Evidence for a single clay/temper source for the manufacture of Middle and Late Helladic Aeginetan pottery from Asine, Greece
Identifieur interne : 000395 ( Istex/Corpus ); précédent : 000394; suivant : 000396Evidence for a single clay/temper source for the manufacture of Middle and Late Helladic Aeginetan pottery from Asine, Greece
Auteurs : Michael J. Dorais ; Michael Lindblom ; Christine M. ShrinerSource :
- Geoarchaeology [ 0883-6353 ] ; 2004-10.
English descriptors
- KwdEn :
- Aegina, Aeginetan, Aeginetan amphiboles, Amphibole, Amphibole compositions, Amphibole trend, Amphiboles overlap, Andesite, Asine, Black grits, Ceramic classes, Chalky, Compositions aeginetan, Dacite, Dacitic, Diam, Dorais, Equivalent values, Fracture, Fracture light, Fytikas, Geoarchaeology, Gold mica, Gray circles, Gray diamonds, Gray squares, Gray triangles, Helladic, International journal, Kolonna, Lava, Lindblom, Lithic, Lower body fragment, Many medium, Mark type, Melos, Melos amphiboles, Methana, Mica, Mommsen, Open circles, Other population, Other sherds, Plagioclase, Platelet, Poros, Poros amphiboles, Saronic gulf, Sherd, Sherd amphiboles, Shriner, Shriner figure, Single source, Single source figure, Sparkling platelets, Stream system, Volcanic rocks, Zerner.
- Teeft :
- Aegina, Aeginetan, Aeginetan amphiboles, Amphibole, Amphibole compositions, Amphibole trend, Amphiboles overlap, Andesite, Asine, Black grits, Ceramic classes, Chalky, Compositions aeginetan, Dacite, Dacitic, Diam, Dorais, Equivalent values, Fracture, Fracture light, Fytikas, Geoarchaeology, Gold mica, Gray circles, Gray diamonds, Gray squares, Gray triangles, Helladic, International journal, Kolonna, Lava, Lindblom, Lithic, Lower body fragment, Many medium, Mark type, Melos, Melos amphiboles, Methana, Mica, Mommsen, Open circles, Other population, Other sherds, Plagioclase, Platelet, Poros, Poros amphiboles, Saronic gulf, Sherd, Sherd amphiboles, Shriner, Shriner figure, Single source, Single source figure, Sparkling platelets, Stream system, Volcanic rocks, Zerner.
Abstract
In an effort to further characterize the Middle and Late Helladic pottery industry on Aegina, we have analyzed amphibole in 23 sherds imported to the coastal settlement of Asine. The sherds derive from vessels of different classes and shapes and range in age from MH I‐II to LH IIIB‐IIIC Early. All sherds come from vessels that carry manufacturing marks, and their amphiboles have compositions that are incompatible with those of Methana, Poros, and Melos. Twenty of the sherds have amphiboles that are identical in composition and overlap a narrow range of amphibole compositions found in specific lava flows on the northern portion of Aegina. Given that the dacites across Aegina contain amphiboles with a wide range in compositions, we suggest that the narrow range of amphibole compositions in the sherds indicates that they were derived from either a specific clay source on the island, located in a stream system southeast of the prehistoric settlement at Kolonna, or that the potters used a specific temper source along the same stream system. Multiple clay or temper sources would have produced sherds with a broader range of amphibole compositions reflecting the diversity of amphibole compositions found on Aegina. One sherd has amphibole compositions indicative of an additional Aeginetan component that is not found in the other sherds. Two sherds have amphiboles with compositions that do not match any known reference amphiboles for Aegina, Methana, Poros, or Melos. These may have been derived from still unsampled dacites on Aegina or have been manufactured from materials located outside the Saronic Gulf. © 2004 Wiley Periodicals, Inc.
Url:
DOI: 10.1002/gea.20017
Links to Exploration step
ISTEX:EC10280AFF0A581C0A7728EAF67FEE3AA50A82EDLe document en format XML
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Multiple clay or temper sources would have produced sherds with a broader range of amphibole compositions reflecting the diversity of amphibole compositions found on Aegina. One sherd has amphibole compositions indicative of an additional Aeginetan component that is not found in the other sherds. Two sherds have amphiboles with compositions that do not match any known reference amphiboles for Aegina, Methana, Poros, or Melos. 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All sherds come from vessels that carry manufacturing marks, and their amphiboles have compositions that are incompatible with those of Methana, Poros, and Melos. Twenty of the sherds have amphiboles that are identical in composition and overlap a narrow range of amphibole compositions found in specific lava flows on the northern portion of Aegina. Given that the dacites across Aegina contain amphiboles with a wide range in compositions, we suggest that the narrow range of amphibole compositions in the sherds indicates that they were derived from either a specific clay source on the island, located in a stream system southeast of the prehistoric settlement at Kolonna, or that the potters used a specific temper source along the same stream system. Multiple clay or temper sources would have produced sherds with a broader range of amphibole compositions reflecting the diversity of amphibole compositions found on Aegina. One sherd has amphibole compositions indicative of an additional Aeginetan component that is not found in the other sherds. Two sherds have amphiboles with compositions that do not match any known reference amphiboles for Aegina, Methana, Poros, or Melos. These may have been derived from still unsampled dacites on Aegina or have been manufactured from materials located outside the Saronic Gulf. © 2004 Wiley Periodicals, Inc.</abstract><qualityIndicators><score>8</score><pdfVersion>1.2</pdfVersion><pdfPageSize>522 x 738 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1654</abstractCharCount><pdfWordCount>8762</pdfWordCount><pdfCharCount>56845</pdfCharCount><pdfPageCount>28</pdfPageCount><abstractWordCount>261</abstractWordCount></qualityIndicators><title>Evidence for a single clay/temper source for the manufacture of Middle and Late Helladic Aeginetan pottery from Asine, 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xml:lang="en">Evidence for a Single Clay/Temper Source</title><author xml:id="author-0000" role="corresp"><persName><forename type="first">Michael J.</forename><surname>Dorais</surname></persName><affiliation>Brigham Young University, Provo, Utah<address><country key="US"></country></address></affiliation><affiliation>Department of Geology, Brigham Young University, Provo, Utah 84602</affiliation></author><author xml:id="author-0001"><persName><forename type="first">Michael</forename><surname>Lindblom</surname></persName><affiliation>Uppsala University, Uppsala, Sweden<address><country key="SE"></country></address></affiliation></author><author xml:id="author-0002"><persName><forename type="first">Christine M.</forename><surname>Shriner</surname></persName><affiliation>Indiana University, Bloomington, Indiana<address><country key="US"></country></address></affiliation></author><idno type="istex">EC10280AFF0A581C0A7728EAF67FEE3AA50A82ED</idno><idno 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Late Helladic pottery industry on Aegina, we have analyzed amphibole in 23 sherds imported to the coastal settlement of Asine. The sherds derive from vessels of different classes and shapes and range in age from MH I‐II to LH IIIB‐IIIC Early. All sherds come from vessels that carry manufacturing marks, and their amphiboles have compositions that are incompatible with those of Methana, Poros, and Melos. Twenty of the sherds have amphiboles that are identical in composition and overlap a narrow range of amphibole compositions found in specific lava flows on the northern portion of Aegina. Given that the dacites across Aegina contain amphiboles with a wide range in compositions, we suggest that the narrow range of amphibole compositions in the sherds indicates that they were derived from either a specific clay source on the island, located in a stream system southeast of the prehistoric settlement at Kolonna, or that the potters used a specific temper source along the same stream system. Multiple clay or temper sources would have produced sherds with a broader range of amphibole compositions reflecting the diversity of amphibole compositions found on Aegina. One sherd has amphibole compositions indicative of an additional Aeginetan component that is not found in the other sherds. Two sherds have amphiboles with compositions that do not match any known reference amphiboles for Aegina, Methana, Poros, or Melos. These may have been derived from still unsampled dacites on Aegina or have been manufactured from materials located outside the Saronic Gulf. © 2004 Wiley Periodicals, Inc.</p></abstract><textClass><classCode scheme="articleCategory">Research Article</classCode><classCode scheme="tocHeading1">Research Article</classCode></textClass><langUsage><language ident="EN"></language></langUsage></profileDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/EC10280AFF0A581C0A7728EAF67FEE3AA50A82ED/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>Wiley Subscription Services, Inc., A Wiley 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type="pageLast">684</numbering></numberingGroup><correspondenceTo>Department of Geology, Brigham Young University, Provo, Utah 84602</correspondenceTo><linkGroup><link type="toTypesetVersion" href="file:GEA.GEA20017.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="18"></count><count type="tableTotal" number="1"></count><count type="referenceTotal" number="35"></count><count type="wordTotal" number="10896"></count></countGroup><titleGroup><title type="main" xml:lang="en">Evidence for a single clay/temper source for the manufacture of Middle and Late Helladic Aeginetan pottery from Asine, Greece</title><title type="short" xml:lang="en">Evidence for a Single Clay/Temper Source</title></titleGroup><creators><creator xml:id="au1" creatorRole="author" affiliationRef="#af1" corresponding="yes"><personName><givenNames>Michael J.</givenNames><familyName>Dorais</familyName></personName></creator><creator xml:id="au2" creatorRole="author" affiliationRef="#af2"><personName><givenNames>Michael</givenNames><familyName>Lindblom</familyName></personName></creator><creator xml:id="au3" creatorRole="author" affiliationRef="#af3"><personName><givenNames>Christine M.</givenNames><familyName>Shriner</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="af1" countryCode="US" type="organization"><unparsedAffiliation>Brigham Young University, Provo, Utah</unparsedAffiliation></affiliation><affiliation xml:id="af2" countryCode="SE" type="organization"><unparsedAffiliation>Uppsala University, Uppsala, Sweden</unparsedAffiliation></affiliation><affiliation xml:id="af3" countryCode="US" type="organization"><unparsedAffiliation>Indiana University, Bloomington, Indiana</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title><p>In an effort to further characterize the Middle and Late Helladic pottery industry on Aegina, we have analyzed amphibole in 23 sherds imported to the coastal settlement of Asine. The sherds derive from vessels of different classes and shapes and range in age from MH I‐II to LH IIIB‐IIIC Early. All sherds come from vessels that carry manufacturing marks, and their amphiboles have compositions that are incompatible with those of Methana, Poros, and Melos. Twenty of the sherds have amphiboles that are identical in composition and overlap a narrow range of amphibole compositions found in specific lava flows on the northern portion of Aegina. Given that the dacites across Aegina contain amphiboles with a wide range in compositions, we suggest that the narrow range of amphibole compositions in the sherds indicates that they were derived from either a specific clay source on the island, located in a stream system southeast of the prehistoric settlement at Kolonna, or that the potters used a specific temper source along the same stream system. Multiple clay or temper sources would have produced sherds with a broader range of amphibole compositions reflecting the diversity of amphibole compositions found on Aegina. One sherd has amphibole compositions indicative of an additional Aeginetan component that is not found in the other sherds. Two sherds have amphiboles with compositions that do not match any known reference amphiboles for Aegina, Methana, Poros, or Melos. These may have been derived from still unsampled dacites on Aegina or have been manufactured from materials located outside the Saronic Gulf. © 2004 Wiley Periodicals, Inc.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Evidence for a single clay/temper source for the manufacture of Middle and Late Helladic Aeginetan pottery from Asine, Greece</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>Evidence for a Single Clay/Temper Source</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Evidence for a single clay/temper source for the manufacture of Middle and Late Helladic Aeginetan pottery from Asine, Greece</title></titleInfo><name type="personal"><namePart type="given">Michael J.</namePart><namePart type="family">Dorais</namePart><affiliation>Brigham Young University, Provo, Utah</affiliation><affiliation>Department of Geology, Brigham Young University, Provo, Utah 84602</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Michael</namePart><namePart type="family">Lindblom</namePart><affiliation>Uppsala University, Uppsala, Sweden</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Christine M.</namePart><namePart type="family">Shriner</namePart><affiliation>Indiana University, Bloomington, Indiana</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Wiley Subscription Services, Inc., A Wiley Company</publisher><place><placeTerm type="text">Hoboken</placeTerm></place><dateIssued encoding="w3cdtf">2004-10</dateIssued><dateCaptured encoding="w3cdtf">2003-11-07</dateCaptured><dateValid encoding="w3cdtf">2004-03-25</dateValid><copyrightDate encoding="w3cdtf">2004</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">18</extent><extent unit="tables">1</extent><extent unit="references">35</extent><extent unit="words">10896</extent></physicalDescription><abstract lang="en">In an effort to further characterize the Middle and Late Helladic pottery industry on Aegina, we have analyzed amphibole in 23 sherds imported to the coastal settlement of Asine. The sherds derive from vessels of different classes and shapes and range in age from MH I‐II to LH IIIB‐IIIC Early. All sherds come from vessels that carry manufacturing marks, and their amphiboles have compositions that are incompatible with those of Methana, Poros, and Melos. Twenty of the sherds have amphiboles that are identical in composition and overlap a narrow range of amphibole compositions found in specific lava flows on the northern portion of Aegina. Given that the dacites across Aegina contain amphiboles with a wide range in compositions, we suggest that the narrow range of amphibole compositions in the sherds indicates that they were derived from either a specific clay source on the island, located in a stream system southeast of the prehistoric settlement at Kolonna, or that the potters used a specific temper source along the same stream system. Multiple clay or temper sources would have produced sherds with a broader range of amphibole compositions reflecting the diversity of amphibole compositions found on Aegina. One sherd has amphibole compositions indicative of an additional Aeginetan component that is not found in the other sherds. Two sherds have amphiboles with compositions that do not match any known reference amphiboles for Aegina, Methana, Poros, or Melos. These may have been derived from still unsampled dacites on Aegina or have been manufactured from materials located outside the Saronic Gulf. © 2004 Wiley Periodicals, Inc.</abstract><relatedItem type="host"><titleInfo><title>Geoarchaeology</title><subTitle>An International Journal</subTitle></titleInfo><titleInfo type="abbreviated"><title>Geoarchaeology</title></titleInfo><genre type="journal">journal</genre><subject><genre>article-category</genre><topic>Research Article</topic></subject><identifier type="ISSN">0883-6353</identifier><identifier type="eISSN">1520-6548</identifier><identifier type="DOI">10.1002/(ISSN)1520-6548</identifier><identifier type="PublisherID">GEA</identifier><part><date>2004</date><detail type="volume"><caption>vol.</caption><number>19</number></detail><detail type="issue"><caption>no.</caption><number>7</number></detail><extent unit="pages"><start>657</start><end>684</end><total>28</total></extent></part></relatedItem><identifier type="istex">EC10280AFF0A581C0A7728EAF67FEE3AA50A82ED</identifier><identifier type="DOI">10.1002/gea.20017</identifier><identifier type="ArticleID">GEA20017</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright © 2004 Wiley Periodicals, Inc.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>Wiley Subscription Services, Inc., A Wiley Company</recordOrigin></recordInfo></mods><json:item><extension>json</extension><original>false</original><mimetype>application/json</mimetype><uri>https://api.istex.fr/document/EC10280AFF0A581C0A7728EAF67FEE3AA50A82ED/metadata/json</uri></json:item></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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