Mount Bombalai
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Mount Bombalai
Mount Bombalai ( ms, Gunung Bombalai) is a volcanic cone mountain in the Tawau Division of Sabah, Malaysia. It reaches a height of approximately . Geology The mountain is part of the Tawau volcanic field which contributed to the prominent topographic features of the Semporna Peninsula in northeastern Borneo and the western side of a valley in its middle section. The low volcanic cone is north of Sebatik Island and has a roughly 300-m-wide crater breached to the south. Two young lava flows extend almost to the coastal plain. The flows are considered younger than a lava flow radiocarbon dated at about 27,000 years before present, and the extrusion of basaltic lavas possibly continued into the Holocene epoch. Presence of geothermal activity has been reported in the surrounding mountains. See also * List of volcanoes in Malaysia There are several volcanoes in the territory of Malaysia, mostly located in the state of Sabah. See also * List of mountains in Malaysia Ref ...
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Tawau Division
Tawau Division ( ms, Bahagian Tawau) is one of the five administrative sub-divisions of Sabah, Malaysia. It occupies a total of 14,905 square kilometres or 20% of Sabah's territory. The main towns include the capital of Tawau, Lahad Datu, Kunak and Semporna. Tawau division has 26% of Sabah's total population, with the main indigenous groups consisting of the Bajau, Suluk, Ida'an, Tidong, Cocos, Murut, Lun Bawang/Lun Dayeh as well as a minority of mixed ethnic groups. Large numbers of both legal and illegal immigrants from Indonesia such as the Buginese and Torajans, from East Timor the Timorese, from the Philippines the Tausūg and Visayans as well South and West Asian immigrants such as Pakistanis, Indians and Arabs can be found in this area. As with the rest of Sabah, the division also has large numbers of ethnic Chinese. Tawau port is the third largest port after Kota Kinabalu and Sandakan. The port serves as a major timber and agricultural products export centre. There a ...
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Sabah
Sabah () is a States and federal territories of Malaysia, state of Malaysia located in northern Borneo, in the region of East Malaysia. Sabah borders the Malaysian state of Sarawak to the southwest and the North Kalimantan province of Indonesia to the south. The Federal Territory (Malaysia), Federal Territory of Labuan is an island just off Sabah's west coast. Kota Kinabalu is the state capital city, the economic centre of the state, and the seat of the Government of Sabah, Sabah state government. Other major towns in Sabah include Sandakan and Tawau. The 2020 census recorded a population of 3,418,785 in the state. It has an equatorial climate with tropical rainforests, abundant with animal and plant species. The state has long mountain ranges on the west side which forms part of the Crocker Range National Park. Kinabatangan River, the second longest river in Malaysia runs through Sabah. The highest point of Sabah, Mount Kinabalu is also the highest point of Malaysia. The ear ...
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Malaysia
Malaysia ( ; ) is a country in Southeast Asia. The federation, federal constitutional monarchy consists of States and federal territories of Malaysia, thirteen states and three federal territories, separated by the South China Sea into two regions: Peninsular Malaysia and Borneo's East Malaysia. Peninsular Malaysia shares a land and maritime Malaysia–Thailand border, border with Thailand and Maritime boundary, maritime borders with Singapore, Vietnam, and Indonesia. East Malaysia shares land and maritime borders with Brunei and Indonesia, and a maritime border with the Philippines and Vietnam. Kuala Lumpur is the national capital, the country's largest city, and the seat of the Parliament of Malaysia, legislative branch of the Government of Malaysia, federal government. The nearby Planned community#Planned capitals, planned capital of Putrajaya is the administrative capital, which represents the seat of both the Government of Malaysia#Executive, executive branch (the Cabine ...
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Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ...
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Volcanic Cone
Volcanic cones are among the simplest volcanic landforms. They are built by ejecta from a volcanic vent, piling up around the vent in the shape of a cone with a central crater. Volcanic cones are of different types, depending upon the nature and size of the fragments ejected during the eruption. Types of volcanic cones include stratocones, spatter cones, tuff cones, and cinder cones. Stratocone Stratocones are large cone-shaped volcanoes made up of lava flows, explosively erupted pyroclastic rocks, and igneous intrusives that are typically centered around a cylindrical vent. Unlike shield volcanoes, they are characterized by a steep profile and periodic, often alternating, explosive eruptions and effusive eruptions. Some have collapsed craters called calderas. The central core of a stratocone is commonly dominated by a central core of intrusive rocks that range from around to over several kilometers in diameter. This central core is surrounded by multiple generations of ...
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Volcanic Field
A volcanic field is an area of Earth's crust that is prone to localized volcanic activity. The type and number of volcanoes required to be called a "field" is not well-defined. Volcanic fields usually consist of clusters of up to 100 volcanoes such as cinder cones. Lava flows may also occur. They may occur as a monogenetic volcanic field or a polygenetic volcanic field. Description Alexander von Humboldt observed in 1823 that geologically young volcanoes are not distributed uniformly across the Earth's surface, but tend to be clustered into specific regions. Young volcanoes are rarely found within cratons, but are characteristic of subduction zones, rift zones, or in ocean basins. Intraplate volcanoes are clustered along hotspot traces. Within regions of volcanic activity, volcanic fields are clusters of volcanoes that share a common magma source. Scoria cones are particularly prone to cluster into volcanic fields, which are typically in diameter and consist of several tens ...
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Semporna Peninsula
The Semporna Peninsula ( ms, Semenanjung Semporna) is a peninsula in Tawau Division, Sabah, Malaysia. It consists of coastal areas and numerous isolated hills and mountains rising to over . The Peninsula is also considered as a volcanic arc of the region with several volcanoes active during the Holocene period is located on the area. Geology The formation of the peninsula involved process of intrusive and volcanic activity with the area consists of erosion surfaces within of sea level, out of which rise hills of the more resistant rocks and upon which volcanic landforms have been superimposed. At the beginning of the Miocene period, much of the area was submerged and widespread volcanic activity of rhyolite with andesite and basalt types occurred during the period, followed by another three periods of activity. Early Pliocene gave intrusive hornblende diorite (particularly to eastern Timbun Mata), associated with volcanic breccia (eastern coast Sabah of Gaya and Boheydulang I ...
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Borneo
Borneo (; id, Kalimantan) is the third-largest island in the world and the largest in Asia. At the geographic centre of Maritime Southeast Asia, in relation to major Indonesian islands, it is located north of Java, west of Sulawesi, and east of Sumatra. The island is politically divided among three countries: Malaysia and Brunei in the north, and Indonesia to the south. Approximately 73% of the island is Indonesian territory. In the north, the East Malaysian states of Sabah and Sarawak make up about 26% of the island. The population in Borneo is 23,053,723 (2020 national censuses). Additionally, the Malaysian federal territory of Labuan is situated on a small island just off the coast of Borneo. The sovereign state of Brunei, located on the north coast, comprises about 1% of Borneo's land area. A little more than half of the island is in the Northern Hemisphere, including Brunei and the Malaysian portion, while the Indonesian portion spans the Northern and Southern hemisph ...
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Sebatik Island
Sebatik Island (Indonesian/Malay: ''Pulau Sebatik'') is an island off the eastern coast of Borneo, partly within Indonesia and partly within Malaysia. It is one of the 92 officially listed outlying islands of Indonesia. Sebatik has an area of approximately . The minimum distance between Sebatik Island and the mainland of Borneo is about . Sebatik Island lies between Tawau Bay (''Teluk Tawau'') to the north and Sibuku Bay (''Teluk Sibuku'') to the south. The town of Tawau lies in Sabah just to the north. The island is bisected at roughly 4° 10' north by the Indonesia–Malaysia border - the northern part belongs to Sabah, Malaysia (''Sebatik Malaysia'') while the southern part belongs to North Kalimantan (previously East Kalimantan), Indonesia (''Sebatik Indonesia''). Sebatik Malaysia has a population estimated to be approximately 25,000; there were 47,571 people in Sebatik Indonesia as at the 2020 Census. The demarcated international border between Malaysia and Indonesia ...
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Geothermal Energy
Geothermal energy is the thermal energy in the Earth's crust which originates from the formation of the planet and from radioactive decay of materials in currently uncertain but possibly roughly equal proportions. The high temperature and pressure in Earth's interior cause some rock to melt and solid mantle to behave plastically. This results in parts of the mantle convecting upward since it is lighter than the surrounding rock. Temperatures at the core–mantle boundary can reach over 4000 °C (7200 °F). Geothermal heating, using water from hot springs, for example, has been used for bathing since Paleolithic times and for space heating since ancient Roman times. More recently geothermal power, the term used for generation of electricity from geothermal energy, has gained in importance. It is estimated that the earth's geothermal resources are theoretically more than adequate to supply humanity's energy needs, although only a very small fraction is currently being ...
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Universiti Malaysia Sabah
, image = Seal of Universiti Malaysia Sabah.png , image_size = , caption = Seal , motto = ''Bertekad Cemerlang'' (Malay) Jawi: , mottoeng = Strive to Excel , established = 24 November 1994 , type = Public University , chancellor = His Excellency the Governor of Sabah Tun Datuk Seri Panglima (Dr.) Haji Juhar bin Haji Mahiruddin , head_label = , head = , vice_chancellor = Professor Datuk Dr. Kasim Hj Mansor , city = Kota Kinabalu, Sabah , country = Malaysia , campus = Kota KinabaluLabuanSandakan , students = , affiliations = , website = , logo = Logo_Universiti_Malaysia_Sabah.png , undergrad = 14,637 (2020) , postgrad = 2,939 (2020) , academic_staff ...
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List Of Volcanoes In Malaysia
There are several volcanoes in the territory of Malaysia, mostly located in the state of Sabah. See also * List of mountains in Malaysia References Further reading {{DEFAULTSORT:Volcanoes in Malaysia Malaysia Volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates a ...
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