KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG

Semarang Urban areas are underlined by tertiary rock of sandstone and plastic mudstone. Those tertiary rock are overlaid unconformly by classic sediment of Old Ungaran Volcano deposited in the late Pleistocene (22.150 years old). Fault and joint structure occurrence that is involving those volcanic...

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Main Author: Perpustakaan UGM, i-lib
Format: Article
Published: [Yogyakarta] : Universitas Gadjah Mada 2008
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author Perpustakaan UGM, i-lib
author_facet Perpustakaan UGM, i-lib
author_sort Perpustakaan UGM, i-lib
collection UGM
description Semarang Urban areas are underlined by tertiary rock of sandstone and plastic mudstone. Those tertiary rock are overlaid unconformly by classic sediment of Old Ungaran Volcano deposited in the late Pleistocene (22.150 years old). Fault and joint structure occurrence that is involving those volcanic classic rock and river terrace reaching 75 m above river bed indicate that the Semarang Urban Areas have been experiencing neo-tectonic. The tectonic activity has uplifted the southern hilly area ofBanyumanik Mijen hills with average uplift rate of 0.4 em/year. On the contrary, subsidence has been taking place within the north part of Semarang Urban areas followed by consolidation and compaction of young sediment material. The subsidence rate is predicted at about 3 -10 em/year. The tectonic process that caused uplift at southern and subsidence at northern part is controlled by Northwest - Southeast fault structure. Those geological setting has bringing about soil creep and landslide hazard in the hilly areas and tide flood (rob) in the north areas. Keywords: Semarang urban area, geological structure, mismanagement, disaster
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spelling oai:generic.eprints.org:284472014-06-18T00:24:56Z https://repository.ugm.ac.id/28447/ KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG Perpustakaan UGM, i-lib Jurnal i-lib UGM Semarang Urban areas are underlined by tertiary rock of sandstone and plastic mudstone. Those tertiary rock are overlaid unconformly by classic sediment of Old Ungaran Volcano deposited in the late Pleistocene (22.150 years old). Fault and joint structure occurrence that is involving those volcanic classic rock and river terrace reaching 75 m above river bed indicate that the Semarang Urban Areas have been experiencing neo-tectonic. The tectonic activity has uplifted the southern hilly area ofBanyumanik Mijen hills with average uplift rate of 0.4 em/year. On the contrary, subsidence has been taking place within the north part of Semarang Urban areas followed by consolidation and compaction of young sediment material. The subsidence rate is predicted at about 3 -10 em/year. The tectonic process that caused uplift at southern and subsidence at northern part is controlled by Northwest - Southeast fault structure. Those geological setting has bringing about soil creep and landslide hazard in the hilly areas and tide flood (rob) in the north areas. Keywords: Semarang urban area, geological structure, mismanagement, disaster [Yogyakarta] : Universitas Gadjah Mada 2008 Article NonPeerReviewed Perpustakaan UGM, i-lib (2008) KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG. Jurnal i-lib UGM. http://i-lib.ugm.ac.id/jurnal/download.php?dataId=11510
spellingShingle Jurnal i-lib UGM
Perpustakaan UGM, i-lib
KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG
title KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG
title_full KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG
title_fullStr KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG
title_full_unstemmed KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG
title_short KAJIAN GEOLOGI UNTUK IDENTIFIKASI BENCANA DIWILAYAH KOTA SEMARANG
title_sort kajian geologi untuk identifikasi bencana diwilayah kota semarang
topic Jurnal i-lib UGM
work_keys_str_mv AT perpustakaanugmilib kajiangeologiuntukidentifikasibencanadiwilayahkotasemarang