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

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Publicado: 25 de julio de 2024
Última modificación: 31 de julio de 2025

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Valdez, Lidio M. "The Archaeology of Rituals." Revista de Arqueología Americana, no. 41 (June 5, 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 recen
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12

Чудинов, Валерий, and Valeriy Chudinov. "Feoglyphics as a sciene of the Earth´s artificial surface relief." Servis Plus 9, no. 1 (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.
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13

Pahl, Gary W. "Lines to the Mountain Gods: Nazca and the Mysteries of Peru. Evan Hadingham. University of Oklahoma Press, Norman, 1988. xii + 307 pp., biblio., index. $15.95 (paper)." American Antiquity 55, no. 2 (1990): 434. http://dx.doi.org/10.2307/281679.

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14

BROWN, JASON L., RAINER SCHULTE, and KYLE SUMMERS. "A new species of Dendrobates (Anura: Dendrobatidae) from the Amazonian lowlands in Perú." Zootaxa 1152, no. 1 (2006): 45. http://dx.doi.org/10.11646/zootaxa.1152.1.2.

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We describe a new species of poison frog from Amazonian Peru. Dendrobates uakarii, sp. nov. is distinguished by the presence of paired parallel dorsolateral lines: one yellow oblique lateral and one red dorsolateral (on each flank), with one vertebral line, similar in color to the dorsolateral lines. Phylogenetic analysis show that D. uakarii, sp. nov. and closely related taxa (D. ventrimaculatus sp. aff. Shreve from Porto Walter, Brazil and another from Amazonas, Brazil) form the sister group to D. fantasticus Boulenger. This new species can be distinguished from its sister taxa on the basis
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15

Rowe, John Howland. "The Nazca Lines: A New Perspective on their Origin and Meaning. Johan Reinhard. editorial los pinos, lima, peru, 1985. 64 pp., illustrations, biblio. (first edition). no price given (paper)." American Antiquity 53, no. 1 (1988): 215. http://dx.doi.org/10.2307/281200.

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16

Aveni, A. F. "Evan Hadingham. Lines to the mountain Gods: Nazca and the mysteries of Peru. London: Harrap & New York: Random House, 1987. xii + 306 pages, 294 illustrations. £12.95 & $22.50 hardback." Antiquity 61, no. 233 (1987): 497–99. http://dx.doi.org/10.1017/s0003598x00073336.

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17

Lau, George F. "Feasting and Ancestor Veneration at Chinchawas, North Highlands of Ancash, Peru." Latin American Antiquity 13, no. 3 (2002): 279–304. http://dx.doi.org/10.2307/972112.

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The present article considers evidence for ancestor veneration and feasting in the North Highlands (Department of Ancash), Peru between A. D. 500-900. The study draws upon ethnohistorical, iconographic, and archaeological comparisons to better understand different lines of data from the ancient Recuay community of Chinchawas (3,850 masl), including public and mortuary architecture, ceramics, faunal remains, and stone sculpture. Two major programs of religious activity can be discerned: one situated within local Recuay traditions (Kayán and Chinchawasi phases, A. D. 500-800), followed by a suit
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18

Zapata, Juan, and Doris Esenarro. "Models for the Analysis of the Structural Capacity of Railway Bridges in Peru in Accordance with the American Railway Engineering and Maintenance-of-Way Association Standard." Construction Materials 5, no. 2 (2025): 38. https://doi.org/10.3390/constrmater5020038.

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This scientific research presents the most significant aspects of the structural analysis and verification of the main steel railway bridges in Peru in accordance with the American standard. To this end, linear and finite element analyses (FEMs) were performed using calculation notes in MATHCAD and structural validation software (SAP2000, CSI Bridge, IDEA STATICA and GE05), among others, based on on-site inspections, which allowed results to be obtained to analyze, evaluate and determine the structural performance factors (RF) of the main railway bridges in Peru. For this, data obtained from s
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19

Lambert, Patricia M., Celeste Marie Gagnon, Brian R. Billman, M. Anne Katzenberg, José Carcelén, and Robert H. Tykot. "Bone Chemistry at Cerro Oreja: A Stable Isotope Perspective on the Development of a Regional Economy in the Moche Valley, Peru During the Early Intermediate Period." Latin American Antiquity 23, no. 2 (2012): 144–66. http://dx.doi.org/10.7183/1045-6635.23.2.144.

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AbstractIn this paper we test the hypothesis that an intensification of maize production preceded the development of a regional Moche political economy in the Moche Valley of north coastal Peru during the Early Intermediate period (400 B.C.—A.D. 600). To do so we analyze stable isotopic signatures of 48 bone apatite and 17 tooth enamel samples from human remains recovered from the site of Cerro Oreja, a large urban and ceremonial center in the Moche Valley. These remains date to the Guañape, Salinar, or Gallinazo phases and provide a diachronic picture of subsistence before the appearance of t
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20

Person, Anna K., Fernanda Maruri, Ellen Brazier, et al. "475. Describing the impact of the COVID-19 pandemic on HIV care in Latin America." Open Forum Infectious Diseases 7, Supplement_1 (2020): S303—S304. http://dx.doi.org/10.1093/ofid/ofaa439.668.

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Abstract Background The effects of the COVID-19 pandemic on people living with HIV (PWH) are unknown. Beyond SARS-CoV-2 co-infection, the pandemic may have devastating consequences for HIV care delivery. Understanding these is crucial as reduced antiretroviral therapy (ART) availability alone could lead to ≥500,000 AIDS-related deaths in 2020–2021. With Latin America now a focal point in the pandemic, we sought to describe the impact of COVID-19 on HIV care at Latin American clinical sites. Methods Caribbean, Central and South America network for HIV epidemiology (CCASAnet) and additional Braz
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21

Enrique, Rico. "Refractory Extranodal Nasal NK/T-Cell Lymphoma with CNS Involvement Treated with Radiotherapy and Pralatrexate: Case Report." Blood 126, no. 23 (2015): 5060. http://dx.doi.org/10.1182/blood.v126.23.5060.5060.

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Abstract Introduction Peripheral T-Cell Lymphoma represents a clinically and biologically heterogeneous group of Non-Hodgkin's lymphomas. One uncommon subtype is extranodal nasal natural killer (NK)/T-cell lymphoma (ENKL) type which occur worldwide, with a strong geographic predilection for Asian, Central and South American populations from Mexico, Peru, Argentina and Brazil, constituting 5% to 15% of lymphomas in these countries1. The clinical course is aggressive, and the prognosis is poor mainly due to the expression of P-glycoprotein, which actively exports several anticancer agents outsid
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22

Sparavigna, Amelia Carolina. "Lines, dots and spirals on Peruvian land." September 16, 2011. https://doi.org/10.5281/zenodo.1171025.

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The most famous geoglyphs of Peru are the "Nazca Lines". Considered as one of the mysteries of the ancient world, they have been included among the UNESCO World Heritage Sites. Located in a large region between the towns of Nazca and Palpa, these lines create shapes of animals ranging in size up to 300 m. The archaeological site is under investigation with remote science technologies.
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23

"Tracking Human-Induced Landscape Disturbance at the Nasca Lines UNESCO World Heritage Site in Peru with COSMO-SkyMed InSAR." Remote Sensing 10, no. 4 (2018): 572. http://dx.doi.org/10.3390/rs10040572.

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24

Hu, Yaping, Yuji Yagi, Ryo Okuwaki, and Kousuke Shimizu. "Back-propagating rupture evolution within a curved slab during the 2019 Mw 8.0 Peru intraslab earthquake." Geophysical Journal International, August 3, 2021. http://dx.doi.org/10.1093/gji/ggab303.

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Summary The 26 May 2019 MW 8.0 Peru intraslab earthquake ruptured the subducting Nazca plate where the dip angle of the slab increases sharply and the strike angle rotates clockwise from the epicentre to north. To obtain a detailed seismic source model of the 2019 Peru earthquake, including not only the rupture evolution but also the spatiotemporal distribution of focal mechanisms, we performed comprehensive seismic waveform analyses using both a newly developed flexible finite-fault teleseismic waveform inversion method and a back-projection method. The source model revealed a complex rupture
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25

Landol, Nicholas, and Elizabeth DiGangi. "The Role of Kinship in Cranial Modification at the Paracas Necropolis." Journal of Student Research 11, no. 1 (2023). http://dx.doi.org/10.47611/jsr.v11i1.1457.

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This article seeks to investigate the motivation for the cranial modification observed on remains recovered from the 2nd century BCE-3rd century CE site in Peru known as the Paracas Necropolis. This article argues that the explanations normally offered by anthropologists for cranial modification, such as that it is representative of sex and status, are not applicable to the Paracas Necropolis and instead, an alternative explanation is put forward which states that each of the different forms of cranial modification seen at the Paracas Necropolis is symbolic of a different kin group that existe
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26

Lajo‐Yáñez, J. A., S. S. Flint, M. Huuse, and R. L. Brunt. "Tectono‐Stratigraphic Insights on the Dynamics of a Complex Subduction Zone, Northern Peruvian Forearc." Tectonics 43, no. 1 (2023). http://dx.doi.org/10.1029/2023tc007860.

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AbstractTwo main types of subduction are recognized around the world: accretionary and erosive. The northern Peruvian margin is a well‐known example of a margin subjected to subduction erosion, but to date the along‐margin variability and temporal changes in subduction process and forearc basin evolution have not been characterized in detail. Interpretation of regional seismic lines and integration of oil‐industry wells and seafloor data captures the erosive nature of subduction underneath the forearc with only a minor accretionary component to the north. Episodes of uplift driven by plate cou
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27

Uceda, Santiago, Henry Gayoso, Feren Castillo, and Carlos Rengifo. "Climate and Social Changes: Reviewing the Equation with Data from the Huacas de Moche Archaeological Complex, Peru." Latin American Antiquity, May 20, 2021, 1–18. http://dx.doi.org/10.1017/laq.2021.35.

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Investigations at the site of Huacas de Moche—also referred to as Huacas del Sol and de la Luna—on the north coast of Peru show a continuous occupational sequence from around AD 100 to 1500. The longest occupation corresponds to the Moche culture from around AD 100 to 850. Based on available archaeological evidence, this article examines the impact of an El Niño-like event in AD 600 on the history of Huacas de Moche. Widely held hypotheses assumed that this kind of climatic event caused the abandonment of the site; however, such explanations do not fit the current data. After almost three deca
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28

Rozwadowski, Andrzej, and Janusz Z. Wołoszyn. "Dances with Zigzags in Toro Muerto, Peru: Geometric Petroglyphs as (Possible) Embodiments of Songs." Cambridge Archaeological Journal, April 3, 2024, 1–21. http://dx.doi.org/10.1017/s0959774324000064.

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Southern Peru is home to one of the richest sites with rock art in South America—Toro Muerto. A unique aspect of the iconography of the petroglyphs of the site is the figures of dancing humans, the so-called danzantes, which are additionally frequently associated with geometric motifs, mostly variants of zigzag lines. Drawing upon intriguing data recorded during Reichel-Dolmatoff's research in Colombia related to the meaning of analogous motifs in Tukano art, as well as broader exploration of the sonic sphere in South American cultures and the thesis that Amazonian animism was a more archaic o
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29

Nelson, Andrew J., Jo Motley, Lucía Watson, et al. "Headless Burials from Pachacamac, Peru." Bioarchaeology International, March 14, 2024. http://dx.doi.org/10.5744/bi.2023.0020.

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A paleoradiographic survey of funerary bundles (fardos) from a Late Intermediate Period (1000 A.D.–1472 A.D.) cemetery in Sector 3 of the site of Pachacamac, Peru, demonstrated that 15 out of 61 individuals had had their head removed when the body was in an advanced state of skeletonization/mummification. Detailed analysis of the field report, the fardos themselves, and X-rays and computed tomography scans of the fardos suggested that nine of these individuals were potential candidates for head removal in antiquity. Of those nine, six appeared to be clear examples of this practice. The analysi
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30

Callaghan, Michaela. "Dancing Embodied Memory: The Choreography of Place in the Peruvian Andes." M/C Journal 15, no. 4 (2012). http://dx.doi.org/10.5204/mcj.530.

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This article is concerned with dance as an embodied form of collective remembering in the Andean department of Ayacucho in Peru. Andean dance and fiesta are inextricably linked with notions of identity, cultural heritage and history. Rather than being simply aesthetic —steps to music or a series of movements — dance is readable as being a deeper embodiment of the broader struggles and concerns of a people. As anthropologist Zoila Mendoza writes, in post-colonial countries such as those in Africa and Latin America, dance is and was a means “through which people contested, domesticated and rewor
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31

Mesquita, Afrânio Rubens de. "Prefácio." Revista Brasileira de Geofísica 31, no. 5 (2013). http://dx.doi.org/10.22564/rbgf.v31i5.392.

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PREFACEThe articles of this supplement resulted from the 5 th International Congress of the Brazilian Geophysical Society held in São Paulo city, Brazil, at the Convention Center of the Transamérica Hotel, from 28 th September to 2 nd of October 1997. The participants of the Round Table Discussions on “Mean Sea Level Changes Along the Brazilian Coast” were Dr. Denizar Blitzkow, Polytechnic School of the University of São Paulo, (POLI-USP), Prof. Dr. Waldenir Veronese Furtado, Institute of Oceanography (IO-USP), Dr. Joseph Harari (IO-USP), Dr. Roberto Teixeira from the Brazilian Institute of Ge
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