The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, Semarang

Recently, the main problem in Semarang City is flood. This area has low relief that consists of coastal alluvial deposits, swamp and marine sediments. The coastline is characterized by muddy, sandy, and rocky coasts, and mangrove coast. Ground Penetrating Radar (GPR) records, show that subsurface ge...

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Bibliographic Details
Main Authors: Purnomo Raharjo, Mira Yosi
Format: Article
Language:English
Published: Marine Geological Institute of Indonesia 2017-10-01
Series:Bulletin of the Marine Geology
Subjects:
Online Access:http://ejournal.mgi.esdm.go.id/index.php/bomg/article/view/351
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spelling doaj-0d6bd96d6ace4a56a1dedf469ba854dd2020-11-24T21:38:18ZengMarine Geological Institute of IndonesiaBulletin of the Marine Geology1410-61752527-88432017-10-01321298The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, SemarangPurnomo Raharjo0Mira Yosi1Marine Geological InstituteMarine Geological InstituteRecently, the main problem in Semarang City is flood. This area has low relief that consists of coastal alluvial deposits, swamp and marine sediments. The coastline is characterized by muddy, sandy, and rocky coasts, and mangrove coast. Ground Penetrating Radar (GPR) records, show that subsurface geological condition of northern part of Semarang is coastal alluvial deposit and in the south is volcanic rocks. The aims of this this research is to determine land subsidence by levelling measurement in 2005 in Tanjung Emas Harbour area built on 1995. During ten years, there are various land subsidance in this area: in Coaster Street (21 – 41 cm), container wharf (62 – 94 cm), north breakwater (64 – 79 cm), west breakwater (74 – 140 cm), east groin (76 – 89 cm), and stacking area ( 77 – 109 cm). According to this research, it is concluded that one reason causes of flooding in this area is land subsidence.http://ejournal.mgi.esdm.go.id/index.php/bomg/article/view/351floodland subsidencelevellingTanjung Emas HarbourSemarang
collection DOAJ
language English
format Article
sources DOAJ
author Purnomo Raharjo
Mira Yosi
spellingShingle Purnomo Raharjo
Mira Yosi
The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, Semarang
Bulletin of the Marine Geology
flood
land subsidence
levelling
Tanjung Emas Harbour
Semarang
author_facet Purnomo Raharjo
Mira Yosi
author_sort Purnomo Raharjo
title The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, Semarang
title_short The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, Semarang
title_full The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, Semarang
title_fullStr The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, Semarang
title_full_unstemmed The Identification of Land Subsidance by Levelling Measurement and GPR Data at Tanjung Emas Harbour, Semarang
title_sort identification of land subsidance by levelling measurement and gpr data at tanjung emas harbour, semarang
publisher Marine Geological Institute of Indonesia
series Bulletin of the Marine Geology
issn 1410-6175
2527-8843
publishDate 2017-10-01
description Recently, the main problem in Semarang City is flood. This area has low relief that consists of coastal alluvial deposits, swamp and marine sediments. The coastline is characterized by muddy, sandy, and rocky coasts, and mangrove coast. Ground Penetrating Radar (GPR) records, show that subsurface geological condition of northern part of Semarang is coastal alluvial deposit and in the south is volcanic rocks. The aims of this this research is to determine land subsidence by levelling measurement in 2005 in Tanjung Emas Harbour area built on 1995. During ten years, there are various land subsidance in this area: in Coaster Street (21 – 41 cm), container wharf (62 – 94 cm), north breakwater (64 – 79 cm), west breakwater (74 – 140 cm), east groin (76 – 89 cm), and stacking area ( 77 – 109 cm). According to this research, it is concluded that one reason causes of flooding in this area is land subsidence.
topic flood
land subsidence
levelling
Tanjung Emas Harbour
Semarang
url http://ejournal.mgi.esdm.go.id/index.php/bomg/article/view/351
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