Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunami

<p><a href="http://dx.doi.org/10.17014/ijog.vol3no2.20084" target="_blank">http://dx.doi.org/10.17014/ijog.vol3no2.20084</a></p><p><em>The coast of West Sumatera Province has two types of beaches: low lying sandy beach and steep rocky beach. St...

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Main Author: Yudhicara Yudhicara
Format: Article
Language:English
Published: Geological Agency 2014-06-01
Series:Indonesian Journal on Geoscience
Subjects:
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/51
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spelling doaj-92608d80cabd43c1af6d969d8cba430a2020-11-25T01:26:12ZengGeological AgencyIndonesian Journal on Geoscience2355-93142355-93062014-06-01329510610.17014/ijog.3.2.95-10651Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunamiYudhicara Yudhicara0Pusat Vulkanologi dan Mitigasi Bencana Geologi, Jl. Diponegoro 57 Bandung<p><a href="http://dx.doi.org/10.17014/ijog.vol3no2.20084" target="_blank">http://dx.doi.org/10.17014/ijog.vol3no2.20084</a></p><p><em>The coast of West Sumatera Province has two types of beaches: low lying sandy beach and steep rocky beach. Straight shoreline beaches at Padang beach until Air Bangis at the north and between Pasir Ganting and Salido beach at the south will have a potential tsunami height lower than bay shape beaches like at Kasai Bay, Kabung Bay, Batung Bay and Nibung Bay.</em></p> <p><em>A tsunami inundation will be further at a low lying area (low lying sandy beaches) compared with a coastal area which has steep slope and high relief (steep rocky beaches). Gosong beach at Pariaman which has a steep angle of beach slope will have lower tsunami height compared with a low angle beach slope like at Sungai Beramas, Kasai, Kabung, Batung and Nibung bays which have a beach slope about 3° to 5°. The maximum tsunami inundation is assumed to be located at Pasaman and Pasir Pariaman Sub-regencies, while the maximum tsunami height is assumed to be located at the middle of mapped area which has a bay shape. Tsunami is assumed to be arrived early at the southern most of mapped area or close to Muko-muko (Bengkulu).</em></p> <p><em>The maximum height difference from sea level was found at Tabai - Pariaman about 5.394 m, while the minimum height difference was found at Carocok Anau about 1.821 m. The horizontal distance measured from the nearest building from the shoreline is about 119 to 173 m.</em></p> <p><em>The worst case of tsunami modeling assumed that the maximum tsunami height will be about 32 m and used for reference to make tsunami prone zonation, such as high, moderate and low prone area.</em></p> <p> </p> <p> </p>https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/51Coastal characteristicsTsunami Prone Zonation
collection DOAJ
language English
format Article
sources DOAJ
author Yudhicara Yudhicara
spellingShingle Yudhicara Yudhicara
Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunami
Indonesian Journal on Geoscience
Coastal characteristics
Tsunami Prone Zonation
author_facet Yudhicara Yudhicara
author_sort Yudhicara Yudhicara
title Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunami
title_short Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunami
title_full Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunami
title_fullStr Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunami
title_full_unstemmed Kaitan antara karakteristik pantai Provinsi Sumatera Barat dengan potensi kerawanan tsunami
title_sort kaitan antara karakteristik pantai provinsi sumatera barat dengan potensi kerawanan tsunami
publisher Geological Agency
series Indonesian Journal on Geoscience
issn 2355-9314
2355-9306
publishDate 2014-06-01
description <p><a href="http://dx.doi.org/10.17014/ijog.vol3no2.20084" target="_blank">http://dx.doi.org/10.17014/ijog.vol3no2.20084</a></p><p><em>The coast of West Sumatera Province has two types of beaches: low lying sandy beach and steep rocky beach. Straight shoreline beaches at Padang beach until Air Bangis at the north and between Pasir Ganting and Salido beach at the south will have a potential tsunami height lower than bay shape beaches like at Kasai Bay, Kabung Bay, Batung Bay and Nibung Bay.</em></p> <p><em>A tsunami inundation will be further at a low lying area (low lying sandy beaches) compared with a coastal area which has steep slope and high relief (steep rocky beaches). Gosong beach at Pariaman which has a steep angle of beach slope will have lower tsunami height compared with a low angle beach slope like at Sungai Beramas, Kasai, Kabung, Batung and Nibung bays which have a beach slope about 3° to 5°. The maximum tsunami inundation is assumed to be located at Pasaman and Pasir Pariaman Sub-regencies, while the maximum tsunami height is assumed to be located at the middle of mapped area which has a bay shape. Tsunami is assumed to be arrived early at the southern most of mapped area or close to Muko-muko (Bengkulu).</em></p> <p><em>The maximum height difference from sea level was found at Tabai - Pariaman about 5.394 m, while the minimum height difference was found at Carocok Anau about 1.821 m. The horizontal distance measured from the nearest building from the shoreline is about 119 to 173 m.</em></p> <p><em>The worst case of tsunami modeling assumed that the maximum tsunami height will be about 32 m and used for reference to make tsunami prone zonation, such as high, moderate and low prone area.</em></p> <p> </p> <p> </p>
topic Coastal characteristics
Tsunami Prone Zonation
url https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/51
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