Geography of Indonesia: Difference between revisions

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{{Short description|none}} <!-- "none" is preferred when the title is sufficiently descriptive; see [[WP:SDNONE]] -->
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{{EngvarB|date=September 2015}}
{{EngvarB|date=September 2014}}
{{Use dmy dates|date=May 2020}}
{{Use dmy dates|date=May 2023}}
{{Country geography
{{Country geography
|name= Indonesia
| name = Indonesia
|map= Indonesia relief location map.jpg|map size=250
| map = Indonesia relief location map.jpg
|continent= [[Asia]] and [[Oceania]]|region=[[Southeast Asia]]
| map size = 250
|coordinates= {{Coord|5.000|S|120.000|E}}
| continent = [[Asia]]
|area ranking= 14th|km area=1,904,569<ref name="CIA">[https://www.cia.gov/the-world-factbook/countries/indonesia/ CIA World Factbook]</ref>
| region = [[Southeast Asia]]
|percent land= 23.62
| coordinates = {{Coord|5.000|S|120.000|E}}
| percent water           = 76.38
| area ranking = 14th
|km coastline=54720
| km area = 1,904,569<ref name="CIA">[https://web.archive.org/web/20260118180205/https://www.cia.gov/the-world-factbook/countries/indonesia/ CIA World Factbook]</ref>
|borders= [[Malaysia]]: {{convert|2019|km|mi|0|abbr=on}}<br />[[Papua New Guinea]]: {{convert|824|km|mi|0|abbr=on}}<br />[[East Timor]]: {{convert|253|km|mi|0|abbr=on}}|highest point=[[Puncak Jaya]] (Carstensz Pyramid)<br />{{convert|4884|m|ft|0|abbr=on}}
| percent land = 23.62
|lowest point= Sea level<br />{{convert|0|m|ft|0|abbr=on}}
| percent water = 76.38
|longest river= [[Kapuas River]]<br />{{convert|1143|km|mi|0|abbr=on}}
| km coastline = 54720
|largest lake= [[Lake Toba]]<br />{{convert|1130|km2|sqmi|0|abbr=on}}
| borders = [[Malaysia]]: {{convert|2019|km|mi|0|abbr=on}}<br />[[Papua New Guinea]]: {{convert|824|km|mi|0|abbr=on}}<br />[[East Timor]]: {{convert|253|km|mi|0|abbr=on}}
|climate= Mostly [[Tropical rainforest climate|tropical rainforest]] (''Af''), Southeastern part is predominantly [[Tropical savanna climate|tropical savanna]] (''Aw''), while some parts of [[Java]] and [[Sulawesi]] are [[Tropical monsoon climate|tropical monsoon]] (''Am'')
| highest point = [[Puncak Jaya]] (Carstensz Pyramid)<br />{{convert|4884|m|ft|0|abbr=on}}
|terrain= Plain in most part of [[Kalimantan]], southern [[New Guinea]], eastern [[Sumatra]] and northern Java; Rugged, volcanic topography in Sulawesi, western Sumatra, southern Java, [[Lesser Sunda Islands]] and [[Maluku Islands]]; Rugged mountains in central, northwestern New Guinea and northern Kalimantan
| lowest point = Sea level<br />{{convert|0|m|ft|0|abbr=on}}
|natural resources= Arable land, coal, petroleum, natural gas, timber, copper, lead, phosphates, uranium, bauxite, gold, iron, mercury, nickel, silver
| longest river = [[Kapuas River]]<br />{{convert|1143|km|mi|0|abbr=on}}
|natural hazards= Tsunamis; volcanoes; earthquake activity except in central part; tropical cyclones along the [[Indian Ocean|Indian]] coasts; mud slides in Java; flooding
| largest lake = [[Lake Toba]]<br />{{convert|1130|km2|sqmi|0|abbr=on}}
|environmental issues= Severe [[deforestation]], air pollution resulting in acid rain, river pollution
| climate = Mostly [[Tropical rainforest climate|tropical rainforest]] (''Af''), Southeastern part is predominantly [[Tropical savanna climate|tropical savanna]] (''Aw''), while some parts of [[Java]] and [[Sulawesi]] are [[Tropical monsoon climate|tropical monsoon]] (''Am'')
|exclusive economic zone= {{convert|6159032|km2|mi2|abbr=on}}
| terrain = Plain in most part of [[Kalimantan]], southern [[New Guinea]], eastern [[Sumatra]] and northern Java; Rugged, volcanic topography in Sulawesi, western Sumatra, southern Java, [[Lesser Sunda Islands]] and [[Maluku Islands]]; Rugged mountains in central, northwestern New Guinea and northern Kalimantan
| natural resources = Arable land, coal, petroleum, natural gas, timber, copper, lead, phosphates, uranium, bauxite, gold, iron, mercury, nickel, silver
| natural hazards = Tsunamis; volcanoes; earthquake activity except in central part; tropical cyclones along the [[Indian Ocean|Indian]] coasts; mud slides in Java; flooding
| environmental issues = Severe [[deforestation]], air pollution resulting in acid rain, river pollution
| exclusive economic zone = {{convert|6159032|km2|mi2|abbr=on}}
}}
}}
[[Indonesia]] is an [[Island country|archipelagic country]] located in [[Southeast Asia]] and [[Oceania]], lying between the [[Indian Ocean]] and the [[Pacific Ocean]]. It is located in a strategic location astride or along major sea lanes connecting [[East Asia]], [[South Asia]] and [[Oceania]]. Indonesia is the largest [[archipelago]] in the world.<ref name="world-atlas"/> Indonesia's various regional cultures have been shaped—although not specifically determined—by centuries of complex interactions with its physical environment.
[[Indonesia]] is an [[Island country|archipelagic country]] located in [[Southeast Asia]], lying between the [[Indian Ocean]] and the [[Pacific Ocean]]. It is located in a strategic location astride or along major sea lanes connecting [[East Asia]], [[South Asia]] and [[Oceania]]. Indonesia is the largest [[archipelago]] in the world.<ref name="world-atlas"/> Indonesia's various regional cultures have been shaped—although not specifically determined—by centuries of complex interactions with its physical environment.


==Overview==
==Overview==
{{main|Indonesian Archipelago|List of islands of Indonesia}}
{{main|Indonesian Archipelago|List of islands of Indonesia}}
Indonesia is an archipelagic country extending about {{convert|5120|km|0}} from east to west and {{convert|1760|km|0}} from north to south.<ref>{{Cite book |last1=Frederick|first1=William H. |last2=Worden |first2=Robert L. |title=Indonesia: A Country Study |series=Area Handbook Series |volume=550 |date=1993 |page=98 |url=https://books.google.com/books?id=6dgmXWMgWcwC&pg=PA98 |publisher=Federal Research Division, Library of Congress |location=Washington, D.C. |language=en|isbn=9780844407906 }}</ref> It is considered to be the largest archipelagic country in the world. According to a geospatial survey conducted between 2007 and 2010 by [[Badan Informasi Geospasial|National Coordinating Agency for Survey and Mapping]] (Bakosurtanal), Indonesia has 17,500 islands.<ref name="NG-Indonesia-Island">{{cite news| title = Hanya ada 13.466 Pulau di Indonesia| date = 8 February 2012 | work = National Geographic Indonesia |url=https://nationalgeographic.grid.id/read/13281675/hanya-ada-13466-pulau-di-indonesia | language=id}}</ref> While earlier survey conducted in 2002 by [[National Institute of Aeronautics and Space]] (LAPAN) stated Indonesia has 18,307 islands. According to the CIA World Factbook, there are 17,508 islands.<ref name="CIA">[https://www.cia.gov/the-world-factbook/countries/indonesia/ CIA World Factbook]</ref> The discrepancy between the surveys is likely caused by the earlier different survey method including [[tide|tidal]] islands, sandy [[cay]]s and rocky [[reef]]s that surface during low tide and submerge during high tide. There are 8,844 named islands according to estimates made by the [[Politics of Indonesia|government of Indonesia]], with 922 of those being permanent. It comprises five main islands: [[Sumatra]], [[Java (island)|Java]], [[Borneo]] (known as ''[[Kalimantan]]'' in Indonesia), [[Sulawesi]], and [[New Guinea]]; two major island groups ([[Nusa Tenggara]] and the [[Maluku Islands]]) and sixty smaller island groups. Four of the islands are shared with other countries: Borneo is shared with [[Malaysia]] and [[Brunei]]; [[Sebatik]], located off the northeastern coast of Kalimantan, shared with Malaysia; [[Timor]] is shared with [[East Timor]]; and [[New Guinea]] is shared with [[Papua New Guinea]].
Indonesia is an archipelagic country extending about {{convert|5120|km|0}} from east to west and {{convert|1760|km|0}} from north to south.<ref>{{Cite book |last1=Frederick|first1=William H. |last2=Worden |first2=Robert L. |title=Indonesia: A Country Study |series=Area Handbook Series |volume=550 |date=1993 |page=98 |url=https://books.google.com/books?id=6dgmXWMgWcwC&pg=PA98 |publisher=Federal Research Division, Library of Congress |location=Washington, D.C. |language=en|isbn=9780844407906 }}</ref> It is considered to be the largest archipelagic country in the world. According to a geospatial survey conducted between 2007 and 2010 by [[Badan Informasi Geospasial|National Coordinating Agency for Survey and Mapping]] (Bakosurtanal), Indonesia has 17,500 islands,<ref name="NG-Indonesia-Island">{{cite news| title = Hanya ada 13.466 Pulau di Indonesia| date = 8 February 2012 | work = National Geographic Indonesia |url=https://nationalgeographic.grid.id/read/13281675/hanya-ada-13466-pulau-di-indonesia | language=id}}</ref> while an earlier survey conducted in 2002 by [[National Institute of Aeronautics and Space]] (LAPAN) stated Indonesia has 18,307 islands. According to the CIA World Factbook, there are 17,508 islands.<ref name="CIA">[https://web.archive.org/web/20260118180205/https://www.cia.gov/the-world-factbook/countries/indonesia/ CIA World Factbook]</ref> The discrepancy between the surveys is likely caused by the earlier different survey method including [[tide|tidal]] islands, sandy [[cay]]s and rocky [[reef]]s that surface during low tide and submerge during high tide. There are 8,844 named islands according to estimates made by the [[Politics of Indonesia|government of Indonesia]], with 922 of those being permanent. Indonesia comprises five main islands: [[Sumatra]], [[Java (island)|Java]], [[Borneo]] (known as ''[[Kalimantan]]'' in Indonesia), [[Sulawesi]], and [[New Guinea]]; two major island groups ([[Nusa Tenggara]] and the [[Maluku Islands]]) and sixty smaller island groups. Four of the islands are shared with other countries: Borneo is shared with [[Malaysia]] and [[Brunei]]; [[Sebatik]], located off the northeastern coast of Kalimantan, is shared with Malaysia; [[Timor]] is shared with [[East Timor]]; and [[New Guinea]] is shared with [[Papua New Guinea]].


Indonesia has total land area of {{convert|1904569|km2|0}}, including {{convert|93000|km2|0}} of inland seas ([[strait]]s, [[bay]]s, and other bodies of water). This makes it the largest [[List of island countries|island country]] in the world.<ref name="world-atlas">{{cite web|url=https://www.worldatlas.com/articles/which-are-the-island-countries-of-the-world.html |title=Island Countries of the World |publisher=WorldAtlas.com |access-date=2019-08-10 |archive-url=https://web.archive.org/web/20171207094959/http://www.worldatlas.com/articles/which-are-the-island-countries-of-the-world.html | archive-date=2017-12-07}}</ref> The additional surrounding sea areas bring Indonesia's generally recognised territory (land and sea) to about 5 million km<sup>2</sup>. The government claims an [[Exclusive economic zone of Indonesia|exclusive economic zone]] of {{convert|6159032|km2|mi2|abbr=on}}. This brings the total area to about 7.9 million km<sup>2</sup>.<ref>{{Cite book|url=https://books.google.com/books?id=E5NafsG5RiEC&q=Indonesia+land+sea+total+area&pg=PA99|title=Prevention and Compensation of Marine Pollution Damage: Recent Developments in Europe, China and the US|last=Faure|first=Michael G.|date=2006|publisher=Kluwer Law International|isbn=9789041123381|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=6dgmXWMgWcwC&q=Indonesia+total+sea+area&pg=PR32|title=Indonesia: A Country Study|last1=Frederick|first1=William H.|last2=Worden|first2=Robert L.|date=2011|publisher=Government Printing Office|isbn=9780844407906|language=en}}</ref>
Indonesia has total land area of {{convert|1904569|km2|0}}, including {{convert|93000|km2|0}} of inland seas ([[strait]]s, [[bay]]s, and other bodies of water). This makes it the largest [[List of island countries|island country]] in the world.<ref name="world-atlas">{{cite web|url=https://www.worldatlas.com/articles/which-are-the-island-countries-of-the-world.html |title=Island Countries of the World |publisher=WorldAtlas.com |access-date=2019-08-10 |archive-url=https://web.archive.org/web/20171207094959/http://www.worldatlas.com/articles/which-are-the-island-countries-of-the-world.html | archive-date=2017-12-07}}</ref> The additional surrounding sea areas bring Indonesia's generally recognised territory (land and sea) to about 5 million km<sup>2</sup>. The government claims an [[Exclusive economic zone of Indonesia|exclusive economic zone]] of {{convert|6159032|km2|mi2|abbr=on}}. This brings the total area to about 7.9 million km<sup>2</sup>.<ref>{{Cite book|url=https://books.google.com/books?id=E5NafsG5RiEC&q=Indonesia+land+sea+total+area&pg=PA99|title=Prevention and Compensation of Marine Pollution Damage: Recent Developments in Europe, China and the US|last=Faure|first=Michael G.|date=2006|publisher=Kluwer Law International|isbn=9789041123381|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=6dgmXWMgWcwC&q=Indonesia+total+sea+area&pg=PR32|title=Indonesia: A Country Study|last1=Frederick|first1=William H.|last2=Worden|first2=Robert L.|date=2011|publisher=Government Printing Office|isbn=9780844407906|language=en}}</ref>


Indonesia is a transcontinental country, where its territory consisted of islands geologically considered as part of either [[Asia]] or [[Australia (continent)|Australia]]. During the [[Pleistocene]], the [[Greater Sunda Islands]] were connected to the Asian mainland while New Guinea was connected to Australia.<ref>{{Cite book|url=https://books.google.com/books?id=VWnxpAxp6TMC&q=Sundaland+Pleistocene&pg=PA70|title=Encyclopedia of Coastal Science|last=Schwartz|first=Maurice|date=2006-11-08|publisher=Springer Science & Business Media|isbn=9781402038808|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=u-k1CwAAQBAJ&q=Sundaland+Pleistocene&pg=PA237|title=Geology and Archaeology: Submerged Landscapes of the Continental Shelf|last1=Harff|first1=J.|last2=Bailey|first2=G.|last3=Lüth|first3=F.|date=2016-01-05|publisher=Geological Society of London|isbn=9781862396913|language=en}}</ref> [[Karimata Strait]], [[Java Sea]] and [[Arafura Sea]] were formed as the [[sea level rise|sea level rose]] at the end of the Pleistocene.
During the [[Pleistocene]], the [[Greater Sunda Islands]] were connected to the Asian mainland while New Guinea was connected to Australia.<ref>{{Cite book|url=https://books.google.com/books?id=VWnxpAxp6TMC&q=Sundaland+Pleistocene&pg=PA70|title=Encyclopedia of Coastal Science|last=Schwartz|first=Maurice|date=2006-11-08|publisher=Springer Science & Business Media|isbn=9781402038808|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=u-k1CwAAQBAJ&q=Sundaland+Pleistocene&pg=PA237|title=Geology and Archaeology: Submerged Landscapes of the Continental Shelf|last1=Harff|first1=J.|last2=Bailey|first2=G.|last3=Lüth|first3=F.|date=2016-01-05|publisher=Geological Society of London|isbn=9781862396913|language=en}}</ref> [[Karimata Strait]], [[Java Sea]] and [[Arafura Sea]] were formed as the [[sea level rise|sea level rose]] at the end of the Pleistocene.


==Geology==
==Geology==
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[[File:Plate setting Sunda megathrust.png|thumb|left|330x330px|The tectonic plates & movements under Indonesia]]
[[File:Plate setting Sunda megathrust.png|thumb|left|330x330px|The tectonic plates & movements under Indonesia]]


The main islands of Sumatra, Java, [[Madura]], and Kalimantan lie on the [[Sunda plate]] and geographers have conventionally grouped them, (along with Sulawesi), as the [[Greater Sunda Islands]]. At Indonesia's eastern extremity is western New Guinea, which lies on the [[Australian plate]]. Sea depths in the Sunda and Sahul shelves average {{convert|300|m|0}} or less. Between these two shelves lie Sulawesi, Nusa Tenggara (also known as the [[Lesser Sunda Islands]]), and the [[Maluku Islands]] (or the Moluccas), which form a second island group with deep, surrounding seas down to {{convert|4500|m|0}} in depth. The term "Outer Islands" is used inconsistently by various writers but it is usually taken to mean those islands other than Java and Madura.
The main islands of Sumatra, Java, [[Madura]], and Kalimantan lie on the [[Sunda plate]] and geographers have conventionally grouped them, (along with Sulawesi), as the [[Greater Sunda Islands]]. At Indonesia's eastern extremity is western New Guinea, which lies on the [[Australian plate]]. Sea depths in the Sunda and Sahul shelves average {{convert|300|m|0}} or less. Between these two shelves lie Sulawesi, Nusa Tenggara (also known as the [[Lesser Sunda Islands]]), and the [[Maluku Islands]] (or the Moluccas), which form a second island group with deep, surrounding seas down to {{convert|4500|m|0}} in depth. The term "Outer Islands" is used inconsistently by various writers, but it is usually taken to mean those islands other than Java and Madura.


Sulawesi is an island lies on three separate plates, the [[Banda Sea plate]], [[Molucca Sea plate]], and Sunda plate. Seismic and volcanic activities are high on its northeastern part, evidenced by the formation of volcanoes in [[North Sulawesi]] and island arcs such as the [[Sangihe Islands|Sangihe]] and [[Talaud Islands]], southwest of the [[Philippine Trench]].<ref>{{Cite book|url=https://books.google.com/books?id=eilFDwAAQBAJ&q=Mindanao+North+Sulawesi+Arc&pg=PT190|title=Mountains: The origins of the Earth's mountain systems|last=Park|first=Graham|date=2018-01-03|publisher=Dunedin Academic Press|isbn=9781780465791|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=S68JAQAAIAAJ&q=North+Sulawesi+tectonics|title=The Geology and Tectonics of Eastern Indonesia: Proceedings of the Ccop-Ioc Seatar Working Group Meeting, Bandung, Indonesia, 9–14 July 1979|last=Wiryosujono|first=S.|date=1981|publisher=Pergamon Press|isbn=9780080287324|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=FyQUAQAAIAAJ&q=Sangihe+Talaud+Philippine+Trench|title=Tectonic Evolution of Southeast Asia|last1=Hall|first1=Robert|last2=Blundell|first2=Derek John|date=1996|publisher=Geological Society|isbn=9781897799529|language=en}}</ref>
Sulawesi is an island that lies on three separate plates, the [[Banda Sea plate]], [[Molucca Sea plate]], and Sunda plate. Seismic and volcanic activities are high on its northeastern part, evidenced by the formation of volcanoes in [[North Sulawesi]] and island arcs such as the [[Sangihe Islands|Sangihe]] and [[Talaud Islands]], southwest of the [[Philippine Trench]].<ref>{{Cite book|url=https://books.google.com/books?id=eilFDwAAQBAJ&q=Mindanao+North+Sulawesi+Arc&pg=PT190|title=Mountains: The origins of the Earth's mountain systems|last=Park|first=Graham|date=2018-01-03|publisher=Dunedin Academic Press|isbn=9781780465791|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=S68JAQAAIAAJ&q=North+Sulawesi+tectonics|title=The Geology and Tectonics of Eastern Indonesia: Proceedings of the Ccop-Ioc Seatar Working Group Meeting, Bandung, Indonesia, 9–14 July 1979|last=Wiryosujono|first=S.|date=1981|publisher=Pergamon Press|isbn=9780080287324|language=en}}</ref><ref>{{Cite book|url=https://books.google.com/books?id=FyQUAQAAIAAJ&q=Sangihe+Talaud+Philippine+Trench|title=Tectonic Evolution of Southeast Asia|last1=Hall|first1=Robert|last2=Blundell|first2=Derek John|date=1996|publisher=Geological Society|isbn=9781897799529|language=en}}</ref>


Nusa Tenggara or Lesser Sunda Islands consists of two strings of islands stretching eastward from Bali toward southern Maluku. The inner arc of Nusa Tenggara is a continuation of the [[Alpide belt]] chain of mountains and volcanoes extending from Sumatra through Java, Bali, and Flores, and trailing off in the volcanic [[Banda Islands]], which along with the [[Kai Islands]] and the [[Tanimbar Islands]] and other small islands in the [[Banda Sea]] are typical examples of the [[Wallacea]] mixture of Asian and Australasian plant and animal life.<ref>{{WWF ecoregion|id=aa0102|name=Banda Sea Islands moist deciduous forests}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref> The outer arc of Nusa Tenggara is a geological extension of the chain of islands west of Sumatra that includes Nias, Mentawai, and Enggano. This chain resurfaces in Nusa Tenggara in the ruggedly mountainous islands of Sumba and Timor.
Nusa Tenggara consists of two strings of islands stretching eastward from Bali toward southern Maluku. The inner arc of Nusa Tenggara is a continuation of the [[Alpide belt]] chain of mountains and volcanoes extending from Sumatra through Java, Bali, and Flores, and trailing off in the volcanic [[Banda Islands]], which along with the [[Kai Islands]] and the [[Tanimbar Islands]] and other small islands in the [[Banda Sea]] are typical examples of the [[Wallacea]] mixture of Asian and Australasian plant and animal life.<ref>{{WWF ecoregion|id=aa0102|name=Banda Sea Islands moist deciduous forests}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref> The outer arc of Nusa Tenggara is a geological extension of the chain of islands west of Sumatra that includes Nias, Mentawai, and Enggano. This chain resurfaces in Nusa Tenggara in the ruggedly mountainous islands of Sumba and Timor.
[[File:Erupsi Gunung Sinabung 9 Juni 2019 oleh Muh Ma'rufin Sudibyo.jpg|thumb|upright|2019 eruption of [[Mount Sinabung|Sinabung]] in [[North Sumatra]]. Sinabung is one of the most active volcanoes in Indonesia.]]
[[File:Erupsi Gunung Sinabung 9 Juni 2019 oleh Muh Ma'rufin Sudibyo.jpg|thumb|upright|2019 eruption of [[Mount Sinabung|Sinabung]] in [[North Sumatra]]. Sinabung is one of the most active volcanoes in Indonesia.]]
The Maluku Islands (or Moluccas) are geologically among the most complex of the Indonesian islands, consisted of four different tectonic plates. They are located in the northeast sector of the archipelago, bounded by the Philippine Sea to the north, Papua to the east, and Nusa Tenggara to the southwest. The largest of these islands include [[Halmahera]], [[Seram]] and [[Buru]], all of which rise steeply out of very deep seas and have unique Wallacea vegetation.<ref>{{WWF ecoregion|id=aa0104|name=Terrestrial Ecoregions - Buru rain forests (AA0104)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref> This abrupt relief pattern from sea to high mountains means that there are very few level coastal plains. To the south lies the [[Banda Sea]]. The convergence between the Banda Sea plate and Australian plate created a chain of volcanic islands called the [[Banda Arc]].<ref>Carter, D. J., Audley-Charles, M. G. & Barber, A. J. Stratigraphical analysis of island arc-continental margin collision in eastern Indonesia. J. Geol. Soc. Lond. 132, 179-189 (1976).</ref><ref>Hamilton, W. Tectonics of the Indonesian Region Vol. 1078 (US Geol. Soc. Prof. Pap., 1979).</ref> The sea also contains the Weber Deep, one of the deepest point in Indonesia.<ref>{{Cite book|url=https://books.google.com/books?id=62zMI9P4Vv8C&q=%22Weber+Deep%22+Banda+Sea+deepest&pg=PA272|title=Ecosystems of the Deep Oceans|last=Tyler|first=P. A.|date=2003-03-27|publisher=Elsevier|isbn=9780080494654|language=en}}</ref><ref>{{Cite news|url=http://www.thejakartapost.com/life/2016/11/29/biggest-exposed-fault-on-earth-found-in-eastern-indonesia.html|title=Biggest exposed fault on earth found in eastern Indonesia|date=29 November 2016|work=The Jakarta Post|access-date=2018-02-17|language=en}}</ref>
The Maluku Islands (or Moluccas) are geologically among the most complex of the Indonesian islands, consisted of four different tectonic plates. They are located in the northeast sector of the archipelago, bounded by the Philippine Sea to the north, Papua to the east, and Nusa Tenggara to the southwest. The largest of these islands include [[Halmahera]], [[Seram]] and [[Buru]], all of which rise steeply out of very deep seas and have unique Wallacea vegetation.<ref>{{WWF ecoregion|id=aa0104|name=Terrestrial Ecoregions - Buru rain forests (AA0104)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref> This abrupt relief pattern from sea to high mountains means that there are very few level coastal plains. To the south lies the [[Banda Sea]]. The convergence between the Banda Sea plate and Australian plate created a chain of volcanic islands called the [[Banda Arc]].<ref>Carter, D. J., Audley-Charles, M. G. & Barber, A. J. Stratigraphical analysis of island arc-continental margin collision in eastern Indonesia. J. Geol. Soc. Lond. 132, 179-189 (1976).</ref><ref>Hamilton, W. Tectonics of the Indonesian Region Vol. 1078 (US Geol. Soc. Prof. Pap., 1979).</ref> The sea also contains the Weber Deep, one of the deepest point in Indonesia.<ref>{{Cite book|url=https://books.google.com/books?id=62zMI9P4Vv8C&q=%22Weber+Deep%22+Banda+Sea+deepest&pg=PA272|title=Ecosystems of the Deep Oceans|last=Tyler|first=P. A.|date=2003-03-27|publisher=Elsevier|isbn=9780080494654|language=en}}</ref><ref>{{Cite news|url=http://www.thejakartapost.com/life/2016/11/29/biggest-exposed-fault-on-earth-found-in-eastern-indonesia.html|title=Biggest exposed fault on earth found in eastern Indonesia|date=29 November 2016|work=The Jakarta Post|access-date=2018-02-17|language=en}}</ref>
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===Tectonism and volcanism===
===Tectonism and volcanism===
{{main|Volcanoes of Indonesia}}
{{main|Volcanoes of Indonesia}}
Most of the larger islands are mountainous, with peaks ranging between {{convert|2000|and|3800|m|0}} meters above sea level in Sumatra, Java, Bali, Lombok, Sulawesi, and Seram.<ref>{{Cite book|url=https://books.google.com/books?id=GwRWAAAAYAAJ&q=Indonesia+landform+mountain+range|title=Focus on Indonesia|date=1976|publisher=Information Division, Embassy of Indonesia|language=en}}</ref> The country's tallest mountains are located in the [[Jayawijaya Mountains]] and the [[Sudirman Range]] in Papua. The highest peak, [[Puncak Jaya]] ({{convert|4884|m|0}}), is located in the Sudirman Mountains. A string of volcanoes stretches from Sumatra to Nusa Tenggara,<ref>{{cite book|title=Indonesia|last=Witton|first=Patrick|publisher=Lonely Planet|year=2003|isbn=1-74059-154-2|location=Melbourne|page=38}}</ref> and then loops around through to the [[Banda Islands]] of Maluku to northeastern Sulawesi. Of the 400 volcanoes, approximately 150 are active.<ref name="gvp">{{cite web|url=http://www.volcano.si.edu/world/region.cfm?rnum=06&rpage=list|title=Volcanoes of Indonesia|work=[[Global Volcanism Program]]|publisher=[[Smithsonian Institution]]|access-date=25 March 2007}}</ref> Two of the most violent volcanic eruptions in modern times occurred in Indonesia; in 1815 [[Mount Tambora]] in [[Sumbawa]] erupted killing 92,000 and in 1883, [[Krakatau]], erupted killing 36,000. While volcanic ashes resulted from eruption has positive effects for the fertility of the surrounding soils, it also makes agricultural conditions unpredictable in some areas.
Most of the larger islands are mountainous, with peaks ranging between {{convert|2000|and|3800|m|0}} meters above sea level in Sumatra, Java, Bali, Lombok, Sulawesi, and Seram.<ref>{{Cite book|url=https://books.google.com/books?id=GwRWAAAAYAAJ&q=Indonesia+landform+mountain+range|title=Focus on Indonesia|date=1976|publisher=Information Division, Embassy of Indonesia|language=en}}</ref> The country's tallest mountains are located in the [[Jayawijaya Mountains]] and the [[Sudirman Range]] in Papua. The highest peak, [[Puncak Jaya]] ({{convert|4884|m|0}}), is located in the Sudirman Mountains. A string of volcanoes stretches from Sumatra to Nusa Tenggara,<ref>{{cite book|title=Indonesia|last=Witton|first=Patrick|publisher=Lonely Planet|year=2003|isbn=1-74059-154-2|location=Melbourne|page=38}}</ref> then loops around through to the [[Banda Islands]] of Maluku to northeastern Sulawesi. Of the 400 volcanoes, approximately 150 are active.<ref name="gvp">{{cite web|url=http://www.volcano.si.edu/world/region.cfm?rnum=06&rpage=list|title=Volcanoes of Indonesia|work=[[Global Volcanism Program]]|publisher=[[Smithsonian Institution]]|access-date=25 March 2007}}</ref> Two of the most violent volcanic eruptions in modern times occurred in Indonesia; in 1815, [[Mount Tambora]] in [[Sumbawa]] erupted, killing 92,000, and in 1883, [[Krakatau]] erupted, killing 36,000. While volcanic ashes resulted from eruption has positive effects for the fertility of the surrounding soils, it also makes agricultural conditions unpredictable in some areas.


[[Image:Map indonesia volcanoes.gif|thumb|446x446px|A map of [[List of volcanoes in Indonesia|Indonesia's volcanoes]].]]
[[Image:Map indonesia volcanoes.gif|thumb|446x446px|A map of [[List of volcanoes in Indonesia|Indonesia's volcanoes]].]]
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== Ecology ==
== Ecology ==
{{see also|List of ecoregions in Indonesia|Biodiversity of Borneo|Deforestation in Indonesia}}
{{see also|List of ecoregions in Indonesia|Biodiversity of Borneo|Deforestation in Indonesia}}
Borneo is the third largest island in the world and the native vegetation was mostly [[Borneo lowland rain forests]] although much of this has been cleared with wildlife retreating to the [[Borneo montane rain forests]] inland. The islands of [[North Maluku]] are the original Spice Islands, a distinct [[rainforest]] [[ecoregion]].<ref>{{WWF ecoregion|id=aa0106|name=Terrestrial Ecoregions - Halmahera rain forests (AA0106)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref> A number of islands off the coast of New Guinea have their own distinctive biogeographic features, including the limestone islands of [[Schouten Islands|Biak]], in the entrance to the large [[Cenderawasih Bay]] at the northwest end of the island.<ref>{{WWF ecoregion|id=aa0105|name=Terrestrial Ecoregions - Central Range montane rain forests (AA0105)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref><ref>{{WWF ecoregion|id=aa0103|name=Terrestrial Ecoregions - Biak-Numfoor rain forests (AA0103)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref>
Borneo is the third largest island in the world, and the native vegetation was mostly [[Borneo lowland rain forests]], although much of this has been cleared with wildlife retreating to the [[Borneo montane rain forests]] inland. The islands of [[North Maluku]] are the original Spice Islands, a distinct [[rainforest]] [[ecoregion]].<ref>{{WWF ecoregion|id=aa0106|name=Terrestrial Ecoregions - Halmahera rain forests (AA0106)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref> A number of islands off the coast of New Guinea have their own distinctive biogeographic features, including the limestone islands of [[Schouten Islands|Biak]], in the entrance to the large [[Cenderawasih Bay]] at the northwest end of the island.<ref>{{WWF ecoregion|id=aa0105|name=Terrestrial Ecoregions - Central Range montane rain forests (AA0105)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref><ref>{{WWF ecoregion|id=aa0103|name=Terrestrial Ecoregions - Biak-Numfoor rain forests (AA0103)}}. Worldwildlife.org. Retrieved on 29 September 2010.</ref>


A recent global remote sensing analysis suggested that there were 14,416&nbsp;km<sup>2</sup> of tidal flats in Indonesia, ranking it 1st in the world in terms of how much tidal flat occurs there.<ref>{{cite journal |last1=Murray |first1=N.J. |last2=Phinn |first2=S.R. |last3=DeWitt |first3=M. |last4=Ferrari |first4=R. |last5=Johnston |first5=R. |last6=Lyons |first6=M.B. |last7=Clinton |first7=N. |last8=Thau |first8=D. |last9=Fuller |first9=R.A. |title=The global distribution and trajectory of tidal flats |journal=Nature |date=2019 |volume=565 |issue=7738 |pages=222–225 |doi=10.1038/s41586-018-0805-8 |pmid=30568300 |s2cid=56481043 |url=https://www.nature.com/articles/s41586-018-0805-8|url-access=subscription }}</ref> Another global analysis also estimated that Indonesia experienced the greatest total tidal wetland change (36% of global net change including [[mangrove]]s, [[Mudflat|tidal flats]], and [[Salt marsh|tidal marshes]]) between 1999 and 2019 with a net loss of {{convert|1,426|km2|mi2|abbr=on}}.<ref name="Murray et al. 2022">{{cite journal |last1=Murray |first1=Nicholas J. |last2=Worthington |first2=Thomas A. |last3=Bunting |first3=Pete |last4=Duce |first4=Stephanie |last5=Hagger |first5=Valerie |last6=Lovelock |first6=Catherine E. |last7=Lucas |first7=Richard |last8=Saunders |first8=Megan I. |last9=Sheaves |first9=Marcus |last10=Spalding |first10=Mark |last11=Waltham |first11=Nathan J. |last12=Lyons |first12=Mitchell B. |title=High-resolution mapping of losses and gains of Earth's tidal wetlands |journal=Science |date=13 May 2022 |volume=376 |issue=6594 |pages=744–749 |doi=10.1126/science.abm9583|pmid=35549414 |bibcode=2022Sci...376..744M |s2cid=248749118 |url=https://www.repository.cam.ac.uk/handle/1810/337253 |doi-access=free |hdl=2160/55fdc0d4-aa3e-433f-8a88-2098b1372ac5 |hdl-access=free }}</ref>
A recent global remote sensing analysis suggested that there were 14,416&nbsp;km<sup>2</sup> of tidal flats in Indonesia, ranking it 1st in the world in terms of how much tidal flat occurs there.<ref>{{cite journal |last1=Murray |first1=N.J. |last2=Phinn |first2=S.R. |last3=DeWitt |first3=M. |last4=Ferrari |first4=R. |last5=Johnston |first5=R. |last6=Lyons |first6=M.B. |last7=Clinton |first7=N. |last8=Thau |first8=D. |last9=Fuller |first9=R.A. |title=The global distribution and trajectory of tidal flats |journal=Nature |date=2019 |volume=565 |issue=7738 |pages=222–225 |doi=10.1038/s41586-018-0805-8 |pmid=30568300 |s2cid=56481043 |url=https://www.nature.com/articles/s41586-018-0805-8|url-access=subscription }}</ref> Another global analysis also estimated that Indonesia experienced the greatest total tidal wetland change (36% of global net change including [[mangrove]]s, [[Mudflat|tidal flats]], and [[Salt marsh|tidal marshes]]) between 1999 and 2019 with a net loss of {{convert|1,426|km2|mi2|abbr=on}}.<ref name="Murray et al. 2022">{{cite journal |last1=Murray |first1=Nicholas J. |last2=Worthington |first2=Thomas A. |last3=Bunting |first3=Pete |last4=Duce |first4=Stephanie |last5=Hagger |first5=Valerie |last6=Lovelock |first6=Catherine E. |last7=Lucas |first7=Richard |last8=Saunders |first8=Megan I. |last9=Sheaves |first9=Marcus |last10=Spalding |first10=Mark |last11=Waltham |first11=Nathan J. |last12=Lyons |first12=Mitchell B. |title=High-resolution mapping of losses and gains of Earth's tidal wetlands |journal=Science |date=13 May 2022 |volume=376 |issue=6594 |pages=744–749 |doi=10.1126/science.abm9583|pmid=35549414 |bibcode=2022Sci...376..744M |s2cid=248749118 |url=https://www.repository.cam.ac.uk/handle/1810/337253 |doi-access=free |hdl=2160/55fdc0d4-aa3e-433f-8a88-2098b1372ac5 |hdl-access=free }}</ref>
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Some regions, such as Kalimantan and Sumatra, experience only slight differences in rainfall and temperature between the seasons, whereas others, such as Nusa Tenggara, experience far more pronounced differences with droughts in the dry season, and floods in the wet. Rainfall in Indonesia is plentiful, particularly in west Sumatra, northwest Kalimantan, west Java, and western New Guinea.
Some regions, such as Kalimantan and Sumatra, experience only slight differences in rainfall and temperature between the seasons, whereas others, such as Nusa Tenggara, experience far more pronounced differences with droughts in the dry season, and floods in the wet. Rainfall in Indonesia is plentiful, particularly in west Sumatra, northwest Kalimantan, west Java, and western New Guinea.


Parts of Sulawesi and some islands closer to Australia, such as [[Sumba]] and [[Timor]], are drier, however, these are exceptions. The almost uniformly warm waters that make up 81% of Indonesia's area ensure that temperatures on land remain fairly constant. The coastal plains averaging {{convert|28|°C|1}}, the inland and mountain areas averaging {{convert|26|°C|1}}, and the higher mountain regions, {{convert|23|°C|1}}. The area's relative humidity ranges between 70 and 90%.
Parts of Sulawesi and some islands closer to Australia, such as [[Sumba]] and [[Timor]], are drier; however, these are exceptions. The almost uniformly warm waters that make up 81% of Indonesia's area ensure that temperatures on land remain fairly constant, with the coastal plains averaging {{convert|28|°C|1}}, the inland and mountain areas averaging {{convert|26|°C|1}}, and the higher mountain regions averaging {{convert|23|°C|1}}. The area's relative humidity ranges between 70 and 90%.


Winds are moderate and generally predictable, with [[monsoon]]s usually blowing in from the south and east in June through October and from the northwest in November through March. [[Typhoon]]s and large scale storms pose little hazard to mariners in Indonesia waters; the major danger comes from swift currents in channels, such as the [[Lombok Strait|Lombok]] and [[Sape Strait|Sape]] straits.
Winds are moderate and generally predictable, with [[monsoon]]s usually blowing in from the south and east in June through October and from the northwest in November through March. [[Typhoon]]s and large scale storms pose little hazard to mariners in Indonesia waters; the major danger comes from swift currents in channels, such as the [[Lombok Strait|Lombok]] and [[Sape Strait|Sape]] straits.
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Indonesia's high population and rapid industrialisation present serious [[Environmental issues in Indonesia|environmental issues]], which are often given a lower priority due to high poverty levels and weak, under-resourced governance.<ref name="forestprob">{{Cite web |author=Jason R. Miller |title=Deforestation in Indonesia and the Orangutan Population |publisher=TED Case Studies |date=30 January 1997 |url=http://www.american.edu/TED/orang.htm |access-date=14 August 2007 |archive-url=https://web.archive.org/web/20160229155532/http://www1.american.edu/TED/orang.htm |archive-date=2016-02-29 |url-status=dead}}</ref> Issues include [[Deforestation in Indonesia|large-scale deforestation]] (much of it [[illegal logging|illegal]]) and related wildfires causing [[Smog#Southeast Asia|heavy smog]] over parts of western Indonesia, Malaysia and Singapore; over-exploitation of marine resources; and environmental problems associated with rapid [[urbanisation]] and [[economic development]], including [[air pollution]], [[traffic congestion]], garbage management, and reliable water and [[Wastewater|waste water]] services.<ref name="forestprob" />
Indonesia's high population and rapid industrialisation present serious [[Environmental issues in Indonesia|environmental issues]], which are often given a lower priority due to high poverty levels and weak, under-resourced governance.<ref name="forestprob">{{Cite web |author=Jason R. Miller |title=Deforestation in Indonesia and the Orangutan Population |publisher=TED Case Studies |date=30 January 1997 |url=http://www.american.edu/TED/orang.htm |access-date=14 August 2007 |archive-url=https://web.archive.org/web/20160229155532/http://www1.american.edu/TED/orang.htm |archive-date=2016-02-29 |url-status=dead}}</ref> Issues include [[Deforestation in Indonesia|large-scale deforestation]] (much of it [[illegal logging|illegal]]) and related wildfires causing [[Smog#Southeast Asia|heavy smog]] over parts of western Indonesia, Malaysia and Singapore; over-exploitation of marine resources; and environmental problems associated with rapid [[urbanisation]] and [[economic development]], including [[air pollution]], [[traffic congestion]], garbage management, and reliable water and [[Wastewater|waste water]] services.<ref name="forestprob" />


Deforestation and the destruction of peatlands make Indonesia the world's third largest emitter of greenhouse gases.<ref>{{cite news |last=Higgins |first=Andrew |title=A climate threat, rising from the soil | newspaper=The Washington Post | url= https://www.washingtonpost.com/wp-dyn/content/article/2009/11/18/AR2009111804162.html |access-date=11 December 2009 | date=19 November 2009}}</ref> [[Habitat destruction]] threatens the survival of indigenous and endemic species, including 140 species of [[mammals]] identified by the [[World Conservation Union]] (IUCN) as [[threatened species|threatened]], and 15 identified as critically endangered, including the Sumatran Orangutan.<ref>{{cite web |last=Massicot |first=Paul |title=Animal Info – Indonesia |publisher=Animal Info – Information on Endangered Mammals |url=http://www.animalinfo.org/country/indones.htm |access-date=14 August 2007}}</ref>
Deforestation and the destruction of peatlands make Indonesia the world's third largest emitter of greenhouse gases.<ref>{{cite news |last=Higgins |first=Andrew |title=A climate threat, rising from the soil | newspaper=The Washington Post | url= https://www.washingtonpost.com/wp-dyn/content/article/2009/11/18/AR2009111804162.html |access-date=11 December 2009 | date=19 November 2008}}</ref> [[Habitat destruction]] threatens the survival of indigenous and endemic species, including 140 species of [[mammals]] identified by the [[World Conservation Union]] (IUCN) as [[threatened species|threatened]], and 15 identified as critically endangered, including the Sumatran Orangutan.<ref>{{cite web |last=Massicot |first=Paul |title=Animal Info – Indonesia |publisher=Animal Info – Information on Endangered Mammals |url=http://www.animalinfo.org/country/indones.htm |access-date=14 August 2007}}</ref>


In 1970, 15% of Indonesians lived in cities compared to over 30% today, and this increases pressure on the urban environment. Industrial pollution is increasing, particularly in Java, and the increasing affluence of the growing middle class drives a rapid increase in the number of motor vehicles and associated emissions. Garbage and waste water services are being placed under increasing pressure. Reliance on septic systems or effluent disposal in open canals and [[List of rivers of Indonesia|river systems]] remains the norm, and is a major polluter of water resources. Very few Indonesians have access to safe drinking water and must boil water before use.
In 1978, 14% of Indonesians lived in cities compared to over 30% today, and this increases pressure on the urban environment. Industrial pollution is increasing, particularly in Java, and the increasing affluence of the growing middle class drives a rapid increase in the number of motor vehicles and associated emissions. Garbage and waste water services are being placed under increasing pressure. Reliance on septic systems or effluent disposal in open canals and [[List of rivers of Indonesia|river systems]] remains the norm, and is a major polluter of water resources. Very few Indonesians have access to safe drinking water and must boil water before use.


The geographical resources of the Indonesian archipelago have been exploited in ways that fall into consistent social and historical patterns. One cultural pattern consists of the formerly Indianized, rice-growing peasants in the valleys and plains of Sumatra, Java, and Bali, another cultural complex is composed of the largely Islamic coastal commercial sector, a third, more marginal sector consists of the upland forest farming communities which exist by means of subsistence swidden agriculture. To some degree, these patterns can be linked to the geographical resources themselves, with abundant shoreline, generally calm seas, and steady winds favouring the use of sailing vessels, and fertile valleys and plains—at least in the Greater Sunda Islands—permitting irrigated rice farming. The heavily forested, mountainous interior hinders overland communication by road or river, but fosters slash-and-burn agriculture.
The geographical resources of the Indonesian archipelago have been exploited in ways that fall into consistent social and historical patterns. One cultural pattern consists of the formerly Indianized, rice-growing peasants in the valleys and plains of Sumatra, Java, and Bali, another cultural complex is composed of the largely Islamic coastal commercial sector, a third, more marginal sector consists of the upland forest farming communities which exist by means of subsistence swidden agriculture. To some degree, these patterns can be linked to the geographical resources themselves, with abundant shoreline, generally calm seas, and steady winds favouring the use of sailing vessels, and fertile valleys and plains—at least in the Greater Sunda Islands—permitting irrigated rice farming. The heavily forested, mountainous interior hinders overland communication by road or river, but fosters slash-and-burn agriculture.