PROSES PENDANGKALAN DI PANTAI DAN LEPAS PANTAI CIREBON AKIBAT LAJU SEDIMENTASI ASAL DARATAN YANG TINGGI

Authors

  • D. Setyadi Pusat Penelitian dan Pengembangan Geologi Kelautan
  • Noor C.D Aryanto Pusat Penelitian dan Pengembangan Geologi Kelautan

DOI:

https://doi.org/10.33332/jgsm.geologi.v18i5.250

Abstract

The litology of Cirebon coastal area is alluvium from the Quarternary sediment. The emerged land in Cirebon coastal area is very wide due to a very flat coastal morphology and very high sedimentary in flux, especially in the river mouth area. The bat imetric map at Cirebon waters shows that the shallow water is in Kalijaga river mouth. Sediments are thicker towards Kalijaga and Sukalila river mouths. Further more, the sediment was deposited offshore and to the planning harboursites. Ingeneral, fluvial current is more dominant than longshore and marine currents and it is responsible for sedimentation along the coastalline and the river mouth.

 

Keywords: emergedland, sedimentary influx, Cirebon waters

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References

Dolan, R., Hayde, B.P., Hornberger, G., Zieman, J and Vincent, M.K., 1972. Classification of the coastal environments of the word.I.The Americas.

Faturachman, A., Purnomo R., Yuningsih, A., Yogi N., Riza, R., Catur P., Sunartono, 2002. Laporan Kajian Proses Sedimentasi Pelabuhan Cirebon, JawaBarat, Puslitbang Geologi Kelautan, Tidak Dipublikasi.

Novico, F., Setiady, D. Purnomo, R. Faturachman, A.,2006. Laporan penyelidikan Rencana Pelabuhan

Cirebon,“MarineCenterâ€. Puslitbang Geologi Kelautan.

Purnomo, R. Setiady, D., Faturachman, A., 2004. Laporan penyelidikan inventarisasi sumberdaya alam

Kabupaten Cirebon, Bappeda Kabupaten Cirebon, Laporan intern

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Published

2008-10-09

Issue

Vol. 18 No. 5 (2008): Jurnal Sumber Daya Geologi

Section

Article

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