A Review on Historical Earth Pigments Used in India's Wall Paintings

Total Page:16

File Type:pdf, Size:1020Kb

A Review on Historical Earth Pigments Used in India's Wall Paintings heritage Review A Review on Historical Earth Pigments Used in India’s Wall Paintings Anjali Sharma 1 and Manager Rajdeo Singh 2,* 1 Department of Conservation, National Museum Institute, Janpath, New Delhi 110011, India; [email protected] 2 National Research Laboratory for the Conservation of Cultural Property, Aliganj, Lucknow 226024, India * Correspondence: [email protected] Abstract: Iron-containing earth minerals of various hues were the earliest pigments of the prehistoric artists who dwelled in caves. Being a prominent part of human expression through art, nature- derived pigments have been used in continuum through ages until now. Studies reveal that the primitive artist stored or used his pigments as color cakes made out of skin or reeds. Although records to help understand the technical details of Indian painting in the early periodare scanty, there is a certain amount of material from which some idea may be gained regarding the methods used by the artists to obtain their results. Considering Indian wall paintings, the most widely used earth pigments include red, yellow, and green ochres, making it fairly easy for the modern era scientific conservators and researchers to study them. The present knowledge on material sources given in the literature is limited and deficient as of now, hence the present work attempts to elucidate the range of earth pigments encountered in Indian wall paintings and the scientific studies and characterization by analytical techniques that form the knowledge background on the topic. Studies leadingto well-founded knowledge on pigments can contribute towards the safeguarding of Indian cultural heritage as well as spread awareness among conservators, restorers, and scholars. Citation: Sharma, A.; Singh, M.R. A Review on Historical Earth Pigments Keywords: red ochre; green earth; black earth; yellow ochre; pigments; wall painting Used in India’s Wall Paintings. Heritage 2021, 4, 1970–1994. https:// doi.org/10.3390/heritage4030112 1. Introduction Academic Editors: Diego Tamburini and Francesco Paolo Romano Since time immemorial, wall paintings have been done in almost all countries. Paint- ings of all kinds, encompassing all types of wall paintings as well, are a valuable part of Received: 17 June 2021 many countries’ cultural heritage. In prehistoric paintings, the artistic style was primitive, Accepted: 23 August 2021 and the techniques were also very basic, with the paint being applied directly onto the Published: 26 August 2021 rock surface. As a result of this, the pigments seep through the pores and coarse surface of rocks. Later, more complex designs and figures were painted on walls, which were often Publisher’s Note: MDPI stays neutral prepared with several layers of plaster [1]. with regard to jurisdictional claims in The uses and evidence of earth pigments in the India begin with the hematite and published maps and institutional affil- quartz crystals found in the Acheulian deposits of the Lower Paleolithic period. One such iations. hematite specimen was discovered in the exposed floor of Hunsgi (Karnataka), locality V, and has a worn facet with characteristic striation patterns, indicating that it was used as a crayon to color or mark a rock surface [2]. Because this material does not occur in its natural state in the area surrounding the site, the site excavators believed that these Copyright: © 2021 by the authors. little hematite nodules were brought-in from afar. Paddaya goes on to say that these Licensee MDPI, Basel, Switzerland. red ochre nodules were probably also utilized for body ornamentation and other similar This article is an open access article purposes [3]. Six other tiny quartz crystals were discovered from the base of the lower distributed under the terms and Paleolithic deposit at Singi Talav (Rajasthan), which was interesting evidence. They were conditions of the Creative Commons virtually fully unchanged and measured 7–25 mm in length, making them too small to Attribution (CC BY) license (https:// have been employed as tools. They had been purposefully transported to the site, as had creativecommons.org/licenses/by/ the Hunsgi hematite nodules, and were collected for their visual attributes [4]. Although 4.0/). Heritage 2021, 4, 1970–1994. https://doi.org/10.3390/heritage4030112 https://www.mdpi.com/journal/heritage Heritage2021, 4 FOR PEER REVIEW 2 Heritage 2021, 4 1971 collected for their visual attributes [4]. Although these are only inferences, it is impossible to theserule out are the only possibility inferences, of ita functioning is impossible reality to rule involving out the possibilityan aesthetic of sense a functioning among our reality fore- involvingfathers. an aesthetic sense among our forefathers. AccordingAccording toto Wakankar,Wakankar, some some of of the the earliest earliest depictions depictions in in Mesolithic Mesolithic rockrock paintings paintings paintedpainted inin greengreen colorcolor couldcould bebe thosethose belongingbelonging toto thethe upperupper PaleolithicPaleolithic eraera ofof IndianIndian antiquity.antiquity. The The discovery discovery of of green green earth earth (what (what he he refers refers toas to terra as terra verte) verte) in upper in upper Paleolithic Paleo- depositslithic deposits in one in of one the excavatedof the excavated rock shelters rock shelters (III A-28) (III atA-28) Bhimbetka at Bhimbetka [5] could [5]could be the be basis the forbasis this for hypothesis. this hypothesis. The chronological The chronological position inposition time of in the time green of paintings, the green however, paintings, is ahowever, point of contention.is a point of Greencontention. pigments Green were pigments discovered were first,discovered followed first, by followed red paintings, by red accordingpaintings, toaccording some scholars to some [6]. Wakankarscholars [6]. also Wakankar discovered also yellow discovered ochre, manganese, yellow ochre, and terramanganese, verte in and Bhimbetka’s terra verte shelter in Bhimbetka’s III A-28 in shel 1975,ter where III A-28 these in 1975, pigments where were these observed pigments to bewere smeared observed on multiple to be smeared areas in on the multiple shelter IIIareas F-23 in [ 2the,7,8 shelter]. These III early F-23 paintings [2,7,8]. These represent early thepaintings beginning represent of known the beginning or surviving of known rock art or in surviving India because rock art of thein India quality because of pigment of the applicationsquality of pigment in the form applications of fine and in controlled the formlines. of fine According and controlled to Mishra, lines. for theAccording paintings to atMishra, Bhimbetka, for the apart paintings from being at Bhimbetka,apart executed in red orfrom white, being bluish-green executed andin red yellowish or white, colors blu- hadish-green also been andused yellowish on occasions. colors had Since also they been were used only on preserved occasions. in Since fragments they were and were only foundpreserved at the in bottom fragments of the and paint were layer; found green at the painted bottom layers of the tend paint to belayer; the oldest.green painted Many shadeslayers tend of red to werebe the visible, oldest. rangingMany shades from of scarlet red were to pale visible, red toranging dark chocolate.from scarlet Natural to pale mineralsred to dark were chocolate. used to makeNatural these minerals pigments were [2 used,9] to make these pigments [2,9] TheThe largestlargest concentrationconcentration ofof prehistoricprehistoric sitessites andand rockrock paintingspaintings areare foundfound inin CentralCentral India’sIndia’s sandstonesandstone regions,regions, whichwhich spanspan threethree distinctdistinct mountainmountain systems:systems: thethe VindhyachalVindhyachal andand SatpuraSatpura inin MadhyaMadhya Pradesh,Pradesh, Chhattisgarh,Chhattisgarh, andand aa portionportion ofof UttarUttar PradeshPradesh andand thethe AravalliAravalli in Rajasthan. In In all all more more than than a thou a thousandsand rock-shelters rock-shelters with with paintings paintings have have been beenexplored explored and studied and studied by archeologists. by archeologists. It is interesting It is interesting to note that to prehistoric note that paintings prehistoric in paintingsIndia were in first India noticed were first12 years noticed earlier 12 years than earlierthe famous than discovery the famous of discovery the cave paintings of the cave of paintingsAltamira of(Spain). Altamira This (Spain). was done This by was Archib doneald by Carllyle, Archibald a superintendent Carllyle, a superintendent of the Archaeo- of thelogical Archaeological Survey of India Survey (ASI) of Indiain 1867, (ASI) in inthe 1867, Mirzapur in the area Mirzapur of the areathen of United the then Provinces. United Provinces.Like Marcelino Like de Marcelino Santuola, de through Santuola, discovery through of discovery Altamira ofin Altamira1879, Carllyle in 1879, was Carllyle the first wasscholar the to first attribute scholar these to attribute paintings these to the paintings Stone-Age to period. the Stone-Age Some of period.the prominent Some sites of the in prominentIndia with sitesshelters in Indiacontaining with sheltersprehistoric containing paintings prehistoric are Panchmari paintings in the are Mahadeo Panchmari Hillsin of theMadhya Mahadeo Pradesh, Hills Adamgarph, of Madhya Pradesh, Raisen, Mirzapur Adamgarph,, etc. Raisen, Mirzapur Mirzapur, has evidence etc. Mirzapur dating from has evidencethe Lower dating Palaeolithic from the
Recommended publications
  • The Behavior of Molybdenum., Tungsten, and Titanium
    The behavior of molybdenum, tungsten, and titanium in the porphyry copper environment Item Type text; Dissertation-Reproduction (electronic) Authors Kuck, Peter Hinckley Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 08/10/2021 00:24:06 Link to Item http://hdl.handle.net/10150/565421 THE BEHAVIOR OF MOLYBDENUM., TUNGSTEN, AND TITANIUM IN THE PORPHYRY COPPER ENVIRONMENT Peter' 'Hinckley Kuck A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES. In Partial.Fulfillment of the Requirements. ' ■ For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College ■ THE UNIVERSITY OF ARIZONA 1 9 7 8 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE I hereby recommend that this dissertation prepared under my Peter Hinckley Kuck direction by ___________ , , The Behavior of Molybdenum, Tungsten, and Titanium entitled ________________________________________________________ in the Porphyry Copper Environment be accepted as fulfilling the dissertation requirement for the Doctor of Philosophy degree of _______________________________________________________ Dissertation Director Date As members of the Final Examination Committee, we certify that we have read this dissertation and agree that it may be presented for final defense. \ R A j r i A hi / 7IT 2 / 1 r 7 - Final approval and acceptance of this dissertation is contingent on the candidate's adequate performance and defense thereof at the final oral examination. STATEMENT BY AUTHOR This dissertation has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of.
    [Show full text]
  • Metamorphism of Sedimentary Manganese Deposits
    Acta Mineralogica-Petrographica, Szeged, XX/2, 325—336, 1972. METAMORPHISM OF SEDIMENTARY MANGANESE DEPOSITS SUPRIYA ROY ABSTRACT: Metamorphosed sedimentary deposits of manganese occur extensively in India, Brazil, U. S. A., Australia, New Zealand, U. S. S. R., West and South West Africa, Madagascar and Japan. Different mineral-assemblages have been recorded from these deposits which may be classi- fied into oxide, carbonate, silicate and silicate-carbonate formations. The oxide formations are represented by lower oxides (braunite, bixbyite, hollandite, hausmannite, jacobsite, vredenburgite •etc.), the carbonate formations by rhodochrosite, kutnahorite, manganoan calcite etc., the silicate formations by spessartite, rhodonite, manganiferous amphiboles and pyroxenes, manganophyllite, piedmontite etc. and the silicate-carbonate formations by rhodochrosite, rhodonite, tephroite, spessartite etc. Pétrographie and phase-equilibia data indicate that the original bulk composition in the sediments, the reactions during metamorphism (contact and regional and the variations and effect of 02, C02, etc. with rise of temperature, control the mineralogy of the metamorphosed manga- nese formations. The general trend of formation and transformation of mineral phases in oxide, carbonate, silicate and silicate-carbonate formations during regional and contact metamorphism has, thus, been established. Sedimentary manganese formations, later modified by regional or contact metamorphism, have been reported from different parts of the world. The most important among such deposits occur in India, Brazil, U.S.A., U.S.S.R., Ghana, South and South West Africa, Madagascar, Australia, New Zealand, Great Britain, Japan etc. An attempt will be made to summarize the pertinent data on these metamorphosed sedimentary formations so as to establish the role of original bulk composition of the sediments, transformation and reaction of phases at ele- vated temperature and varying oxygen and carbon dioxide fugacities in determin- ing the mineral assemblages in these deposits.
    [Show full text]
  • Wildberries Resorts (P) Ltd
    Near Forest Rest House, Kolar Dam. www.ratapani.com / 9165761000 / 9584551234 Wildberries Resorts (P) Ltd Near Forest Rest House, Kolar Dam. www.ratapani.com / 9165761000 / 9584551234 Kathotiya Rock Shelters Therefore at some places one finds different paintings of enchanting Vndhyachal Ranges. The drive to Kehri Ka different era, quite literally overlapping each other. The Mahadev, winds its way through the table top mountains, paintings are primarily in the regular Red Coloured Natural Dye offering a spectacular view of the valleys below, almost but also use the White and what we saw for the first time in the throughout the drive. Deep in the valley below, the Kolar River area, Green Dye, to create a myriad of Rock Art, depicting the winds its way ahead and as you stand atop any of the numerous life and times of the era. Kathotiya, till date remains quite viewpoints all along the way, you can hear the gentle murmur of unexplored and a noted architect from Bhopal, still continues the river meandering its way forward. The drive, a total of about the research and documentation in the area. One can only 30 kms (to-n-fro), winds its way through the lower Vindhyachal imagine the surprises which lie in store, waiting to still be ranges, slowly ascending on to a plateau, whereafter the drive is discovered. The trek begins from Kathotiya Village and after mostly along the edge of the hill, on one side and the beautiful about half a Km of flat land, starts ascending on to the Hills, Ratapani jungles on the other.
    [Show full text]
  • Washington State Minerals Checklist
    Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite
    [Show full text]
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • Study of Fragments of Mural Paintings from the Roman Province Of
    Study of fragments of mural paintings from the Roman province of Germania Superior Thesis submitted in partial fulfilment of the requirements of the degree Doctor rer. nat. of the Faculty of Environment and Natural Resources, Albert-Ludwigs-Universität Freiburg im Breisgau, Germany by Rafaela Debastiani Freiburg im Breisgau, Germany 2016 Name of Dean: Prof. Dr. Tim Freytag Name of Supervisor: Prof. Dr. Michael Fiederle Name of 2nd Reviewer: PD Dr. Andreas Danilewsky Date of thesis' defense: 03.02.2017 “The mind is not a vessel to be filled, but a fire to be kindled” Plutarch Contents Nomenclature ........................................................................................................................ 1 Acknowledgment ................................................................................................................... 3 Abstract ................................................................................................................................. 5 Zusammenfassung ................................................................................................................ 7 1. Introduction .................................................................................................................... 9 2. Analytical techniques in the non-destructive analyses of fragments of mural paintings ..13 2.1 X-ray Fluorescence Spectroscopy ..........................................................................13 2.1.1 Synchrotron-based scanning macro X-ray fluorescence (MA-XRF) .................17
    [Show full text]
  • List of New Mineral Names: with an Index of Authors
    415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis.
    [Show full text]
  • Cortinarius Caperatus (Pers.) Fr., a New Record for Turkish Mycobiota
    Kastamonu Üni., Orman Fakültesi Dergisi, 2015, 15 (1): 86-89 Kastamonu Univ., Journal of Forestry Faculty Cortinarius caperatus (Pers.) Fr., A New Record For Turkish Mycobiota *Ilgaz AKATA1, Şanlı KABAKTEPE2, Hasan AKGÜL3 Ankara University, Faculty of Science, Department of Biology, 06100, Tandoğan, Ankara Turkey İnönü University, Battalgazi Vocational School, TR-44210 Battalgazi, Malatya, Turkey Gaziantep University, Department of Biology, Faculty of Science and Arts, 27310 Gaziantep, Turkey *Correspending author: [email protected] Received date: 03.02.2015 Abstract In this study, Cortinarius caperatus (Pers.) Fr. belonging to the family Cortinariaceae was recorded for the first time from Turkey. A short description, ecology, distribution and photographs related to macro and micromorphologies of the species are provided and discussed briefly. Keywords: Cortinarius caperatus, mycobiota, new record, Turkey Cortinarius caperatus (Pers.) Fr., Türkiye Mikobiyotası İçin Yeni Bir Kayıt Özet Bu çalışmada, Cortinariaceae familyasına mensup Cortinarius caperatus (Pers.) Fr. Türkiye’den ilk kez kaydedilmiştir. Türün kısa deskripsiyonu, ekolojisi, yayılışı ve makro ve mikro morfolojilerine ait fotoğrafları verilmiş ve kısaca tartışılmıştır. Anahtar Kelimeler: Cortinarius caperatus, Mikobiyota, Yeni kayıt, Türkiye Introduction lamellae edges (Arora, 1986; Hansen and Cortinarius is a large and complex genus Knudsen, 1992; Orton, 1984; Uzun et al., of family Cortinariaceae within the order 2013). Agaricales, The genus contains According to the literature (Sesli and approximately 2 000 species recognised Denchev, 2008, Uzun et al, 2013; Akata et worldwide. The most common features al; 2014), 98 species in the genus Cortinarius among the members of the genus are the have so far been recorded from Turkey but presence of cortina between the pileus and there is not any record of Cortinarius the stipe and cinnamon brown to rusty brown caperatus (Pers.) Fr.
    [Show full text]
  • Jhansi - Gwalior - Agra - Jaipur - Pushkar - Udaipur - Aurangabad - Mumbai
    Duration: 16 Nights / 17 Days Places Covered: Delhi - Varanasi - Khajuraho - Jhansi - Gwalior - Agra - Jaipur - Pushkar - Udaipur - Aurangabad - Mumbai Day 01: Arrive Delhi Arrive at Delhi international airport. After warm receiving and greeting by our representative transfer to hotel for check-in. Delhi a bustling metropolis, and the capital city of India, successfully combines in its folds the ancient times with modern times. In fact, more mythological cities are believed to be here, like the city of Indraprastha from the Hindu epic Mahabharata, founded around 5000 BC. Numerous monuments were built over several centuries by different rulers like Qutub-ud- din Aibek, Alauddin Khilji, Tughlaks, Humayun & Shah Jahan, who built the Walled City Shah Jahanabad. Later in first half of 20th century much of New Delhi was planned by Sir Edwin Lutyens, who laid out a grandiose central administrative area as a testament to British rule in India. The division in walled city & New Delhi also marks the division in life styles. Rest of the day at leisure or walk around the city by your own. Over Night stay at hotel. Day 02: Delhi After Breakfast, we will visit the city. Visit “Old Delhi” with its narrow dirt roads, its myriad people and inexpensive and colorful bazaars that keep alive the traditional workmanship for which Delhi has always been famous. The first stop is Raj Ghat, the cremation ground of Mahatma Gandhi), The “Father of the nation”. Drive past the Red Fort, the red sandstone walled fort made in Mughal era by Emperor Shah Jahan. We end up at the Jama Masjid, the largest Muslim mosque in India.
    [Show full text]
  • 40 Common Minerals and Their Uses
    40 Common Minerals and Their Uses Aluminum Beryllium The most abundant metal element in Earth’s Used in the nuclear industry and to crust. Aluminum originates as an oxide called make light, very strong alloys used in the alumina. Bauxite ore is the main source aircraft industry. Beryllium salts are used of aluminum and must be imported from in fluorescent lamps, in X-ray tubes and as Jamaica, Guinea, Brazil, Guyana, etc. Used a deoxidizer in bronze metallurgy. Beryl is in transportation (automobiles), packaging, the gem stones emerald and aquamarine. It building/construction, electrical, machinery is used in computers, telecommunication and other uses. The U.S. was 100 percent products, aerospace and defense import reliant for its aluminum in 2012. applications, appliances and automotive and consumer electronics. Also used in medical Antimony equipment. The U.S. was 10 percent import A native element; antimony metal is reliant in 2012. extracted from stibnite ore and other minerals. Used as a hardening alloy for Chromite lead, especially storage batteries and cable The U.S. consumes about 6 percent of world sheaths; also used in bearing metal, type chromite ore production in various forms metal, solder, collapsible tubes and foil, sheet of imported materials, such as chromite ore, and pipes and semiconductor technology. chromite chemicals, chromium ferroalloys, Antimony is used as a flame retardant, in chromium metal and stainless steel. Used fireworks, and in antimony salts are used in as an alloy and in stainless and heat resisting the rubber, chemical and textile industries, steel products. Used in chemical and as well as medicine and glassmaking.
    [Show full text]
  • Art in the Mirror: Reflection in the Work of Rauschenberg, Richter, Graham and Smithson
    ART IN THE MIRROR: REFLECTION IN THE WORK OF RAUSCHENBERG, RICHTER, GRAHAM AND SMITHSON DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Eileen R. Doyle, M.A. ***** The Ohio State University 2004 Dissertation Committee: Approved by Professor Stephen Melville, Advisor Professor Lisa Florman ______________________________ Professor Myroslava Mudrak Advisor History of Art Graduate Program Copyright by Eileen Reilly Doyle 2004 ii ABSTRACT This dissertation considers the proliferation of mirrors and reflective materials in art since the sixties through four case studies. By analyzing the mirrored and reflective work of Robert Rauschenberg, Gerhard Richter, Dan Graham and Robert Smithson within the context of the artists' larger oeuvre and also the theoretical and self-reflective writing that surrounds each artist’s work, the relationship between the wide use of industrially-produced materials and the French theory that dominated artistic discourse for the past thirty years becomes clear. Chapter 2 examines the work of Robert Rauschenberg, noting his early interest in engaging the viewer’s body in his work—a practice that became standard with the rise of Minimalism and after. Additionally, the theoretical writing the French phenomenologist Maurice Merleau-Ponty provides insight into the link between art as a mirroring practice and a physically engaged viewer. Chapter 3 considers the questions of medium and genre as they arose in the wake of Minimalism, using the mirrors and photo-based paintings of Gerhard Richter as its focus. It also addresses the particular way that Richter weaves the motifs and concerns of traditional painting into a rhetoric of the death of painting which strongly implicates the mirror, ultimately opening up Richter’s career to a psychoanalytic reading drawing its force from Jacques Lacan’s writing on the formation of the subject.
    [Show full text]
  • The Reception of Palaeolithic Art at the Turn of the Twentieth Century: Between Archaeology and Art History
    The reception of Palaeolithic art at the turn of the twentieth century: between archaeology and art history Oscar Moro Abadía If I am asked to define any further what I mean by ‘the primitive’ I must refer the reader to the pages of this book, which will show that the term was associated in its time with early Greek vases, with quattrocento painting and with tribal art.1 These words by Ernst Gombrich summarize some of the main meanings associated with the term ‘primitive’ in the field of art history. In its original sense, the word refers to a movement of taste that, in the story of art, runs parallel to the progress towards naturalism. According to Gombrich, while art history may be described as the story of how ‘the artist got better and better in the imitation of nature’,2 there have been a number of artistic movements that have called for a deliberate abandonment of classical standards.3 This ‘preference for the primitive’ has been expressed in ‘the revulsion from that very perfection that art had been said to aim at’.4 During the last years of the nineteenth century, the theory of evolution ‘gave a new meaning to the term ‘primitive’ which […] came to denote the beginnings of human civilization’.5 As a result of this development, the term ‘primitive art’ was incorporated into art historians’ vocabulary to refer to a set of non-Western arts coming from Africa, America and Oceania.6 At the beginning of the twentieth century, ‘primitive art’ was used interchangeably with terms such as ‘savage art’, ‘tribal art’ and ‘art nègre’.7 Since then, the label has been intensively criticized for Acknowledgements.
    [Show full text]