Samudra Hindia

Sekang Wikipédia, Ènsiklopédhi Bébas basa Banyumasan: dhialék Banyumas, Tegal, Cirebon karo Jawa Serang/Banten lor.
Mlumpat maring: navigasi, goleti
Lima samudra donya

Samudra Hindia, Samudra Indonesia atawa Samudra India kuwe kumpulan banyu paling gedhe kaping telu nang donya, meliputi sekitar 20% permukaan banyu Bumi. Nang sisi lor dibatesi nang Asia bagian kidul; sisi kulon nang Jazirah Arabia lan Afrika; sisi wetan nang Semenanjung Malaya, Sumatera, Jawa, Kepulauan Sunda Kecil, lan Australia; sisi kidul nang Antartika. Samudra kiye dipisahna karo Samudra Atlantik nang 20° wetan meridian, lan karo Samudra Pasifik nang 147° wetan meridian. Samudra Hindia atawa Samudra India kuwe siji-sijine samudra sing nggunakna jeneng negara yakuwe India[1].

Data[sunting | sunting sumber]

Indian Ocean bathymetry srtm.png

Area

Dawane Pantai: 66.526 km

Titik ketinggian:

  • titik paling jero: Palung Jawa -7.258 m
  • titik paling cethek: permukaan laut 0 m

Pelabuhan: Calcutta (India), Chennai (Madras; India), Colombo (Sri Lanka), Durban (Afrika Selatan), Jakarta (Indonesia), Karachi (Pakistan), Fremantle (Australia), Mumbai (Bombay; India), Teluk Richards (Afrika Selatan)

Daftar pustaka[sunting | sunting sumber]

  • Braun, D., The Indian Ocean (1983)
  • Chandra, S., ed., The Indian Ocean (1987);
  • Chaudhuri, K. N., Trade and Civilization in the Indian Ocean (1985);
  • Cousteau, Jacques-Yves, and Diole, Philippe, Life and Death in a Coral Sea (1971);
  • Cubitt, Gerald, Islands of the Indian Ocean (1975);
  • Das Gupta, A., and Pearson, M.N., India and the Indian Ocean (1987);
  • Dowdy, W. L., and Trood, R., eds., The Indian Ocean (1985);
  • Kerr, A., ed., Resources and Development in the Indian Ocean Region (1981);
  • Nairn, A. E., and Stehli, F. G., eds., The Ocean Basins and Margins, Vol. 6: The Indian Ocean (1982);
  • Ostheimer, John M., ed., The Politics of the Western Indian Ocean Islands (1975);
  • Toussaint, Auguste, The History of the Indian Ocean, trans. by June Guicharnaud (1966).

Referensi[sunting | sunting sumber]

Deleng uga[sunting | sunting sumber]

Cithakan:Geo-stub