe erosional problems. Discharge estimates are compared with modern field requirements, using a known ethnographic watering cycle. This demonstrates that in almost every instance the channel size was of the same order of magnitude as that predicted from the requirements. The construction of the Inter-valley canal to bring water to the state lands in Moche was a technological disaster.