Messages Woven Into Textile from Andean Capacocha Burials
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Freshwater Diatoms in the Sajama, Quelccaya, and Coropuna Glaciers of the South American Andes
Diatom Research ISSN: 0269-249X (Print) 2159-8347 (Online) Journal homepage: http://www.tandfonline.com/loi/tdia20 Freshwater diatoms in the Sajama, Quelccaya, and Coropuna glaciers of the South American Andes D. Marie Weide , Sherilyn C. Fritz, Bruce E. Brinson, Lonnie G. Thompson & W. Edward Billups To cite this article: D. Marie Weide , Sherilyn C. Fritz, Bruce E. Brinson, Lonnie G. Thompson & W. Edward Billups (2017): Freshwater diatoms in the Sajama, Quelccaya, and Coropuna glaciers of the South American Andes, Diatom Research, DOI: 10.1080/0269249X.2017.1335240 To link to this article: http://dx.doi.org/10.1080/0269249X.2017.1335240 Published online: 17 Jul 2017. Submit your article to this journal Article views: 6 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tdia20 Download by: [Lund University Libraries] Date: 19 July 2017, At: 08:18 Diatom Research,2017 https://doi.org/10.1080/0269249X.2017.1335240 Freshwater diatoms in the Sajama, Quelccaya, and Coropuna glaciers of the South American Andes 1 1 2 3 D. MARIE WEIDE ∗,SHERILYNC.FRITZ,BRUCEE.BRINSON, LONNIE G. THOMPSON & W. EDWARD BILLUPS2 1Department of Earth and Atmospheric Sciences, University of Nebraska-Lincoln, Lincoln, NE, USA 2Department of Chemistry, Rice University, Houston, TX, USA 3School of Earth Sciences and Byrd Polar and Climate Research Center, The Ohio State University, Columbus, OH, USA Diatoms in ice cores have been used to infer regional and global climatic events. These archives offer high-resolution records of past climate events, often providing annual resolution of environmental variability during the Late Holocene. -
Archaeological, Radiological, and Biological Evidence Offer Insight Into Inca Child Sacrifice
Archaeological, radiological, and biological evidence offer insight into Inca child sacrifice Andrew S. Wilsona,1, Emma L. Browna, Chiara Villab, Niels Lynnerupb, Andrew Healeyc, Maria Constanza Cerutid, Johan Reinharde, Carlos H. Previglianod,2, Facundo Arias Araozd, Josefina Gonzalez Diezd, and Timothy Taylora,3 aDepartment of Archaeological Sciences, and cCentre for Chemical and Structural Analysis, University of Bradford, Bradford BD7 1DP, United Kingdom; bLaboratory of Biological Anthropology, Department of Forensic Medicine, Faculty of Health Sciences, University of Copenhagen, Blegdamsvej 3, DK-2200 Copenhagen N, Denmark; dInstitute of High Mountain Research, Catholic University of Salta, Salta A4400FYP, Argentina; and eNational Geographic Society, Washington, DC 20036 Edited by Charles Stanish, University of California, Los Angeles, CA, and approved June 18, 2013 (received for review March 21, 2013) Examination of three frozen bodies, a 13-y-old girl and a girl and defining, element of a capacocha ritual. We also recognize that boy aged 4 to 5 y, separately entombed near the Andean summit the capacocha rite analyzed here was embedded within a multi- of Volcán Llullaillaco, Argentina, sheds new light on human sac- dimensional imperial ideology. rifice as a central part of the Imperial Inca capacocha rite, de- The frozen remains of the ∼13-y-old “Llullaillaco Maiden,” the scribed by chroniclers writing after the Spanish conquest. The 4- to 5-y-old “Llullaillaco Boy,” and the 4- to 5-y-old “Lightning high-resolution diachronic data presented here, obtained directly Girl” provide unusual and valuable analytical opportunities. Their from scalp hair, implies escalating coca and alcohol ingestion in the posture and placement within the shrine, surrounded by elite lead-up to death. -
Universidad Nacional De San Agustín Facultad De Ingeniería Geológica Geofísica Y Minas Escuela Profesional De Ingeniería Geológica
UNIVERSIDAD NACIONAL DE SAN AGUSTÍN FACULTAD DE INGENIERÍA GEOLÓGICA GEOFÍSICA Y MINAS ESCUELA PROFESIONAL DE INGENIERÍA GEOLÓGICA “ESTUDIO GEOLÓGICO, PETROGRÁFICO Y GEOQUÍMICO DEL COMPLEJO VOLCÁNICO AMPATO - SABANCAYA (Provincia Caylloma, Dpto. Arequipa)” Tesis presentada por: Bach. Rosmery Delgado Ramos Para Optar el Grado Académico de Ingeniero Geólogo AREQUIPA – PERÚ 2012 AGRADECIMIENTOS Quiero manifestar mis más sinceros agradecimientos a todas las personas que fueron parte esencial en mi formación profesional, personal y toda mi vida. Agradezco a mis padres, Victor R. Delgado Delgado y Rosa Luz Ramos Vega, por su constante apoyo y que a pesar de las dificultades y caídas siempre estaban conmigo para cuidarme, ayudarme y sobre todo amarme. A mis hermanos Renzo R. y Angela V. Delgado Ramos que con su optimismo y perseverancia me ayudaron a enfrentar los caminos difíciles de la vida y seguir con mis ideales. Agradezco también a mis asesores al Dr. Marco Rivera y Dr. Pablo Samaniego, que con su paciencia, consejos, regaños, apoyo incondicional y sus grandes enseñanzas, cultivaron en mí la pasión por la investigación y las ganas de alcanzar mis objetivos. Agradezco al Instituto Geológico Minero y Metalúrgico y al convenio de colaboración con el IRD a cargo del Dr. Pablo Samaniego, por la beca que me otorgó durante el período en el cual realice mi tesis. Gracias a mi asesor de tesis el Dr. Fredy García de la Universidad Nacional de San Agustín que por su revisión detallada y gran apoyo benefició en este trabajo. Agradezco al SENAMHI por proporcionarme los datos de clima, fundamentales para el desarrollo de esta tesis. -
La Cosmovisión Religiosa Andina Y El Rito De La Capacocha
La cosmovisión religiosa andina y el rito de la Capacocha The Andean religious world view and the rite of the Capacocha Recibido: 10/09/2009 María del Carmen Martín Rubio Aprobado: 05/10/2009 Universidad Complutense. Madrid [email protected] RESUMEN A raíz de los recientes descubrimientos de ofrendas de niños y niñas de escasa edad en las altas cumbres nevadas del Perú, Chile y Argentina, decidí profundizar las investigaciones acerca de las motivaciones, patrones de comportamiento y las prácticas rituales que acompañaron a esta forma de sacrificios humanos a las deidades andinas. Basamos nuestros estudios en la versión de una serie de arqueólogos y cronistas, especialmente Betanzos, quien narra con lujo de detalles, cómo estos niños eran «enterrados vivos por todos los lugares, donde había estado el inca, mil niños y mil niñas de cuatro y cinco años». Se describe a «la niña de Tanta Cachua», hacemos un detenido análisis de «la momia de Ampato: ‘Juanita’», «Las momias de Salta», la mujeres y niños acompañantes en la muerte, y por último, se señala la supervivencia del ancestral culto a los Apus. Palabras clave: Capacocha, ritual, teocracia, ofrendas, ajuar funerario, culto. ABSTRACT Following recent discoveries of offerings from small children age into snow-covered mountains of Peru, Chile and Argentina, decided to intensify the research on the motivations, behavioral patterns and ritual practices that accompanied this form human sacrifices to Andean deities. We base our studies on the release of a number of archaeologists and writers, especially Betan- zos, who narrates in detail how these children were «buried alive by all the places where the Inca had a thousand children and four thousand girls and five years. -
Scale Deformation of Volcanic Centres in the Central Andes
letters to nature 14. Shannon, R. D. Revised effective ionic radii and systematic studies of interatomic distances in halides of 1–1.5 cm yr21 (Fig. 2). An area in southern Peru about 2.5 km and chalcogenides. Acta Crystallogr. A 32, 751–767 (1976). east of the volcano Hualca Hualca and 7 km north of the active 15. Hansen, M. (ed.) Constitution of Binary Alloys (McGraw-Hill, New York, 1958). 21 16. Emsley, J. (ed.) The Elements (Clarendon, Oxford, 1994). volcano Sabancaya is inflating with U LOS of about 2 cm yr . A third 21 17. Tanaka, H., Takahashi, I., Kimura, M. & Sobukawa, H. in Science and Technology in Catalysts 1994 (eds inflationary source (with ULOS ¼ 1cmyr ) is not associated with Izumi, Y., Arai, H. & Iwamoto, M.) 457–460 (Kodansya-Elsevier, Tokyo, 1994). a volcanic edifice. This third source is located 11.5 km south of 18. Tanaka, H., Tan, I., Uenishi, M., Kimura, M. & Dohmae, K. in Topics in Catalysts (eds Kruse, N., Frennet, A. & Bastin, J.-M.) Vols 16/17, 63–70 (Kluwer Academic, New York, 2001). Lastarria and 6.8 km north of Cordon del Azufre on the border between Chile and Argentina, and is hereafter called ‘Lazufre’. Supplementary Information accompanies the paper on Nature’s website Robledo caldera, in northwest Argentina, is subsiding with U (http://www.nature.com/nature). LOS of 2–2.5 cm yr21. Because the inferred sources are more than a few kilometres deep, any complexities in the source region are damped Acknowledgements such that the observed surface deformation pattern is smooth. -
Area Changes of Glaciers on Active Volcanoes in Latin America Between 1986 and 2015 Observed from Multi-Temporal Satellite Imagery
Journal of Glaciology (2019), 65(252) 542–556 doi: 10.1017/jog.2019.30 © The Author(s) 2019. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Area changes of glaciers on active volcanoes in Latin America between 1986 and 2015 observed from multi-temporal satellite imagery JOHANNES REINTHALER,1,2 FRANK PAUL,1 HUGO DELGADO GRANADOS,3 ANDRÉS RIVERA,2,4 CHRISTIAN HUGGEL1 1Department of Geography, University of Zurich, Zurich, Switzerland 2Centro de Estudios Científicos, Valdivia, Chile 3Instituto de Geofisica, Universidad Nacional Autónoma de México, Mexico City, Mexico 4Departamento de Geografía, Universidad de Chile, Chile Correspondence: Johannes Reinthaler <[email protected]> ABSTRACT. Glaciers on active volcanoes are subject to changes in both climate fluctuations and vol- canic activity. Whereas many studies analysed changes on individual volcanoes, this study presents for the first time a comparison of glacier changes on active volcanoes on a continental scale. Glacier areas were mapped for 59 volcanoes across Latin America around 1986, 1999 and 2015 using a semi- automated band ratio method combined with manual editing using satellite images from Landsat 4/5/ 7/8 and Sentinel-2. Area changes were compared with the Smithsonian volcano database to analyse pos- sible glacier–volcano interactions. Over the full period, the mapped area changed from 1399.3 ± 80 km2 − to 1016.1 ± 34 km2 (−383.2 km2)or−27.4% (−0.92% a 1) in relative terms. -
Archaeological, Radiological, and Biological Evidence Offer Insight Into Inca Child Sacrifice
Archaeological, radiological, and biological evidence offer insight into Inca child sacrifice Andrew S. Wilsona,1, Emma L. Browna, Chiara Villab, Niels Lynnerupb, Andrew Healeyc, Maria Constanza Cerutid, Johan Reinharde, Carlos H. Previglianod,2, Facundo Arias Araozd, Josefina Gonzalez Diezd, and Timothy Taylora,3 aDepartment of Archaeological Sciences, and cCentre for Chemical and Structural Analysis, University of Bradford, Bradford BD7 1DP, United Kingdom; bLaboratory of Biological Anthropology, Department of Forensic Medicine, Faculty of Health Sciences, University of Copenhagen, Blegdamsvej 3, DK-2200 Copenhagen N, Denmark; dInstitute of High Mountain Research, Catholic University of Salta, Salta A4400FYP, Argentina; and eNational Geographic Society, Washington, DC 20036 Edited by Charles Stanish, University of California, Los Angeles, CA, and approved June 18, 2013 (received for review March 21, 2013) Examination of three frozen bodies, a 13-y-old girl and a girl and defining, element of a capacocha ritual. We also recognize that boy aged 4 to 5 y, separately entombed near the Andean summit the capacocha rite analyzed here was embedded within a multi- of Volcán Llullaillaco, Argentina, sheds new light on human sac- dimensional imperial ideology. rifice as a central part of the Imperial Inca capacocha rite, de- The frozen remains of the ∼13-y-old “Llullaillaco Maiden,” the scribed by chroniclers writing after the Spanish conquest. The 4- to 5-y-old “Llullaillaco Boy,” and the 4- to 5-y-old “Lightning high-resolution diachronic data presented here, obtained directly Girl” provide unusual and valuable analytical opportunities. Their from scalp hair, implies escalating coca and alcohol ingestion in the posture and placement within the shrine, surrounded by elite lead-up to death. -
Dirección De Preparación Cepig
DIRECCIÓN DE PREPARACIÓN CEPIG INFORME DE POBLACIÓN EXPUESTA ANTE CAÍDA DE CENIZAS Y GASES, PRODUCTO DE LA ACTIVIDAD DEL VOLCÁN UBINAS PARA ADOPTAR MEDIDAS DE PREPARACIÓN Fuente: La República ABRIL, 2015 1 INSTITUTO NACIONAL DE DEFENSA CIVIL (INDECI) CEPIG Informe de población expuesta ante caída de cenizas y gases, producto de la actividad del volcán Ubinas para adoptar medidas de preparación. Instituto Nacional de Defensa Civil. Lima: INDECI. Dirección de Preparación, 2015. Calle Dr. Ricardo Angulo Ramírez Nº 694 Urb. Corpac, San Isidro Lima-Perú, San Isidro, Lima Perú. Teléfono: (511) 2243600 Sitio web: www.indeci.gob.pe Gral. E.P (r) Oscar Iparraguirre Basauri Director de Preparación del INDECI Ing. Juber Ruiz Pahuacho Coordinador del CEPIG - INDECI Equipo Técnico CEPIG: Lic. Silvia Passuni Pineda Lic. Beneff Zuñiga Cruz Colaboradores: Pierre Ancajima Estudiante de Ing. Geológica 2 I. JUSTIFICACIÓN En el territorio nacional existen alrededor de 400 volcanes, la mayoría de ellos no presentan actividad. Los volcanes activos se encuentran hacia el sur del país en las regiones de Arequipa, Moquegua y Tacna, en parte de la zona volcánica de los Andes (ZVA), estos son: Coropuna, Valle de Andagua, Hualca Hualca, Sabancaya, Ampato, Misti en la Región Arequipa; Ubinas, Ticsani y Huaynaputina en la región Moquegua, y el Yucamani y Casiri en la región Tacna. El Volcán Ubinas es considerado el volcán más activo que tiene el Perú. Desde el año 1550, se han registrado 24 erupciones aprox. (Rivera, 2010). Estos eventos se presentan como emisiones intensas de gases y ceniza precedidos, en algunas oportunidades, de fuertes explosiones. Los registros históricos señalan que el Volcán Ubinas ha presentado un Índice máximo de Explosividad Volcánica (IEV) (Newhall & Self, 1982) de 3, considerado como moderado a grande. -
Source Model for Sabancaya Volcano Constrained by Dinsar and GNSS Surface Deformation Observation
remote sensing Article Source Model for Sabancaya Volcano Constrained by DInSAR and GNSS Surface Deformation Observation Gregorio Boixart 1, Luis F. Cruz 2,3 , Rafael Miranda Cruz 2, Pablo A. Euillades 4, Leonardo D. Euillades 4 and Maurizio Battaglia 5,6,* 1 Instituto de Estudios Andinos, Universidad de Buenos Aires-CONICET, Buenos Aires 1428, Argentina; [email protected] 2 Escuela Profesional de Ingeniería Geofísica, Universidad Nacional de San Agustín de Arequipa, Arequipa 04001, Peru; [email protected] (L.F.C.); [email protected] (R.M.C.) 3 Observatorio Vulcanológico del INGEMMET, Instituto Geológico Minero y Metalúrgico, Arequipa 04001, Peru 4 Facultad de Ingeniería, Instituto CEDIAC & CONICET, Universidad Nacional de Cuyo, Mendoza M5502JMA, Argentina; [email protected] (P.A.E.); [email protected] (L.D.E.) 5 US Geological Survey, Volcano Disaster Assistance Program, NASA Ames Research Center, Moffett Field, CA 94035, USA 6 Department of Earth Sciences, Sapienza-University of Rome, 00185 Rome, Italy * Correspondence: [email protected] Received: 23 April 2020; Accepted: 3 June 2020; Published: 8 June 2020 Abstract: Sabancaya is the most active volcano of the Ampato-Sabancaya Volcanic Complex (ASVC) in southern Perú and has been erupting since 2016. The analysis of ascending and descending Sentinel-1 orbits (DInSAR) and Global Navigation Satellite System (GNSS) datasets from 2014 to 2019 imaged a radially symmetric inflating area, uplifting at a rate of 35 to 50 mm/yr and centered 5 km north of Sabancaya. The DInSAR and GNSS data were modeled independently. We inverted the DInSAR data to infer the location, depth, and volume change of the deformation source. -
Frozen Mummies from Andean Mountaintop Shrines: Bioarchaeology and Ethnohistory of Inca Human Sacrifice
Hindawi Publishing Corporation BioMed Research International Volume 2015, Article ID 439428, 12 pages http://dx.doi.org/10.1155/2015/439428 Review Article Frozen Mummies from Andean Mountaintop Shrines: Bioarchaeology and Ethnohistory of Inca Human Sacrifice Maria Constanza Ceruti Instituto de Investigaciones de Alta Montana,˜ Universidad Catolica´ de Salta, Campus Castanares,˜ 4400 Salta, Argentina Correspondence should be addressed to Maria Constanza Ceruti; [email protected] Received 22 December 2014; Accepted 5 April 2015 Academic Editor: Andreas G. Nerlich Copyright © 2015 Maria Constanza Ceruti. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. This study will focus on frozen mummies of sacrificial victims from mounts Llullaillaco (6739 m), Quehuar (6130 m), ElToro (6160 m), and the Aconcagua massif. These finds provide bioarchaeological data from mountaintop sites that has been recovered in scientifically controlled excavations in the northwest of Argentina, which was once part of the southern province of the Inca Empire. Numerous interdisciplinary studies have been conducted on the Llullaillaco mummies, including radiological evaluations by conventional X-rays and CT scans, which provided information about condition and pathology of the bones and internal organ, as well as dental studies oriented to the estimation of the ages of the three children at the time of death. Ancient DNA studies and hair analysis were also performed in cooperation with the George Mason University, the University of Bradford, and the Laboratory of Biological Anthropology at the University of Copenhagen. Ethnohistorical sources reveal interesting aspects related to the commemorative, expiatory, propitiatory, and dedicatory aspects of human sacrifice performed under Inca rule. -
Glacier Evolution in the South West Slope of Nevado Coropuna
Glacier evolution in the South West slope of Nevado Coropuna (Cordillera Ampato, Perú) Néstor Campos Oset Master Project Master en Tecnologías de la Información Geográfica (TIG) Universidad Complutense de Madrid Director: Prof. David Palacios (UCM) Departamento de Análisis Geográfico Regional y Geografía Física Grupo de Investigación en Geografía Física de Alta Montaña (GFAM) ACKNOWLEDGEMENTS I would like to gratefully and sincerely thank Dr. David Palacios for his help and guidance during the realization of this master thesis. I would also like to thank Dr. José Úbeda for his assistance and support. Thanks to GFAM-GEM for providing materials used for the analysis. And last but not least, a special thanks to my family, for their encouragement during this project and their unwavering support in all that I do. 2 TABLE OF CONTENTS CHAPTER 1 INTRODUCTION...................................................................................... 4 1.1 Geographic settings ................................................................................................ 4 1.2 Geologic settings .................................................................................................... 6 1.3 Climatic setting....................................................................................................... 8 1.4 Glacier hazards ..................................................................................................... 10 1.5 Glacier evolution ................................................................................................. -
GEOLOGY AS a WAY of TURISM PROMOTION.Pdf
ENERGY AND MINES SECTOR TheSPECIAL of the Month GEOLOGICAL, MINING AND METALLURGICAL INSTITUTE Since 2006, the Geological, Mining and Metallurgical Institute - INGEMMET has the "Heritage and Geotourism" project. It promotes the conservation and enhancement of different areas across the country with a high geological value. 1 TOURIST ATTRACTIONS PROMOTED Paracas National Reserve BY INGEMMET It is located 250 kilometers south of Lima, Ica Marcahuasi Region. It is one of the few places where you can see remains of an ancient mountain It is a volcanic plateau located in the town of range with rocks over 400 million years old in eotourism makes reference to a type of G San Pedro de Casta, at 3 185 meters above strata and with plant remains, rocks with sustainable tourism. It aims to highlight the sea level on the left bank of the Santa Eulalia fossils from marine environments. There are geological diversity (geodiversity) and then river basin, and 80 kilometers east of Lima. 25 geosites inventoried by INGEMMET. the geological heritage (geoheritage) of a The geoforms of the Marcahuasi rock forest The geological information in the guide certain territory. Also, to promote the are the result of the effects of rain, snow, ice, elaborated by INGEMMET served as a script conservation of its resources heat and wind. They all molded diverse forms for the current Interpretation Center in the (geoconservation) and education in earth GEOLOGICAL in the volcanic deposits. In this way, it allows reserve, as well as for the signage of some sciences (geoeducation) which develops the visitor to imagine the strangest and most geosites such as La Catedral, Playa La Mina, awareness among the people.