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Coordinates: 5°58′12″N 101°19′37″E / 5.9699°N 101.3269°E / 5.9699; 101.3269
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{{Infobox mountain
{{Infobox mountain
| name=Titiwangsa Mountains
| name=Titiwangsa Mountains
| other_name= ''Banjaran Titiwangsa/Besar'' ([[Malay language|Malay]])<br />ทิวเขาสันกาลาคีรี ([[Thai language|Thai]])
| other_name= ''Banjaran Titiwangsa/Besar'' ([[Malay language|Malay]])<br />ทิวเขาสันกาลาคีรี ([[Thai language|Thai]])<br />蒂迪旺沙山脉 ([[Chinese language|Chinese]])<br />蒂迪旺沙山脈 ([[Chinese language|Chinese]])<br />திதிவாங்சா மலைத்தொடர் ([[Tamil language|Tamil]])


| photo=Ipoh forest (2) near Gunung Suku.jpg
| photo=Ipoh forest (2) near Gunung Suku.jpg
| photo_caption=The view of the Titiwangsa Mountains near Mount Suku.
| photo_caption=The view of the Titiwangsa Mountains near Mount Suku.
| country= {{hlist|[[Thailand]]|[[Malaysia]]}}
| country_type= Countries
| subdivision1 = {{hlist|[[Songkhla Province|Songkhla]]|[[Yala Province|Yala]]|[[Narathiwat Province|Narathiwat]]|[[Perak]]|[[Kelantan]]|[[Pahang]]|[[Selangor]]|[[Negeri Sembilan]]}}
| country= {{enum|[[Thailand]]|[[Malaysia]]}}
| subdivision1 = {{enum|[[Songkhla Province|Songkhla]]|[[Yala Province|Yala]]|[[Narathiwat Province|Narathiwat]]|[[Perak]]|[[Kelantan]]|[[Pahang]]|[[Selangor]]|[[Negeri Sembilan]]}}
| subdivision1_type = Provinces/States
| subdivision1_type = Provinces/States
| parent= [[Tenasserim Hills]]
| parent= [[Tenasserim Hills]]
| geology= {{enum|[[Granite]]|[[limestone]]}}
| geology= {{hlist|[[Granite]]|[[limestone]]}}
| age= {{enum|[[Permian]]|[[Triassic]]}}
| age= {{hlist|[[Permian]]|[[Triassic]]}}
| orogeny=
| orogeny=
| length_km= 480
| length_km= 480
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[[File:Titiwangsa Mountains from Ulu Yam.jpg|thumb|The Titiwangsa during [[Golden hour (photography)|golden hour]] as viewed from the rural town of [[Ulu Yam]], [[Selangor]].]]
[[File:Titiwangsa Mountains from Ulu Yam.jpg|thumb|The Titiwangsa during [[Golden hour (photography)|golden hour]] as viewed from the rural town of [[Ulu Yam]], [[Selangor]].]]


The '''Titiwangsa Mountains''' ([[Malay language|Malay]]: ''Banjaran Titiwangsa''; [[Jawi script|Jawi]]: بنجرن تيتيوڠسا, {{IPA-may|ˈband͡ʒaˈran titiwaŋˈsa|pron}}), also known as ''Banjaran Besar'' (lit. 'main range') by locals, is the chain of mountains that forms the backbone of the [[Malay Peninsula]].
The '''Titiwangsa Mountains''' ([[Malay language|Malay]]: ''Banjaran Titiwangsa''; [[Jawi script|Jawi]]: {{Script/Arabic|بنجرن تيتيوڠسا}}, {{IPA-may|ˈband͡ʒaˈran titiwaŋˈsa|pron}}), also known as ''Banjaran Besar'' (lit. 'main range') by locals, is the chain of mountains that forms the backbone of the [[Malay Peninsula]]. The northern section of the range is in [[southern Thailand]], where it is known as the '''Sankalakhiri Range''' ({{langx|th|ทิวเขาสันกาลาคีรี}}; [[Royal Thai General System of Transcription|RTGS]]: ''Thio Khao Sankalakhiri''; {{IPA|th|tʰīw kʰǎw sǎn.kāːlāːkʰīːrīː|pron}}).
The northern section of the range is in [[southern Thailand]], where it is known as '''Sankalakhiri Range''' ({{lang-th|ทิวเขาสันกาลาคีรี}}; [[Royal Thai General System of Transcription|RTGS]]: ''Thio Khao Sankalakhiri''; {{IPA-th|tʰīw kʰǎw sǎn.kāːlāːkʰīːrīː|pron}}).


The mountain range acts as a natural divider, dividing [[Peninsular Malaysia]], as well as southernmost Thailand, into east and west coast regions. It also serves as a [[drainage divide]] of some major rivers of Peninsular Malaysia such as the [[Pahang River|Pahang]], [[Perak River|Perak]], [[Kelantan River|Kelantan]], [[Klang River|Klang]] and [[Muar River|Muar]]. The length of mountain range is about 480&nbsp;km from north to south.
The mountain range acts as a natural divider, dividing [[Peninsular Malaysia]], as well as southernmost Thailand, into east and west coast regions. It also serves as a [[drainage divide]] of some major rivers of Peninsular Malaysia such as the [[Pahang River|Pahang]], [[Perak River|Perak]], [[Kelantan River|Kelantan]], [[Klang River|Klang]] and [[Muar River|Muar]]. The length of mountain range is about 480&nbsp;km from north to south.
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[[File:Gunung Datuk Rocky Peak.jpg|thumb|A [[granitic]] [[Tor (rock formation)|tor]] on the summit of [[Mount Datuk]], [[Rembau District]], [[Negeri Sembilan]], near the southern end of the range.]]
[[File:Gunung Datuk Rocky Peak.jpg|thumb|A [[granitic]] [[Tor (rock formation)|tor]] on the summit of [[Mount Datuk]], [[Rembau District]], [[Negeri Sembilan]], near the southern end of the range.]]
[[File:Ipoh Kek Lok Dong (8367457996).jpg|229px|thumb|[[Mogote|Mogotes]] dot along the western edge of the range in [[Kinta District]], [[Perak]], part of the [[Kinta Valley National Geopark]].]]
[[File:Ipoh Kek Lok Dong (8367457996).jpg|229px|thumb|[[Mogote]]s dot along the western edge of the range in [[Kinta District]], [[Perak]], part of the [[Kinta Valley National Geopark]].]]


The Titiwangsa Mountains is part of a [[Suture (geology)|suture zone]] that runs north–south, starting in [[Thailand]] at the [[Nan Province|Nan]]-[[Uttaradit]] suture zone (partly coincident with the [[Dien Bien Phu|Dien Bien Phu fault]]), and extending south towards Peninsular [[Malaysia]] ([[Bentong]]-[[Raub District|Raub]] suture zone).<ref>{{cite book |last1=Racey |first1=Andrew |editor1-last=Buffetaut |editor1-first=Eric |title=Late Palaeozoic and Mesozoic Ecosystems in SE Asia |date=2009 |publisher=Geological Society of London |page=46 |url=https://books.google.com/books?id=6wMfMgSmckkC&q=Uttaradit/Dien+Bien+Phu+suture+zone |access-date=20 June 2019 |chapter=Mesozoic red bed sequences in SE Asia and the significance of the Khorat Group of NE Thailand|isbn=9781862392755 }}</ref> The eastern half of the Titiwangsa Mountains in [[Peninsular Malaysia]] is an amalgamation of continental [[terrane]]s known as [[Cimmerian Plate|Cimmeria]] or Indochina, whereas the western half is an amalgamation of continental terranes Sinoburmalaya or [[Sibumasu]]. These two halves of terranes were separated by the [[Paleo-Tethys Ocean]].<ref>Metcalfe, I., 2000, "The Bentong-Raub Suture Zone", ''Journal of Asian Earth Sciences'', v. 18, p. 691-712</ref><ref>Metcalfe, I., 2002, "Permian tectonic framework and palaeogeography of SE Asia", ''Journal of Asian Earth Sciences'', v. 20, p. 551-566</ref>
The Titiwangsa Mountains are predominantly [[granitic]]. The mountain range is part of a [[Suture (geology)|suture zone]] that runs north–south, starting in [[Thailand]] at the [[Nan province|Nan]]-[[Uttaradit]] suture zone (partly coincident with the [[Dien Bien Phu|Dien Bien Phu fault]]), and extending south towards Peninsular [[Malaysia]] ([[Bentong]]-[[Raub District|Raub]] suture zone).<ref>{{cite book |last1=Racey |first1=Andrew |editor1-last=Buffetaut |editor1-first=Eric |title=Late Palaeozoic and Mesozoic Ecosystems in SE Asia |date=2009 |publisher=Geological Society of London |page=46 |url=https://books.google.com/books?id=6wMfMgSmckkC&q=Uttaradit/Dien+Bien+Phu+suture+zone |access-date=20 June 2019 |chapter=Mesozoic red bed sequences in SE Asia and the significance of the Khorat Group of NE Thailand|isbn=9781862392755 }}</ref> The eastern half of the Titiwangsa Mountains in [[Peninsular Malaysia]] is an amalgamation of continental [[terrane]]s known as [[Cimmerian Plate|Cimmeria]] or Indochina, whereas the western half is an amalgamation of continental terranes Sinoburmalaya or [[Sibumasu]]. These two halves of terranes were separated by the [[Paleo-Tethys Ocean]].<ref>Metcalfe, I., 2000, "The Bentong-Raub Suture Zone", ''Journal of Asian Earth Sciences'', v. 18, p. 691-712</ref><ref>Metcalfe, I., 2002, "Permian tectonic framework and palaeogeography of SE Asia", ''Journal of Asian Earth Sciences'', v. 20, p. 551-566</ref>


The Cimmeria was separated from [[Gondwana]] around 400 [[mya (unit)|mya]] during the [[Devonian]] and rifted towards Laurasia, the northeastern arm of [[Pangea]]. It attached to Laurasia completely around 280 mya during the [[Late Permian]].
The Cimmeria was separated from [[Gondwana]] around 400 [[mya (unit)|mya]] during the [[Devonian]] and rifted towards Laurasia, the northeastern arm of [[Pangea]]. It attached to Laurasia completely around 280 mya during the [[Late Permian]].


Sibumasu terranes on the other hand, only started to separate from Gondwana during the [[Early Permian]] and rifted towards Indochina. The collision of Sibumasu terranes and Indochina terranes during 200mya [[Late Triassic]] resulted in the closure of the Paleo-Tethys Ocean and formation of the modern Titiwangsa Mountain belts.
Sibumasu terranes on the other hand, only started to separate from Gondwana during the [[Early Permian]] and rifted towards Indochina. The collision of the Sibumasu terranes and Indochina terranes 200 mya during the [[Late Triassic]] resulted in the closure of the Paleo-Tethys Ocean and formation of the modern Titiwangsa Mountain belts.


===Seismic hazards===
===Seismic hazards===
{{see also|List of earthquakes in Malaysia}}
{{see also|List of earthquakes in Malaysia}}
[[Peninsular Malaysia]], while being tectonically stable, has a history of [[intraplate earthquakes]],<ref>https://www.astroawani.com/berita-malaysia/ada-kebarangkalian-gempa-bumi-berlaku-di-malaysia-nrecc-416163 {{bare URL inline|date=June 2023}}</ref> with most of them are of low magnitude. As the Bentong-Raub suture runs parallel to the Titiwangsa Mountains, a large network of [[fault lines]] also crisscross the mountain range.<ref>{{cite web | url=https://ipm.my/earthquakes-in-malaysia-should-we-be-worried-and-how-to-reduce-its-impact-on-our-buildings/#:~:text=Although%20Peninsular%20Malaysia%20is%20located,Crocker%20Range%20(East%20Malaysia). | title=Earthquakes in Malaysia: Should we be worried and how to reduce its impact on our buildings? | date=12 January 2022 }}</ref> The known major fault lines in the mountains are the [[Bukit Tinggi, Pahang|Bukit Tinggi]], [[Kuala Lumpur]] and [[Seremban]] fault lines, with the first two being the most active.
[[Peninsular Malaysia]], while being tectonically stable, has a history of [[intraplate earthquake]]s,<ref>[https://www.astroawani.com/berita-malaysia/ada-kebarangkalian-gempa-bumi-berlaku-di-malaysia-nrecc-416163 Ada kebarangkalian gempa bumi berlaku di Malaysia - NRECC] astroawani.com 19 April 2023</ref> with most of them of low magnitudes. As the Bentong-Raub suture runs parallel to the Titiwangsa Mountains, a large network of [[fault lines]] crisscross the mountain range.<ref>{{cite web | url=https://ipm.my/earthquakes-in-malaysia-should-we-be-worried-and-how-to-reduce-its-impact-on-our-buildings/#:~:text=Although%20Peninsular%20Malaysia%20is%20located,Crocker%20Range%20(East%20Malaysia). | title=Earthquakes in Malaysia: Should we be worried and how to reduce its impact on our buildings? | date=12 January 2022 }}</ref> The known major fault lines in the mountains are the [[Bukit Tinggi, Pahang|Bukit Tinggi]], [[Kuala Lumpur]] and [[Seremban]] fault lines, with the first two being the most active.


Between 1984 and 2013, there had been tremors ranging from 1.6 to 4.6 on the [[Richter scale]] with local epicentres in [[Kenyir Lake]], [[Manjung]], [[Belum-Temengor|Temenggor]], [[Bukit Tinggi, Pahang|Bukit Tinggi]] and [[Kuala Pilah (town)|Kuala Pilah]], the latter three being situated along the Titiwangsa Mountains. As a precautionary move, the Department of Minerals and Geosciences pitched 23 Earthquake Benchmark (PAG, [[Malay language|Malay]]: ''Penanda Aras Gempa'') stations around earthquake-prone areas in Peninsular Malaysia, with 13 in [[Pahang]], six in [[Selangor]], and two each in [[Perak]] and [[Negeri Sembilan]] to monitor possible movements within the fault network.<ref>{{cite web | url=https://www.hmetro.com.my/mutakhir/2023/05/962481/gempa-bumi-rujuk-peta-bahaya-seismik-sebelum-reka-bangunan | title=Gempa bumi: Rujuk peta bahaya seismik sebelum reka bangunan | date=2 May 2023 }}</ref> The [[Ministry of Natural Resources, Environment and Climate Change]] (NRECC) also pointed out that strong earthquakes centred in neighbouring [[Sumatra]], [[Indonesia]] could potentially activate ancient faults in Peninsular Malaysia and the effects of tremors could be felt around areas along the [[Peninsular Malaysia#Other features|west coast]] of Peninsular Malaysia.
Between 1984 and 2013, there were tremors ranging from 1.6 to 4.6 on the [[Richter scale]] with local epicentres in [[Kenyir Lake]], [[Manjung]], [[Belum-Temengor|Temenggor]], [[Bukit Tinggi, Pahang|Bukit Tinggi]] and [[Kuala Pilah (town)|Kuala Pilah]], the latter three being situated along the Titiwangsa Mountains. As a precautionary move, the Department of Minerals and Geosciences pitched 23 Earthquake Benchmark (PAG, [[Malay language|Malay]]: ''Penanda Aras Gempa'') stations around earthquake-prone areas in Peninsular Malaysia, with 13 in [[Pahang]], six in [[Selangor]], and two each in [[Perak]] and [[Negeri Sembilan]] to monitor possible movements within the fault network.<ref>{{cite web | url=https://www.hmetro.com.my/mutakhir/2023/05/962481/gempa-bumi-rujuk-peta-bahaya-seismik-sebelum-reka-bangunan | title=Gempa bumi: Rujuk peta bahaya seismik sebelum reka bangunan | date=2 May 2023 }}</ref> The [[Ministry of Natural Resources and Environmental Sustainability|Ministry of Natural Resources, Environment and Climate Change]] (NRECC) also pointed out that strong earthquakes centred in neighbouring [[Sumatra]], [[Indonesia]] could potentially activate ancient faults in Peninsular Malaysia and the effects of tremors could be felt around areas along the [[Peninsular Malaysia#Other features|west coast]] of Peninsular Malaysia.


==Geography==
==Geography==
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[[File:West Malaysia relief location map.jpg|300px|thumb|Relief map of [[Peninsular Malaysia]], highlighting its mountainous core. The Titiwangsa Mountains is the longest range running along the border between the states of [[Perak]] and [[Selangor]] on the west coast with [[Kelantan]] and [[Pahang]] on the east coast, eventually straddling across the state of [[Negeri Sembilan]] further south. Nearby systems include [[Keledang Range|Keledang]] and [[Bintang Mountains|Bintang Ranges]] to its northwest, [[Mount Benum|Benom Massif]] to the southeast, and [[Tahan Range]] to the east.]]
[[File:West Malaysia relief location map.jpg|300px|thumb|Relief map of [[Peninsular Malaysia]], highlighting its mountainous core. The Titiwangsa Mountains is the longest range running along the border between the states of [[Perak]] and [[Selangor]] on the west coast with [[Kelantan]] and [[Pahang]] on the east coast, eventually straddling across the state of [[Negeri Sembilan]] further south. Nearby systems include [[Keledang Range|Keledang]] and [[Bintang Mountains|Bintang Ranges]] to its northwest, [[Mount Benum|Benom Massif]] to the southeast, and [[Tahan Range]] to the east.]]


This mountain range is a part of the wider [[Tenasserim Hills]] system. It forms the southernmost section of the Indo-Malayan [[cordillera]] which runs from [[Tibet]] through the [[Kra Isthmus]] into the [[Malay Peninsula]].<ref>Avijit Gupta, ''The Physical Geography of Southeast 0Asia'', Oxford University Press, 2005. {{ISBN|978-0-19-924802-5}}</ref>
This mountain range is a part of the wider [[Tenasserim Hills]]. It forms the southernmost section of the Indo-Malayan [[cordillera]] which runs from [[Tibet]] through the [[Kra Isthmus]] into the [[Malay Peninsula]].<ref>Avijit Gupta, ''The Physical Geography of Southeast 0Asia'', Oxford University Press, 2005. {{ISBN|978-0-19-924802-5}}</ref>


The Titiwangsa Mountains proper begins in the north as the Sankalakhiri Range, a prolongation of the [[Nakhon Si Thammarat Range]] which includes the smaller Pattani, Taluban, and Songkhla sub-ranges. The Sankalakhiri marks the border between the [[Southern Thailand]] provinces of [[Yala Province|Yala]] in west and [[Narathiwat Province|Narathiwat]] in the east. Across the border into Malaysia, the main stretch of the range runs in a northwest–southeast orientation, straddling the borders between the [[Peninsular Malaysia#Other features|west coast]] states of [[Perak]] and [[Selangor]] with [[Kelantan]] and [[Pahang]] on the [[Peninsular Malaysia#Other features|eastern side]] of the peninsula. From the [[tripoint]] of [[Pahang]], [[Selangor]] and [[Negeri Sembilan]] near [[Mount Nuang]], it then transverses through the middle of the state of Negeri Sembilan, also a west coast state, thus dividing the state into two regions - western Negeri Sembilan, which consists of [[Seremban District|Seremban]], [[Port Dickson District|Port Dickson]] and [[Rembau District]]s, and eastern Negeri Sembilan, composed of the districts of [[Jelebu District|Jelebu]], [[Kuala Pilah District|Kuala Pilah]], [[Jempol District|Jempol]] and [[Tampin District|Tampin]] - and ends in the south near [[Tampin]], in the southern part of the state. <ref name="auto">{{cite web|url=http://www.mdtampin.gov.my/en/visitors/places-interest |title=Places of Interest &#124; Official Portal of Tampin District Council (MDT) |publisher=Mdtampin.gov.my |date=1941-01-14 |access-date=2023-04-04}}</ref><ref>{{cite web|url=https://www.researchgate.net/publication/273695651|title=Vegetation of Peninsular Malaysia.}}</ref>
The Titiwangsa Mountains proper begin in the north as the Sankalakhiri Range, a prolongation of the [[Nakhon Si Thammarat Range]] which includes the smaller Pattani, Taluban, and Songkhla sub-ranges. The Sankalakhiri marks the border between the [[Southern Thailand|Southern Thai]] provinces of [[Yala province|Yala]] in west and [[Narathiwat province|Narathiwat]] in the east. Across the border into Malaysia, the main stretch of the range runs in a northwest–southeast orientation, straddling the borders between the [[Peninsular Malaysia#Other features|west coast]] states of [[Perak]] and [[Selangor]] with [[Kelantan]] and [[Pahang]] on the [[Peninsular Malaysia#Other features|eastern side]] of the peninsula. From the [[tripoint]] of [[Pahang]], [[Selangor]] and [[Negeri Sembilan]] near [[Mount Nuang]], it then transverses through the middle of the state of Negeri Sembilan, also a west coast state, thus dividing the state into two regions western Negeri Sembilan, which consists of [[Seremban District|Seremban]], [[Port Dickson District|Port Dickson]] and [[Rembau District]]s, and eastern Negeri Sembilan, composed of the districts of [[Jelebu District|Jelebu]], [[Kuala Pilah District|Kuala Pilah]], [[Jempol District|Jempol]] and [[Tampin District|Tampin]] and terminates in the south near the town of [[Tampin]], in the southern part of the state.<ref>Yaakub Idrus. ''Rumah Melayu Negeri Sembilan: satu analisis seni bina Melayu''. Penerbit Fajar Bakti, 1966, p. 11. https://malaycivilization.com.my/omeka/files/original/a884b36ae16d4af41735580e8b03038b.pdf</ref><ref name="auto">{{cite web|url=http://www.mdtampin.gov.my/en/visitors/places-interest |title=Places of Interest &#124; Official Portal of Tampin District Council (MDT) |publisher=Mdtampin.gov.my |date= |access-date=2023-04-04}}</ref><ref>{{Cite web|url=https://www.researchgate.net/publication/273695651|title=Vegetation of Peninsular Malaysia.|accessdate=3 March 2024}}</ref>
Outcrops of Titiwangsa [[granite]], mainly consisting of [[inselbergs]], project further south into [[Malacca]], where it abuts in the waters of the [[Strait of Malacca]] in [[Besar Island, Malacca|Pulau Besar]].<ref> {{cite web|url=https://www.astroawani.com/berita-malaysia/empat-kawasan-di-melaka-berpotensi-diiktiraf-geopark-kebangsaan-442910|title=Empat kawasan di Melaka berpotensi diiktiraf Geopark Kebangsaan|publisher=Astro Awani|date=2023-10-22}}</ref>
Outcrops of Titiwangsa [[granite]], mainly consisting of [[inselbergs]], project further south into [[Malacca]], where it abuts in the waters of the [[Strait of Malacca]] in [[Besar Island, Malacca|Pulau Besar]].<ref>{{cite web|url=https://www.astroawani.com/berita-malaysia/empat-kawasan-di-melaka-berpotensi-diiktiraf-geopark-kebangsaan-442910|title=Empat kawasan di Melaka berpotensi diiktiraf Geopark Kebangsaan|publisher=Astro Awani|date=2023-10-22}}</ref>


The greatest elevations can be found along the northern and central section of the range, with the highest point measuring 2,183&nbsp;m (7,162&nbsp;ft) on [[Gunung Korbu]], [[Perak]]. On the Thai side the highest point is 1,533 m [[Ulu Titi Basah]] (ยูลูติติ บาซาห์), at the Thai/Malaysian border between [[Yala Province]] and [[Perak]].<ref>{{cite web|url=http://www.geographic.org/geographic_names/name.php?uni=-4622806&fid=6089&c=thailand#MAP|title=Gunong Ulu Titi Basah, Thailand - Geographical Names, map, geographic coordinates}}</ref> In contrast, the height gradually diminishes towards the southern reaches of the range, which mainly runs through Negeri Sembilan, with elevations measuring 1,462&nbsp;m (4,797&nbsp;ft) at its highest on [[Mount Besar Hantu]], on the border between the state and [[Pahang]], as well as 1,193&nbsp;m (3,914&nbsp;ft) on Mount Telapak Buruk on the boundary between the districts of [[Seremban District|Seremban]] and [[Jelebu]] to {{convert|500–700|m|ft}}.
In general, the greatest elevations occur along the northern and central sections of the range, with its highest point measuring 2,183&nbsp;m (7,162&nbsp;ft) on [[Gunung Korbu]], [[Perak]]. On the Thai side, the highest point is 1,533&nbsp;m (5,026&nbsp;ft) [[Ulu Titi Basah]] (ยูลูติติ บาซาห์), at the Thai/Malaysian border between [[Yala province]] and [[Perak]].<ref>{{Cite web|url=https://geographic.org/geographic_names/name.php?uni=-4622806&fid=6089&c=thailand|title=Gunong Ulu Titi Basah, Thailand - Geographical Names, map, geographic coordinates|website=geographic.org|accessdate=3 March 2024}}</ref> On the other hand, the height gradually diminishes towards the southern reaches of the range, which mainly runs through [[Negeri Sembilan]], with elevations ranging from 1,462&nbsp;m (4,797&nbsp;ft) at its highest on [[Mount Besar Hantu]], on the border between the state and [[Pahang]], as well as 1,193&nbsp;m (3,914&nbsp;ft) on Mount Telapak Buruk on the boundary between the districts of [[Seremban District|Seremban]] and [[Jelebu]] to {{convert|500–700|m|ft}}.


==Features==
==Features==
[[File:Titiwangsa Mountains rainforest.jpg|240px|thumb|Tropical rainforest in the Perakian/Pahangese Titiwangsa, part of the Central Forest Spine. Taken near [[Ringlet, Malaysia|Ringlet]]]]
[[File:Titiwangsa Mountains rainforest.jpg|240px|thumb|Tropical rainforest in the Perakian/Pahangese Titiwangsa, part of the Central Forest Spine. Taken near [[Ringlet, Malaysia|Ringlet]]]]
[[File:Central Forest Spine Marker, Bukit Putus.jpg|240px|thumb|Central Forest Spine signboard on Federal Route {{JKR|51}} in the Negri Titiwangsa near [[Bukit Putus]]]]
[[File:Central Forest Spine Marker, Bukit Putus.jpg|240px|thumb|Central Forest Spine signboard on Federal Route {{JKR|51}} in the Negri Titiwangsa near [[Bukit Putus, Negeri Sembilan|Bukit Putus]]]]
The rainforests of the Titiwangsa Mountains form part of the [[Titiwangsa Forest Complex]], which is itself part of the larger [[Central Forest Spine]] conservation area. A number of roads and highways cut through the mountain range, effectively acting as [[mountain passes]] linking both settlements on both sides of the range.
The rainforests of the Titiwangsa Mountains form part of the [[Titiwangsa Forest Complex]], which is itself part of the larger [[Central Forest Spine]] conservation area. A number of roads and highways cut through the mountain range, effectively acting as [[mountain pass]]es linking settlements on either side of the range.


[[File:Cameron Highlands (Tea Plantation).jpg|thumb|[[Camellia sinensis|Tea]] plantation in [[Cameron Highlands]]]]
[[File:Cameron Highlands (Tea Plantation).jpg|thumb|[[Camellia sinensis|Tea]] plantation in [[Cameron Highlands]]]]
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===Thailand===
===Thailand===
*[[San Kala Khiri National Park]]
*[[San Kala Khiri National Park]]
*[[Budo - Su-ngai Padi National Park]]
*[[Budo–Su-ngai Padi National Park]]
*[[Bang Lang National Park]]
*[[Bang Lang National Park]]
*[[Namtok Sai Khao National Park]]
*[[Namtok Sai Khao National Park]]
*[[Hala Bala Wildlife Sanctuary]]
*[[Hala-Bala Wildlife Sanctuary]]


===Malaysia===
===Malaysia===
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File:The Sea of Mist Ai Yerweng, Betong.jpg|View of the Sankalakhiri in [[Aiyoeweng]], [[Yala province|Yala]], near the [[Bang Lang Reservoir]].
File:The Sea of Mist Ai Yerweng, Betong.jpg|View of the Sankalakhiri in [[Aiyoeweng]], [[Yala province|Yala]], near the [[Bang Lang Reservoir]].


File:เมืองเบตง - panoramio.jpg|City of [[Betong, Thailand|Betong]], [[Yala province|Yala]], with the Sankalakhiri Range towering in the background.
File:เมืองเบตง - panoramio.jpg|City of [[Betong, Thailand|Betong]], Yala, with the Sankalakhiri Range towering in the background.


File:Peak of Banjaran Titiwangsa.jpg|The Titiwangsa Mountains seen from a [[layby]] along the [[Malaysia Federal Route 4|East-West Highway]] near [[Gerik]], [[Perak]].
File:Peak of Banjaran Titiwangsa.jpg|The Titiwangsa Mountains seen from a [[layby]] along the [[Malaysia Federal Route 4|East-West Highway]] near [[Gerik]], [[Perak]].
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File:Cameron highland.JPG|As viewed from [[Cameron Highlands]]
File:Cameron highland.JPG|As viewed from [[Cameron Highlands]]


File:Banjaran titiwangsa2.jpg|The Titiwangsa Mountains tower over the [[North-South Expressway (Malaysia)|North-South Expressway]] in [[Slim River]], [[Perak]].
File:Banjaran titiwangsa2.jpg|The Titiwangsa Mountains tower over the [[North-South Expressway (Malaysia)|North-South Expressway]] in [[Slim River]], Perak.


File:View of Titiwangsa range from Fraser's Hill 3.jpg|View from [[Fraser's Hill]]
File:View of Titiwangsa range from Fraser's Hill 3.jpg|View from [[Fraser's Hill]]
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File:KarakTollPlaza.PNG|The eastern flank of the Titiwangsa Mountains, as seen from the [[East Coast Expressway]] near [[Karak, Pahang|Karak]], [[Pahang]].
File:KarakTollPlaza.PNG|The eastern flank of the Titiwangsa Mountains, as seen from the [[East Coast Expressway]] near [[Karak, Pahang|Karak]], [[Pahang]].


File:Chemperoh 5.jpg|A [[ford (crossing)|ford]] in [[Janda Baik]], [[Pahang]] along the trail to [[Mount Nuang]]
File:Chemperoh 5.jpg|A [[ford (crossing)|ford]] in [[Janda Baik]], Pahang, along the trail to [[Mount Nuang]]


File:From a distance - panoramio (1).jpg|The Titiwangsa Mountains near [[Kuala Kubu Baru]], [[Selangor]].
File:From a distance - panoramio (1).jpg|The Titiwangsa Mountains near [[Kuala Kubu Bharu]], [[Selangor]].


File:View of Batang Kali Town.jpg|The Titiwangsa Mountains near [[Batang Kali]], [[Selangor]].
File:View of Batang Kali Town.jpg|The Titiwangsa Mountains near [[Batang Kali]], Selangor.


File:Kuala Lumpur skyline late afternoon from 29-floor apartment 03.jpg|As seen from a residential skyscraper in [[Kuala Lumpur]]
File:Kuala Lumpur skyline late afternoon from 29-floor apartment 03.jpg|As seen from a residential skyscraper in [[Kuala Lumpur]]


File:Banjaran Titiwangsa di Seremban.jpg|The Titiwangsa Mountains seen from the [[North-South Expressway (Malaysia)|North-South Expressway]] near [[Seremban]], [[Negeri Sembilan]]. Visible are Mts. [[Mount Angsi|Angsi]] (the mountain with the darker hue), Berembun and Telapak Buruk (background).
File:Banjaran Titiwangsa di Seremban.jpg|The Titiwangsa Mountains seen from the [[North-South Expressway (Malaysia)|North-South Expressway]] near [[Seremban]], [[Negeri Sembilan]]. Visible are Mts. [[Mount Angsi|Angsi]] (the mountain with the darker hue), Berembun and [[Mount Telapak Buruk|Telapak Buruk]] (background).


File:Titiwangsa Mountains, Kuala Pilah 1.jpg|The Titiwangsa Mountains near [[Kuala Pilah]], [[Negeri Sembilan]].
File:Istana Seri Menanti (30042023) 20.jpg|The Titiwangsa Mountains at [[Seri Menanti]], Negeri Sembilan.


File:Banjaran Titiwangsa, Rembau.jpg|The southern section of the Titiwangsa Mountains in [[Kota, Negeri Sembilan|Kota]], [[Negeri Sembilan]]. [[Mount Datuk]] rises to the east, which is on the right side of the picture.
File:Banjaran Titiwangsa, Rembau.jpg|The southern section of the Titiwangsa Mountains in [[Kota, Negeri Sembilan|Kota]], Negeri Sembilan. [[Mount Datuk]] rises to the east, which is on the right side of the picture.


File:Gunung Tampin.jpg|[[Mount Tampin]], [[Negeri Sembilan]], the southern terminus of contiguous Titiwangsa Mountains. Taken at [[Pulau Sebang]], [[Malacca]]
File:Gunung Tampin.jpg|[[Mount Tampin]], Negeri Sembilan, the southern terminus of contiguous Titiwangsa Mountains. Seen from [[Pulau Sebang]], [[Malacca]].
</gallery>
</gallery>


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*[http://www.thaibirding.com/locations/south/hb.htm Hala Bala Wildlife Sanctuary]
*[http://www.thaibirding.com/locations/south/hb.htm Hala Bala Wildlife Sanctuary]
{{Mountain ranges of Thailand}}
{{Mountain ranges of Thailand}}

{{Mountain ranges of Malaysia}}


[[Category:Titiwangsa Mountains| ]]
[[Category:Titiwangsa Mountains| ]]

Revision as of 05:18, 10 November 2024

Titiwangsa Mountains
Banjaran Titiwangsa/Besar (Malay)
ทิวเขาสันกาลาคีรี (Thai)
蒂迪旺沙山脉 (Chinese)
蒂迪旺沙山脈 (Chinese)
திதிவாங்சா மலைத்தொடர் (Tamil)
The view of the Titiwangsa Mountains near Mount Suku.
Highest point
PeakGunung Korbu
Elevation2,183 m (7,162 ft)
Dimensions
Length480 km (300 mi) NW/SE
Width120 km (75 mi) NE/SW
Geography
Map
Countries
Provinces/States
Range coordinates5°58′12″N 101°19′37″E / 5.9699°N 101.3269°E / 5.9699; 101.3269
Parent rangeTenasserim Hills
Geology
Rock ages
Rock types
The Titiwangsa during golden hour as viewed from the rural town of Ulu Yam, Selangor.

The Titiwangsa Mountains (Malay: Banjaran Titiwangsa; Jawi: بنجرن تيتيوڠسا‎, pronounced [ˈband͡ʒaˈran titiwaŋˈsa]), also known as Banjaran Besar (lit. 'main range') by locals, is the chain of mountains that forms the backbone of the Malay Peninsula. The northern section of the range is in southern Thailand, where it is known as the Sankalakhiri Range (Thai: ทิวเขาสันกาลาคีรี; RTGS: Thio Khao Sankalakhiri; pronounced [tʰīw kʰǎw sǎn.kāːlāːkʰīːrīː]).

The mountain range acts as a natural divider, dividing Peninsular Malaysia, as well as southernmost Thailand, into east and west coast regions. It also serves as a drainage divide of some major rivers of Peninsular Malaysia such as the Pahang, Perak, Kelantan, Klang and Muar. The length of mountain range is about 480 km from north to south.

Geology

A granitic tor on the summit of Mount Datuk, Rembau District, Negeri Sembilan, near the southern end of the range.
Mogotes dot along the western edge of the range in Kinta District, Perak, part of the Kinta Valley National Geopark.

The Titiwangsa Mountains are predominantly granitic. The mountain range is part of a suture zone that runs north–south, starting in Thailand at the Nan-Uttaradit suture zone (partly coincident with the Dien Bien Phu fault), and extending south towards Peninsular Malaysia (Bentong-Raub suture zone).[1] The eastern half of the Titiwangsa Mountains in Peninsular Malaysia is an amalgamation of continental terranes known as Cimmeria or Indochina, whereas the western half is an amalgamation of continental terranes Sinoburmalaya or Sibumasu. These two halves of terranes were separated by the Paleo-Tethys Ocean.[2][3]

The Cimmeria was separated from Gondwana around 400 mya during the Devonian and rifted towards Laurasia, the northeastern arm of Pangea. It attached to Laurasia completely around 280 mya during the Late Permian.

Sibumasu terranes on the other hand, only started to separate from Gondwana during the Early Permian and rifted towards Indochina. The collision of the Sibumasu terranes and Indochina terranes 200 mya during the Late Triassic resulted in the closure of the Paleo-Tethys Ocean and formation of the modern Titiwangsa Mountain belts.

Seismic hazards

Peninsular Malaysia, while being tectonically stable, has a history of intraplate earthquakes,[4] with most of them of low magnitudes. As the Bentong-Raub suture runs parallel to the Titiwangsa Mountains, a large network of fault lines crisscross the mountain range.[5] The known major fault lines in the mountains are the Bukit Tinggi, Kuala Lumpur and Seremban fault lines, with the first two being the most active.

Between 1984 and 2013, there were tremors ranging from 1.6 to 4.6 on the Richter scale with local epicentres in Kenyir Lake, Manjung, Temenggor, Bukit Tinggi and Kuala Pilah, the latter three being situated along the Titiwangsa Mountains. As a precautionary move, the Department of Minerals and Geosciences pitched 23 Earthquake Benchmark (PAG, Malay: Penanda Aras Gempa) stations around earthquake-prone areas in Peninsular Malaysia, with 13 in Pahang, six in Selangor, and two each in Perak and Negeri Sembilan to monitor possible movements within the fault network.[6] The Ministry of Natural Resources, Environment and Climate Change (NRECC) also pointed out that strong earthquakes centred in neighbouring Sumatra, Indonesia could potentially activate ancient faults in Peninsular Malaysia and the effects of tremors could be felt around areas along the west coast of Peninsular Malaysia.

Geography

Relief map of Peninsular Malaysia, highlighting its mountainous core. The Titiwangsa Mountains is the longest range running along the border between the states of Perak and Selangor on the west coast with Kelantan and Pahang on the east coast, eventually straddling across the state of Negeri Sembilan further south. Nearby systems include Keledang and Bintang Ranges to its northwest, Benom Massif to the southeast, and Tahan Range to the east.

This mountain range is a part of the wider Tenasserim Hills. It forms the southernmost section of the Indo-Malayan cordillera which runs from Tibet through the Kra Isthmus into the Malay Peninsula.[7]

The Titiwangsa Mountains proper begin in the north as the Sankalakhiri Range, a prolongation of the Nakhon Si Thammarat Range which includes the smaller Pattani, Taluban, and Songkhla sub-ranges. The Sankalakhiri marks the border between the Southern Thai provinces of Yala in west and Narathiwat in the east. Across the border into Malaysia, the main stretch of the range runs in a northwest–southeast orientation, straddling the borders between the west coast states of Perak and Selangor with Kelantan and Pahang on the eastern side of the peninsula. From the tripoint of Pahang, Selangor and Negeri Sembilan near Mount Nuang, it then transverses through the middle of the state of Negeri Sembilan, also a west coast state, thus dividing the state into two regions – western Negeri Sembilan, which consists of Seremban, Port Dickson and Rembau Districts, and eastern Negeri Sembilan, composed of the districts of Jelebu, Kuala Pilah, Jempol and Tampin – and terminates in the south near the town of Tampin, in the southern part of the state.[8][9][10] Outcrops of Titiwangsa granite, mainly consisting of inselbergs, project further south into Malacca, where it abuts in the waters of the Strait of Malacca in Pulau Besar.[11]

In general, the greatest elevations occur along the northern and central sections of the range, with its highest point measuring 2,183 m (7,162 ft) on Gunung Korbu, Perak. On the Thai side, the highest point is 1,533 m (5,026 ft) Ulu Titi Basah (ยูลูติติ บาซาห์), at the Thai/Malaysian border between Yala province and Perak.[12] On the other hand, the height gradually diminishes towards the southern reaches of the range, which mainly runs through Negeri Sembilan, with elevations ranging from 1,462 m (4,797 ft) at its highest on Mount Besar Hantu, on the border between the state and Pahang, as well as 1,193 m (3,914 ft) on Mount Telapak Buruk on the boundary between the districts of Seremban and Jelebu to 500–700 metres (1,600–2,300 ft).

Features

Tropical rainforest in the Perakian/Pahangese Titiwangsa, part of the Central Forest Spine. Taken near Ringlet
Central Forest Spine signboard on Federal Route FT 51 in the Negri Titiwangsa near Bukit Putus

The rainforests of the Titiwangsa Mountains form part of the Titiwangsa Forest Complex, which is itself part of the larger Central Forest Spine conservation area. A number of roads and highways cut through the mountain range, effectively acting as mountain passes linking settlements on either side of the range.

Tea plantation in Cameron Highlands
Genting Highlands, as seen from Kuala Lumpur

Several popular tourist destinations such as Royal Belum, hill resorts such as Cameron Highlands, Genting Highlands and Fraser's Hill are located on the range.

Two of Malaysia's largest metropolitan areas are located along the western fringes of the mountain range, namely Greater Kuala Lumpur (ranked #1) and Kinta Valley (ranked #4). The Kinta Valley Geopark encompasses the entirety of Kinta Valley, where kegelkarst topography is prevalent.

Protected areas

Thailand

Malaysia

The mountain range was the subject of the patriotic song "Titiwangsa", which was first sung by Saloma. Its lyrics glorifies the magnificence and beauty of the Titiwangsa Mountains, and its significance to Malaya as a whole.

References

  1. ^ Racey, Andrew (2009). "Mesozoic red bed sequences in SE Asia and the significance of the Khorat Group of NE Thailand". In Buffetaut, Eric (ed.). Late Palaeozoic and Mesozoic Ecosystems in SE Asia. Geological Society of London. p. 46. ISBN 9781862392755. Retrieved 20 June 2019.
  2. ^ Metcalfe, I., 2000, "The Bentong-Raub Suture Zone", Journal of Asian Earth Sciences, v. 18, p. 691-712
  3. ^ Metcalfe, I., 2002, "Permian tectonic framework and palaeogeography of SE Asia", Journal of Asian Earth Sciences, v. 20, p. 551-566
  4. ^ Ada kebarangkalian gempa bumi berlaku di Malaysia - NRECC astroawani.com 19 April 2023
  5. ^ "Earthquakes in Malaysia: Should we be worried and how to reduce its impact on our buildings?". 12 January 2022.
  6. ^ "Gempa bumi: Rujuk peta bahaya seismik sebelum reka bangunan". 2 May 2023.
  7. ^ Avijit Gupta, The Physical Geography of Southeast 0Asia, Oxford University Press, 2005. ISBN 978-0-19-924802-5
  8. ^ Yaakub Idrus. Rumah Melayu Negeri Sembilan: satu analisis seni bina Melayu. Penerbit Fajar Bakti, 1966, p. 11. https://malaycivilization.com.my/omeka/files/original/a884b36ae16d4af41735580e8b03038b.pdf
  9. ^ "Places of Interest | Official Portal of Tampin District Council (MDT)". Mdtampin.gov.my. Retrieved 2023-04-04.
  10. ^ "Vegetation of Peninsular Malaysia". Retrieved 3 March 2024.
  11. ^ "Empat kawasan di Melaka berpotensi diiktiraf Geopark Kebangsaan". Astro Awani. 2023-10-22.
  12. ^ "Gunong Ulu Titi Basah, Thailand - Geographical Names, map, geographic coordinates". geographic.org. Retrieved 3 March 2024.