Recent from talks
Nothing was collected or created yet.
Nosy Be
View on WikipediaYou can help expand this article with text translated from the corresponding article in French. (October 2025) Click [show] for important translation instructions.
|
Nosy Be (Malagasy pronunciation: [nusʲ be]; formerly Nossi-bé and Nosse Be, lit. 'big island') 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 320.02 km2 (123.56 sq mi), and its population was 109,465 according to the provisional results of the 2018 Census.
Key Information
Nosy Be 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
[edit]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 Kingdom of Boina came into the possession of Ranavalona I upon the defeat of Queen Tsiomeko's army.[citation needed]
The French colonized the island from 1840, founding an outpost named Hell-Ville (from French Admiral de Hell).[1] The 1848 abolition of slavery in the French colonies resulted in a revolt against the French by the Sakalava people, who were extensively involved in the slave trade.[2] In the late 19th and early 20th centuries, the island was governed by the French as an internal protectorate within the colony of Madagascar. The outpost became an important trade harbor in the Mozambique channel.[3]
During the nineteenth century, the French settlers developed cash crop agriculture (mainly sugar cane) and recruited indentured laborers from East Africa.[4] Though it was difficult for the French to control the littoral, they founded a plantation colony in Nosy Be, mainly producing sugar and cash crops.[5] The French used both military force and diplomacy to maintain their position in the island, appointing the former ruler of Nosy Be Binao as the gouverneur principal of the island.[6]
During the Russo-Japanese War Nosy Be became a supply station for Russia's Second Pacific Squadron. The main fleet led by Admiral Zinovy Rozhestvensky reached Nosy Be on January 9, 1905, where it met a smaller detachment led by Admiral Dmitry von Fölkersam that had arrived already on December 28, 1904.[7] The fleet stayed for two months for refurbishing and coaling, leaving on March 17 to meet its fate ten weeks later at the Battle of Tsushima.[8]
In 2013, two French tourists and one local were lynched (beaten and burned by a mob) after rumors that they were responsible for the death of a local boy.[9][10] A Madagascar court gave four men the maximum hard labour for life over the mob lynching.[11]
Geography
[edit]Nosy Be is located about 8 kilometres (5.0 mi) from the coast of Madagascar in the Mozambique Channel; several smaller islands are located nearby, including Nosy Komba, Nosy Mitsio, Nosy Sakatia, and Nosy Tanikely. The island's main town is Andoany, commonly known as Hell-Ville.
The volcanic island has an area of about 312 km2 (120 sq mi) – 30 km long, 19 km wide[12] – and its highest peak is Mont Lokobe at 450 m (1,480 ft); the volcano is of Pleistocene origin and has not erupted in recent history.[13] There are eleven volcanic crater lakes on the island.
Climate
[edit]Nosy Be has a tropical savanna climate. It is most humid in summer (December, January, February). The Tsaratanana massif partially protects the island from the strong north-east winds affecting the region in August or during tropical depressions. The wet season lasts from October until the beginning of May, followed by a relatively short dry season that lasts through September. As characteristic of its climate however, it still sees moderate amounts of precipitation even during this time. Daytime temperatures remain fairly steady throughout the year, hovering around 30 °C (86 °F), while the nights are slightly cooler during the dry season.
| Climate data for Nosy Be (1991–2020) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °C (°F) | 35.0 (95.0) |
35.0 (95.0) |
36.8 (98.2) |
35.4 (95.7) |
36.0 (96.8) |
34.2 (93.6) |
34.5 (94.1) |
35.4 (95.7) |
34.4 (93.9) |
36.3 (97.3) |
37.0 (98.6) |
36.0 (96.8) |
37.0 (98.6) |
| Mean daily maximum °C (°F) | 31.5 (88.7) |
31.5 (88.7) |
31.9 (89.4) |
32.2 (90.0) |
31.4 (88.5) |
30.2 (86.4) |
29.7 (85.5) |
30.0 (86.0) |
30.6 (87.1) |
31.8 (89.2) |
31.9 (89.4) |
31.6 (88.9) |
31.2 (88.2) |
| Daily mean °C (°F) | 27.7 (81.9) |
27.7 (81.9) |
28.0 (82.4) |
28.0 (82.4) |
26.8 (80.2) |
25.4 (77.7) |
24.6 (76.3) |
24.8 (76.6) |
25.6 (78.1) |
27.1 (80.8) |
27.7 (81.9) |
27.8 (82.0) |
26.8 (80.2) |
| Mean daily minimum °C (°F) | 23.9 (75.0) |
24.0 (75.2) |
24.1 (75.4) |
23.7 (74.7) |
22.3 (72.1) |
20.6 (69.1) |
19.5 (67.1) |
19.5 (67.1) |
20.5 (68.9) |
22.3 (72.1) |
23.4 (74.1) |
23.9 (75.0) |
22.3 (72.1) |
| Record low °C (°F) | 20.2 (68.4) |
20.4 (68.7) |
21.4 (70.5) |
19.0 (66.2) |
15.0 (59.0) |
13.0 (55.4) |
12.7 (54.9) |
13.7 (56.7) |
13.0 (55.4) |
16.0 (60.8) |
17.6 (63.7) |
20.2 (68.4) |
12.7 (54.9) |
| Average precipitation mm (inches) | 392.9 (15.47) |
334.3 (13.16) |
280.9 (11.06) |
106.2 (4.18) |
34.8 (1.37) |
29.3 (1.15) |
21.2 (0.83) |
26.7 (1.05) |
35.0 (1.38) |
29.8 (1.17) |
135.0 (5.31) |
302.1 (11.89) |
1,728.2 (68.04) |
| Average precipitation days (≥ 1 mm) | 19.5 | 17.3 | 16.5 | 9.3 | 4.7 | 4.5 | 3.4 | 3.6 | 4.2 | 4.0 | 9.8 | 15.8 | 112.6 |
| Mean monthly sunshine hours | 187.0 | 171.2 | 224.0 | 245.0 | 271.3 | 248.9 | 263.7 | 284.9 | 277.6 | 281.1 | 249.1 | 219.7 | 2,923.5 |
| Source: NOAA (sun, 1961–1990)[14][15] | |||||||||||||
Flora and fauna
[edit]The island is known for having populations of the world's smallest frogs (Stumpffia pygmaea) and chameleon (Brookesia minima).[16] The Lokobe Reserve is one of Madagascar's five Strict Nature Reserves (Réserves Naturelles Intégrales). Nosy Be is also home to a specific color of panther chameleon (Furcifer pardalis).
Nocturnal animals include lemurs (mouse and dwarf), chameleons (e.g. short nosed, and stump tailed), leaf-tailed geckos, frogs, and birds.[17]

Recent studies indicate that adjacent waters around the channel between Nosy Be[18] and Madagascar host a habitat for a notable number of Omura's whale, enabling researchers to conduct field studies of this rare species.[19][20]
Coral reefs around Nosy Be are impacted by urbanization, the discharge of the sugar industry, and unregulated tourism.[21]
Administration
[edit]The island constitutes a department within Diana Region and is organized as the City of Nosy Be (Commune Urbaine de Nosy Be). Its mayor is Mr. Vita Zarga.
Economy
[edit]Once a major location of sugar cane plantations and production of its derived products (sugar, rum), the island's main activities are now the plantation of ylang-ylang[22] (for the production of essential oils) and tourism. Nosy Be is the most developed tourism destination in Madagascar. This is the only place in Madagascar where all-inclusive large resorts can be found. There are no traffic lights on the island, instead roundabouts are used.
Transportation
[edit]The island is served by Fascene Airport. The airport is served by commercial flights with Air Madagascar, Air Austral, Airlink, Ewa, Ethiopian Airlines, and has direct flights from Europe on Neos. Its main city and harbour, Hell-Ville, can be reached by boat from Ankify. On the island, travel via tuk-tuk, scooters, and boats is common alongside cars.
Education
[edit]This section needs expansion. You can help by adding to it. (May 2015) |
French international schools:
- École primaire française Lamartine[23]
Local public schools:
- EPP Andavakotoko
- EPP Galliéni
- EPP boulevard Manceaut (?)
- CEG Ambalakatakata
- Lycée mixte of Nosy Be
Twin towns—sister cities
[edit]See also
[edit]References
[edit]- ^ Sanchez SF (2008). "Commerce régional et à longue distance dans l'ouest de Madagascar au XIXème siècle". Tsingy: Revue de l'association des professeurs d'histoire et de géographie de Madagascar (9): 44–56.
- ^ « Sanchez S. F., Un mouvement antiabolitionniste et anticolonial : La révolte sakalava de 1849 dans le Nord-Ouest de Madagascar », in Ballarin M.-P., Derat M.-L., Médard H., Vernet T. (dir.), Traite et esclavage en Afrique Orientale et dans l'Océan Indien, Paris, Karthala, 2013, pp. 413–439
- ^ Sanchez, Samuel (2 January 2017). "Complex Strands: Changing Textile Trades in Western Madagascar and the Mozambique Channel in the Nineteenth Century, Evidence from Nosy Be Island". Textile History. 48 (1): 85–100. doi:10.1080/00404969.2017.1294817. S2CID 165135935.
- ^ Rajaonah F. & Sanchez S. F., "De l'engagisme au salariat dans le Sud-Ouest de l'océan Indien. La colonie de plantation de Nosy Be, Madagascar (1840–1960)", in Guerassimoff E. & Mande I. (dir.), Le travail colonial. Engagés et autres travailleurs migrants dans les empires 1850-1950 , Paris, Riveneuve, 2016, p.245-282
- ^ « Sanchez S. F., "Persuasion, escarmouches, prises d'otages. L'exercice du pouvoir dans la colonie française de Nosy Be, Nord-Ouest de Madagascar (1839–1896)", in Chanson-Jabeur Ch., Morlat P., Forest A., Colonisations et Répressions, Paris, Les Indes Savantes, 2015, pp. 413–439
- ^ Allen, Philip M.; Covell, Maureen (2005). Historical dictionary of Madagascar (2nd ed.). Lanham, Md. [u.a.]: Scarecrow Press. ISBN 978-0-8108-4636-4.
- ^ Pierre Van de Boogaerde (2009). Shipwrecks of Madagascar. Strategic Book Publishing. p. 243. ISBN 978-1-60693-494-4.
- ^ Alistair Horne (2015). Hubris. The Tragedy of War in the Twentieth Century. HarperCollins. p. 74ff. ISBN 978-0-06-239780-5.
- ^ "A Madagascar, la folle rumeur qui a mené trois hommes sur le bûcher". Le Monde.fr. Retrieved 23 April 2018.
- ^ "Triple lynchage de Madagascar: coopération judiciaire difficile entre Paris et Antananarivo" (in French). 2013-11-12. Retrieved 2024-09-26.
- ^ "Four sentenced to hard labour for life over Madagascar mob lynching". France 24. 2015-10-09. Retrieved 2024-10-29.
- ^ Lowry, Linda L. (2016-09-01). The SAGE International Encyclopedia of Travel and Tourism. SAGE Publications. ISBN 978-1-4833-6896-2.
- ^ "Nosy-Be". Global Volcanism Program. Smithsonian Institution.
- ^ "Nosybe Climate Normals 1991–2020". World Meteorological Organization Climatological Standard Normals (1991–2020). National Oceanic and Atmospheric Administration. Archived from the original on 25 September 2023. Retrieved 25 September 2023.
- ^ "Nosy Be/Fascene Climate Normals 1961–1990". National Oceanic and Atmospheric Administration (FTP). Retrieved October 19, 2015. (To view documents see Help:FTP)
- ^ Tim Flannery and Peter Schouten, Astonishing Animals: Extraordinary Creatures and the Fantastic Worlds They Inhabit. New York: Atlantic Monthly Press, 2004. Page 126–127.
- ^ Garbutt, Nick; Bradt, Hilary; Schuurman, Derek (2008). Madagascar Wildlife. Bradt Travel Guides. ISBN 978-1-84162-245-3.
- ^ Sakalav Diving (2012). "petit rorqual minke whale.avi". YouTube. Archived from the original on 2021-12-21. Retrieved 2015-10-25.
- ^ Jefferson, Thomas, Marc A. Webber, and Robert L. Pitman (2015). Marine Mammals of the World: A Comprehensive Guide to their Identification. London: Academic.
{{cite book}}: CS1 maint: multiple names: authors list (link) - ^ Cerchio S.; Andrianantenaina B.; Lindsay A.; Rekdahl M.; Andrianarivelo N.; Rasoloarijao T. (2015). "Omura's whales (Balaenoptera omurai) off northwest Madagascar: ecology, behaviour and conservation needs". Royal Society Open Science. 2 (10) 150301. Bibcode:2015RSOS....240301C. doi:10.1098/rsos.150301. PMC 4632516. PMID 26587244.
- ^ McClanahan, T. R.; Sheppard, C. R. C.; Obura, D. O. (2000-10-12). Coral Reefs of the Indian Ocean: Their Ecology and Conservation. Oxford University Press, USA. ISBN 978-0-19-512596-2.
- ^ "Jacarandas cultivates Madagascar scents: from ylang-ylang to pink peppercorn". Premium Beauty News. Retrieved 2024-09-26.
- ^ "École primaire française Lamartine." AEFE. Retrieved on May 7, 2015.
- ^ Vacca, Maria Luisa. "Comune di Napoli -Gemellaggi" [Naples - Twin Towns]. Comune di Napoli (in Italian). Archived from the original on 2013-07-22. Retrieved 2013-08-08.
External links
[edit]Nosy Be
View on GrokipediaHistory
Early Human Settlement and Pre-Colonial Period
Human settlement on Nosy Be aligns with the broader colonization of Madagascar, where archaeological investigations indicate initial arrivals around 700 CE by Austronesian-speaking peoples from Southeast Asia, who navigated the Indian Ocean using outrigger canoes.[6] These migrants established coastal communities focused on slash-and-burn agriculture, fishing, and trade, with linguistic evidence from the Malagasy language—part of the Western Malayo-Polynesian branch—confirming this Austronesian foundation, later augmented by Bantu influences from East Africa evident in genetic admixture and cultural practices like cattle herding.[6] Paleoecological studies on Nosy Be reveal environmental impacts from human activity, including forest fragmentation, predating some dated occupations but consistent with mid-first-millennium CE subsistence patterns involving endemic species exploitation.[7] By the medieval period, nearby sites like the port of Mahilaka on the northwest coast demonstrate active trade networks from the 11th to 14th centuries, involving ceramics and goods exchanged with Arab and Swahili merchants, suggesting Nosy Be's integration into these Indian Ocean circuits as a peripheral settlement zone shaped by geological features and vegetation shifts over two millennia.[8] The island's pre-colonial society was dominated by the Sakalava people, who expanded from the western mainland in the late 16th century, forming one of Madagascar's earliest major kingdoms along the coast, with Nosy Be falling under the Boina Sakalava domain.[9] Sakalava communities emphasized exogamous kinship, ritual ancestor veneration, and land rights tied to agriculture, while engaging in cattle pastoralism and coastal trade that drew diverse migrants for resource exploitation.[8] Prior to French involvement in the 19th century, Nosy Be served as a refuge and strategic outpost for Sakalava rulers, exemplified by Queen Tsiomeko of Boina seeking alliances amid regional conflicts, underscoring the island's role in pre-colonial power dynamics without large-scale urbanization or monumental architecture.[10] These societies remained decentralized, reliant on oral traditions and seasonal mobility, with no evidence of earlier megafauna coexistence or claims of settlement predating the mid-first millennium CE holding up under scrutiny.[11]Colonial Era and French Influence
Nosy Be became a French protectorate on March 5, 1841, following a request for protection by Queen Tsiomeko of the Sakalava against expansion by the Merina kingdom on mainland Madagascar.[12] This arrangement was driven by France's strategic interest in establishing a naval base between East Africa and the island of Réunion, capitalizing on the island's natural harbors.[12] An expedition led by Captain Pierre Passot aboard the Prévoyante arrived in 1839, selecting a site for a military port that became Hell-Ville, named after Admiral de Hell, governor of Bourbon (Réunion).[13] France formally took possession in 1841, renaming the island Nossi-Bé by decree in 1842.[13] The protectorate status predated French control over mainland Madagascar by over 50 years, positioning Nosy Be as an isolated French dependency alongside Mayotte.[14] Under French administration, Nosy Be transformed from a sparsely populated island—virtually uninhabited at the start of the 19th century—into a trading hub and agricultural outpost.[12] Commerce flourished, with ship visits rising from 79 in 1843 to 265 by 1856, linking European markets to ports like Zanzibar and Bombay through exports of sugar and re-exports such as cotton fabrics.[12] From the 1850s, settlers primarily from Réunion, Mauritius, and metropolitan France developed cash crop plantations, including sugarcane, indigo, coffee, sesame, rice, and cassava.[13] The abolition of slavery in 1849 sparked a Sakalava revolt against both the policy and a ban on arms imports, leading to an unsuccessful attack on Hell-Ville; the crisis was resolved by granting Nosy Be free port status, which boosted trade recovery.[13] Population growth incorporated migrant labor, including Kiswahili-speaking communities at ports like Marodoka, drawn from Mozambique and Kenya.[12] French influence extended to economic specialization and infrastructure, with Nosy Be governed jointly with Mayotte until 1897, when it was integrated into the newly conquered French colony of Madagascar following the 1895 invasion of the mainland.[13] Sugar production intensified in the 1920s, establishing the island's first major plantations and a rum distillery at Dzamandzar, while ylang-ylang distillation began in the 1910s, leveraging the island's volcanic soils.[13] [15] This plantation economy relied on indentured labor from East Africa and shaped Nosy Be's role as a key node in French Indian Ocean networks, though it faced challenges like the 1845 joint Anglo-French naval actions elsewhere that indirectly enhanced its commerce.[12] French rule persisted until Madagascar's independence in 1960, leaving a legacy of European-style settlements, export-oriented agriculture, and administrative divisions that influenced the island's post-colonial development.[13]Post-Independence Developments
Following Madagascar's achievement of independence from France on June 26, 1960, Nosy Be remained integrated within the Malagasy Republic, with its economy continuing to rely on agriculture inherited from the colonial era, including sugar cane processing and ylang-ylang plantations established in the early 20th century.[5][13] Ylang-ylang production persisted and expanded post-independence, positioning Nosy Be as a primary source of essential oil exports for the global perfume industry, leveraging the island's tropical climate and established distillation techniques.[16] Tourism emerged as a complementary economic driver starting in the 1960s, coinciding with independence, when initial exploratory visitors arrived, drawn by the island's beaches and marine access.[17] By the 1970s, Nosy Be had solidified as a dedicated tourism destination, with hotels and resorts concentrating along the western and northwestern coasts to accommodate growing international arrivals, though the sector's expansion was constrained by limited road infrastructure improvements despite rising visitor numbers.[13][18] Subsequent decades saw tourism's dominance, with Nosy Be hosting around 200,000 annual visitors by the early 21st century, though only a portion dedicated to leisure amid national economic challenges and periodic political disruptions in Madagascar that affected accessibility and investment.[19] Agricultural exports like ylang-ylang oil provided resilience, with production scaling to meet global demand through small-scale distilleries and family-run plantations.[5]Geography
Location and Physical Features
Nosy Be is a volcanic island situated off the northwestern coast of Madagascar in the Mozambique Channel, approximately 8 kilometers from the mainland in Ampasindava Bay.[20] Its central geographic coordinates are 13°20′S latitude and 48°15′E longitude.[21] The island spans an area of 320 square kilometers, extending roughly 26 kilometers north to south.[20] [22] Physical features include basaltic lava flows originating from cinder cones, indicative of its volcanic formation.[1] Mount Lokobe represents the highest point at 450 meters elevation, while the average elevation across the island is about 32 meters, encompassing forested hills, crater lakes such as Lac Ankarana, and a coastline exceeding 50 kilometers featuring sandy beaches and coral reefs.[23] [24]Geology and Landforms
Nosy Be comprises sedimentary bedrock of Mesozoic age, primarily limestones and schists, intruded and overlain by volcanic vents, plutonic bodies, and mafic alkaline rocks formed during the late Cenozoic and Quaternary periods.[7][1] The island's petrogenesis reflects mantle sources remobilized by rifting events along Madagascar's margins, producing basaltic compositions with alkaline affinities.[25] Volcanic activity spanned from Miocene to Pleistocene phases, with evidence of very recent basaltic flows indicating geologically youthful features.[26][27] Key landforms include well-preserved cinder cones and spatter cones concentrated in the northern and western sectors, alongside extensive basaltic lava flows.[25][27] The central region hosts numerous large crater lakes, remnants of volcanic depressions, while the western side features eleven such lakes, the largest measuring 1.5 km in diameter.[1][28] Extinct volcanic peaks, such as Mount Passot at 329 meters elevation, dominate the topography, providing elevated vantage points amid forested slopes.[29] The island's overall relief rises to approximately 450 meters at peaks like Mont Lokone, shaped by these eruptive processes without recorded historical activity.[30][28]Climate and Weather Patterns
Nosy Be exhibits a tropical monsoon climate classified as Am under the Köppen system, featuring consistently high temperatures, elevated humidity, and pronounced seasonal variations in precipitation driven by the interplay of trade winds and the Indian Ocean's monsoon dynamics.[31][32] Average annual temperatures hover around 25.3°C, with daytime highs ranging from 27°C in the cooler dry season to 30°C during the wet season's peak, while nighttime lows seldom drop below 23°C.[32] The island's proximity to the equator and surrounding warm waters ensures minimal diurnal or annual temperature fluctuations, though relative humidity often exceeds 80%, contributing to a persistently muggy atmosphere.[33] Precipitation totals approximately 2,228 mm annually, concentrated in the wet season from November to April, when convective activity and low-pressure systems amplify rainfall.[32] January stands as the wettest month with an average of 412 mm over 24 rainy days, while February records the highest number of precipitation events at 19.3 days with at least 1 mm of rain.[33] In contrast, the dry season from May to October sees markedly reduced rainfall, often below 50 mm per month, with August as the driest, fostering clearer skies and lower humidity.[34]| Month | Avg. High Temp (°C) | Avg. Low Temp (°C) | Avg. Rainfall (mm) | Rainy Days |
|---|---|---|---|---|
| January | 30 | 25 | 412 | 24 |
| February | 30 | 25 | 300 | 19 |
| March | 30 | 25 | 250 | 18 |
| April | 30 | 24 | 200 | 15 |
| May | 29 | 23 | 100 | 10 |
| June | 28 | 23 | 50 | 8 |
| July | 27 | 22 | 40 | 7 |
| August | 27 | 22 | 30 | 6 |
| September | 28 | 22 | 40 | 7 |
| October | 29 | 23 | 100 | 10 |
| November | 30 | 24 | 200 | 15 |
| December | 30 | 25 | 350 | 22 |