DOCSLIB.ORG

Download Article

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Download Article Advances in Social Science, Education and Humanities Research, volume 473 Proceedings of the 3rd International Conference on Social Sciences (ICSS 2020) Study of Landslide Prone on the Road of Tomohon-Tanawangko in Tomohon City Denny Maliangkay* Geography Deparment Faculty of Social Sciences, State University of Manado Manado, North Sulawesi [email protected] Abstract—Disaster is a series of events caused by anytime people in Indonesia are always at risk to disasters, human nature, or both resulting in casualties and human earthquakes, volcanic eruptions, tsunamis, avalanches, suffering, property damage, environmental damage, floods, droughts, storms, forest fires, and the inter-ethnic damage to infrastructures facilities, and public utilities violence. Each type has a severe impact of the disaster and as well as disturbance of the system raises the life and resulted in casualties and property losses are not small. livelihood. Landslides (landslides) represents a Land landslides (landslides) represents a comprehensive comprehensive disaster in mountainous and hilly regions disaster in mountainous and hilly regions in the world, has in the world, has led to loss of life and material damage. led to loss of life and material damage.The factors causing Factors causing landslides, among others: rainfall, steep landslides, among others: rainfall, steep slopes, soil less slopes, soils that are less dense and thick, rock is less dense and thick, less solid rock, the type of land system, powerful, the kind of governance of land, vibration, and vibration, and shrinkage of the water table by or dams, the shrinkage of the water table by or dams, the extra extra load, abrasion / erosion, their embankment material on burden, erosion / erosion, the embankment material on the cliff, the former long avalanche, the discontinuity field the cliff, the former long avalanche, the discontinuity (field is not continuous), deforestation, waste disposal area field (field is not continuous), deforestation, waste In the event of landslides will disrupt community disposal area. The problem in this research is only activities. The most feared again if fatalities due to falling limited studies landslide-prone land in the lane land landslide would have harmed many people both morally Tanawangko-Tomohon Tomohon. Main purpose of this and materially. study was to determine the points of land landslide hazard on the road lane Tomohon-Tanahwangko Based on the background of the above problems, it can be identified several problems: benefits derived from this research is to be produced a study of geological and geomorphological conditions In Tomohon Tanahwangko lane road in an area prone to Tomohon-Tanawangko lane road. Variables to be landslide disaster land. studied, namely landslide, the physical condition of the study area, and the factors triggering the landslide of the Lack of attention and concern of the community and government on the condition and quality of land in most influential land. Identified three types of land Tomohon-Tanahwangko lane. landslide that occurred in Tomohon-Tanawangko lane road covering; collapse (fall), landslides (slides), and Steep topography / steep in some point and the high flow (flow). Avalanche land is most common creep (flow) rainfall in the rainy season which causes the occurrence of seven (7) points avalanches. Land landslide of landslide prone land. vulnerability study area was divided into four (4) Avalanche danger due and affects the activities of public landslide prone zones include; Low Land landslide- land in the lane Tomohon Tanahwangko prone zones, landslide-prone zones Land moderate, high land landslide-prone zones, landslide-prone zones land is Restricting the problem very high. Interval slope of each point landslide Land is The problems that arise in the study are complex, at 44% -85%, so it can be seen that from every point of therefore the problem in this research is only limited studies avalanches that are in landslide-prone zones landslide- landslide-prone land in the lane Tomohon Tanawangko prone zones of moderate to very high land. Aim Keywords: Landslide, Disaster, Hazard Main purpose of this study was to determine the points of land landslide hazard on the road lane Tomohon I. INTRODUCTION Tanahwangko The need for awareness of that, the Republic of Indonesia Benefits of Research including the island nation of active tectonics, volcanic active, wet tropical climate, densely populated by various This research can directly obtain information for the ethnic groups, so never escape the risk to disasters whether government and the public about the landslide disaster-prone natural or man-made disasters. In other words, anywhere and land in Tomohon Tanawangko lane. While the benefits of Copyright © 2020 The Authors. Published by Atlantis Press SARL. This is an open access article distributed under the CC BY-NC 4.0 license -http://creativecommons.org/licenses/by-nc/4.0/. 27 Advances in Social Science, Education and Humanities Research, volume 473 this research is to be produced a study of geological and determining the level of avalanche danger as can be seen in geomorphological conditions paths Tomohon Tanawangko. the table below: Table 1. Class Scalling Slopes II. METHOD No. Klas large Slope criteria Slope Harkat 1. I 0-8% Flat 1 A. Method 2. II ˃8 - 15% Sloping 2 The method used in this research is qualitative 3. III ˃15 - 25% tilt 3 descriptive method with approach overlay or overlaying 4. IV ˃25 - 40% Steep 4 maps to produce maps prone to landslides. 5. V ˃40% very steep 5 Source: Suprapto Dibyosaputro 1998 B. Tools and Materials 2) Land Use Intended land use various forms of human Clinometer for measuring slope intervention in the use of natural resources for the welfare of Altimeter altitude measurement mankind. Form and land use such as penterasan, hoeing, material planting timber on a slope with a certain slope, which do not map Slopes follow the rules of conservation, it will create new problems Geologic map such as landslides. Scalling on land use, as in the following Map of Land Use table: Soil map Table 2. Scale Class Land Use No. Land Use Scale C. Research Variable 1. similar forest 1 In this study the variables that will be studied, namely 2. No similar forest 2 landslide Land, the physical condition of the study area, and 3. Plantation 3 the factors triggering the landslide of the most influential 4. Settlements and other supporting 4 land cover map: facilities Climate (rainfall) 5. Moor 5 Slope Source: Suratman W. et al 1992) land use 3) Vegetation density The density of the vegetation seen Geology from the level of plant density and canopy of leaves. Land covered by closed, failed to give a chance sunlight reaches D. Data Collection Technique the ground level so that physical weathering hampered, This study used two types of data are primary data and while land that is not covered by vegetation will occur as the secondary data. reverse conditions. Scale vegetation density as in the following table: 1) Primary data Primary data collected among others Table 3. Vegetation density class scalling long slope and slope, land use, soil texture, effective depth / No. class density large density Scale soil, and the primary data will be obtained directly through 1. cheek by jowl 75-100% 1 measurements and observations in the field and see 2. Meeting 50-75% 2 pernelitian previous research-related. 3. moderate 25-50% 3 2) Secondary Data Secondary data collected were: Of 4. Rarely 15-25% 4 base maps such as maps geological maps, soil maps, 5. Very rarely ˃15% 5 topographical maps and land use maps. The maps obtained Source: Suratman et al (1992) from BAPEDA SULUT or other agencies. Rainfall and 4) Steep walls conditions Is one of the steep walls of temperature data obtained through BMKG Kayuwatu rock types constituent pencerminaan landforms, rock Manado. stratigraphic condition constituent, whether in the form of E. Analyze Data fault tectonic processes and folds, or it may be due to the The data analysis was done by scoring or dignity as intensity a notch by surface runoff, which is concentrated in follows: the groove or valley of the river, or also due to human activities. Avalanche relation to land, the steep wall in the 1) Slope Scaling slope based on the concept that region will greatly favor the occurrence of landslide Land. basically affect the slope of the force of gravity and the This is due to the steep walls of both faults, folds, incising, shear force along the slope. The flatter slope, the force of will provide an opportunity receive more sunlight so that the gravity can work entirely, so that the material will not rot weathering will be more intensive. Based on this concept, and loose horizontal shift, but on a steep slope incline to the conceived scalling steep wall condition as shown in Table. resultant force will occur due to the gravitational force and below this. shear force. Besides flat slope, soil water movement is Table 4. Scalling Class Wall Rough slower than on a sloping hillside. Based on previous Class Total Conditions steep No. Scale descriptions compiled class scalling slope in the role of Wall Rough walls 28 Advances in Social Science, Education and Humanities Research, volume 473 Without - very Valley, the slope Climate classification study area has a value of Q = 1 1 little is not steep 6.25%, which indicates that this type of climate is A or very wet which is obtained from: Climate affects the landslide Valley, rather 2 a little 2 Land especially rainfall which is one of the factors triggering steep slope the occurrence of landslide Land. In this study the Valleys, steep 3 moderate 3 relationship between land landslide with rainfall can be seen slope portion from some of the events that occurred landslide land in the Valleys, steep 4 Lots 4 study area in the landslide area produced 14 points Land.
Load more

Recommended publications
  • POTENTIALS and INVESTMENT OPPORTUNITIES GOVERNOR VICE GOVERNOR OLLY DONDOKAMBEY, SE Drs
    GOVERNMENT OF NORTH SULAWESI PROVINCE POTENTIALS AND INVESTMENT OPPORTUNITIES GOVERNOR VICE GOVERNOR OLLY DONDOKAMBEY, SE Drs. S. O. KANDOW NORTH SULAWESI IN THE WORLD MAP GENERAL INFORMATION 1. Geography The Province of North Sulawesi is located in Northern Peninsula of Sulawesi Island, and constitutes one of the three (3) Provinces in Indonesia which located in Northern part of Khatulistiwa Line (equator line), Two other Provinces are; South Sulawesi Province and Aceh Province. On the geographical position perspective, North Sulawesi Province is located between 0.300 – 4.300 North Latitude and 1210-1270 East Longitude. Barang ALKI I ALKI II ALKI III 2. Territory Length and Division 15,272.44 km2 area is spacious, has 4 cities and 11 regancies. Most of the land area consists of mountains, hills and valleys. Height from sea level is varied 0 - > 1,000 meters. Barang Bukit Doa, Tomohon 3. Climate North Sulawesi is a tropical area that is affected by the wind muzon. In November to April the West wind blows that brought rain on the north coast , while in May to October there is a change of dry southerly winds. The average rainfall ranges from 2000-3000 mm per year, and the number of rainy days between 90-139 days. Temperatures range from 20 0C - 32 0C. Barang Mount Lokon , Tomohon Pulau Bunaken 4. Demography Total population of 2.54725 million people, scattered in the regancy/city as follows : REGANCIES/CITIES POPULATION KOTA MANADO 484.744 KOTA BITUNG 223.980 KOTA TOMOHON 97.775 KOTA KOTAMOBAGU 123.623 KAB. MINAHASA UTARA 222.062 KAB.
    [Show full text]
  • Henk Ngantung Painting History Study in CD-ROM
    ID Khazanah : Halaman Situs Blog Source : http://driwancybermuseum.wordpress.com/2012/04/02/heng-ngantung-painting- history-study-in-cd-rom/ Date of publication : 2 April 2012 Capture date : 20 April 2012 Henk Ngantung Painting History study in CD-ROM Posted on April 2, 2012 | Leave a comment 200,481 views all-time Henk Ngantung Painting History Collection Created By Dr Iwan suwandy,MHA Limited Private Edition In DD-ROM Copyright @ 2012 IVAA Documentation 1 ID Khazanah : Halaman Situs Blog Source : http://driwancybermuseum.wordpress.com/2012/04/02/heng-ngantung-painting- history-study-in-cd-rom/ Date of publication : 2 April 2012 Capture date : 20 April 2012 INTRODUCTION Years ago I found a few documents, paintings and sketches,painting book of Henk Ngantung from antique dealer friend in Jakarta, and I have written my blog web driwancybermuseum about the painter and has got quite a lot of responses from friends of the deceased. Last week I found a book written by Baharuddin MS book published earlier in January 1981, entitled Sketches Ngentung with Henk Henk illustration sketch creation Ngantung start puberty until the year 1935 1951.berjumlah 240.Buku begins with an introduction entitled Henk Ngantung The swaya know. Based on these two great discoveries I started doing more research from other sources that there is so into this paper. The next paper is written in English language support so that the deceased can be universally recognized by the world and his collection can be made heritage of the world, and if da links can be made a special
    [Show full text]
  • Review of Policies and Institutional Capacity for Early Warning and Disaster Management in Indonesia January 2007
    U.S. INDIAN OCEAN TSUNAMI WARNING SYSTEM (US IOTWS) PROGRAM REVIEW OF POLICIES AND INSTITUTIONAL CAPACITY FOR EARLY WARNING AND DISASTER MANAGEMENT IN INDONESIA JANUARY 2007 January 2007 This publication was produced for review by the United States Agency for International Development. It was prepared by the IRG-Tetra Tech Joint Venture. U.S. INDIAN OCEAN TSUNAMI WARNING SYSTEM (US IOTWS) PROGRAM REVIEW OF POLICIES AND INSTITUTIONAL CAPACITY FOR EARLY WARNING AND DISASTER MANAGEMENT IN INDONESIA (OCTOBER 1-13, 2006) JANUARY 2007 Prepared for U.S. Agency for International Development by IRG & Tetra Tech Joint Venture under Contract No. EPP-I-02-04-00024-00 U.S. IOTWS Program Document No.14-IOTWS-06 DISCLAIMER The views expressed in this document do not necessarily reflect the views of the United States Agency for International Development or the United States Government. CONTENTS Acronyms ................................................................................................................ 1 Preface ..................................................................................................................... 3 Introduction ............................................................................................................ 4 1. Policy and Legislative Environment for Disaster Management .................... 6 1.1 Legislative Environment .......................................................................................................... 6 1.2 Institutional Environment ......................................................................................................
    [Show full text]
  • Perkembangan Pers Minahasa Pada Masa Kolonial Tahun 1869-1942
    PERKEMBANGAN PERS MINAHASA PADA MASA KOLONIAL TAHUN 1869-1942 JURNAL SKRIPSI Diajukan untuk melengkapi persyaratan mencapai gelar Sarjana Sastra Oleh : Bodewyn Grey Talumewo NIM : 070914003 Jurusan : Ilmu Sejarah UNIVERSITAS SAM RATULANGI FAKULTAS ILMU BUDAYA MANADO 2015 1 ABSTRACT This scientific paper contains about the development of the Minahasan press in the Netherlands’ colonial rule in the time of Dutch East Indies (of Indonesia). Explain about the origin of the press in Minahasa land when the newspaper of Tjahaja Sijang published since year 1869, about the development of the Minahasan press in Dutch East Indies, explain about develompment of the Minahasan press tandem with the national movement for freedom and for the independence of the Indonesia. Exposure of the pioneers and leaders of the Minahasan press in the colonial time. Keyword: press, colonial, Minahasa, North Sulawesi, kawanua, newspaper, journalism I. PENDAHULUAN 1.1. Latar Belakang Penyelidikan sejarah pers merupakan sebuah penelitian yang begitu kompleks sebab selain sebagai media komunikasi sosial-kemasyarakatan, pers juga menjadi media komunikasi politik, komunikasi keagamaan, dan lain sebagainya. Oleh karena itu pers sebagai bagian dari kegiatan jurnalistik, pers merupakan sebuah bagian dari ilmu komunikasi yang menjadi jembatan antara pencari berita dengan sumber berita. Keberadaan pers di daerah Minahasa memberi kontribusi yang besar terhadap perkembangan intelektual dan kesadaran sosial masyarakat Minahasa. Penyelidikan sejarah pers terlebih dahulu memahami pengertian dari kata pers . Kata pers berasal dari bahasa Belanda pers . Kata pers tersebut berasal dari bahasa Latin pressare yang berarti “tekan” atau “cetak”. Kata “pers” dalam bahasa Belanda berarti “alat pemeras/penekan; alat pencetak buku, surat kabar; surat kabar, harian”.
    [Show full text]
  • Morphostructure Control Towards the Development of Mahawu Volcanic Complex, North Sulawesi
    Indonesian Journal of Geology, Vol. 7 No. 1 March 2012: 39-54 Morphostructure Control Towards the Development of Mahawu Volcanic Complex, North Sulawesi Kontrol Morfostruktur Terhadap Perkembangan Kompleks Gunung Api Mahawu, Sulawesi Utara S. PoedjoPrajitno Centre for Geological Survey, Geological Agency, Jln. Diponegoro No. 57 Bandung, Indonesia 40122 AbstrAct The studied area, situated in northeastern part of North Sulawesi Arm, is dominantly occupied by the Mahawu, Linau, Tompusu, and Kasurutan volcanic rocks. Using remote sensing data, such as landsat image, black and white panchromatic aerial photograph, and IFSAR image, morphology-origin unit and morphology lineament can be interpreted. Four morphology-origin units, those are Mahawu Volcano Complex, Intra-montane Plain structure, Linau Volcano Complex, and Lacustrine Plain are recognized. Furthermore, morphological lineament pattern was statistically processed to find out the general stress direction in the area to determine the probability of the structural morphology occurrence in the Mahawu Volcano Complex. The result shows that generally the development pattern of volcanic cones are irregular, except the Mahawu Volcano Complex showing a linear pattern. This lineament pattern is interpreted as a NW - SE fault pattern controlling the rise of magma. At least, two tectonic and two eruption periods occurred regularly at different time from the Quaternary age till the present. Keywords: morphostructure, Mahawu Volcano cone, fault, lineament, magma, North Sulawesi Arm Sari Daerah penelitian, yang terletak di bagian timur laut Lengan Utara Sulawesi, didominasi oleh batuan vulkanik hasil kegiatan Gunung Api Mahawu, Linau, Tompusu, dan Kasurutan. Dengan menggunakan data inderaan jauh, yakni citra landsat, foto udara pankromatis hitam-putih, dan citra IFSAR, satuan bentukan- asal dan kelurusan morfologi ditafsirkan.
    [Show full text]
  • Minahassa, a Summarized History Dirk Teeuwen Msc, Holland
    Minahassa, a summarized history Dirk Teeuwen MSc, Holland Dirk Teeuwen 1996> Contents Introduction 1.Interference from Europe 2. Dutch supremacy 3. Establishment of Dutch authority in Minahassa 4. Important dates 5. Aftermath 6. Maps Sources and notes Minahassan farmer 1935 Introduction I travelled through Minahassa, North Celebes/Sulawesi in 1996. Zig-zag from Manado-Bunaken to Gorontalo. Then, in 1996, I estimated that around 20% of the Minahassans were still able to speak Dutch. No surprise, because I knew some headlines of Minahassan history. Minahassa is very special in the field of colonial history in general, as well as in the field of Dutch colonial history. That goes too, in particular, for Dutch Protestant missionary history. The Dutch period was handled by the Minahassans in a intelligent way very much. The Dutch colonial policy concerning Minahassa was very special as well. This summarized history is composed with full admiration of Minahassans, admiration of Dutch colonial policy in North Celebes, as well as of Dutch Protestant missionary efforts there. 1 1935 Maps in chapter 6 2 1. Interference from Europe During the second half of the 16 th century, both Portuguese and Spanish arrived in North Celebes. Celebes is called Sulawesi now, but from here I shall use the name from the olden days: Celebes. In 1512 the Portuguese set foot ashore in the Moluccan islands Banda and Amboina. The Muslim Sultan of Ternate – he held some sway over the Minahassa area in North Celebes - entered into a treaty with the Portuguese, a treaty aimed against the Sultanate of Tidore and against the Spaniards.
    [Show full text]
  • ASEAN Tourism Investment Guide
    ASEAN Tourism Investment Guide Design and Layout Sasyaz Kreatif Sdn. Bhd. (154747-K) Printer Sasyaz Holdings Sdn. Bhd. (219275-V) [email protected] Copyright © ASEAN National Tourism Organisations Published by : ASEAN National Tourism Organisations First published April 2008 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photography, recording or any other information storage and retrieval system, without prior permission in writing from the publishers. C o n t e n t s Page Preface 5 Asean Fast Fact 6 Brunei Darussalam 7 Cambodia 11 Indonesia 31 Lao PDR 67 Malaysia 81 Myanmar 115 Philippines 137 Singapore 199 Thailand 225 Viet Nam 241 P r e f a c e Tourism is one of the main priority sectors for ASEAN economic integration as envisaged in the Vientiane Action Programme (VAP). The ASEAN National Tourism Organizations (ASEAN NTOs) formulated a Plan of Action for ASEAN Co-operation in Tourism which includes the facilitation of investment within the region. Tourism has become a key industry and an important generator of income and employment for countries in the region. The rapid growth of tourism in recent years has attracted the interest of potential investors who are keen to be involved in this industry. One of the measures under the Implementation of Roadmap for Integration of Tourism Sector (Tourism Investment) is the Incentives for Development of Tourism Infrastructure (Measure no. 20). The objective of this measure is to provide incentives for the development of tourism infrastructure so as to encourage private investment in the ASEAN countries coming from investors within and outside the region.
    [Show full text]
  • Universitas Sam Ratulangi Unsrat Dalam Angka 2011
    Universitas Sam Ratulangi Jln. Kampus Unsrat Bahu Manado Tlp. 0431- 863786, Fax. 0431-822568 Email:[email protected] http://www.unsrat.ac.id Universitas Sam Ratulangi KATA PENGANTAR Buku Laporan UNSRAT DALAM ANGKA 2011 merupakan data dan informasi selang waktu bulan Januari s/d Desember 2011, yang menyajikan beragam jenis data dan informasi bersumber dari seluruh unit kerja seperti Fakultas, Lembaga, Program Pascasarjana, dan Unit Pelaksana Teknis lainnya dalam lingkungan Universitas Sam Ratulangi. Buku Laporan UNSRAT DALAM ANGKA 2011 ini memuat gambaran umum tentang keadaan penyelenggaraan Tri Dharma Perguruan Tinggi di Universitas Sam Ratulangi dan beberapa tabel tertentu juga dilengkapi dengan grafik yang menyajikan data tingkat perkembangan atau kondisi 5 (lima) tahun sebelumnya untuk melihat keterbandingan data dan informasi yang ada setiap tahun. Untuk memenuhi kebutuhan data terkini, buku Laporan UNSRAT DALAM ANGKA 2011 ini menyajikan beberapa data yang diperlukan sebagai acuan dalam penyusunan buku Unsrat Dalam Angka 2012. Semoga buku Laporan UNSRAT DALAM ANGKA 2011 ini bermanfaat untuk kemajuan Universitas Sam Ratulangi ke depan. Manado, Januari 2012 R e k t o r, Prof. Dr. Donald A. Rumokoy, SH.,MH. NIP. 19560828 198203 1 003 Unsrat Dalam Angka 2011 i Universitas Sam Ratulangi DAFTAR ISI KATA PENGANTAR …………………………………………………………………………………………………………………………………………… i DAFTAR ISI ……………………………………………………………………………………………………………………………………………………… ii - iv SEJARAH UNIVERSITAS SAM RATULANGI ………………………………………………………………………………………………………… 1 – 7 BAGAN STRUKTUR UNIVERSITAS SAM RATULANGI ………………………………………………………………………………………… 8 STRUKTUR DAN ORGANISASI KANTOR PUSAT UNSRAT ………………………………………………………………………………….. 9 – 43 AKADEMIK DAN KEMAHASISWAAN TABEL 1 AKREDITASI PROGRAM STUDI MENURUT JENJANG PROGRAM D.III, S1, S2, S3, SPESIALIS DAN PROFESI ……………………………………………………………………………………………………………………………………………. 44 – 46 TABEL 2 DAYA TAMPUNG MENURUT PROGRAM STUDI TAHUN AKADEMIK 2011 - 2012 ……………………………….. 47 – 49 TABEL 3 PEMINAT MENURUT PROGRAM STUDI TAHUN AKADEMIK 2010/2011 ………………………………………….
    [Show full text]
  • Pdf | 299.21 Kb
    WCO-Indonesia Situation Report (SR-1) 25 April 2012 Emergency and Humanitarian Action (EHA) Unit WHO Country Office - Indonesia Title SITREP # 1: 25 April 2012 at 10.00 AM (UCT +7) HIGH LIGHTS On Tuesday, 24 April 2012 at 11.21 AM (UCT+6), Mt. Lokon was erupted. It is located in Konilow village, North Tomohon sub-district, Tomohon, North Sulawesi province. As of 24 April 2012 at 14.00 PM (UCT+7), Centre for Health Crisis (CHC), Ministry of Health (MoH) reported no casualty or damage of health facility. By 25 April 2012 at 06.00 Central Indonesian Time (UCT+6), PVMBG reported that Mt. Lokon’s activity remains in alert level 3 “Watch Status”. Tomohon DHO, North Sulawesi PHO and Center for Health Crisis MOH are monitoring the situation closely; WHO is in close contact with MOH in monitoring the situation through Center for Health Crisis MOH. In case the situation warrant, WHO will provide any assistance needed. Affected Areas and Incident Site Mapping Level 1: Normal, basaltic activity. Level 2: Vigilant, Low activity. Level 3: Ready, Possibility of major eruption within weeks. Level 4: Alert, major eruption is imminent (within 24 hours). 1 WCO-Indonesia Situation Report (SR-1) 25 April 2012 Affected Area Manado Tomohon Situation Analysis Mt.Lokon Mount Lokon is a strato-type volcano located in Tomohon City, approximately 20 Km south west of Manado, North Sulawesi province. Mt. Lokon Eruption on 2011 On 10 July 2011 at 22.00 PM local time (UCT+6), the Center of Volcanology and Geological Disaster Mitigation (PVMBG) has declared Mt.
    [Show full text]
  • Defining Genius Loci and Qualifying Cultural Landscape of the Minahasa Ethnic Community in the North Sulawesi, Indonesia
    DEFINING GENIUS LOCI AND QUALIFYING CULTURAL LANDSCAPE OF THE MINAHASA ETHNIC COMMUNITY IN THE NORTH SULAWESI, INDONESIA Cynthia Erlita Virgin Wuisang Thesis submitted in fulfillment of the requirements for the degree of Doctor of Philosophy Faculty of the Professions School of Architecture and Built Environment Australia, 2014 Page | i Table of Contents Title Page Table of Contents………………………………………………………………………………………............ i List of Figures .…………………………………………………………………………………………… ......vii List of Tables....………………………………………………………………………………………………. xiii THESIS SUMMARY ............................................................................................................................ xv DECLARATION ................................................................................................................................ xvii ACKNOWLEDGEMENT .................................................................................................................... xix CHAPTER 1: INTRODUCTION ........................................................................................................... 1 1.1 Research Background ........................................................................................................... 1 1.2 Research Questions .............................................................................................................. 4 1.3 Research Aims and Objectives …………………………………………………………………… 5 1.4 Significance of Research Thesis ..........................................................................................
    [Show full text]
  • Recommendations for Achieving Community Based Conservation Tondano Watershed, Northern Sulawesi Report on a Rapid Rural Appraisal of Six Villages
    Recommendations for Achieving Community Based Conservation Tondano Watershed, Northern Sulawesi Report on a Rapid Rural Appraisal of Six Villages 17 January, 2001 Recommendations for Achieving Community Based Conservation Tondano Watershed, Northern Sulawesi Report on a Rapid Rural Appraisal of Six Villages 17 January, 2001 Environmental Policy and Institutional Strengthening IQC OUT-PCE-I-833-96-00002-00 Table of Contents Table of Contents ........................................................................................................................... i Executive Summary.....................................................................................................................iii Introduction................................................................................................................................... 1 Purpose of this report.................................................................................................................. 1 Goals of the Survey..................................................................................................................... 2 Methodology.................................................................................................................................. 5 Villages in the sample................................................................................................................. 5 Selection process and criteria for selection................................................................................. 5 Process of collecting
    [Show full text]
  • 1 HIGH LIGHTS Affected Areas and Incident Site Mapping
    WCO-Indonesia Situation Report (SR-1) 2 May 2012 Emergency and Humanitarian Action (EHA) Unit WHO Country Office - Indonesia Title SITREP # 1: 2 May 2012 at 10.00 AM (UCT +7) HIGH LIGHTS On Monday, 1 May 2012 at 12.00 PM Central Indonesian Time (UCT+7), Mt. Lokon which is located in Konilow village, North Tomohon sub-district, Tomohon, North Sulawesi province re-erupted; On 1 May 2012 at 12 PM Central Indonesian Time (UCT+7), Mt. Lokon released 2,500 meter height volcanic ashes from Tompaluan crater; The volcanic ashes flowed to North direction reaching Kakaskasen village; As of 1 May 2012 at 14.00 PM (UCT+7), Centre for Health Crisis (CHC), Ministry of Health (MoH) reported no casualty or damage of health facility; On 25 April 2012 at 06.00 Central Indonesian Time (UCT+6), PVMBG reported that Mt. Lokon’s activity remains in alert level 3 “Watch Status”; BPBD Tomohon has declared the emergency phase from 24 April – 23 May 2012 (30 days) and provided necessary action; Tomohon District Health Office (DHO) provided face masks and coordinated with Regional Crisis Center North Sulawesi and BPBD Tomohon; Tomohon DHO, North Sulawesi Provincial Health Office (PHO) and Center for Health Crisis MOH are monitoring the situation closely; BNPB provided IDR 2.8 billion for emergency response for Mt. Karangetang and Lokon; WHO is in close contact with MOH in monitoring the situation through Center for Health Crisis MOH. In case the situation warrant, WHO will provide any assistance needed. Affected Areas and Incident Site Mapping Level 1: Normal, basaltic activity.
    [Show full text]