L'Associazione Liberi Viandanti propone un'interessante sintesi dell'arte spirituale andina, a cura di Gianmichele Ferrero et al. alla pagina
http://www.liberiviandanti.it/liberiviandanti/?page_id=12
"Il nostro corpo energetico possiede una serie di centri di percezione. Nella Tradizione andina sono chiamati Ñawis, che letteralmente significa “occhio”. Le potenzialità latenti relative agli Ñawis vengono attivate con precisi riti.
Ogni centro si connette con una qualità particolare di energia del cosmo.
Il Pujyu non è considerato un occhio vero e proprio, ma piuttosto una fonte. Si trova nel luogo dov’è la fontanella dei neonati e riceve il Kausay sotto forma di luce bianca
Il Siki ñawi, è situato sull’osso sacro, alla base della colonna vertebrale, ed è collegato con Unu, l’energia dell’acqua di colore verde.
Il Qosqo ñawi, nella regione ombelicale, è collegato a Allpa, l’energia della terra, che ha un colore rosso.
Il Sonqo ñawi, si trova sul petto all’altezza del cuore, ed è collegato ad Inti, il sole con una luce dorata.
Il Kunka ñawi, è nella zona della gola ed è collegato all’energia argentata di Wayra, il vento.
I due occhi fisici, anch’essi considerati centri, sono collegati il destro al potere della visione mistica e il sinistro al potere della visione magica.
Leggermente in alto fra le sopracciglia, è il Qanchis ñawi, che riceve normalmente un’energia viola proveniente dall’Hanaq Pacha, che da accesso al mondo della visione superiore ."
Friday, April 22, 2011
Kausay Puriy
L'Associazione Liberi Viandanti propone un'interessante sintesi dell'arte spirituale andina, a cura di Gianmichele Ferrero et al. alla pagina
http://www.liberiviandanti.it/liberiviandanti/?page_id=12
"La Tradizione andina prende il nome di Kausay Puriy che significa “imparare a camminare insieme all’energia vivente”. che significa “imparare a camminare insieme all’energia vivente”. L’energia vivente è sovrabbondante, tutti i fattori della realtà la emanano secondo la loro propria fisionomia. Semplicemente aprendoci a percepirla, il nostro essere può arrivare a nutrirsi a sufficienza per poter sviluppare le sue potenzialità più elevate.... La Tradizione andina supera il malinteso della dualità positivo-negativo interpretando l’energia scomoda di un’altra persona o la propria in termini di differenza di spessore e di gravità, usando il nome di samiy per l’aspetto leggero e sottile dell’energia e di per l’aspetto leggero e sottile dell’energia e di jucha per quello pesante. Tutti gli esseri viventi e gli elementi della natura producono samiy. Noi umani siamo gli unici a generare jucha quando ostacoliamo il flusso dell’energia vivente."
Molto interessante.
http://www.liberiviandanti.it/liberiviandanti/?page_id=12
"La Tradizione andina prende il nome di Kausay Puriy che significa “imparare a camminare insieme all’energia vivente”. che significa “imparare a camminare insieme all’energia vivente”. L’energia vivente è sovrabbondante, tutti i fattori della realtà la emanano secondo la loro propria fisionomia. Semplicemente aprendoci a percepirla, il nostro essere può arrivare a nutrirsi a sufficienza per poter sviluppare le sue potenzialità più elevate.... La Tradizione andina supera il malinteso della dualità positivo-negativo interpretando l’energia scomoda di un’altra persona o la propria in termini di differenza di spessore e di gravità, usando il nome di samiy per l’aspetto leggero e sottile dell’energia e di per l’aspetto leggero e sottile dell’energia e di jucha per quello pesante. Tutti gli esseri viventi e gli elementi della natura producono samiy. Noi umani siamo gli unici a generare jucha quando ostacoliamo il flusso dell’energia vivente."
Molto interessante.
Hands on earthworks
Earthworks near Titicaca Lake
These earthworks are known as "raised fields" and "waru-warus".
Let us rotate a part of the image and enhance it.
A "hand"?
More on waru-waru
arXiv:1009.4602 [pdf] Geoglyphs of Titicaca as an ancient example of graphic design, Amelia Carolina Sparavigna
Solar power without solar cells - physicsworld.com
"Physicists in the US believe that it is possible to generate solar power without solar cells. Their "optical battery" idea, which would involve performing the energy conversion inside insulators rather than semiconductors, could make for a far cheaper alternative energy source than existing solar-cell technologies."
Solar power without solar cells - physicsworld.com
The Titicaca basin: a paradigmatic region for multidisciplinary studies
The Titicaca basin: a paradigmatic region for multidisciplinary studies
From the point of view of archaeological/anthropological studies, besides of course the researches on the Tiwanaku area with its monumental remains, the “raised fields” are quite important. This system of fields is an old technique of soil and water management, consisting of a series of earthworks on which crops can grow, surrounded by water canals. A known benefit of this system is the frost mitigation during the night, avoiding the damage of crops. An interesting anthropological paper was recently published, approaching the "raised fields" of Titicaca lake in the framework of the organization of ancient intensive farming, comparing the “topdown” and “bottom-up” perspectives [1]. The "top-down" approach is that considering the development of intensive farming and its social organization as attributed to the rule action of a centralized government. The "bottom-up" instead is viewing an intensive farming as the incremental work of local communities or kin-based groups. The authors analysed in particular the Katari Valley [1], near the lake in Bolivia, on a long-term perspective covering 2500 years. They determined that the rural organization changed greatly over time in relation to changing socio-political conditions: that is the local communities played dynamic roles in the development and organization of raised field farming, but growth and ultimate recession were locked to the consolidation and decline of the Tiwanaku state. In fact, the authors are proposing the interesting conclusion that the top-down/bottomup dichotomy is overdrawn.
In [1], we read that the top-down interpretation has roots in a Western social thought, commonly attributing the development of large-scale farming and irrigation systems to centralized governments and nascent states. And in fact, from this point of view, it is paradigmatic the Roman Empire, with its road and hydraulic engineers, where the central government organized the construction and maintenance of roads, aqueducts and also entertainment monumental places. Recent alternative perspectives emphasize that cultural creativity and political power was also the product of local groups, not only the product of central governments: that is, a large-scale economicproduction can be yielded by local kin-based groups, where elites or leaders coordinated such activities [1-3].
On raised fields, “top-down” versus “bottom-up” interpretations have been proposed [4-6]. Proponents of both interpretations argue that intensive production was highly effective in the Titicaca region: in the top-down interpretations, intensive production was driven by the impetus of a centralized state government, whereas in bottom-up interpretations, it was locally developed and organized. As reported in Ref.1, “determining who developed and managed intensive production in any specific case and with what technologies and resources requires rigorous interdisciplinary collaboration and empirical research“. It is clear that only multidisciplinary researches will be able to solve the open questions about Titicaca, that, as reported in [1], are the following: When were raised fields built and by whom? When and why were they abandoned? Did raised fields require state management, or were they the exclusive domain of local communities?
In [1], the researchers focussed on an area in Bolivia on a long-term (ca. 2500 years) characterization of rural society and production dating from the emergence of complex societies until European colonization. The intensive raised field system adapted its predominant production to economic demands and socio-political conditions [1]. Based on research in the northwest Titicaca basin, near Huatta, Peru, Erickson [1,5] proposed that the raised field agriculture developed out of the knowledge and skills of communities and kin-based social groups, or “ayllus“, who survived the subjugation by Andean states. Erickson ([1,7], p. 315) points out that, raised field agriculture “differs... in that there is no necessarily inherent need for large-scale cooperation, in the construction, use, nor maintenance of the system” and concluded that “to suppose that raised field farming could only be planned, executed and maintained by the highly centralized state is to disregard the rich agricultural knowledge and organizational potential of the Andean farmer.” ([1,5], p. 413) Of course, other researchers disagree with this conclusion.
Among the open questions, it remains that on when the raised field system was firstly developed. The debate then centers on the relationship between settlements and raised fields and on the chronology of raised field construction and use. Erickson ([1,7], pp. 377–380) proposes two phases of raised-field construction in the north-western basin of Titicaca: First Phase, dating to the Early and Middle Formative periods (1500–200 BC); and Second Phase, dating to the post-Tiwanaku period [1,7]. In this chronological scheme, raised fields fell into disuse during the intervening Tiwanaku culture. It seems then that the period of growth of the raised fields in Peru is different from that of the opposite region near Tiwanaku, as in a counter-phase phenomenon.
From the analysis of the Google Maps, I have clearly observed that the system of raised fields, canals and artificial ponds in the Peruvian region of Titicaca contains peculiar area where the earthworks form geoglyphs [8-13]. The geoglyphs seems to represent animals (may be, totemic animals), whose eyes are sometimes crated by artificial ponds. In a case, we see that the geoglyphs on the plain land are strongly connected with the terraced hills: in fact, proposing the geoglyphs of Titicaca as an ancient graphic system based on artificial landforms [9]. Who is writing, A.C. Sparavigna, considers that the geoglyphs (signs on the land) were created to mark the land of specific communities and that there was a strong connection between the agricultural system and the worship and burial places of Titicaca. These are personal conclusions coming from inspecting the satellite imagery of Google Maps [8]. It would be fundamental to have high resolution satellite images of all the basin, including the lagoons, to understand the extension of the agricultural system.
About the agricultural and meteorological studies, a quite interesting paper on the management of this system and on the physical process-based models is Ref.[14]: this paper proposed a model to explain the role played by the canals in the nocturnal heat dynamics and the cold mitigation process. This model consists of a two-layer transfer scheme with a vegetation layer and a substrate layer representing the canals. The calculations of Ref.14 show that the presence of a heat flux emanating from the canals and a corresponding water condensation on the crop, are both contributing to mitigate the environmental conditions, avoiding the crops to be frozen.
Another study [15] is about the prehistoric diets, including analysis of stable isotope data from cooking pots, plants, animals and human teeth that have been collected by the Taraco Archaeological Project working in the Titicaca Basin of Bolivia. It is peculiar the analysis of the archaeological fish samples to understand their role in the diet of the Formative Period inhabitants of the southern Lake Titicaca Basin. According to the researchers, to understand the role of ichthyic resources in the human history, it is necessary to analyse the ecology of the fish from their muscle, bone and scales, since muscle is rarely preserved in archaeological contexts, whereas bone and scales are. For this reason, the researchers investigated the modern fish specimens from Lake Titicaca to compare with archaeological fish remains. The physical modelling of this ancient agricultural system and the relevance of fishes in local diets, have to be considered in the framework of the paleoclimatic researches. This is important because the knowledge of the past climate (dry or wet) could help in evaluating the extension of the agricultural system and the amount of ichthyic resources of the lake.
In general, the study of lacustrine records is considered useful for understanding the mechanisms and effects of climate change. This is why Lake Titicaca is an important site for paleoclimatic research in the South American tropics because of the evidence for major lake level changes in the late Quaternary ([16], and references therein). The lake has an outlet, the Rio Desaguadero, but today, the most of the water is lost by the lake due to evaporation. This means that the lake is a nearly closed basin and this fact is increasing the sensitivity of the hydrologic mass balance of the lake to climate change. In [16], the research was performed by means of seismic stratigraphy: this analysis indicates that late-Quaternary lake levels have varied significantly, most likely because of climatic change. The seismic data used in conjunction with sediment core data indicate that there is a basin wide stratigraphic marker, most likely due to volcanic ashes.
According to Ref.17, South America has a scarcity of sites with century-scale paleoclimate data sets, but these data are extremely important because of the El Niño/Southern Oscillation events (ENSO), the migrations of the intertropical convergence zone (ITCZ) and the presence of the vast Amazon basin. According to [17], it is the Lake Titicaca drainage basin and its associated altiplano endorheic system, in particular the nearby alpine glaciers, that are containing important paleoclimate records. In [17], the researchers are describing a finely resolved record of lake-level change driven by climatic variability over the past 3500 years. The paper reports evidence that suggests a rapid lake-level rise of 15 to 20 m about 3500 years before present, and several century-scale low stands at 2900–2800, 2400–2200, 2000–1700, and 900–500 cal yr before present. These findings improve the knowledge of the timing, duration, and magnitude of variations in the precipitation–evaporation balance of the South American altiplano during the late Holocene. The study is based on radiocarbon chronologies necessary to resolve century-scale dynamics of precipitation–evaporation variations on the altiplano. In Ref.18, researchers found two major dust events reaching maximum intensity at A.D. 600 and 920. They note that the dust could have been produced by the combination of extensive use of agricultural raised fields and the exposure of large areas of lake sediment during the periods of lowlake stands. According to [17], the peaks in dust content correspond with periods of major raisedfield activity by the Tiwanaku civilization [19].
According to Ref.17, South America has a scarcity of sites with century-scale paleoclimate data sets, but these data are extremely important because of the El Niño/Southern Oscillation events (ENSO), the migrations of the intertropical convergence zone (ITCZ) and the presence of the vast Amazon basin. According to [17], it is the Lake Titicaca drainage basin and its associated altiplano endorheic system, in particular the nearby alpine glaciers, that are containing important paleoclimate records. In [17], the researchers are describing a finely resolved record of lake-level change driven by climatic variability over the past 3500 years. The paper reports evidence that suggests a rapid lake-level rise of 15 to 20 m about 3500 years before present, and several century-scale low stands at 2900–2800, 2400–2200, 2000–1700, and 900–500 cal yr before present. These findings improve the knowledge of the timing, duration, and magnitude of variations in the precipitation–evaporation balance of the South American altiplano during the late Holocene. The study is based on radiocarbon chronologies necessary to resolve century-scale dynamics of precipitation–evaporation variations on the altiplano. In Ref.18, researchers found two major dust events reaching maximum intensity at A.D. 600 and 920. They note that the dust could have been produced by the combination of extensive use of agricultural raised fields and the exposure of large areas of lake sediment during the periods of lowlake stands. According to [17], the peaks in dust content correspond with periods of major raisedfield activity by the Tiwanaku civilization [19].
As reported in Ref.17, during an on-site travel in the years 1995 and 1996, researchers observed a several-meter decline in lake level that exposed very large areas of totora beds and lake sediment, that were quickly used for agricultural purposes. Time series of the yearly rise for the years 1915 to 1981 have been investigated: the relative spectral density clearly shows peaks with periods of 10.6 and 2.4 years [20]. Let us consider that the level of the lake is also oscillating during the year. In Ref.21, it is claimed that the study of the past climatology of Peruvian altiplano demonstrated that the emergence of agriculture (ca. 1500 B.C.) and the collapse of the Tiwanaku civilization (ca. A.D. 1100) coincided with periods of abrupt and profound climate change. Archaeological evidence establishes spatial and temporal patterns of local agriculture. Prior to 1500 B.C., aridity in the altiplano precluded intensive agriculture. According to Ref.21, during a wet period from 1500 B.C. to A.D. 1100, the Tiwanaku civilization and its immediate predecessors created agricultural methods that stimulated the population growth, with corresponding large human settlements. A prolonged drier period (ca. A.D. 1100–1400) caused the decline of food production, the fields were abandoned and the cultural system collapsed. An analogue detailed study of the Peruvian part of the Lake could be very important to understand the role of climate on the raise of Colla-Sillustani civilization and its connection with Inca civilization, and, of course of previous human settlements. Let us remember that human gatherers are found both North and South of Lima, Peru, as early as 8000 BC. Mountain civilizations were Kotosh (2000 BC), Tiwanaku-Huari 700AD, Collas-Sillustani (Titicaca Lake, 1100AD) and finally the Inca culture 1532 (AD): all these cultures had influences in the Inca culture, including the apparently autochthonous Titicaca Lake (Aymara-speaking) cultures [22]. The Aymara language is considered more ancient than the Inca language and has not only been found in the Titicaca Lake area but also in mountains close to Lima. Aymara-speaking people widespread throughout the Peruvian area: the Quechua language was imposed later by the Inca conquest and also by the Spanish conquerors. Aymara-speaking people were long ago established around Titicaca Lake area in the so called “Collao” area (see [22], and reference therein). According to [22], a tribe coming from this lake area set out for Cuzco, where they established, they spoke Quechua and were called “Inga” or “Inca” people.
 |
| Figure 1: Level of the Titicaca Lake as a function of time. Image adapted from Ref.23. |
In Fig.1, the behaviour of the level of the lake is shown as a function of time [23], we can see clearly the oscillation between dry and wet periods. Other studies on late Pleistocene/Holocene paleoclimates of the Bolivian Altipiano using the analysis of ostracod content, palynology, sedimentology and radiocarbon dating have been proposed [24].
Let us conclude with a discussion on satellite imagery again, connected with the dry and wet periodic behaviour of the local climate. As told in Ref.17, as the lake level declines, the soil is quickly used for agricultural purposes. In observing the Google Maps of the Umayo and Machacmarca Lagoons, we can see that the surface, that is actually subsided under the water, was once covered by raised fields. The lagoons too were subjected to the dry-wet oscillation. As previously told, an analysis as in Ref.17 of the two lagoons could give information on prehistoric human settlements. Let us consider that Sillustani, the burial place of Collas, is a peninsula of the Umayo Lagoon [13] . Near the shore of the Titicaca Lake we see (Figure 4) an area densely covered by the earthworks of the raised fields.
 |
| Earthworks as geoglyphs near the Lake Titicaca |
In Figure, we see details of these earthworks are shown. These images are coming from an area near the shore, the level of the lake is actually subsiding. Other satellite inspections, such as with radar or infrared detectors, could be of great help in detecting all the archaeological sites of this Peruvian region. A complete inspection with Google Maps is in any case necessary to have a total description of the raised fields and the related structure of canals and ponds. Besides the common destiny of any landform composed of fine-grained materials to become wide and flat relieves as a consequence of natural degradation processes, the earthworks of Titicaca are also subjected to the human action that can quickly destroy them.
References
1. Top-down or bottom-up: rural settlement and raised field agriculture in the Lake Titicaca Basin, Bolivia, John Wayne Januseka, Alan L. Kolatab, Journal of Anthropological Archaeology, 2004, 23, 404–430.
2. The Incas and Their Ancestors. Moseley, M.E., 1992, Thames and Hudson, New York.
3. The tragedy of the commoners. Pauketat, T.R., 2000, In: Dobres, M.-A., Robb, J. (Eds.), Agency in Archaeology. Routledge, London, pp. 123–139.
4. Basic concepts in the organization of irrigation. Chambers, R., 1980. In: Coward, J.W.E. (Ed.), Irrigation and Agricultural Development in Asia; Perspectives from the Social Sciences. Cornell University Press, Ithaca, pp. 28–50.
5. The social organization of prehispanic raised field agriculture in the lake Titicaca basin. Erickson, C.L., 1993. In: Scarborough, V.L., Isaac, B.L. Editors, Economic Aspects of Water Management in the Prehispanic New World. JAI Press, Greenwich, pp. 369–426.
6. Intensive agriculture and socio-political development in the Lake Patzcuaro, Fischer, C.T., Pollard, H.P., Frederick, C., Mexico Antiquity, 1999, 73, 642–649.
7. An archaeological investigation of raised field agriculture in the Lake Titicaca Basin of Peru, Erickson, C.L., 1988, unpublished Ph.D. dissertation, University of Illinois at Urbana-Champaign.
8. Andean terraced hills (a use of satellite imagery), Amelia Carolina Sparavigna, 25 Oct 2010, Geophysics (physics.geo-ph), arXiv:1010.5142v1 [physics.geo-ph]
9. Geoglyphs of Titicaca as an ancient example of graphic design, Amelia Carolina Sparavigna, 23 Sep 2010, Graphics (cs.GR), arXiv:1009.4602v1 [cs.GR]
10. Symbolic landforms created by ancient earthworks near Lake Titicaca, Amelia Carolina Sparavigna, 12-16 Sep 2010, Geophysics (physics.geo-ph); Graphics (cs.GR), arXiv:1009.2231v2 [physics.geo-ph]
11. Geoglyphs of Titicaca, Amelia Carolina Sparavigna, Lulu Enterprises, 2010, downloadable at http://www.scribd.com/doc/39011733/Book-Geoglyphs-Titicaca-Sparavigna
12. Landforms of Titicaca, Amazing land, Amelia Carolina Sparavigna, Lulu Enterprises, 2010, downloadable at http://www.scribd.com/doc/39011733/Book-Geoglyphs-Titicaca-Sparavigna
13. Landforms of Titicaca, Near Sillustani, Amelia Carolina Sparavigna, Lulu Enterprises, 2010, at http://www.scribd.com/doc/40227342/Landforms-of-Titicaca-Near-Sillustani-Book-by-A-CSparavigna
14. Modelling nocturnal heat dynamics and frost mitigation in Andean raised field systems, J.-P. Lhomme, J.-J. Vacher, Agricultural and Forest Meteorology, 2002, 112, 179–193.
15. The fish of Lake Titicaca: implications for archaeology and changing ecology through stable isotope analysis, Melanie J. Miller, José M. Capriles, Christine A. Hastorf, Journal of Archaeological Science, 2010, 37, 317–327.
16. Late-Quaternary lowstands of Lake Titicaca: evidence from high-resolution seismic data, Karin D’Agostino, Geoffrey Seltzer, Paul Baker, Sherilyn Fritz, Robert Dunbar Palaeogeography, Palaeoclimatology, Palaeoecology , 2002, 179, 97-111.
17. A 3500 14-C yr High-Resolution Record of Water-Level Changes in Lake Titicaca, Bolivia/Peru, Mark B. Abbott, Michael W. Binford, Mark Brenner, Kerry R. Kelts, Quaternary Research, 1997, 47, 169–180, article no. QR971881.
18. Pre-Incan agriculture activity recorded in dust layers in two tropical ice cores. Thompson, L. G., Davis, M. E., Mosley-Thompson, E., and Liu, K. Nature, 1988, 336, 763–765.
19. The Tiwanaku: Portrait of an Andean Civilization. Kolata, A. L.,1993. Blackwell, Cambridge, Massachusetts.
20. Investigation of level changes of lake Titicaca by maximum entropy spectral analysis. F. Künzel and A. Kessler, Earth and Environmental Science Meteorology and Atmospheric Physics, 1986, 36(3-4), 219-227, DOI: 10.1007/BF02263130.
21. Climate Variation and the Rise and Fall of an Andean Civilization, Michael W. Binford, Alan L. Kolata, Mark Brenner, John W. Janusek, Matthew T. Seddon, Mark Abbott, Jason H. Curtis, Quaternary Research, 1997, 47, 235–248, article no. QR971882.
22. Origin of Bolivian Quechua-Amerindians: their relationship with other American Indians and Asians according to HLA genes, Jorge Martinez-Laso, Nancy Siles, Juan Moscoso, Jorge Zamora, Juan I. Serrano-Vela, Juan I. R-A-Cachafeiro, Maria J. Castro, Manuel Serrano-Rios, Antonio Arnaiz-Villena, European Journal of Medical Genetics, 2006, 49, 169–185.
23. Lake-level fluctuations, M.B. Abbott, L. Anderson, in Encyclopaedia of paleoclimatology and ancient environments edited By Vivien Gornitz, Springer.
24. Late Quaternary climate history of the Bolivian Altiplano, Jaime Argollo, Philippe Mourguiar, Quaternary International, 2000, 72, 37-51.
The Rodadero
Rodadero and Qocha Chincanas at Cusco
"To the north of Chuquipampa we find Suchuna. It is a geologic formation similar to a hill with some waviness forming ruts parallel to the rocks. Nowadays, children use it as it was a slide. Inca Garcilazo says that he also played here when he was a child. At the top there is the famous "Inca Throne" or k'usillup hink'inan (jump of the monkey). ... In Rodadero we also find terraces, tunnels, tombs and stairs carved in stone. Recent works have revealed a spring that provided water to a round puddle from where a complex net of canals started.There is no doubt that Suchuna was a very important religious place as Guamancancha, temple of the fourth ceque of the Chinchaysuyo, was located there.It should have been two small rooms from where they observe the remains to the east side of the slide."
From http://www.incatrailbookings.com/Suchuna-or-Rodadero.html
And also
Let us use Google Maps: in the following image we can see the pond.
"To the north of Chuquipampa we find Suchuna. It is a geologic formation similar to a hill with some waviness forming ruts parallel to the rocks. Nowadays, children use it as it was a slide. Inca Garcilazo says that he also played here when he was a child. At the top there is the famous "Inca Throne" or k'usillup hink'inan (jump of the monkey). ... In Rodadero we also find terraces, tunnels, tombs and stairs carved in stone. Recent works have revealed a spring that provided water to a round puddle from where a complex net of canals started.There is no doubt that Suchuna was a very important religious place as Guamancancha, temple of the fourth ceque of the Chinchaysuyo, was located there.It should have been two small rooms from where they observe the remains to the east side of the slide."
From http://www.incatrailbookings.com/Suchuna-or-Rodadero.html
And also
Let us use Google Maps: in the following image we can see the pond.
After a processing see more clearly the circular pond, Qocha.
Let us note thta "qocha" means lake or lagoon. Therefore there are many places with Qocha in their names: Chakilqocha = Dry Lake, Q'omer-qocha = Green Lake, Qocha Perdida = Lost Lagoon, Qewña-Qocha = Polylepis tree Lagoon, and also Cochabamba = Qocha Pampa = plains with water.
Thursday, April 21, 2011
Bofedales - wetlands
Wiki is reporting that "Bofedal es un humedal de altura y se considera una pradera nativa poco extensa con permanente humedad. Los vegetales o plantas que habitan el bofedal reciben el nombre de vegetales hidrofíticos. Los bofedales se forman en zonas como las de los macizos andinos ubicadas sobre los 3.800 metros de altura, en donde las planicies almacenan aguas provenientes de precipitaciones pluviales, deshielo de glaciares y principalmente afloramientos superficiales de aguas subterráneas."
From the article, Los camellones alrededor del lago Titicaca, by Pierre Morlon, 2006, a bofedal is an artificial wet area used for cultivation, such as the qochas.
The site Atlantisbolivia.org is reporting an interesting image from Google Maps of bofedales near Lake Poopo, Bolivia. The site is telling "...it may not be realised on the ground, but these satellite images show that these ponds were at one time artificially constructed in rows, with interlinking small channels in the Pampa Aullagas region of the Altiplano. On the Altiplano there are many such examples of this type of landscape, some natural, some artificial as above, which are known asbofedales (wetlands)."
http://www.atlantisbolivia.org/corrientes.htm
I have searched the place and processed the images.
I have searched the place and processed the images.
Bolivia, Bofedales near Lake Poopo
Frost mitigation
Very interesting paper on raised fields and their physics (in English and Spanish).
Modelling nocturnal heat dynamics and frost mitigation in Andean raised field systemsJ.-P. Lhomme, J.-J. Vacher, Agricultural and Forest Meteorology 112 (2002) 179–193
The abstract is telling that the raised fields system is an old technique of soil and water management dating back to prehispanic time. Very common in the Lake Titicaca region, it essentially consists of a series of earth platforms on which crops are grown, surrounded by water canals connected to inlet and outlet ditches. A widely recognised benefit of this is its contribution to frost mitigation during the growing season. The paper presents a physical process-based model is presented to explain the role played by the canals in the nocturnal heat dynamics and the cold mitigation process. The model shows that greater heat flux emanating from the canals and greater water condensation on the crop both contribute to the mitigation effect.
La Mitigación de Heladas en Los Camellones del Altiplano andino, Bull. Inst. fr. études andines, 2003, 32 (2): 377-399, Jean-Paul Lhomme, Jean Joinville Vacher
Abstract: "El sistema de camellones o “waru warus” es una antigua técnica agrícola de manejo del suelo y del agua. En los tiempos prehispánicos era muy frecuente en la región del lago Titicaca. Consiste esencialmente en una serie de plataformas de tierra rodeadas por canales de agua. Las plantas se cultivan sobre las plataformas y el nivel del agua en los canales puede controlarse a través de entradas y salidas de agua. Un beneficio importante y ampliamente reconocido de este sistema de manejo en el altiplano es su contribución a la mitigación de heladas nocturnas durante la campaña agrícola. Con el objetivo de cuantificar este fenómeno y describir los procesos físicos responsables de la mitigación, se ha realizado un experimento en la región del lago Titicaca sobre un sistema de camellones cultivado con papas comparándolo con una parcela “testigo”
en la “Pampa”. Se presentan resultados experimentales que evidencian por una parte, el valor elevado de la temperatura del agua con respecto a la del cultivo sobre las plataformas, y por otra, una temperatura de cultivo siempre mayor (1-2 grados) en los camellones que en la Pampa. Conjuntamente se presenta un modelo mecanístico adaptado de un esquema de transferencia bicapa de tipo “Shuttleworth-Wallace” (una capa de vegetación y un sustrato de agua). El modelo precisa el papel que juegan los canales en la dinámica del calor y por lo tanto en la variación de la temperatura del cultivo durante la noche. El efecto de mitigación se debe al flujo de calor que emana del agua y a menudo también a la condensación del vapor de agua sobre las hojas del cultivo. Utilizando el modelo de manera predictiva, se muestra que canales más anchos o
plataformas más estrechas tienen un impacto positivo sobre la temperatura mínima del cultivo alcanzada durante la noche. Aumentar la profundidad del agua mejora también la mitigación de heladas, pero a la inversa, un canal más profundo (con el mismo nivel de agua) tiene un impacto negativo. Aumentar el índice de área foliar (LAI) o la altura del cultivo tiene un efecto positivo sobre la mitigación de heladas (el beneficio marginal, sin embargo, es muy pequeño cuando el índice foliar supera el valor 1). Mayor velocidad de viento o mayor humedad relativa incrementa también el efecto de mitigación de heladas."
http://www.ifeanet.org/publicaciones/boletines/32(2)/377.pdf
Modelling nocturnal heat dynamics and frost mitigation in Andean raised field systemsJ.-P. Lhomme, J.-J. Vacher, Agricultural and Forest Meteorology 112 (2002) 179–193
The abstract is telling that the raised fields system is an old technique of soil and water management dating back to prehispanic time. Very common in the Lake Titicaca region, it essentially consists of a series of earth platforms on which crops are grown, surrounded by water canals connected to inlet and outlet ditches. A widely recognised benefit of this is its contribution to frost mitigation during the growing season. The paper presents a physical process-based model is presented to explain the role played by the canals in the nocturnal heat dynamics and the cold mitigation process. The model shows that greater heat flux emanating from the canals and greater water condensation on the crop both contribute to the mitigation effect.
La Mitigación de Heladas en Los Camellones del Altiplano andino, Bull. Inst. fr. études andines, 2003, 32 (2): 377-399, Jean-Paul Lhomme, Jean Joinville Vacher
Abstract: "El sistema de camellones o “waru warus” es una antigua técnica agrícola de manejo del suelo y del agua. En los tiempos prehispánicos era muy frecuente en la región del lago Titicaca. Consiste esencialmente en una serie de plataformas de tierra rodeadas por canales de agua. Las plantas se cultivan sobre las plataformas y el nivel del agua en los canales puede controlarse a través de entradas y salidas de agua. Un beneficio importante y ampliamente reconocido de este sistema de manejo en el altiplano es su contribución a la mitigación de heladas nocturnas durante la campaña agrícola. Con el objetivo de cuantificar este fenómeno y describir los procesos físicos responsables de la mitigación, se ha realizado un experimento en la región del lago Titicaca sobre un sistema de camellones cultivado con papas comparándolo con una parcela “testigo”
en la “Pampa”. Se presentan resultados experimentales que evidencian por una parte, el valor elevado de la temperatura del agua con respecto a la del cultivo sobre las plataformas, y por otra, una temperatura de cultivo siempre mayor (1-2 grados) en los camellones que en la Pampa. Conjuntamente se presenta un modelo mecanístico adaptado de un esquema de transferencia bicapa de tipo “Shuttleworth-Wallace” (una capa de vegetación y un sustrato de agua). El modelo precisa el papel que juegan los canales en la dinámica del calor y por lo tanto en la variación de la temperatura del cultivo durante la noche. El efecto de mitigación se debe al flujo de calor que emana del agua y a menudo también a la condensación del vapor de agua sobre las hojas del cultivo. Utilizando el modelo de manera predictiva, se muestra que canales más anchos o
plataformas más estrechas tienen un impacto positivo sobre la temperatura mínima del cultivo alcanzada durante la noche. Aumentar la profundidad del agua mejora también la mitigación de heladas, pero a la inversa, un canal más profundo (con el mismo nivel de agua) tiene un impacto negativo. Aumentar el índice de área foliar (LAI) o la altura del cultivo tiene un efecto positivo sobre la mitigación de heladas (el beneficio marginal, sin embargo, es muy pequeño cuando el índice foliar supera el valor 1). Mayor velocidad de viento o mayor humedad relativa incrementa también el efecto de mitigación de heladas."
http://www.ifeanet.org/publicaciones/boletines/32(2)/377.pdf
Qocha
From the article, Los camellones alrededor del lago Titicaca, by Pierre Morlon, 2006.
The article is discussing the traditional agricultural methods used near Lake Titicaca; these methods are more than two thousands years old.
A "qocha" (small lake, lagoon) is an artificial pond used to gain water for cultivation. The text is telling that up to fifty years ago, waru-warus, camellones, qochas were much more extensive on the land but they were deliberately destroyed.
A qocha.
El sueño de la razón
Da Wikipedia
« La fantasía abandonada de la razón produce monstruos imposibles: unida con ella es madre de las artes y origen de las maravillas. » Goya, manoscritto conservato al museo del Prado.