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Comoro River
The Comoro River ( pt, Ribeira de Comoro or , tet, Mota Komoro) is a river in East Timor. It flows north into Ombai Strait, reaching the coast in the north western suburbs of the capital, Dili. In its lower reaches, it is the main and largest of Dili's four major rivers. Course The headwaters of the river are in East Timor's central mountains south of Dili. From there, the river flows northeast to the southern edge of Dili's southwestern suburbs. It then turns north and heads through Dili's western suburbs, initially along the border between the municipalities of Dili and Liquiçá, and then by traversing the Dom Aleixo administrative post in Dili municipality, where it passes under the Hinode Bridge and, further downstream, the CPLP Bridge. In its lower reaches, the river is the main and largest of Dili's four major rivers, and is very wide, with steep banks. It has a bed of stone and gravel, is mostly dry, and is often braided when not either dry or in flood. A short dista ...
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Municipalities Of East Timor
A municipality is usually a single administrative division having municipal corporation, corporate status and powers of self-government or jurisdiction as granted by national and regional laws to which it is subordinate. The term ''municipality'' may also mean the governing body of a given municipality. A municipality is a general-purpose administrative subdivision, as opposed to a special district (United States), special-purpose district. The term is derived from French language, French and Latin language, Latin . The English language, English word ''municipality'' derives from the Latin social contract (derived from a word meaning "duty holders"), referring to the Latin communities that supplied Rome with troops in exchange for their own incorporation into the Roman state (granting Roman citizenship to the inhabitants) while permitting the communities to retain their own local governments (a limited autonomy). A municipality can be any political jurisdiction (area), jurisd ...
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Bank (geography)
In geography, a bank is the land alongside a body of water. Different structures are referred to as ''banks'' in different fields of geography, as follows. In limnology (the study of inland waters), a stream bank or river bank is the terrain alongside the bed of a river, creek, or stream. The bank consists of the sides of the channel, between which the flow is confined. Stream banks are of particular interest in fluvial geography, which studies the processes associated with rivers and streams and the deposits and landforms created by them. Bankfull discharge is a discharge great enough to fill the channel and overtop the banks. The descriptive terms ''left bank'' and ''right bank'' refer to the perspective of an observer looking downstream; a well-known example of this being the sections of Paris as defined by the river Seine. The shoreline of ponds, swamps, estuaries, reservoirs, or lakes are also of interest in limnology and are sometimes referred to as banks. The grade ...
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Berloi Waterfall
The Berloi Waterfall ( pt, Cascata de Berloi, tet, Be Tuda Berloi) is a small waterfall in the municipality of Aileu, East Timor. It forms part of a minor tributary of the Comoro River. Geography The waterfall is located within the ''suco'' of Fatisi and the Laulara administrative post in the Aileu municipality, a short distance from Dili, the capital city. The stream that passes over the waterfall is sometimes referred to as the Berloi River or the Berloi-Fatisi River, and is a minor tributary of the Comoro River. From the base of the waterfall, the stream flows initially in a southwesterly direction for a short distance. It then turns northwest to mark the border between the municipalities of Aileu and Ermera for about , until it flows into the Comoro River about downstream of the village of . History On 19 August 1975, during the , a member of Unetim, the Fretilin youth wing, killed a man who was being detained by Fretilin at the detention centre in Unmenlau, in the then ...
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Commission For Reception, Truth And Reconciliation In East Timor
The Commission for Reception, Truth and Reconciliation in East Timor (more commonly known by its Portuguese acronym CAVR: Comissão de Acolhimento, Verdade e Reconciliação de Timor Leste) was an independent truth commission established in East Timor in 2001 under the UN Transitional Administration in East Timor (UNTAET) and charged to “inquire into human rights violations committed on all sides, between April 1974 and October 1999, and facilitate community reconciliation with justice for those who committed less serious offenses.” The idea of a truth commission in East Timor was first agreed by the National Council of Timorese Resistance in 2000. The Commission had a triple mandate as reflected in its name, to address: (1) reception (acolhimento), the return of Timorese displaced into Indonesian West Timor and their reintegration into their communities, which the Commission described as "people embracing each other as East Timorese, of coming back to our selves, living under ...
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Mindat
Mindat may refer to: Places in Burma/Myanmar *Mindat, Chin State, in Burma *Mindat Township, in Burma *Mindat District in Chin State, Burma Other uses *Mindat Min Kanaung Mintha ( my, ကနောင်မင်းသား; 31 January 1820 – 2 August 1866) was crown prince of Burma and son of King Tharrawaddy and younger brother of King Mindon of Burma. Towards the end of the Second Anglo-Burmese Wa ..., a Burmese prince * Mindat.org, an online mineralogy database {{dab, geo ...
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Hydrodynamic Scour
Hydrodynamic scour is the removal of sediment such as silt, sand and gravel from around the base of obstructions to the flow in the sea, rivers and canals. Scour, caused by fast flowing water, can carve out scour holes, compromising the integrity of a structure. It is an interaction between the hydrodynamics and the geotechnical properties of the substrate. It is a notable cause of Bridge scour, bridge failure and a problem with most marine structures supported by the seabed in areas of significant Tidal scour, tidal and ocean current. It can also affect biological ecosystems and heritage assets. Mechanism file:Kolkschema.svg, lang=en, upright=1.3, Mechanism of formation, alt=sketch Any obstruction within flowing water will produce changes in velocity within the water column. The flow changes that occur in the vicinity of the substrate may cause differential movement in the bed materials near the obstruction. The magnitude of these changes varies with stream velocity, feature sha ...
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Gabion
A gabion (from Italian ''gabbione'' meaning "big cage"; from Italian ''gabbia'' and Latin ''cavea'' meaning "cage") is a cage, cylinder or box filled with rocks, concrete, or sometimes sand and soil for use in civil engineering, road building, military applications and landscaping. For erosion control, caged riprap is used. For dams or in foundation construction, cylindrical metal structures are used. In a military context, earth- or sand-filled gabions are used to protect sappers, infantry, and artillerymen from enemy fire. Leonardo da Vinci designed a type of gabion called a ''Corbeille Leonard'' ("Leonard basket") for the foundations of the San Marco Castle in Milan. Civil engineering The most common civil engineering use of gabions was refined and patented by Gaetano Maccaferri in the late 19th century in Sacerno, Emilia Romagna and used to stabilize shorelines, stream banks or slopes against erosion. Other uses include retaining walls, noise barriers, temporary flood w ...
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Wet Season
The wet season (sometimes called the Rainy season) is the time of year when most of a region's average annual rainfall occurs. It is the time of year where the majority of a country's or region's annual precipitation occurs. Generally, the season lasts at least a month. The term ''green season'' is also sometimes used as a euphemism by tourist authorities. Areas with wet seasons are dispersed across portions of the tropics and subtropics. Under the Köppen climate classification, for tropical climates, a wet season month is defined as a month where average precipitation is or more. In contrast to areas with savanna climates and monsoon regimes, Mediterranean climates have wet winters and dry summers. Dry and rainy months are characteristic of tropical seasonal forests: in contrast to tropical rainforests, which do not have dry or wet seasons, since their rainfall is equally distributed throughout the year.Elisabeth M. Benders-Hyde (2003)World Climates.Blue Planet Biomes. Retr ...
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Coral Reef
A coral reef is an underwater ecosystem characterized by reef-building corals. Reefs are formed of colonies of coral polyps held together by calcium carbonate. Most coral reefs are built from stony corals, whose polyps cluster in groups. Coral belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish. Unlike sea anemones, corals secrete hard carbonate exoskeletons that support and protect the coral. Most reefs grow best in warm, shallow, clear, sunny and agitated water. Coral reefs first appeared 485 million years ago, at the dawn of the Early Ordovician, displacing the microbial and sponge reefs of the Cambrian. Sometimes called ''rainforests of the sea'', shallow coral reefs form some of Earth's most diverse ecosystems. They occupy less than 0.1% of the world's ocean area, about half the area of France, yet they provide a home for at least 25% of all marine species, including fish, mollusks, worms, crustaceans, echinoderms, sp ...
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Bay Of Dili
The Bay of Dili ( pt, Baía de Díli, tet, Baía Dili) is a bay on the north coast of East Timor adjacent to Dili, its capital city. The bay forms part of Ombai Strait, which separates the Alor Archipelago from the islands of Wetar, Atauro, and Timor in the Lesser Sunda Islands. Geography The bay is located on the southern side of Ombai Strait, immediately to the north of the similarly named Dili municipality. It extends from the mouth of the Comoro River in the west to Cristo Rei Beach, Cape Fatucama, and the ''Cristo Rei of Dili'' statue in the north east. History Early records about Timor, especially before the 1700s, are sparse. Portuguese settlers are said to have arrived in the Bay of Dili in 1520, and to have established a small settlement there. A quarter of a millenium later, in 1769, the governor of Portuguese Timor sought to break the influence of powerful local families in Lifau, Oecusse, his then residence, by moving the colonial administration and 1,200 people ...
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Presidente Nicolau Lobato International Airport
Dili Airport , officially Presidente Nicolau Lobato International Airport ( pt, Aeroporto Internacional Presidente Nicolau Lobato, ), and formerly Comoro Airport ( id, Bandar Udara Komoro), is an international airport serving Dili, the capital city of East Timor. Since 2002, the airport has been named after Nicolau dos Reis Lobato (1946–1978), an East Timorese politician and national hero. Location The airport is located in the '' suco'' of , which is part of the Dom Aleixo administrative post, in the western suburbs of Dili. It faces the Ombai Strait to its north and west, and the Comoro River to its east. Its runway (08/26) runs broadly east-west. North of the airport, between the runway and Ombai Strait, is a residential zone that includes houses, a small area of agricultural land, a school, a church, and a cemetery. At the zone's northern edge is Beto Tasi Beach, a hidden stretch of shoreline known to the local community and also used for fishing. History 1939–1975 The ...
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Channel (geography)
In physical geography, a channel is a type of landform consisting of the outline of a path of relatively shallow and narrow body of water or of other fluids (e.g., lava), most commonly the confine of a river, river delta or strait. The word is cognate to canal, and sometimes takes this form, e.g. the Hood Canal. Formation Channel initiation refers to the site on a mountain slope where water begins to flow between identifiable banks.Bierman, R. B, David R. Montgomery (2014). Key Concepts in Geomorphology. W. H. Freeman and Company Publishers. United States. This site is referred to as the channel head and it marks an important boundary between hillslope processes and fluvial processes. The channel head is the most upslope part of a channel network and is defined by flowing water between defined identifiable banks. A channel head forms as overland flow and/or subsurface flow accumulate to a point where shear stress can overcome erosion resistance of the ground surface. Channel he ...
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