The Maldives is a low-lying island nation situated in the central Indian Ocean, southwest of Sri Lanka and India. It consists of approximately 1,200 coral islands grouped into 26 natural atolls that extend in a north–south chain over roughly 870 kilometers. Geologically, the islands are formed from biogenic coral limestone accumulated on the rims of submerged volcanic structures, making the Maldives one of the most geomorphologically distinctive archipelagic systems in the world. The average elevation rarely exceeds 1–1.5 meters above sea level, rendering the country highly vulnerable to sea-level rise, coastal erosion, and storm surge events. The tropical monsoon climate is characterized by a southwest monsoon bringing increased precipitation from May to November and a relatively drier northeast monsoon from December to April, shaping both ecological cycles and human activity.
The historical development of the Maldives is closely tied to its strategic position along ancient Indian Ocean maritime trade routes. Archaeological and linguistic evidence suggests settlement by seafaring populations from South Asia and possibly East Africa more than two millennia ago. By the 12th century CE, Islam had been introduced and rapidly became the dominant religion, transforming the political and cultural structure of the islands into a sultanate governed under Islamic principles. For centuries, the Maldives functioned as an independent sultanate while maintaining extensive trade relations with Arab, South Asian, and Southeast Asian merchants, exporting commodities such as dried tuna, cowrie shells, and coir. In 1887, the archipelago became a British protectorate, retaining internal autonomy while foreign affairs were managed externally. Full independence was achieved in 1965, followed by the establishment of a republic in 1968. Since independence, the national economy has transitioned from subsistence-based fishing and trade toward tourism and marine services, although environmental sustainability has become an increasingly central political concern due to climate change risks.
Agriculture in the Maldives is highly constrained by limited land availability, poor soil quality, and saltwater intrusion. The sandy, porous soils of coral islands possess low nutrient retention capacity, which restricts cultivation primarily to small-scale subsistence farming. Commonly grown crops include coconut, breadfruit, banana, papaya, and taro, often maintained in household plots rather than extensive agricultural fields. As a result, food security is heavily dependent on imports. In contrast, fisheries have historically constituted the backbone of the Maldivian economy and continue to play a critical role in rural livelihoods and export revenue. The fishery sector is dominated by tuna species, particularly skipjack and yellowfin tuna, harvested predominantly through traditional pole-and-line methods that reduce bycatch and support ecological sustainability. Fisheries also form an essential component of national food systems and cultural identity.
Forestry, in the conventional sense, is virtually absent due to the small size and coral composition of the islands. However, coastal and island vegetation—primarily coconut palms, shrubs, and mangrove ecosystems—plays an important ecological role. Mangroves, where present, contribute to shoreline stabilization, sediment trapping, and habitat provision for coastal biodiversity. Overall, the environmental system of the Maldives is tightly interlinked, with human settlement, economic activity, and ecological resilience all fundamentally shaped by the constraints and opportunities of a fragile coral island environment.
2014 Gerold and Klaudia have been one week on the Maldives. Thereby 3 days in the capital Malé in a windowless room and 4 days on Embudu Village Island in a resort, 10 km from Malé.