What Nature Destroyed It Also Preserved Educator Guide
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The Rough Guide to Naples & the Amalfi Coast
HEK=> =K?:;I J>;HEK=>=K?:;je CVeaZh i]Z6bVaÒ8dVhi D7FB;IJ>;7C7B<?9E7IJ 7ZcZkZcid BdcYgV\dcZ 8{ejV HVc<^dg\^d 8VhZgiV HVciÉ6\ViV YZaHVcc^d YZ^<di^ HVciVBVg^V 8{ejVKiZgZ 8VhiZaKdaijgcd 8VhVaY^ Eg^cX^eZ 6g^Zcod / AV\dY^EVig^V BVg^\a^Vcd 6kZaa^cd 9WfeZ_Y^_de CdaV 8jbV CVeaZh AV\dY^;jhVgd Edoojda^ BiKZhjk^jh BZgXVidHVcHZkZg^cd EgX^YV :gXdaVcd Fecf[__ >hX]^V EdbeZ^ >hX]^V IdggZ6ccjco^ViV 8VhiZaaVbbVgZY^HiVW^V 7Vnd[CVeaZh GVkZaad HdggZcid Edh^iVcd HVaZgcd 6bVa[^ 8{eg^ <ja[d[HVaZgcd 6cVX{eg^ 8{eg^ CVeaZh I]Z8Vbe^;aZ\gZ^ Hdji]d[CVeaZh I]Z6bVa[^8dVhi I]Z^haVcYh LN Cdgi]d[CVeaZh FW[ijkc About this book Rough Guides are designed to be good to read and easy to use. The book is divided into the following sections, and you should be able to find whatever you need in one of them. The introductory colour section is designed to give you a feel for Naples and the Amalfi Coast, suggesting when to go and what not to miss, and includes a full list of contents. Then comes basics, for pre-departure information and other practicalities. The guide chapters cover the region in depth, each starting with a highlights panel, introduction and a map to help you plan your route. Contexts fills you in on history, books and film while individual colour sections introduce Neapolitan cuisine and performance. Language gives you an extensive menu reader and enough Italian to get by. 9 781843 537144 ISBN 978-1-84353-714-4 The book concludes with all the small print, including details of how to send in updates and corrections, and a comprehensive index. -
Stories of Ancient Rome Unit 4 Reader Skills Strand Grade 3
Grade 3 Core Knowledge Language Arts® • Skills Strand Ancient Rome Ancient Stories of of Stories Unit 4 Reader 4 Unit Stories of Ancient Rome Unit 4 Reader Skills Strand GraDE 3 Core Knowledge Language Arts® Creative Commons Licensing This work is licensed under a Creative Commons Attribution- NonCommercial-ShareAlike 3.0 Unported License. You are free: to Share — to copy, distribute and transmit the work to Remix — to adapt the work Under the following conditions: Attribution — You must attribute the work in the following manner: This work is based on an original work of the Core Knowledge® Foundation made available through licensing under a Creative Commons Attribution- NonCommercial-ShareAlike 3.0 Unported License. This does not in any way imply that the Core Knowledge Foundation endorses this work. Noncommercial — You may not use this work for commercial purposes. Share Alike — If you alter, transform, or build upon this work, you may distribute the resulting work only under the same or similar license to this one. With the understanding that: For any reuse or distribution, you must make clear to others the license terms of this work. The best way to do this is with a link to this web page: http://creativecommons.org/licenses/by-nc-sa/3.0/ Copyright © 2013 Core Knowledge Foundation www.coreknowledge.org All Rights Reserved. Core Knowledge Language Arts, Listening & Learning, and Tell It Again! are trademarks of the Core Knowledge Foundation. Trademarks and trade names are shown in this book strictly for illustrative and educational purposes and are the property of their respective owners. -
CAPRI È...A Place of Dream. (Pdf 2,4
Posizione geografica Geographical position · Geografische Lage · Posición geográfica · Situation géographique Fra i paralleli 40°30’40” e 40°30’48”N. Fra i meridiani 14°11’54” e 14°16’19” Est di Greenwich Superficie Capri: ettari 400 Anacapri: ettari 636 Altezza massima è m. 589 Capri Giro dell’isola … 9 miglia Clima Clima temperato tipicamente mediterraneo con inverno mite e piovoso ed estate asciutta Between parallels Zwischen den Entre los paralelos Entre les paralleles 40°30’40” and 40°30’48” Breitenkreisen 40°30’40” 40°30’40”N 40°30’40” et 40°30’48” N N and meridians und 40°30’48” N Entre los meridianos Entre les méridiens 14°11’54” and 14°16’19” E Zwischen den 14°11’54” y 14°16’19” 14e11‘54” et 14e16’19“ Area Längenkreisen 14°11’54” Este de Greenwich Est de Greenwich Capri: 988 acres und 14°16’19” östl. von Superficie Surface Anacapri: 1572 acres Greenwich Capri: 400 hectáreas; Capri: 400 ha Maximum height Fläche Anacapri: 636 hectáreas Anacapri: 636 ha 1,920 feet Capri: 400 Hektar Altura máxima Hauter maximum Distances in sea miles Anacapri: 636 Hektar 589 m. m. 589 from: Naples 17; Sorrento Gesamtoberfläche Distancias en millas Distances en milles 7,7; Castellammare 13; 1036 Hektar Höchste marinas marins Amalfi 17,5; Salerno 25; Erhebung über den Nápoles 17; Sorrento 7,7; Naples 17; Sorrento 7,7; lschia 16; Positano 11 Meeresspiegel: 589 Castellammare 13; Castellammare 13; Amalfi Distance round the Entfernung der einzelnen Amalfi 17,5; Salerno 25; 17,5 Salerno 25; lschia A Place of Dream island Orte von Capri, in Ischia 16; Positano 11 16; Positano 11 9 miles Seemeilen ausgedrükt: Vuelta a la isla por mar Tour de l’ île par mer Climate Neapel 17, Sorrento 7,7; 9 millas 9 milles Typical moderate Castellammare 13; Amalfi Clima Climat Mediterranean climate 17,5; Salerno 25; lschia templado típicamente Climat tempéré with mild and rainy 16; Positano 11 mediterráneo con typiquement Regione Campania Assessorato al Turismo e ai Beni Culturali winters and dry summers. -
F. Pingue , G.. De Natale , , P. Capuano , P. De , U
Ground deformation analysis at Campi Flegrei (Southern Italy) by CGPS and tide-gauge network F. Pingue1, G.. De Natale1, F. Obrizzo1, C. Troise1, P. Capuano2, P. De Martino1, U. Tammaro1 1 Istituto Nazionale di Geofisica e Vulcanologia . Osservatorio Vesuviano, Napoli, Italy 2 Dipartimento di Matematica e Informatica, Università di Salerno, Italy CGPS CAMPI FLEGREI NETWORK TIDE GAUGES ABSTRACT GROUND DEFORMATION HISTORY CGPS data analysis, during last decade, allowed continuous and accurate The vertical ground displacements at Campi Flegrei are also tracked by the sea level using tide gauges located at the Campi Flegrei caldera is located 15 km west of the Campi Flegrei, a caldera characterized by high volcanic risk due to tracking of ground deformation affecting Campi Flegrei area, both for Nisida (NISI), Port of Pozzuoli (POPT), Pozzuoli South- Pier (POPT) and Miseno (MISE), in addition to the reference city of Naples, within the central-southern sector of a the explosivity of the eruptions and to the intense urbanization of the vertical component (also monitored continuously by tide gauge and one (NAPT), located in the Port of Naples. The data allowed to monitor all phases of Campi Flegrei bradyseism since large graben called Campanian Plain. It is an active the surrounding area, has been the site of significant unrest for the periodically by levelling surveys) and for the planimetric components, 1970's, providing results consistent with those obtained by geometric levelling, and more recently, by the CGPS network. volcanic area marked by a quasi-circular caldera past 2000 years (Dvorak and Mastrolorenzo, 1991). More recently, providing a 3D displacement field, allowing to better constrain the The data have been analyzed in the frequency domain and the local astronomical components have been defined by depression, formed by a huge ignimbritic eruption the caldera floor was raised to about 1.7 meters between 1968 and inflation/deflation sources responsible for ground movements. -
Cassini RADAR Images at Hotei Arcus and Western Xanadu, Titan: Evidence for Geologically Recent Cryovolcanic Activity S
GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L04203, doi:10.1029/2008GL036415, 2009 Click Here for Full Article Cassini RADAR images at Hotei Arcus and western Xanadu, Titan: Evidence for geologically recent cryovolcanic activity S. D. Wall,1 R. M. Lopes,1 E. R. Stofan,2 C. A. Wood,3 J. L. Radebaugh,4 S. M. Ho¨rst,5 B. W. Stiles,1 R. M. Nelson,1 L. W. Kamp,1 M. A. Janssen,1 R. D. Lorenz,6 J. I. Lunine,5 T. G. Farr,1 G. Mitri,1 P. Paillou,7 F. Paganelli,2 and K. L. Mitchell1 Received 21 October 2008; revised 5 January 2009; accepted 8 January 2009; published 24 February 2009. [1] Images obtained by the Cassini Titan Radar Mapper retention age comparable with Earth or Venus (500 Myr) (RADAR) reveal lobate, flowlike features in the Hotei [Lorenz et al., 2007]). Arcus region that embay and cover surrounding terrains and [4] Most putative cryovolcanic features are located at mid channels. We conclude that they are cryovolcanic lava flows to high northern latitudes [Elachi et al., 2005; Lopes et al., younger than surrounding terrain, although we cannot reject 2007]. They are characterized by lobate boundaries and the sedimentary alternative. Their appearance is grossly relatively uniform radar properties, with flow features similar to another region in western Xanadu and unlike most brighter than their surroundings. Cryovolcanic flows are of the other volcanic regions on Titan. Both regions quite limited in area compared to the more extensive dune correspond to those identified by Cassini’s Visual and fields [Radebaugh et al., 2008] or lakes [Hayes et al., Infrared Mapping Spectrometer (VIMS) as having variable 2008]. -
Stromboli Mount Fuji Ojos Del Salado Mauna Loa Mount Vesuvius Mount
Volcanoes Top Cards Volcanoes Top Cards Volcanoes Top Cards Volcanoes Top Cards Stromboli Mount Fuji Ojos del Salado Mauna Loa Italy Japan Argentina-Chile Border Hawaii Height Height Height Height Eruption Cycle Eruption Cycle Eruption Cycle Eruption Cycle Erupting continuously Last Erupted Last Erupted Last Erupted Last Erupted for hundreds of thousands of years Fact: This volcano is the highest Fact: Nevados Ojos del Salado is the Fact: Mauna Loa is one of the five Fact: This volcano has been erupting volcano and highest peak in world’s highest active volcano. volcanoes that form the Island of for at least 2000 years. Japan and considered one of the 3 Hawaii in the U.S state of Hawaii in holy mountains. the Pacific Ocean. twinkl.com twinkl.com twinkl.com twinkl.com Volcanoes Top Cards Volcanoes Top Cards Volcanoes Top Cards Volcanoes Top Cards Mount Vesuvius Mount Pinatubo Krakatoa Mount St. Helens Italy Philippines Indonesia United States Height Height Height Height Eruption Cycle Eruption Cycle Eruption Cycle Eruption Cycle Last Erupted Last Erupted Last Erupted Last Erupted Fact: The most famous eruption Fact: Mount Pinatubo’s eruption Fact: The famous eruption of 1883 Fact: The deadliest volcanic eruption happened in 79 AD. Mount Vesuvius on 15th June 1991 was one of the generated the loudest sound ever caused by this volcano was on erupted continuously for over a day, largest volcanic eruptions of the reported in history. It was heard as May 18, 1980, destroying 250 completely burying the nearby city 20th Century. far away as Perth, Australia (around homes and 200 miles of highway. -
Journal Pre-Proof
Journal Pre-proof From Historical Seismology to seismogenic source models, 20 years on: Excerpts from the Italian experience Gianluca Valensise, Paola Vannoli, Pierfrancesco Burrato, Umberto Fracassi PII: S0040-1951(19)30296-3 DOI: https://doi.org/10.1016/j.tecto.2019.228189 Reference: TECTO 228189 To appear in: Tectonophysics Received date: 1 April 2019 Revised date: 20 July 2019 Accepted date: 5 September 2019 Please cite this article as: G. Valensise, P. Vannoli, P. Burrato, et al., From Historical Seismology to seismogenic source models, 20 years on: Excerpts from the Italian experience, Tectonophysics(2019), https://doi.org/10.1016/j.tecto.2019.228189 This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. © 2019 Published by Elsevier. Journal Pre-proof From Historical Seismology to seismogenic source models, 20 years on: excerpts from the Italian experience Gianluca Valensise, Paola Vannoli, Pierfrancesco Burrato & Umberto Fracassi Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy Contents 1. Introduction 1.1. Why Historical Seismology 1.2. A brief history of Historical Seismology 1.3. Representing and exploiting Historical Seismology data 2. -
Boccaccio Angioino Materiali Per La Storia Culturale Di Napoli Nel Trecento
Giancarlo Alfano, Teresa D'Urso e Alessandra Perriccioli Saggese (a cura di) Boccaccio angioino Materiali per la storia culturale di Napoli nel Trecento Destini Incrociati n° 7 5 1-6.p65 5 19/03/2012, 14:25 Il presente volume è stato stampato con i fondi di ricerca della Seconda Università di Napoli e col contributo del Dipartimento di Studio delle componenti culturali del territorio e della Facoltà di Lettere e Filosofia. Si ringraziano Antonello Frongia ed Eliseo Saggese per il prezioso aiuto offerto. Toute représentation ou reproduction intégrale ou partielle faite par quelque procédé que ce soit, sans le consentement de l’éditeur ou de ses ayants droit, est illicite. Tous droits réservés. © P.I.E. PETER LANG S.A. Éditions scientifiques internationales Bruxelles, 2012 1 avenue Maurice, B-1050 Bruxelles, Belgique www.peterlang.com ; [email protected] Imprimé en Allemagne ISSN 2031-1311 ISBN 978-90-5201-825-6 D/2012/5678/29 Information bibliographique publiée par « Die Deutsche Nationalbibliothek » « Die Deutsche Nationalbibliothek » répertorie cette publication dans la « Deutsche Nationalbibliografie » ; les données bibliographiques détaillées sont disponibles sur le site http://dnb.d-nb.de. 6 1-6.p65 6 19/03/2012, 14:25 Indice Premessa ............................................................................................... 11 In forma di libro: Boccaccio e la politica degli autori ...................... 15 Giancarlo Alfano Note sulla sintassi del periodo nel Filocolo di Boccaccio .................. 31 Simona Valente Appunti di poetica boccacciana: l’autore e le sue verità .................. 47 Elisabetta Menetti La “bona sonoritas” di Calliopo: Boccaccio a Napoli, la polifonia di Partenope e i silenzi dell’Acciaiuoli ........................... 69 Roberta Morosini «Dal fuoco dipinto a quello che veramente arde»: una poetica in forma di quaestio nel capitolo VIII dell’Elegia di Madonna Fiammetta ................................................... -
Continuity of Culture: Romans in Pompeii Lesson Overview
Continuity of Culture: Romans in Pompeii Lesson Overview Unit: Lessons: 1. Grades 3 – 6 Continuity of Culture: Lesson One: Map study of 2. 5 -7 Class Periods Romans in Pompeii Italy. 3. Authors: Lori Howell, Lesson Two: History of Melody Nishinaga, Sarah Pompeii. Poku & Warren Soper Lesson Three: Pliny the 4. Social Sciences, Younger. English and History Lesson Four: Comparison of “Then and Now.” Lesson Five: Literature review. Lesson Six: Graphic Organizes. Lesson Seven: Writing Overview “A typical day in this town means going shopping, stopping by the laundry, catching a sporting event at the amphitheater, or maybe taking in a play – and that was 2000 years ago. “Can you guess where this is? Not where you might expect: You’re in ancient Pompeii, an Italian village where life came to a fiery halt when Mt. Vesuvius erupted in AD 79. “ -Discover Kids Pompeii Magazine 1 | Page The eruption of Vesuvius on August 24, 79 A.D. froze a moment in time under thick layers of ash and molten mud. It preserved elements of Roman culture that demonstrate the remarkable continuity of human life and history, proving that life in the past, even the far distant past, was remarkably similar to our own. In this lesson, by taking a closer look at the remains of Pompeii, students will gain a broad appreciation of people in the past. They will study Roman culture by locating Pompeii on a map, identifying important elements of its geography, and examining the remains of Pompeii to explain how the Ancient Romans in Pompeii are similar to people today. -
Robert Harris • Enigma
LITERARY BITS Module 2 WORKING IN DIGITAL ROBERT HARRIS • ENIGMA ABOUT THE AUTHOR ROBERT HARRIS Robert Harris was born in Nottingham, UK, in 1957. After graduating at Cambridge, he worked as a journalist for the BBC and assisted on shows that covered important current events. He became a political commentator, was the editor of The Observer, a UK political paper, and wrote articles on politics in many other newspapers. He started his writing career in the 1980s and since then he has written a number of fictional thrillers, often related to political events, and eight novels have become bestsellers. He wrote novels related to World War Two such as ‘Fatherland’ (1992), his first bestseller, and ‘Enigma’ (1995), but also stories set in other historical periods like ‘Pompeii’ (2003). R. Harris ABOUT THE NOVEL ENIGMA The novel is a blend between a historical novel and a mystery novel which mixes up reality and fiction. The story is set in 1943 when much of Nazi Enigma Code has already been cracked. However, Shark, the impenetrable cipher used to hide the movements of the U-boats, the German submarines, to the Allies, is still a mystery. A top secret team of British cryptographers led by the brilliant mathematician Tom Jericho has the task of deciphering it. They succeed in breaking the code, but unfortunately the Germans change it. As an Allied convoy crosses the North Atlantic Ocean full of U-boats, Jericho has to solve three mysteries with the help of his girlfriend’s roommate who is on the convoy: the code, whether his girlfriend Claire is a spy and if she has been murdered. -
Mount Vesuvius Is Located on the Gulf of Naples, in Italy
Mount Vesuvius is located on the Gulf of Naples, in Italy. It is close to the coast and lies around 9km from the city of Naples. Despite being the only active volcano on mainland Europe, and one of the most dangerous volcanoes, almost 3 million people live in the immediate area. Did you know..? Mount Vesuvius last erupted in 1944. Photo courtesy of Ross Elliot(@flickr.com) - granted under creative commons licence – attribution Mount Vesuvius is one of a number of volcanoes that form the Campanian volcanic arc. This is a series of volcanoes that are active, dormant or extinct. Vesuvius Campi Flegrei Stromboli Mount Vesuvius is actually a Vulcano Panarea volcano within a volcano. Mount Etna Somma is the remain of a large Campi Flegrei del volcano, out of which Mount Mar di Sicilia Vesuvius has grown. Did you know..? Mount Vesuvius is 1,281m high. Mount Etna is another volcano in the Campanian arc. It is Europe’s most active volcano. Mount Vesuvius last erupted in 1944. This was during the Second World War and the eruption caused great problems for the newly arrived Allied forces. Aircraft were destroyed, an airbase was evacuated and 26 people died. Three villages were also destroyed. 1944 was the last recorded eruption but scientists continue to monitor activity as Mount Vesuvius is especially dangerous. Did you know..? During the 1944 eruption, the lava flow stopped at the steps of the local church in the village of San Giorgio a Cremano. The villagers call this a miracle! Photo courtesy of National Museum of the U.S. -
Torches and Torch Relays of the Olympic Summer Games from Berlin 1936 to London 2012 Reference Document
Olympic Studies Centre Torches and Torch Relays of the Olympic Summer Games from Berlin 1936 to London 2012 Reference document Presentation and visuals of the Olympic torches. Facts and figures on the Torch Relay for each edition. November 2014 © IOC – John HUET Reference document TABLE OF CONTENTS Introduction .................................................................................................................. 3 Berlin 1936 ................................................................................................................... 5 London 1948 ................................................................................................................ 9 Helsinki 1952 .............................................................................................................. 13 Melbourne/Stockholm 1956 ...................................................................................... 17 Rome 1960 .................................................................................................................. 23 Tokyo 1964 ................................................................................................................. 27 Mexico City 1968 ........................................................................................................ 31 Munich 1972 ............................................................................................................... 35 Montreal 1976 ............................................................................................................