Sillar Chapter 4 Powerful Places
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Viracocha 1 Viracocha
ווירָאקוצֱ'ה http://www.google.com/url?sa=t&rct=j&q=&esrc=s&source=web&cd=37&ved=0COYCEBYwJA&url=http %3A%2F%2Fxa.yimg.com%2Fkq%2Fgroups%2F35127479%2F1278251593%2Fname%2F14_Ollantaytam bo_South_Peru.ppsx&ei=TZQaVK- 1HpavyASW14IY&usg=AFQjCNEHlXgmJslFl2wTClYsRMKzECmYCQ&sig2=rgfzPgv5EqG-IYhL5ZNvDA ויראקוצ'ה http://klasky-csupo.livejournal.com/354414.html https://he.wikipedia.org/wiki/%D7%A7%D7%95%D7%9F_%D7%98%D7%99%D7%A7%D7%99 ווירקוצ'ה فيراكوتشا http://www.startimes.com/?t=20560975 Viracocha 1 Viracocha Viracocha Great creator god in Inca mythology Offspring (according to some legends) Inti, Killa, Pachamama This article is about the Andean deity. For other uses, see Wiraqucha (disambiguation). Viracocha is the great creator god in the pre-Inca and Inca mythology in the Andes region of South America. Full name and some spelling alternatives are Wiracocha, Apu Qun Tiqsi Wiraqutra, and Con-Tici (also spelled Kon-Tiki) Viracocha. Viracocha was one of the most important deities in the Inca pantheon and seen as the creator of all things, or the substance from which all things are created, and intimately associated with the sea.[1] Viracocha created the universe, sun, moon, and stars, time (by commanding the sun to move over the sky) and civilization itself. Viracocha was worshipped as god of the sun and of storms. He was represented as wearing the sun for a crown, with thunderbolts in his hands, and tears descending from his eyes as rain. Cosmogony according to Spanish accounts According to a myth recorded by Juan de Betanzos,[2] Viracocha rose from Lake Titicaca (or sometimes the cave of Paqariq Tampu) during the time of darkness to bring forth light. -
31 a Preliminary Study Of
31 A PRELIMINARY STUDY OF THE: TERTIARY VOLCANIC AND SEDIMENTARY ROCKS, GÜMELE, ESKİŞEHİR Eskişehir, Gümele Çevresindeki Tersiyer Volkanik ve Sedimanter Kayaçlarda Bir Ön Çalışma Taylan Lünel Middle East Technical University, Department of Geological Engineering Ankara ÖZ. — Seyitgazi-Eskişehir antiklinoriumu'nun çok fazla deforme olmuş ve metamorfizmaya uğramış kayaçlarının kuzey-kuzeybatısında bulunan sedimanter ve volkanik kayaçlar incelenmiştir. Karasal ve gölsel fasiyesde meydana gelen Tersi- yer sedimanter kayaçlar Güney Eskişehir küvetinde olunmuşlardır. Karasal fasiye- si meydana getiren kayaç birimlerini kaba kumtaşları, kumtaşları, bitki kalıntıları ihtiva eden kil ve marnlar ve serpantinit blokları taşıyan bazal konglomerası teşkil etmektedir. Gölsel fasiyes ise genellikle killi ve tüflü kalkerler, kalkerler, marnlar, kon- glomeralar ve tüflerden meydana gelmiştir. Küvetteki en eski sedimanlar ve piroklas- tikler Alt Miosen'de oluşmuşlardır. Yataya yakın konumlanmış bazik-intermediyar lav akıntıları Pliosen yaşlı olup Altüst Neojen sedimantasyon kesikliğinde meyda- na gelmiştir. Üst Neojen sedimanter kayaçları intermediyar-basaltik volkaniklerin üzerinde ince bandlar şeklinde bulunurlar. Bu birim marn ve kalkerlerden meyda- na gelmiştir. Alt Miosen’de asid volkanik faaliyetler neticesinde meydana gelen sil- lar (unweldd tuffs) oligomikt konglomeralardan evvel teşekkül etmiştir. Bu volkanik aktitivite muhtemelen kesikli ve kısıtlı olarak devam etmiş ve tüflü kalkerleri mey- dana getirmiştir. Pliosen yaşlı bazik-intermediyar -
Viracocha Christ Among the Ancient Peruvians?
Viracocha Christ among the Ancient Peruvians? Scott Hoyt There came from a southern direction a white man of great stature, who, by his aspect and presence, called forth great veneration and obedience. This man who thus appeared had great power, insomuch that he could change plains into mountains, and great hills into valleys, and make water flow out of stones. As soon as such power was beheld, the people called him the Maker of created things, the Prince of all things, Father of the Sun. For they say that he performed other wonders, giving life to men and animals, so that by his hand marvellous great benefits were conferred on the people. In many places he gave orders to men how they should live, and he spoke lovingly to them . admonishing them that they should do good . and that they should be loving and charitable to all. In most parts he is generally called Ticiviracocha. [And] that wherever [he] . came and there were sick, he healed them, and where there were blind he gave them sight by only uttering words.1 —Pedro de Cieza de León, Catholic Historian, 1550 iracocha was the principal deity of ancient Peru, and according to Vthe cronistas (Catholic historians, mostly priests, arriving in Peru 1. Pedro de Cieza de León, The Second Part of the Chronicle of Peru (El Seno- rio de los Incas), trans. and ed. Clements R. Markham (1874; London: Hakluyt Society, 1883; repr. Boston: Elibron Classics, 1999), 5–6. Senorio was originally handwritten in 1550. Citations are to the 1999 edition. BYU Studies Quarterly 54, no. -
Myths of Survival and Heritage in Incan Religion
Viva Los Incas: Myths of Survival and Heritage in Incan Religion Emily Scarbrough ___________________________________________________________ Religion has taken on many forms throughout history, each revealing much about those who believed in them. In the Incan empire, religion was embraced as an explanation for natural phenomena and the formation of society. Religion served an important purpose as it developed into a complex set of myths that governed the empire. Their polytheistic religion had several deities who controlled how the world functioned, with most important of these gods controlling the sun. Looking at the mythology that developed in the Incan empire reveals unrelenting dedication to surviving as individuals and as a united society. Incan mythology seems to enshrine, above all else, a belief in preservation; the mythology suggests a belief in preserving the societal hierarchy, livelihood, and the lineage of the Inca leader. Standing as the cornerstone of Incan religion was Inti, the sun god. As the expression of the sun and light, Inti was responsible for the success of the harvest season. The sun gave life to maize, potatoes, and quinoa, which in turn ensured a steady food supply. While he did not create the Incas, he ensured their livelihood. To thank Inti, temples of the sun were built, prayers spoke, and tribute paid through the sacrifice of crops, llamas, and, in extreme cases, young children.1 Inti was also the subject of the most important of the many Incan festivals, Inti Raymi. Despite centuries of Spanish influence, the festival is still celebrated in modern day Peru, as a reminder of their Incan heritage. -
Geology of the South-Central Pueblo Mountains, Oregon-Nevada
AN ABSTRACT OF THE THESIS OF WINTHROP ALLEN ROWE for the MASTER OF SCIENCE (Name) (Degree) in GEOLOGY presented on lurd IL 1q4() Major) (Sate) Title: GEOLOGY OF THE SOUTH-CENTRAL PUEBLO MOUNTAINS, OREGON-NEVADA Abstract approved: Redacted for Privacy Dr. Harold E. En lows The thesis area consists of 33 square miles in the south-central Pueblo Mountains of Humboldt County, Nevada and Harney County, Oregon.The Pueblo Mountains are tilted fault block mountains found in the extreme northwestern part of the Basin and Range province and were produced during Early Tertiary Basin and Range orogeny. Northwest and northeast trending faults of Late Tertiary time have since cut the entire stratigraphic sequence. The oldest rocks exposed are metamorphosed Permian to Triassic eugeosynclinal sedimentary rocks.The metamorphic sequence is intruded by several granitic plutons of Late Jurassic to Middle Cretaceous age. A thick sequence of Miocene basalt flows unconformably overlies the pre- Tertiary rocks. A slight angular unconformity separates the basalt sequence from overlying Miocene tuffaceous sedimentary rocks, sillar flows, and welded tuffs. Unconsolidated deposits of Quaternary alluvium include alluvial fan and lacustrine sediments. Mineralization within the area includes several gold prospects, a mercury prospect, and a possible copper deposit.The copper prospect consists of a large gossan (6, 000 feet by 3, 000 feet). Mineralization and alteration from a Cretaceous porphyritic quartz monzonite intrusion has produced potassic and quartz sericite -
Neogene Ignimbrites in the Area of Arequipa Southern Peru
NEOGENE IGNIMBRITES IN THE AREA OF AREQUIPA, SOUTHERN PERU: CORRELATIONS BASED ON FIELD OBSERVATIONS, GEOCHElVIISTRY AND GEOCHRONOLOGY Perrine PAQUEREAU (1), Jean-Claude THOURET (1), Gerhard WORNER (2), and Michel FORNARl (3) (1) Laboratoire Magmas et Volcans, Universite Blaise Pascal et CNRS, 63038 Clermont-Ferrand, France ([email protected]) ([email protected] -bpclermont.fr) (2) GZG, Abt. Geochemie, Goldschmidstrasse 1, Universitat Gottingen, 37077 Gottingen, Germany ([email protected]) (3) IRD, UMR Geosciences Azur, Sophia Antipolis, Pare Valrose, 06108 Nice cedex 2, France ([email protected]) KEY WORDS: ignimbrite, Arequipa, Peru, correlation, mineralogy, chronology. INTRODUCTION In the area of Arequipa, the ignimbrites termed "sillars" (Fenner, 1948; Jenks and Goldich, 1956) are indurated, generally nonwelded pyroclastic-flow deposits of dacitic and rhyolitic composition and middle Miocene to late Pliocene in age (this study). They encompass incipiently welded or sintered vitric tuffs, indurated by vapor-phase crystallisation, and previously welded but devitrified tuffs. They mantle an area of roughly 600 km2 around the quaternary stratovolcanoes of Chachani and Misti and they fill the depression of Arequipa with a thickness of 100 m to as much as 200 m in the Rio Chili canyon (Fig. 1). Similar ignimbrites 461 have flowed downvalley the Rio Chili and Rio Yura at least 30 km south and southwest of Arequipa beyond the confluence ofthe three rivers into the Rio Vitor canyon. Figure 2 shows two stratigraphic sections in the valley of Rio Chili that cuts the flank of the Western Cordi1lera. They encompass COMPOSITE SECTION RIOCHILl, EASTSIDE,CHARCANI two ignimbrite _'" cooling units above lyJ fT' Misti lava flows 0.83 Ma T, 00000 scona flow deposit the Jurassic ~----- nonwelded ignimbrite "pre-Misti" basement: the lavallOW ..... -
Field T Rip Guide Book
Volume n° 3 - from D01 to P13 32nd INTERNATIONAL GEOLOGICAL CONGRESS IGNIMBRITIC DEPOSITS IN CENTRAL ITALY: PYROCLASTIC PRODUCTS OF THE QUATERNARY AGE AND ETRUSCAN FOOTPATHS Leader: G. Nappi Associate Leaders: L. Valentini, M. Mattioli Field Trip Guide Book - P09 Field Trip Florence - Italy August 20-28, 2004 Post-Congress P09 P09_copertina_R_OK C 25-05-2004, 9:25:21 The scientific content of this guide is under the total responsibility of the Authors Published by: APAT – Italian Agency for the Environmental Protection and Technical Services - Via Vitaliano Brancati, 48 - 00144 Roma - Italy Series Editors: Luca Guerrieri, Irene Rischia and Leonello Serva (APAT, Roma) English Desk-copy Editors: Paul Mazza (Università di Firenze), Jessica Ann Thonn (Università di Firenze), Nathalie Marléne Adams (Università di Firenze), Miriam Friedman (Università di Firenze), Kate Eadie (Freelance indipendent professional) Field Trip Committee: Leonello Serva (APAT, Roma), Alessandro Michetti (Università dell’Insubria, Como), Giulio Pavia (Università di Torino), Raffaele Pignone (Servizio Geologico Regione Emilia-Romagna, Bologna) and Riccardo Polino (CNR, Torino) Acknowledgments: The 32nd IGC Organizing Committee is grateful to Roberto Pompili and Elisa Brustia (APAT, Roma) for their collaboration in editing. Graphic project: Full snc - Firenze Layout and press: Lito Terrazzi srl - Firenze P09_copertina_R_OK D 25-05-2004, 9:24:28 Volume n° 3 - from D01 to P13 32nd INTERNATIONAL GEOLOGICAL CONGRESS IGNIMBRITIC DEPOSITS IN CENTRAL ITALY: PYROCLASTIC PRODUCTS OF THE QUATERNARY AGE AND ETRUSCAN FOOTPATHS AUTHORS: G. Nappi, L. Valentini, M. Mattioli (Università di Urbino - Italy) Florence - Italy August 20-28, 2004 Post-Congress P09 P09_R_OK A 25-05-2004, 9:28:38 Front Cover: Necropolis of Sovana, Tomba Ildebranda. -
Geochemical Characterization and Fission Track
Geochemical characterization and fission track ages of historical ignimbrite flows : the sillar of Arequipa (Western cordillera, Southern Peru) Nicole Vatin Perignon, Gérard Poupeau, Richard Oliver, Ludovic Bellot-Gurlet, Erika Labrin, Francine Keller, Salas Guido To cite this version: Nicole Vatin Perignon, Gérard Poupeau, Richard Oliver, Ludovic Bellot-Gurlet, Erika Labrin, et al.. Geochemical characterization and fission track ages of historical ignimbrite flows : the sillarof Arequipa (Western cordillera, Southern Peru). Géodynamique andine : résumés étendus, ORSTOM, pp.461-464, 1993, Géodynamique Andine : Symposium International 2, Oxford (UK), 21-23 october 1993, 2-7099-1154-X. hal-02133522 HAL Id: hal-02133522 https://hal.archives-ouvertes.fr/hal-02133522 Submitted on 18 May 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Second ISAG, Oxford (UK),21 -23f911993 461 GEOCHEMICAL CHARACTERIZATION AND FISSION TRACK OFAGES HISTORICAL IGNIMBRITE FLOWS: THE SILLAR OF AREQUIPA (WESTERN CORDILLERA, SOUTHERN PERU) ATIN-PERIGNON( 1, Gérard PO ( 1, Richar?, p. OLIVERNico1?2Y , Ludovic BELL T-GURLET ('1 yPyril@)LABRIN , Francine KELLER?' ) & Guido SALAS A . (1) Laboratoire de Géologie,UA 69 CNRS, Université Joseph- Fourier, 15, rue Maurice Gignoux, 38031 Grenoble Cedex, France (2) Institut Laüe-Langevin, B.P.I56X, Avenue des Martyrs, 38042 Grenoble Cedex, France (3) Universidad Nacional San Agustin, Casilla 1203, Areq- uipa, PerG RESUMEN El SA tufo corresponde a unahica venida volchica de en- friamiento con dos unidades. -
Pedro Sarmiento De Gamboa History of the Incas Translated by Sir Clements Markham K.C.B
Pedro Sarmiento de Gamboa History of the Incas Translated by Sir Clements Markham K.C.B. (1907) In parentheses Publications Peruvian Series Cambridge, Ontario 2000 To His Sacred C¾sarian Majesty the King, Don Felipe, Our Lord. Among the excellencies, O sovereign and catholic Philip, that are the glorious decorations of princes, placing them on the highest pinnacle of estimation, are, according to the father of Latin eloquence, generosity, kindness, and liberality. And as the Roman Consuls held this to be the principal praise of their glory, they had this title curiously sculptured in marble on the Quirinal and in the forum of TrajanÑÒMost powerful gift in a Prince is liberality.Ó1 For this kings who desired much to be held dear by their own people and to be feared by strangers, were incited to acquire the name of liberal. Hence that royal sentence became immortal ÒIt is right for kings to give.Ó As this was a quality much valued among the Greeks, the wise Ulysses, conversing with Antinous, 2 King of the Ph¾acians, saidÑÒYou are something like a king, for you know how to give, better than others.Ó Hence it is certain that liberality is a good and necessary quality of kings. I do not pretend on this ground, most liberal monarch, to insinuate to your Majesty the most open frankness, for it would be very culpable on my part to venture to suggest a thing which, to your Majesty, is so natural that you would be unable to live without it. Nor will it happen to so high minded and liberal a lord and king, what befell the Emperor Titus who, remembering once, during suppertime, that he had allowed one day to pass without doing some good, gave utterance to this laudable animadversion of himself ÒO friends! I have lost a day.Ó3 For not only does your Majesty not miss a day, but not even an hour, without obliging all kinds of people with benefits and most gracious liberality. -
Censimento E Selezione Dei Geositi Della Provincia Di Viterbo
DIPARTIMENTO DI ECOLOGIA E SVILUPPO ECONOMICO SOSTENIBILE (DECOS) PROGETTO PILOTA GEOPARCO DELLA TUSCIA CENSIMENTO E SELEZIONE DEI GEOSITI DELLA PROVINCIA DI VITERBO RELAZIONE GENERALE Responsabile scientifico: Prof. Giuseppe Nascetti Gruppo di studio: Dott.ssa Antonella Baiocchi Dott.ssa Francesca Lotti Prof. Vincenzo Piscopo Dott. Mario Valletta Febbraio, 2010 1 INDICE 1. Introduzione pag. 1 2. Lineamenti geomorfologico pag. 2 3. Quadro geologico del Geoparco della Tuscia pag. 6 3.1 Unità sedimentarie pag. 6 3.1.1 Unità della Successione Toscana e basamento metamorfico pag. 6 3.1.2 Unità dei flysch alloctoni pag. 9 3.1.3 Unità postorogene pag. 10 3.1.4 Unità del Quaternario pag. 13 3.2 Formazioni vulcaniche pag. 14 3.2.1 Distretto Vulcanico Vulsino pag. 16 3.2.2 Distretto Vulcanico Cimino pag. 21 3.2.3 Distretto Vulcanico Vicano pag. 23 4. Principali emergenze geologico-applicative, geominerarie e idrogeologiche pag. 26 5. Il concetto di Geosito pag. 30 6. Selezione dei Geositi dell’area della Provincia di Viterbo pag. 33 7. Bibliografia consultata pag. 50 2 1. INTRODUZIONE La presente relazione illustra i risultati delle indagini geologiche condotte nell’ambito del territorio della Provincia di Viterbo, finalizzate alla individuazione di quei Geositi che, per avere una particolare rilevanza per esemplarità di processi non comuni, non ripetitivi e non ubiquitari e di eventi del passato geologico, rivestissero peculiare importanza per la candidatura del Geoparco della Tuscia. Le ricerche condotte a tal fine si sono articolate in due fasi. La prima, si è identificata con l’esame, minuzioso ed integrato, di tutta la bibliografia esistente; la seconda, ha compreso una intensa e, ove ritenuto necessario, capillare attività di campagna. -
Mitos Y Leyendas De Colombia
MITOS Y LEYENDAS DE COLOMBIA VOLUMEN III Eugenia Villa Posse Para facilitar la lectura, se ha incluido en el primer tomo la bibliografía general de la obra. COLECCIÓN "Integración cultural" MITOS Y LEYENDAS DE COLOMBIA Investigación y compilación Eugenia Villa Posse ISBN 9978-60-003-5 (Colección) ISBN 9978-60-004-3 Editorial © IADAP Diego de Atienza y Av. América Telfs : 553684 - 554908 Fax : 593.2.563096 Apartados postales: 17-07-9184 / 17-01-555 Quito - Ecuador Derechos reservados conforme a la ley primera edición, diciembre 1993,1000 ejemplares DIRECTOR EJECUTIVO Eugenio Cabrera Merchán COORDINADOR DIFUSIÓN Víctor Manuel Guzmán DIAGRAMACION Y PORTADA Wilfrido Acosta Pineda LEVANTAMIENTO DE TEXTOS Nelly Jiménez Viana IMPRESIÓN Washington Padilla M. PARTE III MITOS PREHISPANICOS MUISCAS 5 Este tercer volumen denominado "Mitos Prehispánicos Muiscas", corresponde a la colección"Mitos y Leyendas de Colombia", que es una recopilación en tres tomos preparada por la investigadora colombiana Eugenia Villa Posse. 29. BOCHICA Chibcha - Región Cundiboyacense NOTA: TRIANA, Miguel, La civilización Chibcha, Cali, Edición Limitada por Carvajal y Compañía, 1972, p. 97-104. Esta versión del mito de Bochica es parte de un estudio más amplio, realizado por Miguel Triaría sobre aspectos culturales de los Chibchas, partiendo para su documentación de textos históricos y de escritos de cronistas. 9 Es lógica la concepción indígena de una entidad divina que personificase y simbolizase la potencialidad de las aguas en acción piadosa. A esta divinidad magnánima la llamaron los Chibchas Bochica. Era este dios incorpóreo, según lo estima el cronista; pero respondía a las plegarias de los fieles y dictaba leyes y modos de vivir. -
Thin-Skinned Tectonics in the Cordillera Oriental
NEOGENE IGNIMBRITES IN THE AREA OF AREQUIPA, SOUTHERN PERU: CORRELATIONS BASED ON FIELD OBSERVATIONS, GEOCHEMISTRY AND GEOCHRONOLOGY Perrine PAQUEREAU (1), Jean-Claude THOURET (1), Gerhard WÖRNER (2), and Michel FORNARI (3) (1) Laboratoire Magmas et Volcans, Université Blaise Pascal et CNRS, 63038 Clermont-Ferrand, France ([email protected]) ([email protected]) (2) GZG, Abt. Geochemie, Goldschmidstrasse 1, Universität Göttingen, 37077 Göttingen, Germany ([email protected]) (3) IRD, UMR Géosciences Azur, Sophia Antipolis, Parc Valrose, 06108 Nice cedex 2, France ([email protected]) KEY WORDS: ignimbrite, Arequipa, Peru, correlation, mineralogy, chronology. INTRODUCTION In the area of Arequipa, the ignimbrites termed "sillars" (Fenner, 1948; Jenks and Goldich, 1956) are indurated, generally nonwelded pyroclastic-flow deposits of dacitic and rhyolitic composition and middle Miocene to late Pliocene in age (this study). They encompass incipiently welded or sintered vitric tuffs, indurated by vapor-phase crystallisation, and previously welded but devitrified tuffs. They mantle an area of roughly 600 km² around the quaternary stratovolcanoes of Chachani and Misti and they fill the depression of Arequipa with a thickness of 100 m to as much as 200 m in the Rio Chili canyon (Fig.1). Similar ignimbrites Fig.1: Landsat image showing the extent and the probable source of ignimbrites 461 have flowed downvalley the Rio Chili and Rio Yura at least 30 km south and southwest of Arequipa beyond the confluence of the three rivers into the Rio Vitor canyon. Figure 2 shows two stratigraphic sections in the valley of Rio Chili that cuts the flank of the Western Cordillera.