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Sankala Khiri Mountain Range
The Titiwangsa Mountains (Malay: ''Banjaran Titiwangsa,'' بنجرن تيتيوڠسا, ), also known as ''"Banjaran Besar"'' (Big 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 Sankalakhiri Range ( th, ทิวเขาสันกาลาคีรี, ). The range acts as a natural divider, dividing Peninsular Malaysia, as well as southernmost Thailand, into east and west coast regions. It is also the source 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 The Titiwangsa 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). The western ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Malay Language
Malay (; ms, Bahasa Melayu, links=no, Jawi alphabet, Jawi: , Rejang script, Rencong: ) is an Austronesian languages, Austronesian language that is an official language of Brunei, Indonesia, Malaysia, and Singapore, and that is also spoken in East Timor and parts of the Philippines and Thailand. Altogether, it is spoken by 290 million people (around 260 million in Indonesia alone in its own literary standard named "Indonesian language, Indonesian") across Maritime Southeast Asia. As the or ("national language") of several states, Standard Malay has various official names. In Malaysia, it is designated as either ("Malaysian Malay") or also ("Malay language"). In Singapore and Brunei, it is called ("Malay language"). In Indonesia, an autonomous normative variety called ("Indonesian language") is designated the ("unifying language" or lingua franca). However, in areas of Central to Southern Sumatra, where vernacular varieties of Malay are indigenous, Indonesians refe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klang River
The Klang River ( ms, Sungai Klang) is a river which flows through Kuala Lumpur and Selangor in Malaysia and eventually flows into the Straits of Malacca. It is approximately in length and drains a basin of about . The Klang River has 11 major tributaries. Because the river flows through Klang Valley, which is a heavily populated area of more than four million people, it is considerably polluted, because of deep siltation caused by human waste from informal settlers of the riverbank and even from some business establishments without septic tanks or sewage treatment plants and by soil carried by mudflows from mountains. Heavy development has narrowed certain stretches of the river to the point that it resembles a large storm drain in some places. This contributes to flash floods in Kuala Lumpur, especially after heavy rain. Course , The Klang River originates from the Klang Gates Quartz Ridge in Gombak, near the border with Pahang, northeast of Kuala Lumpur. It is joine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleo-Tethys Ocean
The Paleo-Tethys or Palaeo-Tethys Ocean was an ocean located along the northern margin of the paleocontinent Gondwana that started to open during the Middle Cambrian, grew throughout the Paleozoic, and finally closed during the Late Triassic; existing for about 400 million years. Paleo-Tethys was a precursor to the Tethys Ocean (also called the Neo-Tethys) which was located between Gondwana and the Hunic terranes (continental fragments that broke-off Gondwana and moved north). It opened as the Proto-Tethys Ocean subducted under these terranes and closed as the Cimmerian terranes (that also broke-off Gondwana and moved north) gave way to the Tethys Ocean. Confusingly, the Neo-Tethys is sometimes defined as the ocean south of a hypothesised mid-ocean ridge separating Greater Indian from Asia, in which case the ocean between Cimmeria and this hypothesised ridge is called the Meso-Tethys, i.e. the "Middle-Tethys". The so-called Hunic terranes are divided into the ''European Hunic' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cimmerian Plate
Cimmeria was an ancient continent, or, rather, a string of microcontinents or terranes, that rifted from Gondwana in the Southern Hemisphere and was accreted to Eurasia in the Northern Hemisphere. It consisted of parts of present-day Turkey, Iran, Afghanistan, Pakistan, Tibet, China, Myanmar, Thailand, and Malaysia. Cimmeria rifted from the Gondwanan shores of the Paleo-Tethys Ocean during the Early Permian and as the Neo-Tethys Ocean opened behind it, during the Permian, the Paleo-Tethys closed in front of it. Because the different chunks of Cimmeria drifted northward at different rates, a Meso-Tethys Ocean formed between the different fragments during the Cisuralian. Cimmeria rifted off Gondwana from east to west, from Australia to the eastern Mediterranean. It stretched across several latitudes and spanned a wide range of climatic zones. History of the concept First concepts A "large, ancient Mediterranean Sea" was first proposed by Austrian palaeontologist Melchior Neumay ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Terrane
In geology, a terrane (; in full, a tectonostratigraphic terrane) is a crust fragment formed on a tectonic plate (or broken off from it) and accreted or " sutured" to crust lying on another plate. The crustal block or fragment preserves its own distinctive geologic history, which is different from that of the surrounding areas—hence the term "exotic" terrane. The suture zone between a terrane and the crust it attaches to is usually identifiable as a fault. A sedimentary deposit that buries the contact of the terrane with adjacent rock is called an overlap formation. An igneous intrusion that has intruded and obscured the contact of a terrane with adjacent rock is called a stitching pluton. Older usage of ''terrane'' simply described a series of related rock formations or an area having a preponderance of a particular rock or rock groups. Overview A tectonostratigraphic terrane is not necessarily an independent microplate in origin, since it may not contain the full thickness ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raub District
Raub District is a district in Pahang, Malaysia. Located in the west of Pahang, the district bordered Lipis District, Jerantut District, Temerloh District, Bentong District and Hulu Selangor District of Selangor clockwisely. Raub district consists of 7 ''mukim'' (sub-districts), namely Batu Talam, Sega, Semantan Ulu, Dong, Ulu Dong, Gali and Tras. With an area of 2,271 km², Raub district is situated in west of Pahang and between two range, Titiwangsa Range and Benom Mountain Range. Raub district also is home to Fraser's Hill. The administrative seat of this district is the town of Raub. Demographics The following is based on Department of Statistics Malaysia 2010 census. Federal Parliament and State Assembly Seats Raub district representative in the Federal Parliament (Dewan Rakyat) List of Raub district representatives in the State Legislative Assembly (Dewan Undangan Negeri) Subdistricts Raub District is divided into 7 mukims, which are: * Batu Talam (5 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bentong
Bentong (Jawi alphabet, Jawi: ﺑﻨﺘﻮڠ), the seat of Bentong District, is a town located in western Pahang, Malaysia, at the border with the state of Selangor in the west and the state of Negeri Sembilan in the south. Government Bentong Municipal Council ( ms, Majlis Perbandaran Bentong) is the local authority for the whole of Bentong District including Bentong town. From 5 May 1955 until 30 June 1981, Bentong town was governed by the Bentong Town Council ( ms, Majlis Bandaran Bentong). On 1 July 1981, the Bentong Town Council was merged with 5 local councils of Karak, Sungai Dua, Telemong, Manchis and Bukit Tinggi and 8 village councils of Kampung Shafie, Kampung Simpang Pelangai, Sungai Gapoi New Village, Kampung Jambu Rias, Kampung Benus, Genting Sempah, Kampung Janda Baik and Sungai Penjuring New Village to form the Bentong District Council ( ms, Majlis Daerah Bentong). The administrative area of Bentong District Council at the time of establishment was , consisting ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uttaradit
The original name of Mueang district, Uttaradit, was Bang Pho. This district was under the control of Phi Chai District. Later, it was established as Uttaradit Province and Bang Pho District became the capital district. It was changed to Mueang Uttaradit District recently. The district is the seat of government and the center of economic activity of Uttaradit Province. Uttaradit is 483 km north of Bangkok. Geography The district is surrounded by the following districts: * North – Den Chai District ( Phrae Province) and Tha Pla District. * East – Tha Pla and Thong Saen Khan Districts. * South – Thong Saen Khan and Tron Districts. * West – Laplae District. History In the past, Mueang District was called ''Bang Pho Tah It''. It grew rapidly due to its harbor. King Rama V ordered the capital moved from Phi Chai District to Muang District. Next, in the reign of King Rama VI, the king ordered the incorporation of Mueang District into Uttaradit Province. Climate Ut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suture (geology)
In structural geology, a suture is a joining together along a major fault zone, of separate terranes, tectonic units that have different plate tectonic, metamorphic and paleogeographic histories. The suture is often represented on the surface by an orogen or mountain range. Overview In plate tectonics, sutures are the remains of subduction zones, and the terranes that are joined together are interpreted as fragments of different palaeocontinents or tectonic plates. Outcrops of sutures can vary in width from a few hundred meters to a couple of kilometers. They can be networks of mylonitic shear zones or brittle fault zones, but are usually both. Sutures are usually associated with igneous intrusions and tectonic lenses with varying kinds of lithologies from plutonic rocks to ophiolitic fragments. An example from Great Britain is the Iapetus Suture which, though now concealed beneath younger rocks, has been determined by geophysical means to run along a line roughly paralle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
