Tsunami Evidence in South Coast Java, Case Study: Tsunami Deposit along South Coast of Cilacap

2nd Transdisciplinary Research on Environmental Problems in Southeast Asia

地球科学;生态环境科学

Rizal, Yan^1 ; Aswan^1 ; Zaim, Yahdi^1 ; Santoso, Wahyu Dwijo^1 ; Rochim, Nur^1 ; Daryono^2 ; Anugrah, Suci Dewi^2 ; Wijayanto^2 ; Gunawan, Indra^2 ; Yatimantoro, Tatok^2 ; Hidayanti^2 ; Rahayu, Resti Herdiyani^2 ; Priyobudi^2

Geology Department, Institute of Technology Bandung (ITB), Jl. Ganesha 10, Bandung

40132, Indonesia^1

Tsunami Mitigation Division-Meteorological Climatological and Geophysical Agency (BMKG), Jakarta, Indonesia^2

关键词: Active tectonics;    Cilacap;    Dating;    Earthquake activity;    Paleotsunami layers;    Random grains;    Tsunami deposits;    Tsunami hazards;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/71/1/012001/pdf
DOI  :  10.1088/1755-1315/71/1/012001

学科分类：环境科学（综合）

来源: IOP

【 摘 要 】

Cilacap Area is situated in coastal area of Southern Java and directly affected by tsunami hazard in 2006. This event was triggered by active subduction in Java Trench which active since long time ago. To detect tsunami and active tectonic in Southern Java, paleo-tsunami study is performed which is targeted paleo-tsunami deposit older than fifty years ago. During 2011 - 2016, 16 locations which suspected as paleo-tsunami location were visited and the test-pits were performed to obtain characteristic and stratigraphy of paleo-tsunami layers. Paleo-tsunami layer was identified by the presence of light-sand in the upper part of paleo-soil, liquefaction fine grain sandstone, and many rip-up clast of mudstone. The systematic samples were taken and analysis (micro-fauna, grainsize and dating analysis). Micro-fauna result shows that paleo-tsunami layer consist of benthonic foraminifera assemblages from different bathymetry and mixing in one layer. Moreover, grainsize shows random grain distribution which characterized as turbulence and strong wave deposit. Paleo-tsunami layers in Cilacap area are correlated using paleo-soil as marker. There are three paleo-tsunami layers and the distribution can be identified as PS-A, PS-B and PS-C. The samples which were taken in Glempang Pasir layer are being dated using Pb - Zn (Lead-Zinc) method. The result of Pb - Zn (Lead-Zinc) dating shows that PS-A was deposited in 139 years ago, PS-B in 21 years ago, and PS C in 10 years ago. This result indicates that PS -1 occurred in 1883 earthquake activity while PS B formed in 1982 earthquake and PS-C was formed by 2006 earthquake. For ongoing research, the older paleo-tsunami layers were determined in the Gua Nagaraja, close to Selok location and 6 layers of Paleo-tsunami suspect found which shown a similar characteristic with the layers from another location. The three layers deeper approximately have an older age than another location in Cilacap.