Bibliographies thématiques / Nazca Lines Site (Peru)

Littérature scientifique sur le sujet « Nazca Lines Site (Peru) »

Auteur : Grafiati
Publié le 25 juillet 2024

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Articles de revues sur le sujet "Nazca Lines Site (Peru)"

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Karl, Hans-Volker, Amtyaz Safi et Gottfried Tichy. « Identifying of a bird figure of the Nazca pampas of southern coast of Peru : a discussion post ». International Journal of Biological Research 10, no 1 (30 novembre 2023) : 8–10. http://dx.doi.org/10.14419/fc9nys18.

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Nazca is a city and system of valleys on the southern coast of Peru. The name is derived from the Nazca culture, which flourished in the area between 100 BC and 800 AD. Nazca Lines contain over 800 straight lines, 300 geometric figures and 70 biomorphic designs. Some of the straight lines are 30 miles long, while the largest bio morphs stretch up to 1200 feet. Among the zoomorphic figures are the famous Nazca condor, hummingbird, pelican, shark, bird, fish, spider, lizard, parrot, flamingo, iguana, dog, llamas, jaguar, fox, whale and monkey. We have identified a studied figure of Nazca Pampas as a species of umbrella birds (Cephalopterus) and this geoglyph has more resemblances with the short-lobed parasol (Cephalopterus ornatus) than any other species.
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Ruggles, Clive, et Nicholas J. Saunders. « Desert labyrinth : lines, landscape and meaning at Nazca, Peru ». Antiquity 86, no 334 (décembre 2012) : 1126–40. http://dx.doi.org/10.1017/s0003598x00048298.

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The shapes drawn out by the famous Nazca lines in the Peruvian desert are at their most evident from the air—giving rise to some famously fantastic theories about their origin. The new understanding offered here is the result of a piece of straightforward brilliance on the part of our authors: get down on the ground, where the original users were, and see where your feet lead you. Using stratigraphic and taphonomic reasoning to decide which lines were contemporary, they discover an itinerary so complex they can justify calling it a labyrinth, and see it as serving ceremonial progressions.
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Silverman, Helaine, et David Browne. « New evidence for the date of the Nazca lines ». Antiquity 65, no 247 (juin 1991) : 208–20. http://dx.doi.org/10.1017/s0003598x00079667.

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Surface features that possess no useful stratigraphy and are not, by their own nature, informative about their age, are notoriously hard to date. A study of associations now defines with good confidence the dates of the surface arrangements of stones and of cleared areas that make up some of the celebrated Nazca lines, Peru.
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Silverman, Helaine. « Paracas in Nazca : New Data on the Early Horizon Occupation of the Rio Grande de Nazca Drainage, Peru ». Latin American Antiquity 5, no 4 (décembre 1994) : 359–82. http://dx.doi.org/10.2307/971822.

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Nasca culture and, particularly, Nasca ceramic iconography are held to evolve directly and smoothly out of antecedent Paracas. Yet the data reviewed in this article indicate that Paracas remains in the Río Grande de Nazca drainage, the heartland of Nasca culture on the south coast of Peru, are limited in nature, a fact that makes it difficult to derive Nasca from Paracas in Nazca. In contrast, there are rich and abundant Paracas remains in the Ica, Pisco, and Chincha valleys, at the Paracas type site itself, and along the Bahía de la Independencia. I look to the Ica Valley for the origins of the Nasca style.
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Calvès, Gérôme, Alan Mix, Liviu Giosan, Peter D. Clift, Stéphane Brusset, Patrice Baby et Mayssa Vega. « The Nazca Drift System – palaeoceanographic significance of a giant sleeping on the SE Pacific Ocean floor ». Geological Magazine 159, no 3 (2 novembre 2021) : 322–36. http://dx.doi.org/10.1017/s0016756821000960.

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AbstractThe evolution and resulting morphology of a contourite drift system in the SE Pacific oceanic basin is investigated in detail using seismic imaging and an age-calibrated borehole section. The Nazca Drift System covers an area of 204 500 km2 and stands above the abyssal basins of Peru and Chile. The drift is spread along the Nazca Ridge in water depths between 2090 and 5330 m. The Nazca Drift System was drilled at Ocean Drilling Program Site 1237. This deep-water drift overlies faulted oceanic crust and onlaps associated volcanic highs. Its thickness ranges from 104 to 375 m. The seismic sheet facies observed are associated with bottom current processes. The main lithologies are pelagic carbonates reflecting the distal position relative to South America and water depth above the carbonate compensation depth during Oligocene time. The Nazca Drift System developed under the influence of bottom currents sourced from the Circumpolar Deep Water and Pacific Central Water, and is the largest yet identified abyssal drift system of the Pacific Ocean, ranking third in all abyssal contourite drift systems globally. Subduction since late Miocene time and the excess of sediments and water associated with the Nazca Drift System may have contributed to the Andean orogeny and associated metallogenesis. The Nazca Drift System records the evolution in interactions between deep-sea currents and the eastward motion of the Nazca Plate through erosive surfaces and sediment remobilization.
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Shawcross, William E. « Book Review : Lines to the Mountain Gods : Nazca and the Mysteries of Peru ». Journal for the History of Astronomy 18, no 11 (février 1987) : S70—S71. http://dx.doi.org/10.1177/002182868701801107.

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Pulido, Nelson, Shoichi Nakai, Hiroaki Yamanaka, Diana Calderon, Zenon Aguilar et Toru Sekiguchi. « Estimation of a Source Model and Strong Motion Simulation for Tacna City, South Peru ». Journal of Disaster Research 9, no 6 (1 décembre 2014) : 925–30. http://dx.doi.org/10.20965/jdr.2014.p0925.

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We estimate several scenarios for source models of megathrust earthquakes likely to occur on the Nazca-South American plates interface in southern Peru. To do so, we use a methodology for estimating the slip distribution of megathrust earthquakes based on an interseismic coupling (ISC) distribution model in subduction margins and on information about historical earthquakes. The slip model obtained from geodetic data represents large-scale features of asperities within the megathrust that are appropriate for simulating long-period waves and tsunami modelling. To simulate broadband frequency strong ground motions, we add small scale heterogeneities to the geodetic slip by using spatially correlated random noise distributions. Using these slip models and assuming several hypocenter locations, we calculate a set of strong ground motions for southern Peru and incorporate site effects obtained from microtremors array surveys in Tacna, the southernmost city in Peru.
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McCool, Weston C. « COPING WITH CONFLICT : DEFENSIVE STRATEGIES AND CHRONIC WARFARE IN THE PREHISPANIC NAZCA REGION ». Latin American Antiquity 28, no 3 (8 août 2017) : 373–93. http://dx.doi.org/10.1017/laq.2017.28.

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Warfare was a prevalent phenomenon throughout the Andes during the Late Intermediate period (LIP; AD 1000–1450). A salient research topic within broader investigations of conflict is how populations cope with chronic warfare. This article utilizes statistical and GIS-based analyses of architectural features and settlement patterns to reconstruct defensive coping mechanisms among groups living in 15 fortified settlements in the Nazca region of Peru. This research evaluates how populations deployed artificial defenses (fortifications), natural defensibility, and settlement placement to best protect themselves and critical resources from enemy incursions. Intersite variation in fortification was primarily driven by population size: the smallest and most vulnerable settlements were the most heavily fortified and occupied the least accessible areas. Variation in fortification investment within each site was driven by differences in the accessibility of approaches leading to the residential sector of a site. Settlement patterns were largely driven by natural defensibility, large viewsheds, and proximity to economic resources. This research demonstrates that LIP populations made optimal trade-offs between competing defensive variables, revealing highly patterned regional defensive strategies. Broader spatial, settlement, and architectural data indicate that warfare in the region was chronic and internecine.
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Valdez, Lidio M. « The Archaeology of Rituals ». Revista de Arqueología Americana, no 41 (5 juin 2024) : 365–401. http://dx.doi.org/10.35424/rearam.i41.1112.

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Ever since the discovery made back in 1926 at the site of Pacheco of the Nazca Valley, on the south coast of Peru, it is known that an important aspect of the ritual celebrations staged by the Wari state consisted on the deliberate smashing of large-sized and finely painted ceramic vessels that afterwards were buried in the ground. Subsequent research has shown that this tradition was initiated by the Wari and the earliest known purposely shattered vessels are found in the Ayacucho Valley, heartland of the Wari state. As Wari expanded, similar celebrations were performed elsewhere in the recently annexed regions, as the finding of analogous ceramic deposits indicate. One such deposit has been found in the Acari Valley of the south coast of Peru. The finding from Acari is described here, and it is argued that the act of shattering the vessels marked the culmination of a complex ritual celebration probably performed to spread Wari religion and Wari deities, as well as to befriend the locals, which ultimately helped to legitimize Wari’s intrusive presence in the region.
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Чудинов, Валерий, et Valeriy Chudinov. « Feoglyphics as a sciene of the Earth´s artificial surface relief ». Servis Plus 9, no 1 (6 mars 2015) : 86–97. http://dx.doi.org/10.12737/7587.

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The article covers a new scientific branch — the science of geoglyphics, which studies space-eye view (1,000 and over km from the surface of the earth) of ancient inscriptions, images, symbols and traces of ancient settlements. The author provides a brief description of the history ofgeoglyph studies, geoglyph types, interpretations of a geoglyph, and makes seven conclusions concerning the signification ofgeoglyphs for research into the history of different ethnic groups. The author defines a geoglyph as at least a 4-metre all-angle image or inscription on the surface of the Earth. Throughout the 20th century it was the Nazca Lines in Peru were the only scientifically acclaimed geogplyphs. However, there seems to be noplace on the planet that could not boast a geoglyph of its own. Despite the fact that for a long time Russian researchers have abstained from studying geoglyphs, at present Russian science has produced interesting reports, for example byAleksei Loktev. However, pessimistic views are also voiced, for example, Oleg Utkin claims that the topic receives undeservedly little attention. Men of art also resort to creating geoglyphs of nonexistent objects such as, for example, the fictitious land ofAtlaropa (also referred to as Panropa). Private collections of the geoglyphs of the past century are being created as well.
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Thèses sur le sujet "Nazca Lines Site (Peru)"

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Tiballi, Anne E. « Castoffs and snippets the textile evidence from Casa Vieja, Ica Valley, Peru / ». Online access via UMI:, 2005.

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Livres sur le sujet "Nazca Lines Site (Peru)"

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Nascimento, Márcia, et Nuno Costa, dir. Käräjäkivet 03 : Mystery on the Desert : The secret of Pampa : the most important astronomical monument of the world. Barcelos, Portugal : Käräjäkivet, 2019.

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Hadingham, Evan. Lines to the mountain gods : Nazca and the mysteries of Peru. London : Harrap, 1987.

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Hadingham, Evan. Lines to the mountain gods : Nazca and the mysteries of Peru. New York : Random House, 1987.

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Hadingham, Evan. Lines to the mountain gods : Nazca and the mysteries of Peru. Norman : University of Oklahoma Press, 1988.

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5

Hinman, Bonnie. Mystery of the Nazca Lines. Core Library, 2016.

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Ruggles, Clive L. N. Ancient Astronomy. ABC-CLIO, 2005. http://dx.doi.org/10.5040/9798400612749.

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An authoritative introduction to the fascinating topic of archaeoastronomy—ancient peoples' understanding and use of the skies. Ancient Astronomy: An Encyclopedia of Cosmologies and Mythdraws on archaeological evidence and oral traditions to reveal how prehistoric humans perceived the skies and celestial phenomena. With over 200 entries, it offers a number of ways to approach ancient astronomy, from key examples and case studies worldwide (Stonehenge; Mexican and Egyptian pyramids; Chaco Canyon, New Mexico; the Nazca lines in Peru) to general themes (cosmologies, calendars, ancient ideas of space and time, origin myths), to fundamental concepts and methods (how the sky has changed over the centuries, how to survey a site), and to the field's most frequently asked questions (How did ancient peoples navigate the ocean using the stars? How does astrology relate to ancient astronomy? Can ancient sites be dated astronomically?) By revealing the astronomical significance of some of the world's most famous ancient landmarks and enduring myths and by showing how different themes and concepts are connected,Ancient Astronomy: An Encyclopedia of Cosmologies and Mythbrings a unique authoritative perspective to an area too often left to speculation and sensationalism.
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Hinman, Bonnie. Mystery of the Nazca Lines. ABDO Publishing Company, 2015.

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McMullen, David W. Mystery in Peru : The Lines of Nazca (Great Unsolved Mysteries Series). Raintree Steck-Vaughn Publishers, 1997.

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Beyond the Nasca Lines : Ancient Life at la Tiza in the Peruvian Desert. University Press of Florida, 2016.

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Beyond the Nasca Lines : Ancient Life at la Tiza in the Peruvian Desert. University Press of Florida, 2016.

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Chapitres de livres sur le sujet "Nazca Lines Site (Peru)"

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Gomez-Pando, Luz, Jesus Bernardo-Rojas, Denisse Deza-Montoya, Martha Ibañez-Tremolada et Enrique Aguilar-Castellanos. « Mutation induction to improve quinoa (Chenopodium quinoa) resistance to downy mildew (Peronospora variabilis). » Dans Mutation breeding, genetic diversity and crop adaptation to climate change, 194–202. Wallingford : CABI, 2021. http://dx.doi.org/10.1079/9781789249095.0019.

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Abstract Quinoa is an important crop due to its nutritional characteristics (better than cereals) and its tolerance to abiotic stresses. However, various factors such as high susceptibility to diseases, especially downy mildew caused by Peronospora variabilis, limit its agricultural performance. Genetic improvement of quinoa could reduce the need to use fungicides for this crop and maintain the organic quality of Peruvian production in small-scale farms. Seeds of var. 'Amarilla Marangani', irradiated with 150 and 250 Gy of gamma-rays (60Co), were evaluated in two experimental locations in Peru: coastland at La Molina and highland at Huancayo. Resistance to downy mildew and other agricultural traits in the M3 and M4 generations was studied. In both locations, downy mildew was observed in susceptible plants under natural infection, from the seedling stage to plant maturity. At the coastland site, six mutants with 30% leaf infection were obtained in the progeny of plants exposed to 150 Gy. Five additional mutants with 40% leaf infection were found in the progeny of plants exposed to 250 Gy. In the highland trial, only seven lines were identified with 30% severity (foliar area with symptoms) among the plants from the 150 Gy experiment. The parent materials showed 70-80% disease severity. Mutant lines with quantitative resistance and tolerance to downy mildew, high yield potential, reduced duration, shorter plant height, altered inflorescence shape and grain colour mutations were selected from both doses. This study showed that quantitative resistance and tolerance to downy mildew could be obtained in quinoa and this resulted in increased grain yields.
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