New Methodologies for Volcanic-Hosted Copper Sulphide Mineralization on Cyprus: a GIS–Prospectivity Analysis-Based Approach
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SUPPLEMENT No. 3 Το the CYPRUS GAZETTE No. 3648 of .15TH OCTOBER, 1952
SUPPLEMENT No. 3 το THE CYPRUS GAZETTE No. 3648 OF .15TH OCTOBER, 1952. SUBSIDIARY LEGISLATION. No. 449. THE ELEMENTARY EDUCATION LAW. CAP. 203 AND LAWS 22 OF 1950 AND 17 OF 1952. ORDER MADE UNDER SECTION 73. A. B. WRIGHT, Governor. Whereas-on the report of the Director of Education it appears to me that it is desirable to compel the Town Committees and Village Commissions for the Greek-Orthodox Schools of the towns and villages mentioned in the first column of the Schedule hereto (hereinafter referred to as " the Committees arid Commissions "), in their respective towns and villages, to provide, erect, repair, extend, improve or develop the school buildings, premises, playgrounds, yards, gardens or teachers' dwellings, as the case may be, particulars whereof are given in the second column of the said Schedule (hereinafter referred to as " the premises "): Now, therefore, in exercise of the powers vested in me by section 73 of the Cap. 203 z Elementary Education Law, I, the Governor, do hereby order that the * °^ *95o Committees and Commissions shall in their respective towns or villages provide, erect, repair, extend, improve or develop the premises. SCHEDULE. Nicosia District. Town or village. Particulars. Argaki Extension of, the school building. Astromeritis · .. Repairs to the school building. Evrykhou .. .. Repairs to the school building. Kaimakli Repairs to the Girls' School. Kalopanayiotis Repairs to the school premises. Karavostasi-Xeros Repairs to the school latrines. Khrysidha Erection of new school. Lakatamia, Pano and Kato Repairs to the teachers' dwellings. Latsia Repairs to the school premises. Loutros Erection of a teacher's dwelling and repairs to the school building. -
Cyprus Island of Saints
NHSOS KYPROS-Engl.-dec2015:Layout 1 12/20/15 11:20 AM Page 1 Monastery of he Office of the Pilgrimage Tours of the Church Timios Stavros, of Cyprus opens its doors like a big Mansion to Church - - - Limit of area under Turkish Omodos Τwelcome the pilgrim and treat him with the holy of Ieron occupation since 1974 Apostolon, gifts of an entire religious world. Inviting him to experience Pera Chorio in the blessed place of the “Island of Saints”, through travels The Five Domed Church of that are real but also noetic, in everliving spiritual Agioi Varnavas and Ilarionas, landscapes, in the most fascinating geography, in Agios Irakleidios, Peristerona from the Church worshipping places that smell incense and from which Scenes of the Second Coming. Church of Archangelos of Panagia spurt spiritual fragrance. Saints and Donors, view of the Michail, Pedoulas tou Araka, The Virgin Narthex, Church of Panagia tis Lagoudera of Kykkou, Asinou Where Archbishop, Bishops, Abbots, Priests, deacons, hermits, Kykkos monks, church wardens and laics, all those who form the Museum body of the Church of Cyprus, with their spiritual work Stavrovouni Monastery lead the human/pilgrim in a “in spirit and truth” worship. “Monasteries bloom on sheer mountains of the island” In Churches, Monasteries, Cloisters, Ecclesiastical Museums Holy Cross in Omodos where a small piece of the rope and Holy Sacristies that gifted many years ago healing to that the soldiers humans. It is not by chance that pilgrims came from afar to used to bind Monastery be cured of their afflictions and seek solace at the shelter of Christ is kept Monastery of Apostle Andreas of Macheras this holyplace island, in the spiritual glow of Christianity’s temperate clime. -
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450000 E 500000 E 550000 E 600000 E 650000 32o 30' 33o 00' 33o 30' 34o 00' 34o 30' Cape Andreas 395000 N 395000 N HQ UNFICYP MEDITERRANEAN SEA ﺍﻧﺘﺸﺎﺭ ﻗﻮﺓ ﺍﻷﻣﻢ ﺍﳌﺘﺤﺪﺓ ﳊﻔﻆ ﺍﻟﺴﻼﻡ ﰲ ﻗﱪﺹ Rizokarpaso 联塞部队部署 HQ UNPOL UNFICYP DEPLOYMENT FMPU Multinational Ayia Trias DÉPLOIEMENT DE L’UNFICYP Yialousa o o Vathylakas 35 30' 35 30' ДИСЛОКАЦИЯ ВСООНК MFR UNITED KINGDOM Sector 2 Leonarisso DESPLIEGUE DE L A UNFICYP HQ ARGENTINA Ephtakomi UNITED KINGDOM Galatia Cape Kormakiti SLOVAKIA Akanthou Komi Kebir UNPOL 500 m HQ Sector 1 Ardhana Karavas KYRENIA 500 m Kormakiti Lapithos Ayios Amvrosios Temblos Boghaz ARGENTINA / PARAGUAY / BRAZIL Dhiorios Myrtou 500 m Bellapais Trypimeni Trikomo ARGENTINA / CHILE 500 m 500 m Famagusta SECTOR 1 Lefkoniko Bay Sector 4 UNPOL VE WE K. Dhikomo Chatos WE XE HQ 390000 N UNPOL Kythrea 390000 N UNPOL VD WD ari WD XD Skylloura m Geunyeli Bey Keuy K. Monastir SLOVAKIA Mansoura Morphou am SLOVAKIA K. Pyrgos Morphou Philia Dhenia M Kaimakli Angastina Strovilia Post Kokkina Bay P. Zodhia LP 0 Prastio 90 Northing 9 Northing Selemant Limnitis Avlona UNPOL Pomos NICOSIA UNPOL 500 m Karavostasi Xeros UNPA Tymbou (Ercan) FAMAGUSTA UNPOL s s Cape Arnauti ti it a Akaki SECTOR 2 o Lefka r Kondea Kalopsidha Varosha Yialia Ambelikou n e o Arsos m m r a Khrysokhou a ro te rg Dherinia s t s Athienou SECTOR 4 e Bay is s ri SLOVAKIA t Linou A e P ( ) Mavroli rio P Athna Akhna 500 m u Marki Prodhromi Polis ko Evrykhou 500 m Klirou Troulli 1000 m S Louroujina UNPOL o o Pyla 35 00' 35 00' Kakopetria 500 mKochati Lymbia 1000 m DHEKELIA Ayia Napa Cape 500 m Pedhoulas SLOVAKIA S.B.A. -
Resolving the Variscan Evolution of the Moldanubian Sector of The
Journal of Geosciences, 52 (2007), 9–28 DOI: 10.3190/jgeosci.005 Original paper Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo–Moldanubian tectonometamorphic phases Fritz FINGER1*, Axel GERDEs2, Vojtěch JANOušEk3, Miloš RENé4, Gudrun RIEGlER1 1University of Salzburg, Division of Mineralogy, Hellbrunnerstraße 34, A-5020 Salzburg, Austria; [email protected] 2University of Frankfurt, Institute of Geoscience, Senckenberganlage 28, D-60054 Frankfurt, Germany 3Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic 4Academy of Sciences, Institute of Rock Structure and Mechanics, V Holešovičkách 41, 182 09 Prague 8, Czech Republic *Corresponding author The Variscan evolution of the Moldanubian sector in the Bohemian Massif consists of at least two distinct tectonome- tamorphic phases: the Moravo–Moldanubian Phase (345–330 Ma) and the Bavarian Phase (330–315 Ma). The Mora- vo–Moldanubian Phase involved the overthrusting of the Moldanubian over the Moravian Zone, a process which may have followed the subduction of an intervening oceanic domain (a part of the Rheiic Ocean) beneath a Moldanubian (Armorican) active continental margin. The Moravo–Moldanubian Phase also involved the exhumation of the HP–HT rocks of the Gföhl Unit into the Moldanubian middle crust, represented by the Monotonous and Variegated series. The tectonic emplacement of the HP–HT rocks was accompanied by intrusions of distinct magnesio-potassic granitoid melts (the 335–338 Ma old Durbachite plutons), which contain components from a strongly enriched lithospheric mantle source. Two parallel belts of HP–HT rocks associated with Durbachite intrusions can be distinguished, a western one at the Teplá–Barrandian and an eastern one close to the Moravian boundary. -
The Geology of England – Critical Examples of Earth History – an Overview
The Geology of England – critical examples of Earth history – an overview Mark A. Woods*, Jonathan R. Lee British Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG *Corresponding Author: Mark A. Woods, email: [email protected] Abstract Over the past one billion years, England has experienced a remarkable geological journey. At times it has formed part of ancient volcanic island arcs, mountain ranges and arid deserts; lain beneath deep oceans, shallow tropical seas, extensive coal swamps and vast ice sheets; been inhabited by the earliest complex life forms, dinosaurs, and finally, witnessed the evolution of humans to a level where they now utilise and change the natural environment to meet their societal and economic needs. Evidence of this journey is recorded in the landscape and the rocks and sediments beneath our feet, and this article provides an overview of these events and the themed contributions to this Special Issue of Proceedings of the Geologists’ Association, which focuses on ‘The Geology of England – critical examples of Earth History’. Rather than being a stratigraphic account of English geology, this paper and the Special Issue attempts to place the Geology of England within the broader context of key ‘shifts’ and ‘tipping points’ that have occurred during Earth History. 1. Introduction England, together with the wider British Isles, is blessed with huge diversity of geology, reflected by the variety of natural landscapes and abundant geological resources that have underpinned economic growth during and since the Industrial Revolution. Industrialisation provided a practical impetus for better understanding the nature and pattern of the geological record, reflected by the publication in 1815 of the first geological map of Britain by William Smith (Winchester, 2001), and in 1835 by the founding of a national geological survey. -
Geology of Cyprus and Eastern Mediterranean Department: Sciences and Engineering Host Institution: University of Nicosia, Nicosia, Cyprus
Global Semesters Course Syllabus Course: GEOL 315 Geology of Cyprus and Eastern Mediterranean Department: Sciences and Engineering Host Institution: University of Nicosia, Nicosia, Cyprus Course Summary Course Code Course Title Recommended Credit Hours Geology of Cyprus and Eastern GEOL-315 3 Mediterranean Subject Contact Hours Prerequisites Geology 42-45 At least a 2nd year student Department Level of Course Language of Instruction Sciences & Engineering Upper-Division English Course Description The course introduces students to the science and the basics of geology, and studies the formation of Cyprus and the Mediterranean Basin and specially the unique geological formations of Cyprus. The Troodos mountain range, a unique place in the world for the understanding of an oceanic plate and the relevant geodynamic phenomena, will be of special focus. The course includes several site visits. The course can be taken by any science student. Prerequisites (if applicable) At least a 2nd year student Instructor Information Nicki Nicolaidou, [email protected]: Mrs.Nicki Nicolaidou received her Degree in Geology from the Aristotle University of Thessaloniki, Greece in 2007. Since 2010 she is working as a project geologist for the Canadian gold exploration company Northern Lion, in Cyprus. Previous work experience as a geologist includes geotechnical and environmental impact assessment studies. Ifigenia Gavriel, [email protected]: Mrs.Ifigenia Gavriel is a postgraduate student of the MSc Environmental Engineering of the Department of Civil and Environmental Engineering at the University of Cyprus. She received her Degree in Geology from the National and Kapodestrian University of Athens, Greece in 2009. From 2010 she is working as a project geologist for the Canadian gold exploration company Northern Lion, in Cyprus. -
Study of the Geomorphology of Cyprus
STUDY OF THE GEOMORPHOLOGY OF CYPRUS FINAL REPORT Unger and Kotshy (1865) – Geological Map of Cyprus PART 1/3 Main Report Metakron Consortium January 2010 TABLE OF CONTENTS PART 1/3 1 Introduction 1.1 Present Investigation 1-1 1.2 Previous Investigations 1-1 1.3 Project Approach and Scope of Work 1-15 1.4 Methodology 1-16 2 Physiographic Setting 2.1 Regions and Provinces 2-1 2.2 Ammochostos Region (Am) 2-3 2.3 Karpasia Region (Ka) 2-3 2.4 Keryneia Region (Ky) 2-4 2.5 Mesaoria Region (Me) 2-4 2.6 Troodos Region (Tr) 2-5 2.7 Pafos Region (Pa) 2-5 2.8 Lemesos Region (Le) 2-6 2.9 Larnaca Region (La) 2-6 3 Geological Framework 3.1 Introduction 3-1 3.2 Terranes 3-2 3.3 Stratigraphy 3-2 4 Environmental Setting 4.1 Paleoclimate 4-1 4.2 Hydrology 4-11 4.3 Discharge 4-30 5 Geomorphic Processes and Landforms 5.1 Introduction 5-1 6 Quaternary Geological Map Units 6.1 Introduction 6-1 6.2 Anthropogenic Units 6-4 6.3 Marine Units 6-6 6.4 Eolian Units 6-10 6.5 Fluvial Units 6-11 6.6 Gravitational Units 6-14 6.7 Mixed Units 6-15 6.8 Paludal Units 6-16 6.9 Residual Units 6-18 7. Geochronology 7.1 Outcomes and Results 7-1 7.2 Sidereal Methods 7-3 7.3 Isotopic Methods 7-3 7.4 Radiogenic Methods – Luminescence Geochronology 7-17 7.5 Chemical and Biological Methods 7-88 7.6 Geomorphic Methods 7-88 7.7 Correlational Methods 7-95 8 Quaternary History 8-1 9 Geoarchaeology 9.1 Introduction 9-1 9.2 Survey of Major Archaeological Sites 9-6 9.3 Landscapes of Major Archaeological Sites 9-10 10 Geomorphosites: Recognition and Legal Framework for their Protection 10.1 -
Pre-Mesozoic Geology of Saxo-Thuringia from the Cadomian Active Margin to the Variscan Orogen
GEOLOGICA CARPATHICA, FEBRUARY 2011, 62, 1, 42 BOOK REVIEW Pre-Mesozoic Geology of Saxo-Thuringia From the Cadomian Active Margin to the Variscan Orogen Editors: ULF LINNEMANN & ROLF L. ROMER 26–28 April 2010 2010. Schweizerbart Science Publishers, Stuttgart. 488 pages, 190 figures, 6 tables, 1 Sheet Map, 1 DVD, 1 foldout, 25x 17 cm, 1400 g. Language: English ISBN 978-3-510-65259-4, bound, price: 84.90 EUR The monographic work is a summary of results of a wider team of authors, who have contributed to the five dominant Parts, each of which consists of several Chapters focused on individual problems of the Saxo-Thuringian Region, its geological structure and its development in time and space. It is a classical analysis of the development of the Pre-Mesozoic stage from the Cadomian Active Margin to the Variscan Orogene. Saxo-Thuringia represents a very important region displaying development of the Variscides in one part of the Pangea supercontinent. The first chapter of the first part (Introduction) of the book is absolutely devoted to the location of this region of Saxo-Thuringia in the context of the Pangea supercontinent, followed by detailed recapitulation of the geological maps and results from geological mapping in historical survey from oldest documents to almost present- day works, which are well preserved and represent for the reader the classical and modern shool of regional geology of this region. The third chapter of this part completely untraditionally, but in a very interesting way shows the region of Saxo- Thuringia from the point of view of geochemical potential. -
Cyprus Authentic Route 2
Cyprus Authentic Route 2 Safety Driving in Cyprus Comfort Rural Accommodation Tips Useful Information Only DIGITAL Version A Village Life Larnaka • Livadia • Kellia • Troulloi • Avdellero • Athienou • Petrofani • Lympia • Ancient Idalion • Alampra • Mosfiloti • Kornos • Pyrga • Stavrovouni • Kofinou • Psematismenos • Maroni • Agios Theodoros • Alaminos • Mazotos • Kiti • Hala Sultan Tekke • Larnaka Route 2 Larnaka – Livadia – Kellia – Troulloi – Avdellero – Athienou – Petrofani – Lympia - Ancient Idalion – Alampra – Mosfiloti – Kornos – Pyrga – Stavrovouni – Kofinou – Psematismenos – Maroni – Agios Theodoros – Alaminos – Mazotos – Kiti – Hala Sultan Tekke – Larnaka Margo Agios Arsos Pyrogi Spyridon Agios Tremetousia Tseri Golgoi Sozomenos Melouseia Athienou Potamia Pergamos Petrofani Troulloi Margi Nisou Dali Pera Louroukina Avdellero Pyla Chorio Idalion Kotsiatis Lympia Alampra Agia Voroklini Varvara Agios Kellia Antonios Kochi Mathiatis Sia Aradippou Mosfiloti Agia Livadia Psevdas Anna Ε4 Kalo Chorio Port Kition Kornos Chapelle Delikipos Pyrga Royal LARNAKA Marina Salt LARNAKA BAY Lake Hala Sultan Stavrovouni Klavdia Tekkesi Dromolaxia- Dipotamos Meneou Larnaka Dam Kiti Dam International Alethriko Airport Tersefanou Anglisides Panagia Kivisili Menogeia Kiti Aggeloktisti Perivolia Aplanta Softades Skarinou Kofinou Anafotida Choirokoitia Alaminos Mazotos Cape Kiti Choirokoitia Agios Theodoros Tochni Psematismenos Maroni scale 1:300,000 0 1 2 4 6 8 10 Kilometers Zygi AMMOCHOSTOS Prepared by Lands and Surveys Department, Ministry of Interior, -
Tertiary Uplift History of the Troodos Massif, Cyprus
Tertiary uplift history of the Troodos massif, Cyprus A.H.F. ROBERTSON* Department of Geology, University of Cambridge, Sedgwick Museum, Downing Street, Cambridge CB2 3EQ, England ABSTRACT INTRODUCTION Troodos massif that he took as an indica- tion of possible subaerial exposure. The detailed uplift history of a portion of In the recent debate about the mech- Subsequently, in Maastrichtian time, the Late Cretaceous Tethyan oceanic litho- anisms of formation and subsequent de- open oceanic stage in the evolution of the sphère is documented by in situ sedimentary formation of the Troodos massif of Cyprus, Troodos massif was terminated by major sequences around the Troodos massif of little account has been taken of the various tectonic movements that simultaneously af- Cyprus. The pre-uplift tectonic setting first in situ Upper Cretaceous and Tertiary fected the whole belt stretching from Greece involved genesis of the Troodos massif at a sedimentary sequences that are exposed through Cyprus to Oman and beyond spreading ocean ridge of Late Cretaceous around the perimeter of the Troodos mas- (Smith, 1971). In the south and southwest age, followed by deformation in Maas- sif. This paper has two main objectives. of Cyprus, substantial thrust sheets and trichtian time. Then, after a brief period of First, it outlines the sedimentary develop- mélange were emplaced directly over the latest Cretaceous deep-water pelagic ment of southern Cyprus in the Tertiary Troodos ocean floor. This deformation is sedimentation, much of the area was blan- Period, of interest to many working in the suggestive of subduction and a trench envi- keted in early Tertiary time by a wedge of East Mediterranean. -
The Blue Beret
The Blue Beret Airborne The UNFICYP Magazine November/December 2011 Contents Editorial . .3 “Peacing” Cyprus together . .4 Inter-Mission Force Commanders’ Conference . .5 Unite to end violence . .6 Women in Peacekeeping/UNPOL Raises Serbian Flag/ New Faces in Maple Leaf Camp . .7 World AIDS Day Marked . .8/9 Culturally Significant Monuments in the Buffer Zone . .10/11 Service of Remembrance/Peace concert . .12 Honouring UNFICYP’s Fallen . .13 UN Staff Day . .14/15 Service for Peace Recognised . .16 New Bell for UN Flight / On duty in the ‘Magic Mansion’ . .17 UNFICYP Military Skills Competition . .18/19 Slovak Santa/ Carol Service . .20 Children visit Dhekelia SBA/ Cyprus Wedding for Liaison Officer . .21 New Faces . .22 Visits . .23 Serving UNFICYP’s civilian, military and police personnel The Blue Beret is UNFICYP’s in-house journal. Views expressed are of the authors concerned, and do not necessarily conform with official policy. Articles of general interest (plus photos with captions) are invited from all members of the Force Copyright of all material is vested in UN publications, but may be repro-duced with the Editor’s permission. The Blue Beret Editorial Team Unit Press Officers Published bi-monthly by the: Michel Bonnardeaux Sector 1 Capt. Marcelo Alejandro Quiroz Public Information Office Netha Kreouzos Sector 2 Capt. Matt Lindow United Nations Force in Cyprus Ersin Öztoycan Sector 4 Capt. 1Lt Jozef Zimmerman HQ UNFICYP Agnieszka Rakoczy MFR Capt. Alexander Hartwell PO Box 21642 1Sgt.Rastislav Ochotnicky UNPOL Deputy Senior Police Adviser 1590 Nicosia Cyprus (Photographer) Miroslav Milojevic Capt. Michal Harnadek UN Flt Lt. Jorgelina Camarzana FMPU Capt. -
Sustainable Energy Action Plan
Sustainable Energy Action Plan Lakatamia Municipality - Cyprus 5 September 2011 Sustainable Energy Action Plan Lakatamia Municipality - Cyprus Brief Summary The “Pact of Islands” (ISLE-PACT project) is committed to developing Local Energy Action Plans, with the aim of achieving European sustainability objectives as set by the EU for 2020, that is of reducing CO2 emissions by at least 20% through measures that promote renewable energy, energy saving and sustainable transport. The Cyprus Energy Agency is a participating partner in the ISLE-PACT project and has invited Cyprus local authorities to demonstrate their political commitment by signing the “The Pact of Islands”; agreement in order to achieve the EU sustainability targets for 2020. Cyprus participation involves 12 Municipalities and 2 Communities, including Lakatamia Municipality. The Lakatamia is today one of the seven major municipalities of Nicosia with a population of approximately 40,000 residents and an area of 29 square kilometers. The year 2009 was designated as the year of referencing/recording energy consumption and CO2 emissions in the Municipality’s territory. According to actual consumption data collected by the Electricity Authority of Cyprus (utility), the oil companies, the Statistical Service of Cyprus, etc, the total energy consumption in 2009 in Larnaka was 598.151 MWh The largest consumer of energy in the municipality is transport with 375.210 followed by the residential sector with 119.394 MWh and less with the tertiary sector 75.273 MWh. The CO2 emissions in 2009 attributable to the overall energy consumption in the municipality are 215.611 tons. For the forecast of CO2 emissions in the period 2010 to 2020, the scenario of expected evolution was established, where it was estimated that without taking any measures emissions will amount to 225.591 tons.