Kirindy Forest

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Kirindy Forest

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Kirindy Forest, Nature reserve in western Madagascar

The Kirindy Forest extends across 120 square kilometers of dry deciduous forest, containing three distinct species of baobab trees and numerous endemic plants.

The forest transformed from a Swiss forestry training station in the 1970s into a German primate research center focused on wildlife protection.

Local communities near Kirindy Forest maintain traditions of agriculture while researchers study eight lemur species including the Madame Berthe's Mouse Lemur.

Visitors can access the reserve through guided day walks and night tours, with accommodations available at basic bungalows equipped with mosquito nets.

The reserve houses 31 mammal species, including the fossa predator, along with 50 reptile species and 40 bird varieties in its protected environment.

GPS coordinates: -20.07391,44.63071

Latest update: March 4, 2025 07:55

Madagascar photography: baobabs, Tsingy, national parks

Madagascar features natural landscapes ranging from the baobab avenues near Morondava to the limestone formations of the Tsingy and coastal areas with coral reefs. The country's national parks protect tropical rainforests inhabited by lemurs, along with geological features including crater lakes and sandstone formations. The highest peaks rise in the northern mountain ranges, while the southern regions are characterized by dry landscapes. Photogenic locations include the Isalo Massif with its eroded sandstone canyons, the Masoala Peninsula with its rainforests along the Indian Ocean, and the island of Nosy Be off the northwest coast. The beaches at Ifaty and Anakao attract visitors for their reefs, while Sainte-Marie Island is known for whale watching between July and September. The Kirindy forests in the west are home to nocturnal lemurs and fossas. Historic sites include the royal hill of Ambohimanga, a UNESCO World Heritage site, and the Rova palace in Antananarivo. The geysers at Ampefy and the crater lake Tritriva showcase the volcanic history of the highlands. The red Tsingy near Sadjoavato formed through erosion of iron-rich sandstone and contrast with the gray limestone Tsingy in the west.

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