GRE Testing Locations
Decided to take GRE exam? Now it is time to determine where to take the test. This site provides a full list of GRE testing centers in Madagascar, among which, you can choose one that is nearest to you. Good news is that the following GRE test locations in Madagascar offer both GRE general test and the GRE subject tests.
Paper-delivered Test Centers for General Test
| Code | Name |
| 10636 | Antananarivo, US Embassy/English Teaching Program |
GRE Test Dates
There are two types of test format offered by the test maker – ETS: Computer-delivered and Paper-delivered GRE general tests. For computer based test format, the GRE General Test is offered year-round on a continuous basis, and available for registration on a first-come, first-served basis. For paper based general test, testing is available three times per year. The following test dates apply:
| Test Dates for Paper Based | Deadlines for Registration | Scores Available |
|---|---|---|
| November 09, 2019 | October 4, 2019 | December 20, 2019 |
| February 1, 2020 | December 27, 2019 | March 13, 2020 |
GRE Subject Tests in Madagascar
The GRE Subject Tests are available on paper based only. In all GRE test centers throughout the world (both inside and outside United States), the exam is available three times a year. The three test dates are:
- April
- September
- October
More about Madagascar
Madagascar, the fourth largest island in the world, is 1,580 km long and up to 580 km wide. The coasts are only slightly subdivided by bays and largely accompanied by coral reefs, and are therefore not very accessible to shipping. The interior is a highland on which volcanic massifs are placed: Tsaratanana with the highest elevation in Madagascar, the Maromokotro (2,876 m above sea level), in the north, the Ankara Mountains in the middle, overlooking the capital (2,643 m above sea level), and the Andringitra massif (2,658 m above sea level) in the south. The eastern slope of the mountains is short and steep, while the western slope is comparatively flat and spacious. This asymmetry corresponds to the watershed near the steep eastern edge with larger rivers facing west, whose water flow varies according to the season. The main rivers of Madagascar have their source in the highlands near the east coast, flow in a westerly direction through fertile valleys and flow into the Mozambique Strait. The longest river with 560 km is the Mangoky. The 525 km long Betsiboka and its tributary Ikopa are navigable with motor boats in the rainy season 240 km inland to Maevatanana. Against this are many rivers which flow into the Indian Ocean, in short, have a steep gradient and are not navigable due to waterfalls in the upper and middle reaches and alluvial banks in the lower reaches. The largest lake in Madagascar is the Alaotra lake northwest of Antananarivo.
About two thirds of the island, the eastern roof and the highlands, are formed by Precambrian rocks (gneiss, clay and mica schist, quartzite, limestone, marble and amphibolite) and are interspersed with younger granite intrusions. In the west, this old base (once part of Gondwana) is submerged under a bundle of sedimentary rocks several thousand meters thick, which includes all geological systems from the turn of the Permian / Triassic to the Tertiary. The basis is formed by glacial conglomerates of the Karoo series that bear witness to a Paleozoic glaciation. A recent tilt to the west has given the island the shape of a pult and the sedimentary rocks a western stratiform incursion. Old and young tectonic lines have been revived, including the trenches of the Antongilbai and the Alaotrasee as well as the fracture and flexure stage Bongo Lava in the west, all in the general direction of the island and contributing to this itself. The related volcanism produced extensive basalt layers and numerous volcanic mountains in the period from the Upper Cretaceous to the Quaternary.
The eastern roofing is characterized by two rifts parallel to the coast, by a dense and deep subdivision with ridge-like watersheds and an associated coastal floodplain. The west is filled with a layered landscape bound to the sedimentary rocks with multiple karst stepped surfaces.
Industry
Due to the lack of raw material supply, the manufacturing industry is not of great importance. In addition to the textile industry, the processing industry includes the Toamasina oil refinery, companies in the food and beverage industry and the chemical industry, as well as metal processing and the manufacture of building materials. The industrial sector (including mining and construction) generated (2015) 24.1% of GDP.
Tourism
Despite its high potential (tropical beaches, cultural wealth, nature reserves), tourism in Madagascar is still at the beginning of its development. The lack of infrastructure and, in particular, the unstable political situation have an inhibiting effect. The number of foreign visitors fell to 163,000 in the unrest year 2009, after 375,000 guests were counted in the previous year (2013: 181,000). Income from tourism in 2013 was US $ 76.5 million. Even so, tourism still makes a major contribution to the Malagasy economy.
Transportation
In terms of traffic, Madagascar is only insufficiently developed. The 836 km long railway network consists of two isolated railway lines, each leading from the east coast into the mountains. The 530 km long main connection leads from the port city of Toamasina via Antananarivo to Antsirabe. The road network covers around 37,500 km, of which around 6,100 km are paved. The remaining routes are paved slopes that are hardly passable in the rainy season. The main road connects the port city of Mahajanga on the west coast with Antananarivo and Antsirabe. As a result of the unfavorable land connections, coastal shipping (the most important port is Toamasina) and air traffic (around 80 airports and landing sites) are of considerable importance. The main international airport is Ivato north of Antananarivo.
Natural resources
With the exception of titanium ore (extraction volume in 2014: 341,000 t), chrome ore (53,900 t) and nickel ore (37,100 t), existing mineral resources have so far hardly been mined due to difficult topographical conditions and inadequate infrastructure. Are known inter alia. also deposits of bauxite, cobalt, gold, iron and copper ores, coal, oil shale and petroleum. The development of a mining industry is still in its infancy.