SUMBER DAYA ALAM DI KAWASAN PESISIR PULAU NUSA PENIDA DAN SEKITARNYA, KABUPATEN KLUNGKUNG, NUSA TENGGARA BARAT

Authors

  • P. Astjario Pusat Penelitian dan Pengembangan Geologi Kelautan

DOI:

https://doi.org/10.33332/jgsm.geologi.v18i6.256

Abstract

Nusa Penida, Lembongan and Ceningan islands consist of Pliocene reef limestone at some place. The limestone forms dolomite characterized, white in color and soft. The southern coastal of Nusa Penida Island exposed bedded limestone, re-crystallization and weakened. Karts topography widely spread in this island, however it has been eroded.

The coastal zone of Nusa Penida, Lembongan and Ceningan islands have been utilized for sea water tourism and sea grass cultivation. However, these areas still have various renewable energy resources which have not yet been developed optimally. In order to support Renewable Energy Park Programs in Nusa Penida, the current energy of Ceningan strait can be used for electricity power energy.

 

Keywords: coastal, renewable energy, current and limestone.

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References

Astjario, P., 1995. Buku Panduan Penelitian Pantai Dengan Permasalahannya, Sie Geol. Wil. Pantai, Bid. Geol. Kelautan, Pusat Pengembangan Geologi Kelautan.

Dolan, R. Hayden, B.P., Hornberger, G., Zeiman J., and Vincent, M.K., 1972. Classification of the coastal environment of the wold. 1. The Americas charlottesville, Va: Department of environmentals Sciences, University of Virginia, Tech.Rept. 1, 163 p.

Lovelock, C., 1993. Field guide to the Mangroves of Queensland, Published by the Australian Institute of Marine Science.

Suprapto, TA., 2007. Buku Pegangan Pengolahan Data Digital Citra untuk Pemetaan Geologi Lingkungan Pesisir Dengan Perangkat Lunak ER Mapper, Bid.Prog.Inf, Puslitbang Geologi Kelautan.

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Published

2008-12-01

Issue

Vol. 18 No. 6 (2008): Jurnal Sumber Daya Geologi

Section

Article

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