Governance in Ptolemaic Egypt: from Raphia to Cleopatra Vii (217 - 31 B.C.), Class-Based ‘Colonialism’? 1
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The Coinage System of Cleopatra Vii, Marc Antony and Augustus in Cyprus
1 / 140 THE COINAGE SYSTEM OF CLEOPATRA VII, MARC ANTONY AND AUGUSTUS IN CYPRUS THE COINAGE SYSTEM OF CLEOPATRA VII, MARC ANTONY AND AUGUSTUS IN CYPRUS By Matthew Kreuzer 2 / 140 THE COINAGE SYSTEM OF CLEOPATRA VII, MARC ANTONY AND AUGUSTUS IN CYPRUS THE COINAGE SYSTEM OF CLEOPATRA VII, MARC ANTONY AND AUGUSTUS IN CYPRUS By Matthew Kreuzer Second Edition Springfield, Mass. Copyright Matthew Kreuzer 2000-2009. 3 / 140 THE COINAGE SYSTEM OF CLEOPATRA VII, MARC ANTONY AND AUGUSTUS IN CYPRUS Contents Summary 5 Historical Background 9 Coins Circulating in Cleopatra’s Cyprus 51-30 BC 10 What Were the Denominations in Cleopatra’s Cyprus? 12 The Tetradrachm 13 The Drachm 28 The Full-Unit 29 The Half-Unit 35 The Quarter-Unit 39 The Eighth-Unit 41 The Tiny Sixteenth-Unit 45 Other Small Late Ptolemaic Bronzes 48 Archeological Context – A Late Ptolemaic Bronze Mint 50 Making Small Change 53 Relationship Between the Denominations 55 Circulating Earlier Ptolemaic and Foreign Coinage 56 Cypriot Bronze of Cleopatra, After Actium 58 Silver denarii of Marc Antony, 37-30 BC 61 Cypriot Coinage Under Augustus, 30-22 BC 69 Cypriot Bronze of Augustus, CA coinage 70 Non-Export Obols and Quadrans 75 Silver Quinarii and Denarii of Augustus, 28-22 BC 78 Cyprus as a Senatorial Province under Augustus, 22 BC to 14 AD 87 Cypriot Coinage under Tiberius and Later, After 14 AD 92 Table of Suggested Attribution Changes 102 Appendix I - Analysis of Declining Obol Weight Standard 121 Appendix II - Octavia or Cleopatra? Credits and Bibliography 139 4 / 140 THE COINAGE SYSTEM OF CLEOPATRA VII, MARC ANTONY AND AUGUSTUS IN CYPRUS "If the nose of Cleopatra had been a little shorter, the whole face of the world would have been changed." Blaise Pascal 5 / 140 THE COINAGE SYSTEM OF CLEOPATRA VII, MARC ANTONY AND AUGUSTUS IN CYPRUS Summary During the late reign of Cleopatra VII a cornucopia of coinage circulated in Cyprus. -
Cleopatra II and III: the Queens of Ptolemy VI and VIII As Guarantors of Kingship and Rivals for Power
Originalveröffentlichung in: Andrea Jördens, Joachim Friedrich Quack (Hg.), Ägypten zwischen innerem Zwist und äußerem Druck. Die Zeit Ptolemaios’ VI. bis VIII. Internationales Symposion Heidelberg 16.-19.9.2007 (Philippika 45), Wiesbaden 2011, S. 58–76 Cleopatra II and III: The queens of Ptolemy VI and VIII as guarantors of kingship and rivals for power Martina Minas-Nerpel Introduction The second half of the Ptolemaic period was marked by power struggles not only among the male rulers of the dynasty, but also among its female members. Starting with Arsinoe II, the Ptolemaic queens had always been powerful and strong-willed and had been a decisive factor in domestic policy. From the death of Ptolemy V Epiphanes onwards, the queens controlled the political developments in Egypt to a still greater extent. Cleopatra II and especially Cleopatra III became all-dominant, in politics and in the ruler-cult, and they were often depicted in Egyptian temple- reliefs—more often than any of her dynastic predecessors and successors. Mother and/or daughter reigned with Ptolemy VI Philometor to Ptolemy X Alexander I, from 175 to 101 BC, that is, for a quarter of the entire Ptolemaic period. Egyptian queenship was complementary to kingship, both in dynastic and Ptolemaic Egypt: No queen could exist without a king, but at the same time the queen was a necessary component of kingship. According to Lana Troy, the pattern of Egyptian queenship “reflects the interaction of male and female as dualistic elements of the creative dynamics ”.1 The king and the queen functioned as the basic duality through which regeneration of the creative power of the kingship was accomplished. -
Macedonian Kings, Egyptian Pharaohs the Ptolemaic Family In
Department of World Cultures University of Helsinki Helsinki Macedonian Kings, Egyptian Pharaohs The Ptolemaic Family in the Encomiastic Poems of Callimachus Iiro Laukola ACADEMIC DISSERTATION To be publicly discussed, by due permission of the Faculty of Arts at the University of Helsinki in auditorium XV, University Main Building, on the 23rd of September, 2016 at 12 o’clock. Helsinki 2016 © Iiro Laukola 2016 ISBN 978-951-51-2383-1 (paperback.) ISBN 978-951-51-2384-8 (PDF) Unigrafia Helsinki 2016 Abstract The interaction between Greek and Egyptian cultural concepts has been an intense yet controversial topic in studies about Ptolemaic Egypt. The present study partakes in this discussion with an analysis of the encomiastic poems of Callimachus of Cyrene (c. 305 – c. 240 BC). The success of the Ptolemaic Dynasty is crystallized in the juxtaposing of the different roles of a Greek ǴdzȅǻǽǷȏȄ and of an Egyptian Pharaoh, and this study gives a glimpse of this political and ideological endeavour through the poetry of Callimachus. The contribution of the present work is to situate Callimachus in the core of the Ptolemaic court. Callimachus was a proponent of the Ptolemaic rule. By reappraising the traditional Greek beliefs, he examined the bicultural rule of the Ptolemies in his encomiastic poems. This work critically examines six Callimachean hymns, namely to Zeus, to Apollo, to Artemis, to Delos, to Athena and to Demeter together with the Victory of Berenice, the Lock of Berenice and the Ektheosis of Arsinoe. Characterized by ambiguous imagery, the hymns inspect the ruptures in Greek thought during the Hellenistic age. -
The History of Ancient Egypt “Passionate, Erudite, Living Legend Lecturers
“Pure intellectual stimulation that can be popped into Topic Subtopic the [audio or video player] anytime.” History Ancient History —Harvard Magazine The History of Ancient Egypt “Passionate, erudite, living legend lecturers. Academia’s best lecturers are being captured on tape.” —The Los Angeles Times The History “A serious force in American education.” —The Wall Street Journal of Ancient Egypt Course Guidebook Professor Bob Brier Long Island University Professor Bob Brier is an Egyptologist and Professor of Philosophy at the C. W. Post Campus of Long Island University. He is renowned for his insights into ancient Egypt. He hosts The Learning Channel’s popular Great Egyptians series, and his research was the subject of the National Geographic television special Mr. Mummy. A dynamic instructor, Professor Brier has received Long Island University’s David Newton Award for Teaching Excellence. THE GREAT COURSES® Corporate Headquarters 4840 Westfields Boulevard, Suite 500 Chantilly, VA 20151-2299 Guidebook USA Phone: 1-800-832-2412 www.thegreatcourses.com Cover Image: © Hemera/Thinkstock. Course No. 350 © 1999 The Teaching Company. PB350A PUBLISHED BY: THE GREAT COURSES Corporate Headquarters 4840 Westfi elds Boulevard, Suite 500 Chantilly, Virginia 20151-2299 Phone: 1-800-TEACH-12 Fax: 703-378-3819 www.thegreatcourses.com Copyright © The Teaching Company, 1999 Printed in the United States of America This book is in copyright. All rights reserved. Without limiting the rights under copyright reserved above, no part of this publication may be reproduced, stored in or introduced into a retrieval system, or transmitted, in any form, or by any means (electronic, mechanical, photocopying, recording, or otherwise), without the prior written permission of The Teaching Company. -
The Christianisation of Adulis in Light of the Material Evidence
chapter 17 The Christianisation of Adulis in Light of the Material Evidence Serena Massa and Caterina Giostra 1 The Archaeological Research in the Ancient Town of Adulis The site of Adulis is located on the south-western coast of the Red Sea, in the well-protected bay of Zula, about 40 km south of Massawa, Eritrea.1 In the ancient world it was one of the most important ports connecting East Africa and the Mediterranean along the spice trade route from India. The Adulis commercial vocation was probably already active in the Pharaonic era, in the context of the traffic in precious materials not found in Egypt and sought in the Land of Punt.2 From the size of village3 and oppidum4 reported by the sources in the second half of the first century CE, an increasing development and importance of the site until the Byzantine period is concomitant with the rise of the Aksumite kingdom, of which Adulis represented the gate to the sea.5 1 An independent state since 1993, in antiquity the area was part of the same context of the highland territories that are currently included within the borders of Ethiopia. 2 The location of Adulis can be included in the area of the Land of Punt, identified in the regions bordering the southern Red Sea and perhaps coinciding with the locality of WDDT recorded in the geographical list of the 18th Dynasty. Archaeological levels dating to the lat- ter half of the second millennium–early first millennium BCE were documented by archae- ological excavations: Adulis in this period is considered part of the Afro-Arabian cultural complex, which extends from southern Arabian regions to the Eritrean plateau: R. -
Art and Royalty in Sparta of the 3Rd Century B.C
HESPERIA 75 (2006) ART AND ROYALTY Pages 203?217 IN SPARTA OF THE 3RD CENTURY B.C. ABSTRACT a The aim of this paper is to demonstrate that revival of the arts in Sparta b.c. was during the 3rd century owed mainly to royal patronage, and that it was inspired by Alexander s successors, the Seleukids and the Ptolemies in particular. The tumultuous transition from the traditional Spartan dyarchy to a and to its dominance Hellenistic-style monarchy, Sparta's attempts regain in the P?loponn?se (lost since the battle of Leuktra in 371 b.c.), are reflected in the of the hero Herakles as a role model promotion pan-Peloponnesian at for the single king the expense of the Dioskouroi, who symbolized dual a kingship and had limited, regional appeal. INTRODUCTION was Spartan influence in the P?loponn?se dramatically reduced after the battle of Leuktra in 371 b.c.1 The history of Sparta in the 3rd century b.c. to ismarked by intermittent efforts reassert Lakedaimonian hegemony.2 A as a means to tendency toward absolutism that end intensified the latent power struggle between the Agiad and Eurypontid royal houses, leading to the virtual abolition of the traditional dyarchy in the reign of the Agiad Kleomenes III (ca. 235-222 b.c.), who appointed his brother Eukleides 1. For the battle of Leuktra and its am to and Ellen Millen 2005.1 grateful Graham Shipley Paul Cartledge and see me to am consequences, Cartledge 2002, and Ellen Millender for inviting der for historical advice. I also 251-259. -
The Ptolemies: an Unloved and Unknown Dynasty. Contributions to a Different Perspective and Approach
THE PTOLEMIES: AN UNLOVED AND UNKNOWN DYNASTY. CONTRIBUTIONS TO A DIFFERENT PERSPECTIVE AND APPROACH JOSÉ DAS CANDEIAS SALES Universidade Aberta. Centro de História (University of Lisbon). Abstract: The fifteen Ptolemies that sat on the throne of Egypt between 305 B.C. (the date of assumption of basileia by Ptolemy I) and 30 B.C. (death of Cleopatra VII) are in most cases little known and, even in its most recognised bibliography, their work has been somewhat overlooked, unappreciated. Although boisterous and sometimes unloved, with the tumultuous and dissolute lives, their unbridled and unrepressed ambitions, the intrigues, the betrayals, the fratricides and the crimes that the members of this dynasty encouraged and practiced, the Ptolemies changed the Egyptian life in some aspects and were responsible for the last Pharaonic monuments which were left us, some of them still considered true masterpieces of Egyptian greatness. The Ptolemaic Period was indeed a paradoxical moment in the History of ancient Egypt, as it was with a genetically foreign dynasty (traditions, language, religion and culture) that the country, with its capital in Alexandria, met a considerable economic prosperity, a significant political and military power and an intense intellectual activity, and finally became part of the world and Mediterranean culture. The fifteen Ptolemies that succeeded to the throne of Egypt between 305 B.C. (date of assumption of basileia by Ptolemy I) and 30 B.C. (death of Cleopatra VII), after Alexander’s death and the division of his empire, are, in most cases, very poorly understood by the public and even in the literature on the topic. -
Antiochus IV Rome
Chapter 22 Chapter 7 Chapter 8 Chapter 9 Chapter 11 & 12 Babylon Medo- 445BC 4 Persian Kings Persia Alex the Great Greece N&S Kings Antiochus IV Rome Gap of Time Time of the Gentiles 1wk 3 ½ years Opposing king. Greek Empire Chapter 8 Alexander The Great King of the South King of the North 1. Ptolemy I Soter 1. Seleucus I Nicator 2. Antiochus I Soter 2. Ptolemy II Philadelphus 3. Antiochus II Theos 3. Ptolemy III Euergetes 4. Seleucus II Callinicus 5. Seleucus III Ceraunus 4. Ptolemy IV Philopator 6. Antiochus III Great 5. Ptolemy V Epiphanes 7. Seleucus IV Philopator 6. Ptolemy VI Philometor 8. Antiochus IV Epiphanes Daniel 9:27 The 70th Week 1 Week = 7 years 3 ½ years 3 ½ years Apostasy Make a covenant Stop to Temple sacrifice with the many Stop to grain offering Abomination of Desolation Crush the elect (Jews) Jacob’s Distress Jacob’s Trouble Tribulation Daniel 11:35 Some of those who have insight will fall, in order to refine, purge and make them pure until the end time; because it is still to come at the appointed time 1 John 3:2-3 2 Beloved, now we are children of God, and it has not appeared as yet what we will be. We know that when He appears, we will be like Him, because we will see Him just as He is. 3 And everyone who has his hope fixed on Him purifies himself, just as He is pure. Zechariah 13:7-9 8 “It will come about in all the land,” Declares the LORD, “That two parts in it will be cut off and perish; But the third will be left in it. -
Greece) During Unrest and Rest Period
Harokopio University of Athens Department of Geography Deformation time series monitoring of Nisyros Volcano (Greece) during unrest and rest period. Derdelakos K.1, Papageorgiou E.2, Parcharidis I.1, Benekos G. 1 1 Harokopio University of Athens, Department of Geography, El. Venizelou 70 Kallithea, 17671 Athens, Greece, [email protected], [email protected] 2 National Research Council of Italy, Rome, Italy, [email protected] Abstract The Hellenic Volcanic Arc, which stretches from Aegina and Methana in the west over Milos and Santorini and terminates at Kos and Nisyros in the east of Aegean Sea, is a result of northeastward-directed subduction (started around 4 Ma at the beginning of Pliocene) of the African plate beneath the Aegean microplate. Santorini volcano in the central sector of the arc and Nisyros in the eastern sector, are the two active volcanoes of the arc. Nisyros shows an unrest phase during 1996-97 accompanied by intensive seismic activity in the broader area at the beginning of 1996 and lasted through the end of 1997 and returned to the background level at the beginning of 1998. Spaceborne radar interferometry has already shown its ability in mapping ground deformation, like co-seismic deformation, as well as long-term movements as is the ground deformation in volcanoes, landslides and subsidence. This technique can be used to identify Fig. 1 Location of the study area ground-surface deformation associated with movement of magma and/or hydrothermal fluids beneath volcanoes. Ground deformation monitoring is one of the main parameters that should be considered to assess volcanic hazard. -
An Interactive Story Map for the Methana Volcanic Peninsula
An Interactive Story Map for the Methana Volcanic Peninsula Varvara Antoniou1, Paraskevi Nomikou1, Pavlina Bardouli1, Danai Lampridou1, Theodora Ioannou1, Ilias Kalisperakis2, Christos Stentoumis2, Malcolm Whitworth3, Mel Krokos4 and Lemonia Ragia5 1Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece 2up2metric P.C., Engineering - Research - Software Development, Michail Mela 21, GR-11521, Athens, Greece 3School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, U.K. 4School of Creative Technologies, University of Portsmouth, Winston Churchill Avenue, Portsmouth PO1 2DJ, U.K. 5Natural Hazards, Tsunami and Coastal Engineering Laboratory, Technical University of Crete, Chania, Greece {ilias, christos}@up2metric.com, {malcolm.whitworth, mel.krokos}@port.ac.uk, [email protected] Keywords: GIS Story Map, Geomorphology, Methana Peninsula, Greece, Volcano, Geotope, Hiking Trails. Abstract: The purpose of this research is the identification, recording, mapping and photographic imaging of the special volcanic geoforms as well as the cultural monuments of the volcanic Methana Peninsula. With the use of novel methods the aim is to reveal and study the impressive topographic features of the Methana geotope and discover its unique geodiversity. The proposed hiking trails along with the Methana’s archaeology and history, will be highlighted through the creation of an ‘intelligent’ interactive map (Story Map). Two field trips have been conducted for the collection of further information and the digital mapping of the younger volcanic flows of Kammeni Chora with drones. Through the compiled data, thematic maps were created depicting the lava flows and the most important points of the individual hiking paths. -
Queen Arsinoë II, the Maritime Aphrodite and Early Ptolemaic Ruler Cult
ΑΡΣΙΝΟΗ ΕΥΠΛΟΙΑ Queen Arsinoë II, the Maritime Aphrodite and Early Ptolemaic Ruler Cult Carlos Francis Robinson Bachelor of Arts (Hons. 1) A thesis submitted for the degree of Master of Philosophy at The University of Queensland in 2019 Historical and Philosophical Inquiry Abstract Queen Arsinoë II, the Maritime Aphrodite and Early Ptolemaic Ruler Cult By the early Hellenistic period a trend was emerging in which royal women were deified as Aphrodite. In a unique innovation, Queen Arsinoë II of Egypt (c. 316 – 270 BC) was deified as the maritime Aphrodite, and was associated with the cult titles Euploia, Akraia, and Galenaië. It was the important study of Robert (1966) which identified that the poets Posidippus and Callimachus were honouring Arsinoë II as the maritime Aphrodite. This thesis examines how this new third-century BC cult of ‘Arsinoë Aphrodite’ adopted aspects of Greek cults of the maritime Aphrodite, creating a new derivative cult. The main historical sources for this cult are the epigrams of Posidippus and Callimachus, including a relatively new epigram (Posidippus AB 39) published in 2001. This thesis demonstrates that the new cult of Arsinoë Aphrodite utilised existing traditions, such as: Aphrodite’s role as patron of fleets, the practice of dedications to Aphrodite by admirals, the use of invocations before sailing, and the practice of marine dedications such as shells. In this way the Ptolemies incorporated existing religious traditions into a new form of ruler cult. This study is the first attempt to trace the direct relationship between Ptolemaic ruler cult and existing traditions of the maritime Aphrodite, and deepens our understanding of the strategies of ruler cult adopted in the early Hellenistic period. -
A West-East Traverse Along the Magmatism of the South Aegean Volcanic Arc in the Light of Volcanological, Chemical and Isotope Data
65 A West-East Traverse along the magmatism of the south Aegean volcanic arc in the light of volcanological, chemical and isotope data L. Francalanci1,2,∗, G.E. Vougioukalakis 3, G. Perini1, P. Manetti1,2 1 Dipartimento di Scienze della Terra, Università degli Studi di Firenze, via La Pira, 4, I-50121, Firenze, Italy. 2 C.N.R., I.G.G., Sezione di Firenze, via La Pira 4, I-50121, Firenze, Italy. 3 I.G.M.E, Mesogeion, 70, Athens, Greece. ABSTRACT The volcanic rocks of the South Aegean arc (SAAVA) form a chain from the Gulf of Saronikos (Susaki, Egina, Poros, Methana) at West, to an area close to the Anatolian coast at East (Kos, Nisyros and minor islands), through the central part (Milos and Santorini island groups). The volcanic activity began in the Lower Pliocene at Egina (4.7 Ma) and lasted until present days, with the still active Methana, Milos, Santorini and Nisyros volcanoes. The beginning of volcanism is younger in the central sector of the arc. Volcanic center location was controlled by large tectonic lineaments, most of them still active, trending E-W to NW-SE for the western part and mainly NE-SW for the central and eastern parts of the arc. Volcanic fields developed along ellipse shaped areas with the longest axis oriented perpendicular to the subduction front. In the western volcanic fields (Susaki, Egina-Poros-Methana and Milos), volcanic centers are mostly monogenetic and no composite volcanic structures are present. In the eastern sector of the arc, Santorini and Nisyros are important composite volcanoes with caldera structures.