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Väikesaarte Rõõmud Ja Mured 2019
Väikesaarte rõõmud ja mured Maa-ameti andmetel on Eestis üle 2000 saare. Enamik saartest on pindalalt aga niivõrd väikesed, et elatakse vaid üksikutel. Püsielanikega asustatud saared jagunevad kuue maakonna vahel. Meie riik eristab saartega suhtlemisel suursaari ja püsiasustusega väikesaari, kellele on kehtestatud teatud erisusi. Tänane ettekanne on koostatud just nende poolt kirja- pandu alusel. Koostas Linda Tikk [email protected] Abruka Saaremaa vald, Saaremaa Suurus: 8,8 km2 Rõõmud Soovid ja vajadused • SAAREVAHT olemas • Keskkonnakaitselisi probleeme pole eriti olnud,nüüd ILVES • Elekter - merekaabel Saaremaaga, • taastuvenergia - vaja päikesepaneelid • Püsiühendus Abruka-Roomassaare toimib, kuid talvise liikluskorralduse jaoks oleks vaja • Sadam kaasaegne • puudub seade kauba laadimiseks • . • • vaja kaatrile radar, öövaatlusseadmed Päästeteeistus toimib, kaater, 12 jne vabatahtlikku päästjat • Külateed tolmuvabaks • Teehooldus korras, • Internet kohe valmib • Haridus- kool ,lasteaed puudub • Pood puudub • • Kaladus 1 kutseline kalur, igas talus Perspektiivi oleks kutselistele kaluritele hobikalurid • Turismiga tegeleb 2 talu • Põllumajandus 250 veist pluss 100 Sisuliselt puudub veiste äraveo võimalus, lammast, 375 ha maad, PLK müük raskendatud hooldus • Toitlustus ja ehitus Aegna Tallinna kesklinna linnaosa, Harjumaa Suurus: 3,01 km2 Rõõmud Soovid ja vajadused Põhiline eluks vajalik saarel olemas Pääste puudulik, vajalik aastaringne päästevõimekus Heinlaid Hiiumaa vald, Hiiumaa Suurus: 1,62 km2 Soovid ja vajadused Vaja kommunikatsioone, -
Permanently Inhabited Small Islands Act
Issuer: Riigikogu Type: act In force from: 20.06.2010 In force until: 31.08.2015 Translation published: 30.04.2014 Permanently Inhabited Small Islands Act Passed 11.02.2003 RT I 2003, 23, 141 Entry into force 01.01.2004 Amended by the following acts Passed Published Entry into force 22.02.2007 RT I 2007, 25, 133 01.01.2008 20.05.2010 RT I 2010, 29, 151 20.06.2010 Chapter 1 GENERAL PROVISIONS § 1. Area of regulation of Act This Act prescribes the specifications which arise from the special nature of the insular conditions of the permanently inhabited small island and which are not provided for in other Acts. § 2. Definitions used in Act In this Act, the following definitions are used: 1) island rural municipality– rural municipality which administers a permanently inhabited small island or an archipelago as a whole; [RT I 2007, 25, 133 - entry into force 01.01.2008] 2) rural municipality which includes small islands – rural municipality which comprises permanently inhabited small islands, but is not constituting part of island rural municipalities; 3) permanently inhabited small islands (hereinafter small islands) – Abruka, Kihnu, Kessulaid, Kõinastu, Manija, Osmussaar, Piirissaar, Prangli, Ruhnu, Vilsandi and Vormsi; [RT I 2007, 25, 133 - entry into force 01.01.2008] 4) large islands – Saaremaa, Hiiumaa and Muhu. 5) permanent inhabitation – permanent and predominant residing on a small island; [RT I 2007, 25, 133 - entry into force 01.01.2008] 6) permanent inhabitant – a person who permanently and predominantly resides on a small island and data on whose residence are entered in the population register to the accuracy of a settlement unit located on a small island. -
Tõnisson, H., Orviku, K., Lapinskis, J., Gulbinskas, S., and Zaromskis, R
Text below is updated version of the chapter in book: Tõnisson, H., Orviku, K., Lapinskis, J., Gulbinskas, S., and Zaromskis, R. (2013). The Baltic States - Estonia, Latvia and Lithuania. Panzini, E. and Williams, A. (Toim.). Coastal erosion and protection in Europe (47 - 80). UK, US and Canada: Routledge. More can be found: Kont, A.; Endjärv, E.; Jaagus, J.; Lode, E.; Orviku, K.; Ratas, U.; Rivis, R.; Suursaar, Ü.; Tõnisson, H. (2007). Impact of climate change on Estonian coastal and inland wetlands — a summary with new results. Boreal Environment Research, 12, 653 - 671. It is also available online: http://www.borenv.net/BER/pdfs/ber12/ber12-653.pdf Introduction Estonia is located in a transition zone between regions having a maritime climate in the west and continental climate in the east and is a relatively small country (45,227 km2), but its geographical location between the Fenno-scandian Shield and East European Platform and comparatively long coastline (over 4000 km) due to numerous peninsulas, bays and islands (>1,500 island), results in a variety of shore types and ecosystems. The western coast is exposed to waves generated by prevailing westerly winds, with NW waves dominant along the north-facing segment beside the Gulf of Finland, contrasting with southern relatively sheltered sectors located on the inner coasts of islands and along the Gulf of Livonia (Riga). The coastline classification is based on the concept of wave processes straightening initial irregular outlines via erosion of Capes/bay deposition, or a combination (Orviku, 1974, Orviku and Granö, 1992, Gudelis, 1967). Much coast (77%) is irregular with the geological composition of Capes and bays being either hard bedrock or unconsolidated Quaternary deposits, notably glacial drift. -
Lõputöö-Hookan-Lember.Pdf (2.127Mb)
Sisekaitseakadeemia Päästekolledž Hookan Lember RS150 PÄÄSTESÜNDMUSTE ANALÜÜS PÜSIASUSTUSEGA VÄIKESAARTEL Lõputöö Juhendaja: Häli Allas MA Kaasjuhendaja: Andres Mumma Tallinn 2018 ANNOTATSIOON Päästekolledž Kaitsmine: juuni 2018 Töö pealkiri eesti keeles: Päästesündmuste analüüs püsiasustusega väikesaartel Töö pealkiri võõrkeeles: The analysis of rescue events on small islands with permanent settlements Lühikokkuvõte: Töö on kirjutatud eesti keeles ning eesti ja inglise keelse kokkuvõttega. Töö koos lisadega on kirjutatud kokku 61 lehel, millest põhiosa on 38 lehekülge. Lõputöö koosneb kolmest peatükist, kus on kasutatud kahte tabelit ja seitseteist joonist. Valitud teema uurimisprobleemiks on tervikliku ülevaate puudumine väikesaarte sündmustest, mis kuuluvad Päästeameti valdkonda. Väikesaartele toimub reageerimine erinevalt ning sõltuvalt aastaajast on reageerimine raskendatud. Ühtseid põhimõtteid rahvaarvu või sündmuste arvu kohta ei ole. Lõputöö eesmärk on analüüsida päästesündmusi väikesaartel aastatel 2009-2017 ning järeldada, millist päästevõimekust vajavad püsiasutustega väikesaared. Lõputöös antakse saartest ülevaade, mis on valimis välja toodud ning visualiseeritakse joonise abil saartel elavate püsielanike arv. Eesmärgi saavutamiseks kasutati kvantitatiivset uurimismeetodit, kus Häirekeskuselt saadud andmed korrastati ja analüüsiti. Lõputöös anti ülevaade, millised on sündmused saartel ning tehti järeldused, kuidas tagada kiire ja kvaliteetse abi kättesaadavus. Saartel, kus elanike arv on väike ning sündmuste arv minimaalne, -
Wave Climate and Coastal Processes in the Osmussaar–Neugrund Region, Baltic Sea
Coastal Processes II 99 Wave climate and coastal processes in the Osmussaar–Neugrund region, Baltic Sea Ü. Suursaar1, R. Szava-Kovats2 & H. Tõnisson3 1Estonian Marine Institute, University of Tartu, Estonia 2Institute of Ecology and Earth Sciences, University of Tartu, Estonia 3Institute of Ecology, Tallinn University, Estonia Abstract The aim of the paper is to investigate hydrodynamic conditions in the Neugrund Bank area from ADCP measurements in 2009–2010, to present a local long-term wave hindcast and to study coastal formations around the Neugrund. Coastal geomorphic surveys have been carried out since 2004 and analysis has been performed of aerial photographs and old charts dating back to 1900. Both the in situ measurements of waves and currents, as well as the semi-empirical wave hindcast are focused on the area known as the Neugrund submarine impact structure, a 535 million-years-old meteorite crater. This crater is located in the Gulf of Finland, about 10 km from the shore of Estonia. The depth above the central plateau of the structure is 1–15 m, whereas the adjacent sea depth is 20– 40 m shoreward and about 60 m to the north. Limestone scarp and accumulative pebble-shingle shores dominate Osmussaar Island and Pakri Peninsula and are separated by the sandy beaches of Nõva and Keibu Bays. The Osmussaar scarp is slowly retreating on the north-western and northern side of the island, whereas the coastline is migrating seaward in the south as owing to formation of accumulative spits. The most rapid changes have occurred either during exceptionally strong single storms or in periods of increased cyclonic and wave activity, the last high phase of which occurred in 1980s–1990s. -
Nature Tourism Marketing on Central Baltic Islands
Baltic Sea Development & Media Center Nature tourism marketing on Central Baltic islands Tallinn, 2011 Nature tourism marketing on Central Baltic islands. Tallinn, 2011. ISBN 978-9985-9973-5-2 Compilers: Rivo Noorkõiv Kertu Vuks Cover photo: Aerial view on Osmussaar, NW Estonia (photo: E. Lepik) © Baltic Sea Development & Media Center © NGO GEOGUIDE BALTOSCANDIA E-mail: [email protected] EUROPEAN UNION EUROPEAN REGIONAL DEVELOPMENT FUND INVESTING IN YOUR FUTURE Release of this report was co-financed by European Re- gional Development Fund and NGO Geoguide Baltoscandia. It was accomplished within the framework of the CENTRAL BALTIC INTERREG IVA Programme 2007-2013. Disclaimer: The publication reflects the authors views and the Managing Authority cannot be held liable for the information published by the project partners. CONTENTS 1. INTRODUCTION....................................................................................... 5 2. THE DEVELOPMENT OF NATURE TOURISM ............................................... 6 2.1. THE HISTORY AND TERMINOLOGY OF NATURE TOURISM ����������������������������� 6 2.2. NATURE TOURISM AND ENVIRONMENTAL AWARENESS ............................... 7 2.3. DEVELOPMENT PERSPECTIVES OF NATURE TOURISM IN BALTIC SEA AREA ���� 10 2.3.1. THE MARKET SITUATION OF ESTONIAN TOURISM SECTOR ....................... 10 2.3.2. TOURISM DEVELOPMENT IN GOTLAND, ÅLAND AND TURKU ARCHIPELAGOS 13 3. OVERVIEW OF THE TOURISM RESOURCES IN THE CENTRAL BALTIC REGION ................................................................................................................ -
Woodworking in Estonia
WOODWORKING IN ESTONIA HISTORICAL SURVEY By Ants Viires Translated from Estonian by Mart Aru Published by Lost Art Press LLC in 2016 26 Greenbriar Ave., Fort Mitchell, KY 41017, USA Web: http://lostartpress.com Title: Woodworking in Estonia: Historical Survey Author: Ants Viires (1918-2015) Translator: Mart Aru Publisher: Christopher Schwarz Editor: Peter Follansbee Copy Editor: Megan Fitzpatrick Designer: Meghan Bates Index: Suzanne Ellison Distribution: John Hoffman Text and images are copyright © 2016 by Ants Viires (and his estate) ISBN: 978-0-9906230-9-0 First printing of this translated edition. ALL RIGHTS RESERVED No part of this book may be reproduced in any form or by any electronic or mechanical means including information storage and retrieval systems without permission in writing from the publisher, except by a reviewer, who may quote brief passages in a review. This book was printed and bound in the United States. CONTENTS Introduction to the English Language Edition vii The Twisting Translation Tale ix Foreword to the Second Edition 1 INTRODUCTION 1. Literature, Materials & Methods 2 2. The Role Played by Woodwork in the Peasants’ Life 5 WOODWORK TECHNOLOGY 1. Timber 10 2. The Principal Tools 19 3. Processing Logs. Hollowing Work and Sealed Containers 81 4. Board Containers 96 5. Objects Made by Bending 127 6. Other Bending Work. Building Vehicles 148 7. The Production of Shingles and Other Small Objects 175 8. Turnery 186 9. Furniture Making and Other Carpentry Work 201 DIVISION OF LABOR IN THE VILLAGE 1. The Village Craftsman 215 2. Home Industry 234 FINAL CONCLUSIONS 283 Index 287 INTRODUCTION TO THE ENGLISH-LANGUAGE EDITION feel like Captain Pike. -
Looduslik Ja Antropogeenne Morfodünaamika Eesti Rannikumere
THESIS ON CIVIL ENGINEERING F22 Lithohydrodynamic processes in the Tallinn Bay area ANDRES KASK TUT PRESS TALLINN UNIVERSITY OF TECHNOLOGY Faculty of Civil Engineering Department of Mechanics The dissertation was accepted for the defence of the degree of Doctor of Philosophy on June 28, 2009 Supervisor: Prof. Tarmo Soomere Department of Mechanics and Institute of Cybernetics Tallinn University of Technology, Estonia Opponents: Prof. Dr. Jan Harff Foundation for Polish Science Fellow, Institute of Marine Sciences University of Szczecin, Poland Prof. Dr. Anto Raukas Leading research scientist, Institute of Geology Tallinn University of Technology, Member of Estonian Academy of Sciences Defence of the thesis: August 21, 2009, Institute of Cybernetics at Tallinn University of Technology, Akadeemia tee 21, 12618 Tallinn, Estonia Declaration: Hereby I declare that this doctoral thesis, my original investigation and achievement, submitted for the doctoral degree at Tallinn University of Technology has not been submitted for any academic degree. Andres Kask Copyright: Andres Kask, 2009 ISSN 1406-4766 ISBN 978-9985-59-923-5 3 EHITUS F22 Litohüdrodünaamilised protsessid Tallinna lahe piirkonnas ANDRES KASK TUT PRESS 4 Contents List of tables .............................................................................................................. 7 List of figures ............................................................................................................ 7 Introduction .............................................................................................................. -
2017 Lighthouse Tours a Better Way to See Lighthouses! What Can You Expect from a USLHS Tour?
UNITED STATES LIGHTHOUSE SOCIETY 2017 LIGHTHOUSE TOURS A BETTER WAY TO SEE LIGHTHOUSES! WHAT CAN YOU EXPECT FROM A USLHS TOUR? You will be in the company of lighthouse lovers, history buffs, world travelers, and life-long learners A MESSAGE FROM THE DIRECTOR who enjoy the camaraderie of old friends and new. Our members are known for being fun-loving and People all over the world are naturally drawn to inclusive! Single travelers are always welcome. lighthouses. Typically located in the most beautiful locations on the planet, they reward those We are often able to explore, climb, and/or of us who love to travel with stunning natural photograph lighthouses, not open to the public, landscapes and transcendent vistas. Historically, usually found in remote locations. Your journey lighthouses were built to save lives, giving them to a lighthouse could involve charter boats, off a human connection unlike any other historic road vehicles, helicopters, float planes, or perhaps horse drawn carriages! Travelers have even found landmark. They represent attributes all of us themselves on golf carts, jet boats, and lobster strive for: compassion, courage, dedication, selflessnessand humility...and trawlers just to get that perfect lighthouse when you visit a lighthouse, you are destined to be moved in ways that viewpoint! connect you with something larger than yourself. U.S. Lighthouse Society tours are designed intentionally for those who Tour itineraries are designed to provide love traveling to amazing places and who desire to connect with others opportunities to visit other regional landmarks and who share a common passion for lighthouses and what they stand for. -
Storminess-Related Rhythmic Ridge Patterns on the Coasts of Estonia
Estonian Journal of Earth Sciences, 2017, 66, 4, 220–237 https://doi.org/10.3176/earth.2017.16 Storminess-related rhythmic ridge patterns on the coasts of Estonia Ülo Suursaara and Hannes Tõnissonb a Estonian Marine Institute, University of Tartu, Mäealuse St. 14, 12618 Tallinn, Estonia; [email protected] b Institute of Ecology at Tallinn University, Uus-Sadama 5-537, 10120 Tallinn, Estonia; [email protected] Received 29 March 2017, accepted 14 September 2017, available online 10 November 2017 Abstract. Buried or elevated coastal ridges may serve as archives of past variations in sea level and climate conditions. Sometimes such ridges or coastal scarps appear in patterns, particularly on uplifting coasts with adequate sediment supply. Along the seacoasts of Estonia, where relative-to-geoid postglacial uplift can vary between 1.7 and 3.4 mm/yr, at least 27 areas with rhythmic geomorphic patterns have been identified from LiDAR images and elevation data. Such patterns were mainly found on faster emerging and well-exposed, tideless coasts. These are mostly located at heights between 1 and 21 m above sea level, the formation of which corresponds to a period of up to 7500 years. Up to approximately 150 individual ridges were counted on some cross-shore sections. Ten of these ridge patterns that formed less than 4500 years ago were chosen for detailed characterization and analysis in search of possible forcing mechanisms. Among these more closely studied cases, the mean ridge spacing varied between 19 and 28 m. Using land uplift rates from the late Holocene period, the timespans of the corresponding cross sections were calculated. -
Contents of Elibrary of Folia Cryptog. Estonica Fasc. 31–42
Folia Cryptog. Estonica, Fasc. 31–42 (1997–2006) ISSN 1406-2070 FOLIA CRYPTOGAMICA ESTONICA Fasc. 31–42 CONTENTS Folia Cryptog. Estonica 31 (1997) ............................................................ 2 Folia Cryptog. Estonica 32 (1998)............................................................ 3 Folia Cryptog. Estonica 33 (1998)............................................................ 4 Folia Cryptog. Estonica 34 (1999)............................................................ 6 Folia Cryptog. Estonica 35 (1999)............................................................ 7 Folia Cryptog. Estonica 36 (2000)............................................................ 8 Folia Cryptog. Estonica 37 (2000)............................................................ 9 Folia Cryptog. Estonica 38 (2001)...........................................................10 Folia Cryptog. Estonica 39 (2002)........................................................... 11 Folia Cryptog. Estonica 40 (2003, publ. 2004) .........................................12 Folia Cryptog. Estonica 41 (2005)...........................................................13 Folia Cryptog. Estonica 42 (2006)...........................................................14 Published and distributed by Estonian Naturalists’ Society BOX 48, 51003 Tartu ESTONIA FCE T A R T U ©Go Estonianto CONTENTS Naturalists’ Society Folia Cryptog. Estonica, Fasc. 31–42 (1997–2006) Folia Cryptog. Estonica 31 (1997) Kannukene, L., Ingerpuu, N., Vellak, K. & Leis, M. Additions and amendments -
Estonia Estonia
Estonia A cool country with a warm heart www.visitestonia.com ESTONIA Official name: Republic of Estonia (in Estonian: Eesti Vabariik) Area: 45,227 km2 (ca 0% of Estonia’s territory is made up of 520 islands, 5% are inland waterbodies, 48% is forest, 7% is marshland and moor, and 37% is agricultural land) 1.36 million inhabitants (68% Estonians, 26% Russians, 2% Ukrainians, % Byelorussians and % Finns), of whom 68% live in cities Capital Tallinn (397 thousand inhabitants) Official language: Estonian, system of government: parliamen- tary democracy. The proclamation of the country’s independ- ence is a national holiday celebrated on the 24th of February (Independence Day). The Republic of Estonia is a member of the European Union and NATO USEFUL INFORMATION Estonia is on Eastern European time (GMT +02:00) The currency is the Estonian kroon (EEK) ( EUR =5.6466 EEK) Telephone: the country code for Estonia is +372 Estonian Internet catalogue www.ee, information: www.1182.ee and www.1188.ee Map of public Internet access points: regio.delfi.ee/ipunktid, and wireless Internet areas: www.wifi.ee Emergency numbers in Estonia: police 110, ambulance and fire department 112 Distance from Tallinn: Helsinki 85 km, Riga 307 km, St. Petersburg 395 km, Stockholm 405 km Estonia. A cool country with a warm heart hat is the best expression of Estonia’s character? Is an extraordinary building of its own – in the 6th century Wit the grey limestone, used in the walls of medieval Oleviste Church, whose tower is 59 metres high, was houses and churches, that pushes its way through the the highest in the world.