Literatura académica sobre el tema "Nazca Lines Site (Peru)"

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Artículos de revistas sobre el tema "Nazca Lines Site (Peru)"

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Karl, Hans-Volker, Amtyaz Safi, and 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 (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
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Ruggles, Clive, and Nicholas J. Saunders. "Desert labyrinth: lines, landscape and meaning at Nazca, Peru." Antiquity 86, no. 334 (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, and David Browne. "New evidence for the date of the Nazca lines." Antiquity 65, no. 247 (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 (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 t
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Delle Rose, Marco, Giuseppe Orefici, Laura Panzeri, et al. "Optically Stimulated Luminescence (OSL) Dating of Alluvial Deposits from the Cahuachi Archaeological Site (South Peru)." Geosciences 14, no. 12 (2024): 323. http://dx.doi.org/10.3390/geosciences14120323.

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Cahuachi (Nazca River Valley, South Peru) was the major ceremonial center of the Nasca civilization. According to previous studies, it was struck and destroyed by three El Niño-Southern Oscillation events, which would have occurred around 100 BCE, 600 CE and 1000 CE, respectively. At the end of the series of events, the ceremonial center would have been buried by a cap of conglomerates. Despite this hypothesis raised well-founded doubts regarding its geochronological and paleoenvironmental implications, it is uncritically used as a reference in geoarchaeological research. In the present study,
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Calvès, Gérôme, Alan Mix, Liviu Giosan, et al. "The Nazca Drift System – palaeoceanographic significance of a giant sleeping on the SE Pacific Ocean floor." Geological Magazine 159, no. 3 (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 seismi
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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 (1987): S70—S71. http://dx.doi.org/10.1177/002182868701801107.

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Sparavigna, Amelia Carolina. "Maria Reiche's line to archaeoastronomy." Archaeoastronomy and Ancient Technologies 1, no. 2 (2013): 48–54. https://doi.org/10.5281/zenodo.3921896.

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Maria Reiche was a German mathematician and archaeologist that, from 1940, devoted her life to the study of the Nazca Lines, the most famous Peruvian geoglyphs, gaining recognition and preservation of them. Created by removing the upper most layer of the arid soil of the Nazca desert, these geoglyphs, declared in 1995 a UNESCO World Heritage Site, are composed by very long straight and trapezoidal lines, spirals and large figures representing animals. Maria Reiche, in fact an archaeoastronomer too, proposed for the Lines some interesting astronomical interpretations, t
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Pulido, Nelson, Shoichi Nakai, Hiroaki Yamanaka, Diana Calderon, Zenon Aguilar, and Toru Sekiguchi. "Estimation of a Source Model and Strong Motion Simulation for Tacna City, South Peru." Journal of Disaster Research 9, no. 6 (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 str
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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 (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 prot
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Tesis sobre el tema "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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Libros sobre el tema "Nazca Lines Site (Peru)"

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Nascimento, Márcia, and Nuno Costa, eds. Käräjäkivet 03: Mystery on the Desert: The secret of Pampa: the most important astronomical monument of the world. Käräjäkivet, 2019.

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F, Aveni Anthony, ed. The Lines of Nazca. American Philosophical Society, 1990.

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

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

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5

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 sp
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Lines of Nazca: Memoirs, American Philosophical Society. American Philosophical Society, 1990.

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8

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

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Capítulos de libros sobre el tema "Nazca Lines Site (Peru)"

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Gomez-Pando, Luz, Jesus Bernardo-Rojas, Denisse Deza-Montoya, Martha Ibañez-Tremolada, and Enrique Aguilar-Castellanos. "Mutation induction to improve quinoa (Chenopodium quinoa) resistance to downy mildew (Peronospora variabilis)." In Mutation breeding, genetic diversity and crop adaptation to climate change. 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 (<sup>60</sup>Co), were evaluated in two experimental locati
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