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  • 21 Aug, 2019

  • By, Wikipedia

Kudat Peninsula
The Kudat Peninsula (Malay: Semenanjung Kudat) is a peninsula in northern of Sabah, Malaysia. It consists of high coastal with windy shorelines and swamp areas. The peninsula become the area where the South China Sea meets the Sulu Sea.

Geology

Kudat formation is originated from deep marine environment. The peninsula is geologically high flanked by deep structural depressions with the northern terrane comprises thick-bedded sandstone with interbeds of silty mudstone and contains calcareous nannofossil of Early Eocene to Middle Eocene that were deposited in deep-water setting in contrast to shallow-marine environments declared in previously published material. In the central area of the peninsula in Sikuati located an oil seep in a tidal mangrove swamp surrounded by an adjacent green area of primary and secondary vegetation.

Climate and biodiversity

The peninsula generally received mean annual rainfall ranging from 2,000 millimetres to 2,500 millimetres while part in the southern received rainfall between 2,500 millimetres to 3,000 millimetres. Together with Bengkoka Peninsula, it is part of the Tun Mustapha Marine Park which includes coral reefs conservation.

References

  1. ^ Rough Guides (6 January 2018). The Rough Guide to Malaysia, Singapore & Brunei. Apa Publications (UK) Limited. p. 618. ISBN 978-1-78919-418-0.
  2. ^ Zarinah Waheed; Harald G. J. van Mil; Muhammad Ali Syed Hussein; Robecca Jumin; Bobita Golam Ahad; Bert W. Hoeksema (2015). "Coral Reefs at the Northernmost Tip of Borneo: An Assessment of Scleractinian Species Richness Patterns and Benthic Reef Assemblages". PLOS One. 10 (12): e0146006. Bibcode:2015PLoSO..1046006W. doi:10.1371/journal.pone.0146006. PMC 4697805. PMID 26719987.
  3. ^ Samira Ghaheri; Mohd Suhaili; Nasiman Sapari; Mohammadsadegh Momeni (2017). Sedimentary architecture and depositional environment of Kudat Formation, Sabah, Malaysia. IOP Conference Series: Materials Science and Engineering, IOP Publishing. Vol. 291. p. 012025. doi:10.1088/1757-899X/291/1/012025.
  4. ^ M.B. Gassim; Sanudin Tahir; D. A. Brunotte (2003). "Tectonic evolution of the Marudu Bay, Sabah, Malaysia". Journal of Southeast Asian Earth Sciences, Department of Earth Sciences, UKM Sabah Campus. 8 (1–4): 513–527. doi:10.1016/0743-9547(93)90049-U.
  5. ^ F. Tongkul (2003). "Structural style of Kudat Peninsula, Sabah". Geology Program, School of Science and Technology, Universiti Malaysia Sabah. 29 (6): 290. Retrieved 31 May 2019 – via Geological Society of Malaysia.
  6. ^ "Forest Management Plan [2016-2025]" (PDF). 2017: 7. Archived from the original (PDF) on 9 July 2021. Retrieved 31 May 2019 – via Acacia Forest Industries. {{cite journal}}: Cite journal requires |journal= (help)
  7. ^ Ahmad Ridhwan Rahim; Zainey Konjing; Junaidi Asia; Nursyazwani Abdul Jalil; Abdul Jalil Muhamad; Norazhar Ibrahim; A. Munif Koraini; Razali Che Kob; Hisham Mazlan; H.D Tjia (2017). "Tectonostratigraphic terranes of Kudat Peninsula, Sabah" (PDF). Bulletin of the Geological Society of Malaysia, Geological Survey of Malaysia: 123 & 125. Archived from the original (PDF) on 31 May 2019. Retrieved 31 May 2019 – via Geological Society of Malaysia.
  8. ^ Nurul Izzati Azman; Siti Nur Fathiyah Jamaludin (2017). Relationship of oil seep in Kudat Peninsula with surrounding rocks based on geochemical analysis. IOP Conf. Series: Earth and Environmental Science, IOP Publishing. Vol. 88. p. 1. doi:10.1088/1755-1315/88/1/012014.
  9. ^ "Annual rainfall pattern of Sabah [Kudat Peninsula]". Government of Sabah. Retrieved 31 May 2019.
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