Ambondromahabo
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Ambondromahabo
Ambondromahabo is a village near Ambondromamy, Boeny, Madagascar. An extinct mammal from the Jurassic period, ''Ambondro mahabo'', is named after the village, which is close to the locality within the Isalo III geological formation A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exp ... where the fossil was found. References Populated places in Boeny {{Boeny-geo-stub ...
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Ambondro Mahabo
''Ambondro mahabo'' is a mammal from the Middle Jurassic (Bathonian) Isalo III Formation (about 167 million years ago) of Madagascar. The only described species of the genus ''Ambondro'', it is known from a fragmentary lower jaw with three teeth, interpreted as the last premolar and the first two molars. The premolar consists of a central cusp with one or two smaller cusps and a cingulum (shelf) on the inner, or lingual, side of the tooth. The molars also have such a lingual cingulum. They consist of two groups of cusps: a trigonid of three cusps at the front and a talonid with a main cusp, a smaller cusp, and a crest at the back. Features of the talonid suggest that ''Ambondro'' had tribosphenic molars, the basic arrangement of molar features also present in marsupial and placental mammals. It is the oldest known mammal with putatively tribosphenic teeth; at the time of its discovery it antedated the second oldest example by about 25 million years. Upon its description in 1999 ...
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Isalo III Formation
The Isalo III Formation is a geological formation in Madagascar, off the eastern coast of Africa. It dates back to the Middle Jurassic.Weishampel et al., 2004, pp.542-543 The use of the term "Isalo III" is somewhat controversial as the two prior units Isalo I and II are Triassic cross-bedded sandstone units that form a continuous depositional sequence, while the "Isalo III" sandstones are not part of the same depositional sequence, and were deposited considerably later. and are perhaps better treated as part of several separate formations.Geiger et al., 2004 It is traditionally divided into two subunits the lower, Bajocian aged Isalo IIIa unit also known as the Beronono Formation and the upper, Bathonian aged Isalo IIIb unit also known as the Sakaraha Formation or Sakahara Formation. The Sakaraha Formation consists of sandstones, marls and carbonates and represents a coastal plain environment, and is laterally equivalent to the predominantly carbonate Bemaraha Formation, which ...
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Regions Of Madagascar
Madagascar is divided into 23 regions (''faritra''). These formerly second-tier administrative divisions became first-level administrative divisions when the former six provinces were dissolved on 4 October 2009. Elections Elections for the regional councils were held on 16 March 2008. See also * Subdivisions of Madagascar * Provinces of Madagascar * Districts of Madagascar *List of regions of Madagascar by Human Development Index This is a list of the 22 regions of Madagascar (since 2009) by Human Development Index as of 2018. See also * List of countries by Human Development Index References {{reflist Madagascar Madagascar Human Development Index ... * List of cities in Madagascar References Sources * Population, area: ''Madagascar: Profil des marchés pour les évaluations d’urgence de la sécurité alimentaire'* (in French:Découpage Territorial - L'Express.mg Regions of Madagascar, Subdivisions of Madagascar Madagascar, ...
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Boeny Region
Boeny is a region in northwestern Madagascar. It borders Sofia Region to the northeast, Betsiboka to the south and Melaky to the southwest. The capital of the region is Mahajanga, and the population was 931,171 in 2018. The area of Boeny is . Administrative divisions Boeny Region is divided into six districts, which are sub-divided into 43 communes. * Ambato-Boeni District - 11 communes * Mahajanga I District - 1 commune * Mahajanga II District - 5 communes * Marovoay District - 12 communes * Mitsinjo District - 7 communes * Soalala District - 3 communes Transport Airports * Mahajanga Airport *Soalala Airport Protected areas * Mahavavy-Kinkony Wetland Complex * Bombetoka Beloboka New Protected Area * Antrema New Protected Area *Ankarafantsika National Park *Baie de Baly National Park * Tsingy de Namoroka National Park See also *Boina Kingdom The Kingdom of Boina (sometimes known as Iboina) was a traditional state situated in what is now Madagascar. History The kingdom was ...
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Districts Of Madagascar
Districts are second-level administrative divisions of Madagascar below the regions. There are 114 districts in Madagascar. Districts are in their turn divided into communes; while some of the districts in urban areas (such as the City districts of Antananarivo, Antsirabe I, Antsiranana I, Fianarantsoa I, Toamasina I and Toliara I) and offshore islands (such as the districts of Nosy Be and Nosy Boraha) each consist of only one commune, most of the districts are divided typically into 5–20 communes. List of districts * Note that Isandra, Lalangina and Vohibato Districts previously formed Fianarantsoa II District (within Haute Matsiatra Region) which has now been split into these three new districts. Another new district was formed by the splitting off of the new Mandoto District from Betafo District (within Vakinankaratra Region). See also * Subdivisions of Madagascar * Provinces of Madagascar * Regions of Madagascar Madagascar is divided into 23 region ...
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Ambato-Boeni District
Ambato-Boeni is a district of Boeny in Madagascar. Communes The district is further divided into 11 communes: * Ambato Ambarimay * Ambondromamy * Andranofasika * Andranomamy Andranomamy is a town and commune ( mg, kaominina) in Madagascar. It belongs to the district of Ambato-Boeni, which is a part of Boeny Region. The population of the commune was estimated to be approximately 13,000 in 2001 commune census. Primary ... * Anjiajia * Ankijabe * Ankirihitra * Madirovalo * Manerinerina * Sitampiky * Tsaramandroso References Districts of Boeny {{Madagascar-geo-stub ...
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Ambondromamy
Ambondromamy is a town and commune ( mg, kaominina) in Madagascar. It belongs to the district of Ambato-Boeni, which is a part of Boeny Region. The population of the commune was estimated to be approximately 8,000 in 2001 commune census. Primary and junior level secondary education are available in town. The majority 60% of the population of the commune are farmers, while an additional 30% receives their livelihood from raising livestock. The most important crop is peanuts, while other important products are maize and sweet potatoes. Services provide employment for 5% of the population. Additionally fishing employs 5% of the population. Geography Ambondromamy is situated at the intersection of the Route nationale 6 (to Diego Suarez) and RN 4 (Mahajanga - Antananarivo Antananarivo ( French: ''Tananarive'', ), also known by its colonial shorthand form Tana, is the capital and largest city of Madagascar. The administrative area of the city, known as Antananarivo-Renivo ...
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East Africa Time
East Africa Time, or EAT, is a time zone used in eastern Africa. The time zone is three hours ahead of UTC ( UTC+03:00), which is the same as Moscow Time, Arabia Standard Time, Further-eastern European Time and Eastern European Summer Time. As this time zone is predominantly in the equatorial region, there is no significant change in day length throughout the year and so daylight saving time is not observed. East Africa Time is observed by the following countries: * * * * * * * * * See also *Moscow Time, an equivalent time zone covering Belarus, Turkey and most of European Russia, also at UTC+03:00 *Arabia Standard Time, an equivalent time zone covering Bahrain, Iraq, Kuwait, Qatar, Saudi Arabia and Yemen, also at UTC+03:00 * Eastern European Summer Time, an equivalent time zone covering European and Middle Eastern countries during daylight saving, also at UTC+03:00 *Israel Summer Time, an equivalent time zone covering the State of Israel during daylight saving, also ...
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Madagascar
Madagascar (; mg, Madagasikara, ), officially the Republic of Madagascar ( mg, Repoblikan'i Madagasikara, links=no, ; french: République de Madagascar), is an island country in the Indian Ocean, approximately off the coast of East Africa across the Mozambique Channel. At Madagascar is the world's second-largest island country, after Indonesia. The nation is home to around 30 million inhabitants and consists of the island of Madagascar (the fourth-largest island in the world), along with numerous smaller peripheral islands. Following the prehistoric breakup of the supercontinent Gondwana, Madagascar split from the Indian subcontinent around 90 million years ago, allowing native plants and animals to evolve in relative isolation. Consequently, Madagascar is a biodiversity hotspot; over 90% of its wildlife is endemic. Human settlement of Madagascar occurred during or before the mid first millennium AD by Austronesian peoples, presumably arriving on outrigger cano ...
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Jurassic
The Jurassic ( ) is a geologic period and stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and is the only boundary between geological periods to remain formally undefined. By the beginning of the Jurassi ...
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Geological Formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by Abraham Gottlob ...
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