
Kisar, also known as Yotowawa, is a small island in the Southwestern Moluccas in Indonesia, located to the northeast of Timor Island. The island now forms two districts ("North Kisar" and "South Kisar") within the Southwest Islands Regency of Maluku Province. South Kisar District was previously called Kecamatan Pulau Pulau Terselatan and at one time included the larger (but less populated) Roma or Romang Island further north, but this with its own outliers was subsequently split off to form its own district (Kecamatan Kepulauan Roma). The rest of the island forms the North Kisar District (Keca
Kisar, also known as Yotowawa, is a small island in the Southwestern Moluccas in Indonesia, located to the northeast of Timor Island. The island now forms two districts ("North Kisar" and "South Kisar") within the Southwest Islands Regency of Maluku Province. South Kisar District was previously called Kecamatan Pulau Pulau Terselatan and at one time included the larger (but less populated) Roma or Romang Island further north, but this with its own outliers was subsequently split off to form its own district (Kecamatan Kepulauan Roma). The rest of the island forms the North Kisar District (Kecamatan Kisar Utara) within the regency. It is one of the 92 officially listed outlying islands of Indonesia. The principal town is Wonreli, with 6,652 inhabitants at the 2010 Census.
==Geography, geology and ecology== Kisar is similar geographically and geologically to the nearby islands of Timor, Leti, and Moa. The interior of the island is hilly, with several small mountains lined roughly east–west. The highest of these, Gunung Taitulu, rises approximately above sea level, and from the top, nearby Wetar and Timor are easily seen. The entire island is encircled by a series of rugged limestone cliffs that look like giant stairsteps rising from the coast. These uplifted terraces represent former coral reefs that have been thrust from the sea due to the active tectonics of the region. Those terraces are also gently warped. An uplift rate of the island of approximately 0.5 mm/yr over the past several hundred thousand years has been calculated by obtaining ages of coral samples from the terraces.
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