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Nosy Bé
Nosy Be (; formerly Nossi-bé and Nosse Be, ) is a volcanic island off the northwest coast of Madagascar. Nosy Be is Madagascar's largest and busiest tourist destination. It has an area of , and its population was 109,465 according to the provisional results of the 2018 Census. means "big island" in the Malagasy language. The island was called Assada by the French during the early 17th century. Nosy Be has been given several nicknames over the centuries, including "Nosy Manitra" (the scented island). History The first human inhabitants of Nosy Be were small bands from Antankarana and Zafinofotsy ethnic groups, before the Sakalava people migrated there and became the largest group on the island. These people were joined later by some Comorians, Indians and Antandroy. Nosy Be made its first major appearance in Madagascar's history when King Radama I announced that he intended to conquer the whole west of Madagascar. That plan was eventually achieved in 1837 when the Sakalava Ki ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diana Region
Diana is a region in Madagascar at the northern part of the island. It borders the regions of Sava to the southeast and Sofia to the southwest. It covers an area of 19,266 km2, and had a population of 889,736 in 2018. The regional capital is Antsiranana (previously known as ''Diego Suarez''). Geography Rivers The main rivers of the Diana region are: * Besokatra River * Irodo River * Loky River * Mahavavy River * Ramena River * Saharenana River * Sambirano River Protected areas and visitors' attractions The following national parks, reserves and visitors' attractions are located in Diana: * Ambodivahibe New Protected Area * Andrafiamena Andavakoera New Protected Area * Nosy Antsoha New Protected Area * Ampasindava New Protected Area * Galoko Kalobinono New Protected Area * Oronjia New Protected Area * Amber Mountain National Park * Analamerana Reserve * Ankarana Reserve * Lokobe National Park * Manongarivo Reserve * Tsaratanana National Park * Nosy Hara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tsiomeko Of Boina
Tsiomeko (1828–1843) was the last queen and monarch of the Boina Kingdom in 1836-1839.Histoire politique et coloniale: Histoire des populations autres que les Merina. f. 1. Betsileo, Betsimisaraka, Antanosy, Sihanaka, Tsimihety, Bezanozano, Antanala, Antankarana, Bara, Mahafaly, Antandroy, par G. Grandidier et R. Decary. Guillaume Grandidier, Impr. officielle, 1958 Tsiomeko was the daughter of Taratra and a grand-niece of King Andriantsoly, who was driven out of Boina by the Merina armies and whom her father had served as a "souer". She became queen in 1836, at age eight, succeeding Queen Oantitsy, the sister of King Andriantsoly. In 1839 she was driven out of her residence by Hova and fled to Nosy Komba. There, she asked for French protection and Admiral de Hell signed a deal with the queen to make Boina a French protectorate. Tsiomeko ceased to be Queen when her Kingdom was annexed to the Merina Kingdom The Kingdom of Merina, also known as the Kingdom of Madagascar and o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Crater Lake
A volcanic crater lake is a lake in a volcanic crater, crater that was formed by explosive eruption, explosive activity or a caldera, collapse during a types of volcanic eruptions, volcanic eruption. Formation Lakes in calderas fill large craters formed by the collapse of a volcano during an eruption. Lakes in maars fill medium-sized craters where an eruption deposited debris around a vent. Crater lakes form as the created depression, within the Rim (craters), crater rim, is filled by water. The water may come from Precipitation (meteorology), precipitation, groundwater circulation (often Hot Spring, hydrothermal fluids in the case of volcanic craters) or melted ice. Its level rises until an equilibrium is reached between the rates of incoming and outgoing water. Sources of water loss singly or together may include evaporation, subsurface seepage, and, in places, surface leakage or overflow when the lake level reaches the lowest point on its rim. At such a saddle location, the u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holocene
The Holocene () is the current geologic time scale, geological epoch, beginning approximately 11,700 years ago. It follows the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene is an interglacial period within the ongoing Ice age, glacial cycles of the Quaternary, and is equivalent to Marine isotope stages, Marine Isotope Stage 1. The Holocene correlates with the last maximum axial tilt towards the Sun of the Earth#Axial tilt and seasons, Earth's obliquity. The Holocene corresponds with the rapid proliferation, growth, and impacts of the human species worldwide, including Recorded history, all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban culture, urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global significance for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nosy Mitsio
Nosy Mitsio is an island off the northwest coast of Madagascar. It is located 70 km north-east of Nosy Be and 60 km north-west of the city of Ambilobe. Owing to the Mitsio archipelago being distant from other large bodies of land, Nosy Mitsio offers crystal clear waters, white sandy beaches, lush coconut palms and a marine fauna with abundant reefs distant from the island perimeter. Nosy Mitsio is the only inhabited island of the Mitsio archipelago (other than Tsarabanjina, which has a small population that caters to tourism for the hotel on the island). Nosy Mitsio is very rural: it has no infrastructural development and is populated mainly by small family villages, that belong to the municipality of Antsohimbondrona Antsohimbondrona (also called: Port Saint-Louis) is a municipality in Madagascar. It belongs to the district of Ambilobe, which is a part of Diana Region. It is situated in the delta of the Mahavavy River into the Indian Ocean. According to 2001 .... Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nosy Komba
Nosy Komba (; ), also known as Nosy Ambariovato, is a small island in Madagascar, situated between the island of Nosy Be and the northwestern coast of the main island of Madagascar. Roughly circular, it rises sharply towards a plateau and the summit of Antaninaomby at the center of the island. Administered as an arrondissement of the unitary commune and Districts of Madagascar, district of Nosy-Be within Diana Region, the island is divided into five fokontany (villages), with Ampangorina as the main village and administrative center. The population is mainly restricted to the northern half of the island. The economy is reliant on tourism and handicrafts, supplemented by a wide range of agricultural products. Hotels and guest houses support tourists to the island, mainly on excursions from Nosy Be. The lowlands of the island are divided between secondary forest and a patchwork of farmland and plantations (notably including shade-grown coffee), while the highlands are mainly Shrubl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Lemurs
Black is a color that results from the absence or complete absorption of visible light. It is an achromatic color, without chroma, like white and grey. It is often used symbolically or figuratively to represent darkness.Eva Heller, ''Psychologie de la couleur – effets et symboliques'', pp. 105–26. Black and white have often been used to describe opposites such as good and evil, the Dark Ages versus the Age of Enlightenment, and night versus day. Since the Middle Ages, black has been the symbolic color of solemnity and authority, and for this reason it is still commonly worn by judges and magistrates. Black was one of the first colors used by artists in Neolithic cave paintings. It was used in ancient Egypt and Greece as the color of the underworld. In the Roman Empire, it became the color of mourning, and over the centuries it was frequently associated with death, evil, witches, and magic. In the 14th century, it was worn by royalty, clergy, judges, and government off ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
