EROSI PANTAI PADA ZONA STABIL SEBAGAI DAMPAK REKLAMASI LOKAL DI PERAIRAN ANYER SELAT SUNDA, BANTEN

Authors

  • Delyuzar Ilhaude Pusat Penelitian dan Pengembangan Geologi Kelautan

DOI:

https://doi.org/10.33332/jgsm.geologi.v17i5.310

Abstract

The studied area is geographically located on the Sunda Strait, Banten Province,  known  as touris  area.  The erosion and sedimentation processes occur along Anyer longshore area.  The mechanism of erosion is strongly caused by the irregular pattern of longshore current and the wave difraction of which they are affected by the breakwater system in the Anyer coast.  The erosion process occurs because of the tidal wave and the maximum height is in the west monsoon in December until februari.

 

Keywords: touristarea, longshore current, erosion coast

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References

Anonim, 2002 , Stasiun Meteorologi Serang-Banten 1998-2002, Badan Meteorologi dan Geofisika. Laporan bulanan.

Bijker, E.W., 1988. An international journal for coastal, harbour and offshore engineers. Coastal Engineering, 12 (3): 285-297.

ljima and Tang F.L.W., 1967. Numerical calculation of wind wave at shallow water. Proc.10th Coastal Eng.: 3-45.

Mustafa, A., Naibaho, T., Raharjo, P., Arifin, D., llahude, 0., Aryawan, K., 2004. Penyelidikan geologi dan geofisikaperairan Selat Sunda dan sekitarnya, Kabupaten Serang Propinsi Banten. Pusat Penelitian dan PengembanganGeologi Kelautan, Laporan internal.

Sukardjono, Faturachman, A., Silitonga, F., Oewi, KT., Kurnio, H., 1989. Penyelidikan geologi dan geofisika di perairanAnyerdan sekitamya, Selat Sunda, Jawa Barat. Pusat Pengembangan Geologi Kelautan, Laporan internal.

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Published

2007-10-10

Issue

Vol. 17 No. 5 (2007): Jurnal Sumber Daya Geologi

Section

Article

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