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Статті в журналах з теми "Lessinia"
1
Zanetti, Adriano, Alberto Sette, Roberto Poggi, and Andrea Tagliapietra. "Biodiversity of Staphylinidae (Coleoptera) in the Province of Verona (Veneto, Northern Italy)." Memorie della Società Entomologica Italiana 93, no. 1-2 (December 20, 2016): 3. http://dx.doi.org/10.4081/memoriesei.2016.3.
Повний текст джерелаАнотація:
A commented catalogue of Coleoptera Staphylinidae present in Verona province (Veneto, Northern Italy) is provided. It is based on published as well as mostly unpublished records, with the Sette collection at the Museo Civico di Storia Naturale di Verona as main source. These records are filed in a freely downloadable database (http://www.societaentomologicaitaliana.it/it/archivio-comunicazioni/78-archiviati/269-database-staphylinidae-verona.html). Verona province is a very diverse area, with habitats ranging from montane/alpine to hill and plain, which are natural, seminatural or anthropogenic. A total of 988 species are listed. Localities, habitats, microhabitats, collecting methods, altitudinal range, months of capture, latest year of capture and number of specimens are given for each species. Comments are added for 149 remarkable species or genera (<em>i.e</em>. new to Italy, endemic, with particular geographic distribution, living in particular habitats, introduced, problematic from a taxonomic point of view), 7 species are new records for Italy (<em>Tachyporus corpulentus J.</em> Sahlberg, 1876, <em>Aleochara bellonata</em> Krása, 1922, <em>Aleochara marmotae</em> Sainte-Claire Deville, 1927, <em>Atheta (Ceritaxa) flavipes</em> (Hochhuth, 1860), <em>Atheta (Philhygra) pseudoelongatula</em> Bernhauer, 1907, <em>Stenomastax platygaster</em> (Kraatz, 1859), <em>Carpelimus boops rondaensis</em> (Fagel, 1957)), one is very probably new to science (<em>Leptusa</em> sp.). The biogeographic analysis of the data is mostly based on the comparison of the main areas of the province (Monte Baldo, Lessinia, Morene del Garda, course of Adige river, and plain). The presence of a good percentage (5%) of endemic species is pointed out. The communities inhabiting the principal habitats and microhabitats are commented on, and remarkable species living in the protected areas of the province are listed.
2
Takács, Attila, Csaba Szabóky, Gusztáv Boldog, Sándor Jordán, Miklós Bozsó, Dávid Fülöp, and Balázs Tóth. "Biology and DNA barcode analysis of Coleophora lessinica Baldizzone, 1980 and Coleophora impalella Toll, 1961 (Lepidoptera, Coleophoridae) with description of their larval cases." Nota Lepidopterologica 45 (April 21, 2022): 191–205. http://dx.doi.org/10.3897/nl.45.80106.
Повний текст джерелаАнотація:
Host plants and cases of several species in the genus Coleophora Hübner, 1822 have remained unknown until now, while the latter structures provide important characters for identification. Host plants and cases of Coleophora lessinica Baldizzone, 1980 and Coleophora impalella Toll, 1961 were discovered by the authors and are presented here for the first time. New data on the distribution and biology of the two species in Hungary are given. Coleophora lessinica is recorded as new for the fauna of Romania. DNA barcode sequencing was performed for both Coleophora species and loaded into the BOLD System and to GenBank.
3
Podhraski, Antonia Sophia. "Lessings Preussenbild." Forschungen zur Brandenburgischen und Preußischen Geschichte: Volume 30, Issue 1-2 30, no. 1-2 (January 1, 2020): 25–45. http://dx.doi.org/10.3790/fbpg.30.1-2.25.
Повний текст джерела
4
Lamport, Francis, Jürgen Stenzel, and Roman Lach. "Lessings Skandale." Modern Language Review 102, no. 3 (July 1, 2007): 876. http://dx.doi.org/10.2307/20467496.
Повний текст джерела
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Allert, Beate. "Lessings Skandale." Monatshefte 99, no. 1 (2007): 106–8. http://dx.doi.org/10.1353/mon.2007.0000.
Повний текст джерела
6
Valentin, Jean-Marie. "Theaterästhetik im europäischen Kontext. Zu Lessings Hamburgischer Dramaturgie." Jahrbuch für Internationale Germanistik 50, no. 1 (January 1, 2018): 149–59. http://dx.doi.org/10.3726/ja501_149.
Повний текст джерелаАнотація:
Abstract ,,Internationalität“, wie sie vom JIG angestrebt wird, ist mit Bevorzugung des europäischen Erbes weitestgehend identisch. Dies gilt insbesondere für die Debatten, die im Dreieck Deutschland – England – Frankreich im Bereich der Theaterästhetik ausgefochten wurden. Die Neuübersetzung ins Französische von Lessings Hamburgischer Dramaturgie mit Einleitung und Kommentar ist ein willkommener Anlass, diese epochale Sachlage zu exemplifizieren. Konkret gehe ich dabei von meiner Edition aus, versuche Lessings impliziten Gedankengang zu rekonstruieren, indem ich den Nachdruck auf die wichtigsten, vom Autor verfochtenen Thesen lege. Die darauf fußenden Analysen sind durchaus historisch-philologisch, eine Verfahrensweise, die übrigens der Lessings in seiner Corneille-Kritik und Aristoteles-Interpretation entspricht.
7
Rozner, Anna. "Lessings Lustspielkonzeption im Spiegel der „Minna von Barnhelm oder das Soldatenglück“." Initium, no. 1 (September 14, 2020): 6–27. http://dx.doi.org/10.33934/initium.2020.1.2.
Повний текст джерелаАнотація:
Im vorliegenden Beitrag wird Gotthold Ephraim Lessings „Minna von Barnhelm oder Das Soldatenglück“ untersucht, das oft als eines der meistgespielten deutschen Lustspiele oder sogar als Wendepunkt in der Geschichte der deutschen Dramatik bezeichnet wird. Die Arbeit geht diesen Behauptungen nach und sucht nach den Gründen für den Erfolg des Werks. Als Ausgangspunkt dienen Lessings eigene dramentheoretische Konzeptionen. Lessings Lustspielkonzeption wurde durch seine Zeitgenossen (wie Gellert, J.E. Schlegel) eindeutig beeinflusst bzw. durch seine Auseinandersetzung mit Theorien seiner Zeit (wie die Gottsched’sche Verlachkomödie) geprägt. „Minna von Barnhelm“ entstand in der produktivstenPhase von Lessings Schaffen, als er sich noch mit seinem dramentheoretischen Hauptwerk, der „Hamburgischen Dramaturgie“, befasste. Dennoch treten die in der „Hamburgischen Dramaturgie“ behandelten Elemente seiner ramenkonzeption bereits in „Minna von Barnhelm“ markant hervor, wie etwa die Hinwendung zur Charakterkomödie, die mitleiderregenden Eigenschaften der Figuren oder die Selbstreflexivität. Die Verwendung solcher Elemente wirkte neuartig in der deutschen Literatur und erregte großes Interesse. Die Beleibtheit des Stückes ist bis heute ungebrochen.
8
Markos, Staci. "TAXONOMIC CHANGES IN LESSINGIA (COMPOSITAE: ASTEREAE)." Madroño 52, no. 1 (January 2005): 60–61. http://dx.doi.org/10.3120/0024-9637(2005)52[60:tcilca]2.0.co;2.
Повний текст джерела
9
Schmidt, Frauke, and Günter Schweigert. "The San Vigilio Group (Toarcian/Aalenian) of the Lessini Mountains (Southern Alps, Northern Italy)." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1991, no. 7 (July 1, 1991): 409–26. http://dx.doi.org/10.1127/njgpm/1991/1991/409.
Повний текст джерела
10
Sebestyen, Amanda, and Doris Lessing. "Mixed Lessing." Women's Review of Books 3, no. 5 (February 1986): 14. http://dx.doi.org/10.2307/4019871.
Повний текст джерелаДисертації з теми "Lessinia"
1
Ferrari, Alice <1994>. "Turismo lento e valorizzazione dell'altopiano della Lessinia: verso una governance partecipata della destinazione." Master's Degree Thesis, Università Ca' Foscari Venezia, 2019. http://hdl.handle.net/10579/16122.
Повний текст джерелаАнотація:
L’elaborato cerca di fornire inizialmente una descrizione dell’altopiano della Lessinia, in provincia di Verona, facendone emergere aspetti geografici, storici e culturali. Si tratta di un territorio fragile e dagli elevati pregi ambientali, tanto da essere individuato come Parco Naturale Regionale della Lessinia.
La ricerca ripercorre i principali momenti della storia del turismo in Lessinia fino ai giorni nostri, riportando informazioni relative alle strutture ricettive presenti così come i flussi turistici degli ultimi anni. Si è voluto poi somministrare un questionario online, rivolto in primis agli abitanti e agli operatori turistici della Lessinia, ed in secondo luogo ai turisti, cercando di far emergere oltre che le loro opinioni, i punti di forza e di debolezza, le opportunità e minacce alle quali la Lessinia deve prestare attenzione.
In seguito si è posta l’attenzione sul concetto di destinazione, sui social media e sulla creazione di una brand identity. Grazie al progetto di marketing territoriale Destinazione Lessinia, che vede la collaborazione tra pubblico e privato, l’altopiano sta muovendo i primi importanti passi verso una vera governance della destinazione. Altre importanti progettualità si stanno sviluppando, come l’iniziativa di candidare gli Alti Pascoli della Lessinia nel Registro Nazionale dei paesaggi rurali storici, arrivando a certificarne il livello di integrità ed unicità del paesaggio.
Ciò consente infine di identificare la Lessinia come possibile meta di un turismo lento, in grado di rispettare i ritmi dell’ambiente, la natura ma anche le tradizioni e la cultura della destinazione.
2
Ciołek-Jóźwiak, Agnieszka. "Gotthold Ephraim Lessings Briefe, 1760 - 1769 : Texte und Erläuterungen /." Stuttgart : Heinz, 2007. http://d-nb.info/988228858/04.
Повний текст джерела
3
Brucker, Barbara S. "Das Ganze, dessen Teile wir sind : zu Tradition und Erfahrung des inneren Raumes bei Doris Lessing /." Würzburg : Königshausen & Neumann, 1999. http://catalogue.bnf.fr/ark:/12148/cb38919699z.
Повний текст джерела
4
Kutter, Marion. "Junge Schreiber auf Lessings Spuren." Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2011. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-79969.
Повний текст джерелаАнотація:
Zum 20. Tag der Sachsen vom 2. bis 4. September 2011 in Kamenz hatte die Stadtbibliothek Kamenz einen außergewöhnlichen Auftritt. Das traditionelle und größte sächsische Vereinsfest bot den Rahmen und die Kulisse für die Auszeichnungsveranstaltung des Kami-Schreibwettbewerbs. Die Bibliothek hatte im Mai 2011 die Schüler der dritten und vierten Klassen der Kamenzer Grundschulen aufgerufen, sich eine Abenteuergeschichte für das dicke und lustige Maskottchen Kami zum 20. Tag der Sachsen auszudenken. Das lebensgroße grüne Männchen besuchte die Kamenzer Grundschulen, stellte den Wettbewerb vor und war dann auch bei der Auszeichnungsveranstaltung dabei. Die Schüler hatten zwei Monate Zeit, den vorgegebenen Textanfang „Die Vögel erwachen und die Lessingstadt wird munter …“ zu ergänzen.
5
Muslim, Zahim Mohammed. "Lessing und der Islam." Doctoral thesis, Humboldt-Universität zu Berlin, Philosophische Fakultät II, 2010. http://dx.doi.org/10.18452/16147.
Повний текст джерелаАнотація:
„Lessing und der Islam“ beschäftigt sich unparteiisch mit Lessings Auseinandersetzung mit dem Islam. Die Arbeit setzt sich das Ziel, den Leser und den Literaturkennern sowie der deutschen Bibliothek der Germanistik etwas von Lessings Auseinandersetzung mit dem Islam in die Hand zu geben, die bis heute als großes Modell für die interkulturelle und interreligiöse Menschheitstoleranzdebatte im Gedächtnis der deutschen Literatur vorhanden ist. Im ersten Teil widmet sich die vorliegende Arbeit den historisch-traditionellen literarischen Hintergründen und Vorkenntnissen Lessings zur islamischen Kultur, und deren Wirkung auf die deutsche Aufklärung im 18. Jahrhundert. In den nächsten Teilen (2-6) beschäftigt sich die Arbeit mit dem Islam in Lessings Werk und den historischen Texten von Voltaire und Marin. Sie konzentriert sich z. B. auf die dramatischen Schaffen und philosophisch-theologischen Schriften dieses deutschen Aufklärers über den Islam wie „Rettung des Hieronymus Cardanus“(1754), „Fatime“- Trauerspiel (1759) und „Nathan der Weise“ (1759) usw. Am Ende wird das Treffen der Religionsvertreter von - Judentum, Christentum und Islam - in „Nathan“ mit der erforderlichen, interkulturellen und interreligiösen Toleranzdebatte als aktuelle Weltfrage verbunden, die als Resultat für diese wissenschafts-literarische Darstellung von Lessings Auseinandersetzung mit dem Islam betrachtet werden kann.„Lessing and Islam“ deals impartially with Lessings discussion with Islam. The work aims to itself to give the reader and the literature experts as well as the German library of the German studies to somewhat of Lessings discussion with Islam in the hand which exists till this day as a big model for the intercultural and interreligious human tolerance debate in memory of the German literature. In the first part the present work devotes itself to the historical-traditional literary backgrounds and foreknowledge Lessings to the Islamic culture, and their effect on the German clarification in the 18th century. In the next parts (2-6) the work deals with Islam in Lessings to work and the historical texts of Voltaire and Marine. She concentrates, e.g., upon the dramatic creating and philosophical-theological writings of this German reconnaissance plane about Islam like „Rescue Hieronymus Cardanus“(1754), "Fatime" (1759) and „Nathan of the manner“ (1779) etc. At the end is connected the meeting of the religious representatives from - Judaism, Christianity and Islam - in "Nathan" with the necessary, intercultural and interreligious tolerance debate as a topical world question which can be looked as a result for this science-literary representation of Lessings discussion with Islam.
6
CAVALLO, GIOVANNI. "Characterisation, sourcing, and processing of Upper Palaeolithic ochre in the Lessini Mountains (NE Italy)." Doctoral thesis, Università degli studi di Pavia, 2016. http://hdl.handle.net/11571/1203395.
Повний текст джерелаАнотація:
Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves.
The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune).
In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR).
Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement.
Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration.
According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves. The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune). In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR). Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement. Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration. According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.
7
CAVALLO, GIOVANNI. "Characterisation, sourcing, and processing of Upper Palaeolithic ochre in the Lessini Mountains (NE Italy)." Doctoral thesis, Università degli studi di Pavia, 2016. http://hdl.handle.net/11571/1263889.
Повний текст джерелаАнотація:
Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves.
The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune).
In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR).
Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement.
Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration.
According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves. The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune). In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR). Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement. Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration. According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.
8
CAVALLO, GIOVANNI. "Characterisation, sourcing, and processing of Upper Palaeolithic ochre in the Lessini Mountains (NE Italy)." Doctoral thesis, Università degli studi di Pavia, 2016. http://hdl.handle.net/11571/1263910.
Повний текст джерелаАнотація:
Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves.
The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune).
In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR).
Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement.
Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration.
According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves. The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune). In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR). Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement. Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration. According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.
9
CAVALLO, GIOVANNI. "Characterisation, sourcing, and processing of Upper Palaeolithic ochre in the Lessini Mountains (NE Italy)." Doctoral thesis, Università degli studi di Pavia, 2016. http://hdl.handle.net/11571/1264030.
Повний текст джерелаАнотація:
Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves.
The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune).
In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR).
Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement.
Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration.
According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves. The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune). In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR). Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement. Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration. According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.
10
CAVALLO, GIOVANNI. "Characterisation, sourcing, and processing of Upper Palaeolithic ochre in the Lessini Mountains (NE Italy)." Doctoral thesis, Università degli studi di Pavia, 2016. http://hdl.handle.net/11571/1263949.
Повний текст джерелаАнотація:
Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves.
The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune).
In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR).
Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement.
Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration.
According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.Goethite and hematite based geomaterials commonly referred as “ochre” were employed in a variety of utilitarian ways by early humans. They used these geomaterials as abrasives and skin protection, in food preservation and pharmacological applications, and for hide tanning and hafting. In addition, these materials were used in symbolic and funerary practices. However, the most well-known use of ochre in Prehistory is as a pigment for the creation of painted scenes in caves. The Western sector of the Lessini Mountains in NE Italy is an ideal location for studying ochre sourcing and processing due to the presence of the important archaeological sites Fumane cave and Tagliente rockshelter. The goethite and hematite based geological raw materials in the Lessini Mountains are found as infilling sediments of palaeokarst caves (Ponte di Veja, Cà de la Pela, Via Tirapelle and Colombare mines), karst fractures, and caves (Sant’Andrea, San Bortolo); they are found associated with basalts (San Giovanni Ilarione and Salgari), or in the form of limited outcrops (Cà del Paver, Manune). In order to approach the study of these materials, a specific analytical program was designed, taking into account the particularities of the geological and archaeological contexts. Microscopic (stereomicroscope, Polarizing Light Microscopy PLM, and Scanning Electron Microscopy coupled with Energy Dispersive X-Ray Spectrometer SEM/EDXS) and Diffractometric (X-Ray Powder Diffraction XRPD) techniques were used in a preliminary investigation of the collected raw materials and archaeological ochre; analysed materials were then grouped on the basis of characteristic mineral assemblages, as well as typical textural and microstructural features; and following these analyses, representative samples were selected in order to study the geochemistry of major and trace elements (Inductively Coupled Plasma Mass Spectrometry ICP-MS). Finally, the heat treatment of some samples of goethite-based ochre was investigated and confirmed using Transmission Electron Microscopy (TEM) whilst the presence of organic compounds in possible artificial mixture was checked with micro-Infrared Spectroscopy (-FTIR). Two potential principal districts were identified for the procurement of Fe-based resources: Ponte di Veja where both quartz-rich and calcite-rich goethite with detrital quartz occur associated with San Vigilio Oolite (Early-Middle Jurassic) and Rosso Ammonitico Veronese (Middle-Late Jurassic) and the sites associated with Mesozoic Dolomitised Limestones (San Bortolo and Sant’Andrea). These sites are in an aerial distance that varies between 7-20 kilometres indicating local procurement. Thermal induced transformation of goethite into hematite was initially supported by the results of the XRPD analyses due to the presence of selective broadening of some reflections and later proven on selected samples through TEM analysis based on the presence of characteristic pores formed during the process of goethite dehydration. According to the scientific and archaeological evidence, ochre was transported to the sites, fragmented, powdered and then used as painting material at Fumane cave. Both yellow and red ochre was mixed with bone fragments for the preparation of a paste whose composition is comparable with that evidenced at Blombos cave in South Africa where a tool-kit containing these ingredients was found. Due to the lack of wear marks on the archaeological ochre from Tagliente rockshelter, it is very difficult to understand the use of ochre in this site. A change in the procurement strategy was identified as quartz-rich materials were exploited during the oldest occupation phases of the site whilst dolomite-based and calcite-based raw materials were selected during the late phases of occupation. No strategy was identified for Fumane cave where dolomite-based raw materials where selected during the different phases of the occupation of the site.
Книги з теми "Lessinia"
1
Il ponte sugli oceani: Lessinia, Veneto, Italia : storie di emigranti. Sommacampagna (Verona): Cierre, 2006.
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2
Franco, Viviani Giuseppe, ed. Cerro Veronese: Un territorio e una comunità della Lessinia centrale. Verona: Bi & Gi, 1985.
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3
Conati, Marcello. Canti veronesi di tradizione orale: Da una ricerca in Valpolicella e in Lessinia, 1969-1982. Negarine di S. Pietro in Cariano (Verona): Il segno dei Gabrielli editori, 2005.
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4
Poli, Emanuele. Geografia dei beni geologici e culturali: Il patrimonio della Lessinia veronese centro-orientale e il geosito di Bolca. Verona, Italy: QuiEdit, 2012.
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5
Lessing und Zinzendorf, eine vergleichende Studie zu Lessings Glauben. New York: P. Lang, 1989.
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6
Mirto, Giacomo. Lessinia e il Segreto Di Selmo. Independently Published, 2021.
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7
Formentini, Corrado, Lucia Maggio, Isabella Formentini, and Marta Saccani. Secret Visions, Verona Mountains Landscape: Fotografie Della Lessinia Verona. Independently Published, 2018.
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8
Formentini, Corrado, Lucia Maggio, Isabella Formentini, and Marta Saccani. Secret Visions Verona Mountains Landscapes: Photographs of Lessinia Territory Verona, Italy. Independently Published, 2018.
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9
Muncker, Franz, G. E. Lessing, and Karl Goedecke. G. E. Lessing: Lessings Werke. Band 1. de Gruyter GmbH, Walter, 2020.
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10
Muncker, Franz, G. E. Lessing, and Karl Goedecke. G. E. Lessing: Lessings Werke. Band 4. de Gruyter GmbH, Walter, 2020.
Знайти повний текст джерелаЧастини книг з теми "Lessinia"
1
Hölzing, Philipp. "Lessing." In Ein Laboratorium der Moderne, 53–61. Wiesbaden: Springer Fachmedien Wiesbaden, 2015. http://dx.doi.org/10.1007/978-3-658-08427-1_4.
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2
Fick, Monika. "Lessing-Bilder." In Lessing-Handbuch, 2–13. Stuttgart: J.B. Metzler, 2016. http://dx.doi.org/10.1007/978-3-476-05399-2_1.
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3
Gymnich, Marion. "Lessing, Doris." In Kindlers Literatur Lexikon (KLL), 1. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_22896-1.
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4
Schuhmann, Karl. "Theodor Lessing." In Edmund Husserl: Briefwechsel, 821–37. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-0745-7_37.
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5
Jakubanis, Matthias. "Lessing, Theodor." In Kindlers Literatur Lexikon (KLL), 1. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_12389-1.
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6
Griem, Eberhard, and Sabine Volk-Birke. "Doris Lessing." In Kindler Kompakt Englische Literatur 20. Jahrhundert, 134–36. Stuttgart: J.B. Metzler, 2015. http://dx.doi.org/10.1007/978-3-476-05526-2_34.
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7
Fick, Monika. "Lessing-Bilder." In Lessing-Handbuch, 23–32. Stuttgart: J.B. Metzler, 2000. http://dx.doi.org/10.1007/978-3-476-03784-8_2.
Повний текст джерела
8
Fick, Monika. "Lessing-Bilder." In Lessing-Handbuch, 23–32. Stuttgart: J.B. Metzler, 2004. http://dx.doi.org/10.1007/978-3-476-03785-5_2.
Повний текст джерела
9
Fick, Monika. "Lessing-Bilder." In Lessing-Handbuch, 2–13. Stuttgart: J.B. Metzler, 2010. http://dx.doi.org/10.1007/978-3-476-00330-0_1.
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10
Ter-Nedden, Gisbert. "Einleitung: Lessings Fehler." In Lessings Trauerspiele, 1–12. Stuttgart: J.B. Metzler, 1986. http://dx.doi.org/10.1007/978-3-476-03215-7_1.
Повний текст джерелаТези доповідей конференцій з теми "Lessinia"
1
Boci, Flutura. "Differences and Similarities of Style, Values, Challenges and Achievements between Doris Lessing and Virginia Woolf." In 3rd International Conference on Social Science, Humanities and Education. Acavent, 2020. http://dx.doi.org/10.33422/3rd.icshe.2020.03.16.
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2
Boci, Flutura. "Differences and Similarities of Style, Values, Challenges and Achievements between Doris Lessing and Virginia Woolf." In 3rd International Conference on Social Science, Humanities and Education. Acavent, 2020. http://dx.doi.org/10.33422/3rd.icshe.2020.03.16.
Повний текст джерела
3
REZKIYANA, Putri Ayu. "Deconstruction Analysis: The Ideas of Keeping Tradition in qNo Witchcraft for Saleq by Doris Lessing." In Sixth International Conference on Languages and Arts (ICLA 2017). Paris, France: Atlantis Press, 2018. http://dx.doi.org/10.2991/icla-17.2018.39.
Повний текст джерелаЗвіти організацій з теми "Lessinia"
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TURLOVA, E., E. ELIZAROVA, and A. ROZHNOVA. LEXICAL AND STYLISTIC MEANS OF GENDER REPRESENTATIONS IN J.M. LESSING'S NOVEL "THE GOLDEN NOTEBOOK". Science and Innovation Center Publishing House, 2021. http://dx.doi.org/10.12731/2077-1770-2021-13-4-3-137-143.
Повний текст джерелаАнотація:
The article deals with the identification of lexical and stylistic means of gender representation in the novel “The Golden Notebook” by the English writer J.M. Lessing. The paper considers the definition of “gender” and distinguishes between the concepts of “gender” and “sex”. A short description of lexical and stylistic means is given and their role in an artistic text is pointed out. D.M. Lessing's novel “The Golden Notebook” is investigated in order to identify lexical and stylistic means of gender representation.