Search results
Results from the WOW.Com Content Network
Paul Bert Rahasimanana was born in 1960 to a working-class family. [1] At the age of seven, he was given an accordion as a gift and began teaching himself to play. [2] In the early 1970s, Rahasimanana and a group of friends formed an a capella group called Hazo Midoroboka and began singing traditional consolatory songs (mamonjy jaobany) for those grieving at wakes held in their neighborhood of ...
Bombetoka Bay is a bay on the northwestern coast of Madagascar near the city of Mahajanga, where the Betsiboka River flows into the Mozambique Channel. Numerous islands and sandbars have formed in the estuary from the large amount of sediment carried in by the Betsiboka River and have been shaped by the flow of the river and the push and pull ...
Main page; Contents; Current events; Random article; About Wikipedia; Contact us
This file contains additional information, probably added from the digital camera or scanner used to create or digitize it. If the file has been modified from its original state, some details may not fully reflect the modified file.
Betaimboay is a municipality in western Madagascar in Betsiboka Region approximately 200 kilometres (120 mi) north-west of the capital Antananarivo. [ 1 ] References
The altitude is low and as it is located far from the coast, temperatures tend to be high. The city belongs to the district of Maevatanana, which is a part of Betsiboka Region. Maevatanana is the capital of the Betsiboka region, and the population of the commune was estimated to be approximately 24,000 in 2001 commune census. [2]
Betsiboka River is a 525-kilometre (326 mi) long river in central-north Madagascar. It flows northwestward and empties to Bombetoka Bay, forming a large delta. It originates to the east of Antananarivo. The river is surrounded in mangroves. [3] The river is distinctive for its red-coloured water, which is caused by river sediments.
It flows from south to north through the regions of Melaky, Betsiboka, Bongolava and Boeny. It has a length of approximately 410 km (250 mi), and drains a basin of 16,475 km 2 (6,361 sq mi). It is distinct from the Mahavavy Nord several hundred km to the north. [2] The Mahavavy Sud rises on the Andranofotsibe Massif at about 1000 meters elevation.