Encountering Environments
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0. Introduction L2/12-386
Doc Type: Working Group Document Title: Revised Proposal to Encode Additional Old Italic Characters Source: UC Berkeley Script Encoding Initiative (Universal Scripts Project) Author: Christopher C. Little ([email protected]) Status: Liaison Contribution Action: For consideration by JTC1/SC2/WG2 and UTC Replaces: N4046 (L2/11-146R) Date: 2012-11-06 0. Introduction The existing Old Italic character repertoire includes 31 letters and 4 numerals. The Unicode Standard, following the recommendations in the proposal L2/00-140, states that Old Italic is to be used for the encoding of Etruscan, Faliscan, Oscan, Umbrian, North Picene, and South Picene. It also specifically states that Old Italic characters are inappropriate for encoding the languages of ancient Italy north of Etruria (Venetic, Raetic, Lepontic, and Gallic). It is true that the inscriptions of languages north of Etruria exhibit a number of common features, but those features are often exhibited by the other scripts of Italy. Only one of these northern languages, Raetic, requires the addition of any additional characters in order to be fully supported by the Old Italic block. Accordingly, following the addition of this one character, the Unicode Standard should be amended to recommend the encoding of Venetic, Raetic, Lepontic, and Gallic using Old Italic characters. In addition, one additional character is necessary to encode South Picene inscriptions. This proposal is divided into five parts: The first part (§1) identifies the two unencoded characters (Raetic Ɯ and South Picene Ũ) and demonstrates their use in inscriptions. The second part (§2) examines the use of each Old Italic character, as it appears in Etruscan, Faliscan, Oscan, Umbrian, South Picene, Venetic, Raetic, Lepontic, Gallic, and archaic Latin, to demonstrate the unifiability of the northern Italic languages' scripts with Old Italic. -
Culture E Studi Del Sociale Cussoc ISSN: 2531-3975
Culture e Studi del Sociale CuSSoc ISSN: 2531-3975 Movement to Another Place. Cultural Expressions of Migration as Source of Reflection Contributing to Social Theory PAICH SLOBODAN DAN Come citare / How to cite Paich, S.D. (2017). Movement to Another Place. Cultural Expressions of Migration as Source of Ref- lection Contributing to Social Theory. Culture e Studi del Sociale, 2(2), 129-141. Disponibile / Retrieved from http://www.cussoc.it/index.php/journal/issue/archive 1. Affiliazione Autore / Authors’ information The Artship Foundation, San Francisco-USA 2. Contatti / Authors’ contact Slobodan Dan Paich: [email protected] Articolo pubblicato online / Article first published online: Dicembre/December 2017 - Peer Reviewed Journal Informazioni aggiuntive / Additional information Culture e Studi del Sociale Movement to Another Place. Cultural Expressions of Migration as Source of Reflection Contributing to Social Theory Slobodan Dan Paich The Artship Foundation – San Francisco, USA E-mail: [email protected] Abstract Methodologies are explored to enriching migration theory, with an inter-disciplinary look into cultural expressions resulting from migration. Cultural and migration maps offer a comparative and diachronic insight into migration impulses and waves.Migration of ideas and techniques is also examined through artifacts resulting from forced or intended move- ment of people and experts. Two contemporary plays evolved from the stories of mi- grants/refugees offer probing and open-ended speculation about itinerancy, vagrancy, reset- tlement and economic emigration as part of social plurality. The tangible, visceral qualities of expression may shed light on issues too complex for verbal theory only. Approached is comparative examination of stylization in art and abstraction in theoretical inquiry. -
Geologia Della Sicilia - Geology of Sicily IV - Vulcanismo - Volcanism
Geologia della Sicilia - Geology of Sicily IV - Vulcanismo - Volcanism BRANCA S. (*) 1. - VuLCANISMO QuATERNARIO DELLA ratterizzavano questo settore dell’Altipiano Ibleo SICILIA ORIENTALE (SChMINCkE et alii, 1997). La prosecuzione dell’at- tività vulcanica verso nord durante il Pleistocene La fase più recente del vulcanismo ibleo è da- inferiore-medio è evidenziata da anomalie magne- tata Pliocene inferiore-Pleistocene inferiore, ed è tiche (GRASSO & BEN-AVRAhAM, 1992) e da dati caratterizzata da un’attività vulcanica sia sottoma- di pozzi perforati dall’AGIP (LONGARETTI et alii, rina che subaerea ad affinità da alcalina a subalca- 1991; TORELLI et alii, 1998) in corrispondenza della lina (CARBONE et alii, 1986, 1987; CARVENI et alii, Piana di Catania, che mostrano la presenza di 1991; SChMINCkE et alii, 1997). grossi corpi di vulcaniti, con spessori di alcune Le vulcaniti affiorano estesamente lungo il centinaia di metri, che si approfondiscono verso bordo settentrionale dell’Avampaese Ibleo mo- nord per la presenza di sistemi di faglie dirette. In strando una leggera migrazione verso nord rispetto particolare, le vulcaniti più recenti in sottosuolo, alle manifestazioni vulcaniche del Miocene supe- attribuite al Pleistocene inferiore (LONGARETTI et riore (CARBONE et alii, 1982c). Le vulcaniti plioce- alii, 1991), sono localizzate nella parte più setten- niche del margine occidentale dell’Altipiano Ibleo, trionale della Piana di Catania in prossimità della sono rappresentate da una potente successione, periferia meridionale dell’Etna fra Paternò e Cata- costituita da prevalenti ialoclastiti e da brecce vul- nia. Tali vulcaniti presentano una composizione canoclastiche e colate a pillow. Lungo il bordo basaltica ad affinità sia tholeiitica che alcalina orientale del plateau si rinvengono prevalentemente (LONGARETTI & ROCChI, 1990). -
And Correlation to the Late Triassic Newark Astrochronological Polarity Time Scale
Tethyan magnetostratigraphy from Pizzo Mondello (Sicily) and correlation to the Late Triassic Newark astrochronological polarity time scale Giovanni Muttoni† Department of Earth Sciences, University of Milan, Via Mangiagalli 34, I-20133 Milan, Italy Dennis V. Kent Lamont-Doherty Earth Observatory, Palisades, New York 10964, USA and Department of Geological Sciences, Rutgers University, Piscataway, New Jersey 08854, USA Paul E. Olsen Lamont-Doherty Earth Observatory, Palisades, New York 10964, USA Piero Di Stefano Department of Geology and Geodesy, University of Palermo, Corso Tukory 131, I-90134 Palermo, Italy William Lowrie Stefano M. Bernasconi Fátima Martín Hernández Departement Erdwissenschaften, ETH-Zentrum, CH-8092 Zürich, Switzerland ABSTRACT early part of the Newark APTS. We prefer marine stages, historically based on ammonoid option #2 in which the Carnian-Norian biostratigraphy, to continental successions. For We present the magnetostratigraphy and boundary based on conodonts, as well as the Late Triassic, an astrochronology anchored stable isotope stratigraphy from an expanded its closely associated positive δ13C shift, cor- to magnetostratigraphy and radiometric dates is (~430-m-thick) Upper Triassic marine lime- respond to Newark magnetozone E7 at ca. available from the Newark continental section stone section at Pizzo Mondello, Sicily, and 228–227 Ma (adopting Newark astrochronol- (Kent et al., 1995; Kent and Olsen, 1999; Olsen review published biostratigraphic informa- ogy), implying a long Norian with a duration and Kent, 1999), while magnetostratigraphy is tion that can be used to defi ne the location of ~20 m.y., and a Rhaetian of ~6 m.y. dura- thus far available in conjunction with marine of the conodont Carnian-Norian and Norian- tion. -
Halyciae – Salemi : Un Caso Di Parziale Continuità Fra L'età Bizantina
GLI ABITATI DELLA SICILIA OCCIDENTALE DAL PERIODO BIZANTINO ALL’ETÀ NORMANNO-SVEVA INTRODUZIONE I Halyciae – Salemi : Un caso di parziale continuità fra l’età bizantina e il periodo normanno-svevo II Le attestazioni documentarie e letterarie di epoca medievale III Attestazioni documentarie e letterarie dei siti fortificati e casali nell’agro salemitano IV Testimonianze archeologiche Prima analisi di ricognizione 1 PREMESSA Il presente progetto di ricerca, il cui quadro cronologico riguarda le modalità insediative in Sicilia occidentale dall’età bizantina al periodo normanno e svevo, si prefigge la ricostruzione della storia e degli insediamenti che caratterizzano il paesaggio dal periodo bizantino alla feudalità normanna e sveva al fine di meglio comprenderne le trasformazioni dell’abitato medievale della Sicilia occidentale. La prospettiva di ricerca qui assunta vede il tentativo di saldare i temi propri della ricerca archeologica e topografica (le modificazioni dell’habitat, le dinamiche del popolamento) con quelli della ricerca storica, collocando nel contesto concreto di un territorio le istituzioni e i meccanismi messi in atto per il suo controllo e il suo dominio. La prima parte, sviluppata nel corso del primo anno di ricerca, è costituita dallo studio dei documenti degli Archivi, delle Biblioteche di ogni singolo comune della provincia di Trapani (Sicilia). Malgrado la documentazione archivistica siciliana a nostra disposizione cominci soltanto dalla conquista normanna1, la ricerca si prefigge, un’analisi delle attestazioni documentarie utili quali atti privati e pubblici, presso l’Archivio del vescovado di Mazara, presso l’Archivio di Stato di Trapani e di Palermo, dove prevalgono in genere i testi in lingua latina. Nella ricerca delle fonti documentarie, verranno inclusi gli archivi (previa autorizzazione) delle chiese. -
Paleozoic Evolution of Pre-Variscan Terranes: from Gondwana to the Variscan Collision
Geological Society of America Special Paper 364 2002 Paleozoic evolution of pre-Variscan terranes: From Gondwana to the Variscan collision Gérard M. Stamp×i Institut de Géologie et Paléontologie, Université de Lausanne, CH-1015 Lausanne, Switzerland Jürgen F. von Raumer Institut de Minéralogie et Pétrographie, Université de Fribourg, CH-1700 Fribourg, Switzerland Gilles D. Borel Institut de Géologie et Paléontologie, Université de Lausanne, CH-1015 Lausanne, Switzerland ABSTRACT The well-known Variscan basement areas of Europe contain relic terranes with a pre-Variscan evolution testifying to their peri-Gondwanan origin (e.g., relics of Neo- proterozoic volcanic arcs, and subsequent stages of accretionary wedges, backarc rift- ing, and spreading). The evolution of these terranes was guided by the diachronous subduction of the proto-Tethys oceanic ridge under different segments of the Gond- wana margin. This subduction triggered the emplacement of magmatic bodies and the formation of backarc rifts, some of which became major oceanic realms (Rheic, paleo- Tethys). Consequently, the drifting of Avalonia was followed, after the Silurian and a short Ordovician orogenic event, by the drifting of Armorica and Alpine domains, ac- companied by the opening of the paleo-Tethys. The slab rollback of the Rheic ocean is viewed as the major mechanism for the drifting of the European Variscan terranes. This, in turn, generated a large slab pull force responsible for the opening of major rift zones within the passive Eurasian margin. Therefore, the µrst Middle Devonian Variscan orogenic event is viewed as the result of a collision between terranes detached from Gondwana (grouped as the Hun superterrane) and terranes detached from Eurasia. -
Ph.D Thesis: Stratigraphic, Structural and Geomorphological Features of the Sicilian Continental Shelf: Study Cases from Southern Tyrrhenian and Sicily Channel
Ph.D Thesis: Stratigraphic, structural and geomorphological features of the Sicilian continental shelf: study cases from Southern Tyrrhenian and Sicily Channel. Ph.D Thesis: Stratigraphic, structural and geomorphological features of the Sicilian continental shelf: study cases from Southern Tyrrhenian and Sicily Channel. Ph.D Thesis: Stratigraphic, structural and geomorphological features of the Sicilian continental shelf: study cases from Southern Tyrrhenian and Sicily Channel. INDEX GENERAL INTRODUCTION PART I: METHODOLOGY 1.0 INTRODUCTION 1.1 SONAR PRINCIPLES IN THE WATER 1.2 ECHOSOUNDING 1.3 MULTIBEAM 1.4 CHIRP SUB-BOTTOM 1.5 SPARKER SYSTEM 1.6 BATHYMETRIC AND SEISMIC INTERPRETATION SOFTWARES 1.6.1 GLOBAL MAPPER 1.6.2 SWANPRO™ 1.6.3 GEOSUITE ALLWORKS 1.7 SEISMIC STRATIGRAPHY PRINCIPLES 1.8 THE SEISMIC RESOLUTION PART II: CONTINENTAL SHELF ENVIRONMENT: STRUCTURAL-STRATIGRAPHIC EVOLUTION OF LAMPEDUSA ISLAND AND SOUTH-EAST SICILY OFFSHORE 2.0 INTRODUCTION 2.1 PHYSIOGRAPHIC FEATURES OF THE CONTINENTAL SHELF 2.2 DEPOSITIONAL ENVIROMENTS: AUTOGENIC AND ALLOGENIC CONTROLS 2.3 SEQUENCE STRATIGRAPHY 2.3.1 SEQUENCE STRATIGRAPHIC UNITS 2.3.2 SEQUENCE STRATIGRAPHIC SURFACES 2.4 LATE MIOCENE TO QUATERNARY STRUCTURAL EVOLUTION OF THE LAMPEDUSA ISLAND OFFSHORE 1 Ph.D Thesis: Stratigraphic, structural and geomorphological features of the Sicilian continental shelf: study cases from Southern Tyrrhenian and Sicily Channel. 2.4.1 GEOLOGICAL SETTING 2.4.2 DATA DESCRIPTION AND INTERPRETATION 2.4.2.1 Northern sector 2.4.2.2 Southern Sector 2.4.2.3 Eastern -
Demeter Malophoros and Zeus Meilichios in Selinus
Journal of Ancient History 2019; 7(1): 62–110 Allaire B. Stallsmith* A Divine Couple: Demeter Malophoros and Zeus Meilichios in Selinus https://doi.org/10.1515/jah-2018-0019 Abstract: This paper concerns a collection of rough-hewn flat stelae excavated from the precinct of Zeus Meilichios in Selinus, Sicily between 1915 and 1926, a majority with two heads or busts, one male and one female, carved at their tops. These crudely fashioned idols are unique in their iconography. They combine the flat inscribed Punic stela with the Greek figural tradition, with some indigenous features. Their meaning is totally obscure – especially since they lack any literary reference. No comparable monuments have been found in ancient Mediterranean cult. The twin stelae were often set up above a collection of burnt rodent and bird bones, ashes, lamps, broken and burnt pottery and terracotta figurines, as a mem- orial of a sacrifice. The stelae were the objects of a gentilicial cult, similar to that posited for the inscribed “Meilichios stones” with which they shared the Field of Stelae of Zeus Meilichios. The theory advanced here interprets these diminutive stelae (average height 30 cm) as the objects of domestic cult. It was customary in many parts of the ancient Mediterranean, from the Bronze Age down to the Ro- man period, to venerate household or family gods who protected the health and the wealth of the family. They were thought to embody the spirits of the ancestors and could at times be identified with the gods of the state religion. This divine couple whose effigies were dedicated in the Field of Stelae over a period of four centuries, into the third century, cannot be claimed as Greek or Punic deities. -
Sicily Before the Greeks. the Interaction with Aegean and the Levant in the Pre-Colonial Era
Open Archaeology 2020; 6: 172–205 Review Article Davide Tanasi* Sicily Before the Greeks. The Interaction with Aegean and the Levant in the Pre-colonial Era https://doi.org/10.1515/opar-2020-0107 received April 17, 2020; accepted July 1, 2020. Abstract: The relationship between Sicily and the eastern Mediterranean – namely Aegean, Cyprus and the Levant – represents one of the most intriguing facets of the prehistory of the island. The frequent and periodical contact with foreign cultures were a trigger for a gradual process of socio-political evolution of the indigenous community. Such relationship, already in inception during the Neolithic and the Copper Age, grew into a cultural phenomenon ruled by complex dynamics and multiple variables that ranged from the Mid-3rd to the end of the 2nd millennium BCE. In over 1,500 years, a very large quantity of Aegean and Levantine type materials have been identified in Sicily alongside with example of unusual local material culture traditionally interpreted as resulting from external influence. To summarize all the evidence during such long period and critically address it in order to attempt historical reconstructions is a Herculean labor. Twenty years after Sebastiano Tusa embraced this challenge for the first time, this paper takes stock on two decades of new discoveries and research reassessing a vast amount of literature, mostly published in Italian and in regional journals, while also address the outcomes of new archaeometric studies. The in-depth survey offers a new perspective of general trends in this East-West relationship which conditioned the subsequent events of the Greek and Phoenician colonization of Sicily. -
K2SO4 Across the Neogene: Implications, Part 4 of 4
www.saltworkconsultants.com Salty MattersJohn Warren - Tuesday, May 12, 2015 Danakil potash: K2SO4 across the Neogene: Implications, Part 4 of 4 marine brine feeds that most of the world’s larger Phaneorzo- How to deal with K2SO4 ic (SOP) potash ore deposits were precipitated (Warren, 2015). In this the fourth blog focusing on Danakhil potash, we look SOP is also produced from Quaternary Lake brines in China at the potash geology of formerly mined Neogene deposits in and Canada (see Cryogenic salt blog; 24 Feb. 2015). Sicily and the Ukraine, then compare them and relevant pro- cessing techniques used to exploit their K2SO4 ore feeds. This information is then used to hlep guide a discussion of process- ing implications for potash extraction in the Danakhil, where SOP in Messinian evaporites, Sicily kainite is the dominant widespread potash salt. As seen in the A number of potash mines on the island extracted kainitite from previous three blogs there are other potash mineral styles present the late Miocene Solofifera Series of Sicily (Figure 1). The last in the Danakhil, which constitute more re- stricted ore fairways than the widespread bedded kainaite, these other potash styles Sicilian-Maghrebian units (deep meteoiric -blog 2 of 4 and hydro- thermal - blog 3 of 4), could be processed Palermo X Kabylian-Calabrian units to extract MOP, but these other potash Calatami inner C styles are also tied to high levels of MgCl2, im Madonie M. in Petralia Nebrodi M. na b which must be dealt with in the brine pro- S. Ninfa asin Nicosia Be M. -
Transactions of the Botanical Society of Edinburgh I. Notes on the Botany
This article was downloaded by: [UQ Library] On: 14 March 2015, At: 14:07 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Transactions of the Botanical Society of Edinburgh Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/tped18 I. Notes on the Botany and Agriculture of Malta and Sicily H. Cleghorn M.D. Published online: 01 Dec 2010. To cite this article: H. Cleghorn M.D. (1870) I. Notes on the Botany and Agriculture of Malta and Sicily , Transactions of the Botanical Society of Edinburgh, 10:1-4, 106-139, DOI: 10.1080/03746607009468660 To link to this article: http://dx.doi.org/10.1080/03746607009468660 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content. -
A Seismic Model for Moho and Crustal Structure in Europe, Greenland, and the North Atlantic Region☆
Tectonophysics 609 (2013) 97–153 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Review Article EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region☆ Irina M. Artemieva ⁎, Hans Thybo IGN, University of Copenhagen, Denmark article info abstract Article history: We present a new digital crustal model for Moho depth and crustal structure in Europe, Greenland, Iceland, Received 27 November 2012 Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W–62E, 30N–84N). Our compilation is based Received in revised form 18 July 2013 on digitization of original seismic profiles and Receiver Functions from ca. 650 publications which provides a Accepted 4 August 2013 dense regional data coverage. Exclusion of non-seismic data allows application of the database to potential Available online 15 August 2013 field modeling. EUNAseis model includes Vp velocity and thickness of five crustal layers, including the sedimen- tary cover, and Pn velocity. For each parameter we discuss uncertainties associated with theoretical limitations, Keywords: Moho regional data quality, and interpolation. Crustal thickness By analyzing regional trends in crustal structure and links to tectonic evolution illustrated by a new tectonic map, Crystalline crust we conclude that: (1) Each tectonic setting shows significant variation in depth to Moho and crustal structure, Sedimentary cover essentially controlled by the age of latest tectono-thermal processes; (2) Published global averages of crustal pa- Pn velocity rameters are outside of observed ranges for any tectonic setting in Europe; (3) Variation of Vp with depth in the Crustal evolution sedimentary cover does not follow commonly accepted trends; (4) The thickness ratio between upper-middle (Vp b 6.8 km/s) and lower (Vp N 6.8 km/s) crystalline crust is indicative of crustal origin: oceanic, transitional, platform, or extended crust; (5) Continental rifting generally thins the upper-middle crust significantly without changing Vp.