Maldives

The Republic of Maldives is a small island nation in the Indian Ocean, situated southwest of Sri Lanka and India. Unlike most countries, Maldives has no continental landmass at all. Its territory consists entirely of coral islands arranged into a long chain of atolls stretching across the central Indian Ocean. This physical arrangement makes Maldives one of the most geographically distinctive countries on Earth: a nation built almost entirely from coral, sand, and reef, with an average land elevation measured in centimeters rather than meters.

This unusual geography shapes nearly every aspect of life in the country. The dispersed pattern of small, low-lying islands influences where people live, how goods and people move between islands, how the economy is organized, and how the country manages its freshwater supply. It also determines the nature of the hazards Maldives faces, from storm surges to long-term sea-level rise. Understanding the physical geography of Maldives is therefore a starting point for understanding its population distribution, economic structure, transportation systems, fisheries, tourism industry, and vulnerability to environmental change.

Geographical Location and Regional Setting

Maldives lies in the northern Indian Ocean, southwest of the Indian subcontinent. The archipelago sits south of the Lakshadweep island group, which belongs to India, and extends across a long north-south axis roughly parallel to the west coast of India and Sri Lanka. The nearest large landmass to the north is India, while Sri Lanka lies to the northeast across open ocean.

The country’s north-south extent covers a considerable distance across the Indian Ocean, even though its total land area is extremely small. This elongated chain of atolls places Maldives along established maritime routes connecting the Arabian Sea, the west coast of India, and the wider Indian Ocean basin, including shipping lanes that link the Middle East, East Africa, and South and Southeast Asia. The country’s location between the Indian subcontinent and the open waters of the central Indian Ocean has historically given it a role as a maritime crossroads, a position that continues to shape its economic and transport geography today.

Area, Geographic Extent, and Island Distribution

Maldives has one of the smallest land areas of any sovereign country, generally cited at around 298 square kilometers. This land area, however, is scattered across a much larger expanse of ocean. The exclusive economic zone associated with Maldives extends across a far greater area of the Indian Ocean than the land area itself, a common feature of small island nations whose maritime territory vastly exceeds their terrestrial footprint.

The islands of Maldives are grouped into natural coral atolls, which are themselves distributed along the long north-south chain described above. Within this structure, individual islands vary considerably in character. Some are inhabited by permanent communities, others remain uninhabited and are used for agriculture, industry, or conservation, and a significant number have been developed exclusively as resort islands for the tourism sector. Still others host airports, harbors, or other specialized infrastructure.

Because the islands are coral formations rather than continental fragments, most are extremely small in area, often just a few hundred meters across. This means the human footprint on any single island is limited, and the built environment of most communities is compact and dense compared with mainland settlements. Where population or economic statistics are cited elsewhere in this article, the reference year is identified, and the distinction between administrative and purely descriptive island counts is explained rather than treated as interchangeable.

Geological and Coral-Atoll Formation

The geological origin of Maldives is fundamentally different from that of continental countries or volcanic island nations with mountainous terrain. Maldives sits atop a submarine ridge structure in the Indian Ocean, and its atolls formed through a long process of coral reef growth on the flanks of ancient, now-submerged volcanic or oceanic foundations. As these underlying foundations subsided gradually over geological time, coral organisms continued growing upward toward sunlight, building thick accumulations of calcium carbonate reef material. This process, first described in general terms by Charles Darwin’s subsidence theory of atoll formation, explains why the reefs of Maldives rest on submerged platforms far below current sea level, capped by living and fossil reef structures near the surface.

Reef-building corals require sunlight and stable warm-water conditions, so growth remained concentrated near the ocean surface even as the underlying seafloor sank. Over long timescales, this dynamic produced ring-shaped or elongated atoll structures encircling shallow lagoons. Waves and currents broke down reef material into sand and rubble, which accumulated on the reef platform to form low sand cays. Many of these cays eventually stabilized with vegetation and became the coral islands that support human settlement today.

A typical Maldivian atoll includes several recognizable zones. The outer reef faces the open ocean and absorbs the force of incoming waves. Just inside this lies the reef crest, the shallow, wave-battered rim where reef growth is often most vigorous. Behind the crest sits the reef flat, a shallow platform that extends toward a central lagoon. The lagoon itself is a relatively calm, shallow body of water enclosed by the surrounding reef structure. Within or along the edges of this lagoon, sand accumulates to form cays, some of which grow large and stable enough to become the coral islands that make up the inhabited and uninhabited land of the country.

This atoll geology differs sharply from the geomorphology of continental countries built on ancient bedrock, and it also differs from volcanic islands with steep terrain formed by lava accumulation. Maldives has essentially no exposed bedrock; its entire land surface is composed of unconsolidated coral sand and reef rubble sitting on top of much older submerged carbonate platforms.

Major Atolls, Islands, and Physical Landscapes

The Maldivian archipelago is organized into a series of natural atolls arranged along its north-south axis, each composed of numerous individual reef islands. Administratively, these natural atolls have been grouped and named differently for governance purposes, a distinction addressed in more detail in the administrative geography section below.

Malé, the capital, occupies one of the smallest yet most densely developed islands in the country, located within the Kaafu Atoll region. Its extremely limited land area has led to extensive land reclamation and vertical construction to accommodate population growth. Nearby, Hulhumalé is a largely artificial island created through land reclamation on a reef platform near Malé. It was developed specifically to relieve pressure on the capital and now hosts substantial housing, infrastructure, and administrative functions.

In the far south, Addu City comprises a cluster of islands within Addu Atoll, connected in part by causeways and linked roads that join formerly separate islands into a more continuous settlement pattern. Addu Atoll is also notable for containing the highest recorded natural elevation point in the country, situated on Vaadhoo Island.

Across the wider archipelago, island morphology varies according to local reef shape, exposure to wave energy, and the extent of any land reclamation. Some islands retain largely natural beach ridges and vegetation lines, while others, particularly resort islands and urbanized centers, show visible modification through reclamation, seawalls, or harbor construction. This variation in landscape, rather than any single uniform “typical island,” characterizes the physical geography of the archipelago.

Topography, Elevation, and Coastal Geography

Maldives has an extremely low natural topography. Most islands rise only slightly above sea level, and average elevation across the country is frequently cited as roughly one to two meters, with the highest recorded natural point reaching approximately five meters on Vaadhoo Island in Addu Atoll. This makes Maldives the lowest-lying country in the world by maximum elevation.

The islands typically consist of flat coral sand terrain, often bordered by low beach ridges formed from wave-deposited sand and coral fragments. Reef flats extend outward from many shorelines, providing a shallow buffer between the island edge and the deeper lagoon or open ocean beyond. Because relief is so minimal, small differences in elevation, sometimes less than half a meter, can determine whether a stretch of land floods during storm surges or remains dry during high tides.

Coastal geography in Maldives is highly dynamic. Sediment naturally moves along shorelines in response to seasonal changes in wave direction linked to the monsoon cycle, causing some beaches to erode during one season and accrete during another. Coral reefs surrounding each island play a critical role in reducing wave energy before it reaches the shoreline, acting as a natural buffer against erosion. Human modification, including seawalls, harbor construction, and land reclamation, has altered these natural sediment patterns on many islands, particularly in and around Malé and other developed centers. Distinguishing natural shoreline dynamics from human-caused coastal change is important, since both processes can produce similar visible effects but require different management responses.

Marine Geography, Coral Reefs, and Lagoons

The marine environment surrounding and within the Maldivian archipelago is central to the country’s physical geography. Extensive coral reef systems encircle each atoll, enclosing shallow lagoons that separate the reef rim from individual islands. Reef channels periodically break the outer reef, allowing water exchange between the lagoon and the open ocean and enabling navigation for boats.

Seagrass meadows occur in some shallow lagoon areas, providing habitat for marine grazers and contributing to sediment stabilization. Mangrove stands are present on a limited number of islands where suitable low-energy, brackish conditions exist, though they are far less extensive than in continental deltaic environments.

Coral reefs perform several interconnected functions. They generate the sand and rubble that form and replenish island land through ongoing biological and physical breakdown of reef material. They support extraordinarily high marine biodiversity, providing habitat for reef fish and numerous invertebrate species. They absorb wave energy, protecting islands from erosion and storm damage. They sustain reef fisheries that supply food and income to island communities. And they form the ecological foundation for much of the tourism sector, which depends on clear water, visible coral structures, and abundant marine life. This layered relationship between reef structure and human settlement means that reef health is not simply an environmental concern but a factor directly tied to land stability, food security, and economic activity.

Climate and Weather Patterns

Maldives has a tropical maritime climate shaped strongly by its surrounding ocean and by seasonal monsoon circulation. Two principal monsoon seasons affect the country: a southwest monsoon, generally associated with wetter conditions and stronger winds, and a northeast monsoon, generally associated with drier, calmer weather. The exact timing and intensity of each season vary from year to year.

Temperatures across Maldives remain relatively stable throughout the year, a pattern typical of tropical maritime locations where the surrounding ocean moderates temperature swings that would otherwise occur on continental landmasses. Humidity remains consistently high, and cloud cover fluctuates with the monsoon cycle, generally increasing during the wetter southwest monsoon period.

Rainfall patterns show both seasonal and regional variation across the archipelago, with different atolls experiencing somewhat different totals and timing depending on their position relative to prevailing monsoon winds. Tropical storm activity in the immediate vicinity of Maldives is relatively limited compared with other parts of the Indian Ocean basin, though the country can still experience heavy rainfall events, strong winds, and swells generated by distant storm systems. Interannual variability, including fluctuations linked to broader Indian Ocean climate patterns, can influence rainfall totals and storm activity from one year to the next.

Oceanography and Water Resources

Freshwater availability in Maldives is shaped directly by its coral-island geography. Rainfall is the principal natural source of freshwater, since the small size and low elevation of most islands prevent the formation of rivers, streams, or large surface water bodies. On many islands, freshwater has traditionally been drawn from shallow groundwater lenses, layers of fresh water that float above denser saltwater within the porous coral sand beneath each island.

These groundwater lenses are inherently fragile. Because the islands are small and composed of highly permeable sand, groundwater lenses are vulnerable to saltwater intrusion from storm surges, sea-level fluctuations, and over-extraction. Contamination from inadequate sanitation infrastructure has also degraded groundwater quality on a number of inhabited islands. As a result, many communities and resorts now rely heavily on rainwater harvesting and desalination to supplement or replace groundwater use, particularly in the capital region and on islands with high population density or intensive tourism development.

The relationship between rainfall, island size, and freshwater availability is direct: smaller islands with limited land area have correspondingly limited capacity to store rainwater and support groundwater recharge, meaning that population density and infrastructure investment in desalination or storage capacity are closely linked to the physical scale of each island.

Natural Environment and Biodiversity

The natural environment of Maldives spans both terrestrial and marine ecosystems, though the marine realm is by far the more extensive and ecologically significant of the two. Terrestrial vegetation on most islands is limited to coastal and beach vegetation adapted to sandy, salt-affected soils, including low shrubs, coconut palms, and other salt-tolerant plant species suited to the tropical island environment.

The marine ecosystem is considerably richer. Coral reefs support high biodiversity of reef fish species, while seagrass meadows and reef flats provide feeding grounds for herbivorous marine species. Sea turtles, including species that nest on some Maldivian beaches, rely on both the reef environment and adjacent sandy shorelines. A wide range of shark and ray species inhabit the surrounding waters, reflecting the productivity of the reef and open-ocean environments. Dolphins are commonly found in the channels and open waters around the atolls, and numerous seabird species use islands and reef areas for feeding and, in some cases, nesting.

These species and ecosystems are best understood as components of a broader ecological geography rather than as isolated attractions. Reef fish populations, for instance, depend on healthy coral structure, which in turn depends on water quality and temperature conditions shaped by the surrounding oceanography.

Population and Demographic Geography

According to the most recent official census, conducted in 2022, the population of Maldives numbered several hundred thousand people, concentrated disproportionately within a small fraction of the country’s total land area. Population density at the national level is unusually high when measured against total land area, though this figure is heavily influenced by extreme concentration in and around the capital.

Distribution of population across the archipelago is highly uneven. A large share of the population resides in the greater Malé region, while numerous other inhabited islands have comparatively small populations, sometimes numbering only in the hundreds. This concentration reflects both historical settlement patterns and more recent internal migration toward the capital region in search of employment, education, and services. Maldives also hosts a significant foreign-worker population, employed primarily in construction, tourism, and other sectors, though the precise scale of this population varies depending on the source and year of measurement.

Urbanization in Maldives is closely tied to this pattern of concentration, with the capital region functioning as the primary urban center for administration, commerce, and services, while other inhabited islands remain comparatively rural or small in scale.

Urban Geography and Malé

Malé stands out as one of the most densely populated urban islands in the world relative to its extremely small land area. This extreme concentration developed as administrative, economic, and educational functions increasingly centralized in the capital over recent decades, drawing migration from other islands despite the island’s limited physical space.

Land scarcity in Malé has driven extensive reclamation along its shoreline and pushed development toward vertical construction, with multi-story residential buildings replacing the low-rise housing more typical of outer islands. This density places significant pressure on infrastructure, including housing supply, road networks designed for a small land area, waste management systems, and freshwater supply, which relies substantially on desalination given the limited capacity for rainwater storage and groundwater recharge on such a small, heavily built-up island.

Hulhumalé, a reclaimed island connected to Malé by a bridge, has been developed specifically to relieve this pressure, providing additional residential and infrastructural capacity. The geographic relationship between the two islands reflects a broader strategy of managing land scarcity through reclamation rather than through outward expansion onto naturally occurring but limited land.

Languages, Culture, and Human Geography

Dhivehi is the national and official language of Maldives, spoken across the inhabited islands with some regional variation in dialect, particularly in more geographically isolated southern atolls. The dispersed island environment has historically shaped how communities organized themselves, with each inhabited island typically developing a degree of local identity and self-sufficiency due to the practical difficulty of frequent travel between islands before the advent of modern transportation.

Maritime culture runs through much of Maldivian society, reflected in longstanding fishing traditions and boatbuilding knowledge adapted to reef and open-ocean conditions. Historical and cultural links extend across the wider Indian Ocean, connecting Maldives to trading and cultural exchange with South Asia, the Arabian Peninsula, and East Africa over centuries.

The archipelago’s dispersed geography has directly influenced communication and economic organization, as inter-island travel by boat, and more recently by air, remains necessary for the movement of goods, services, and people between otherwise isolated communities.

Administrative and Political Geography

Maldives is administratively organized around its capital, Malé, along with a number of administrative atolls and designated cities. These administrative atolls are political and governance groupings that do not always correspond exactly to the natural, geographically defined atolls described in the geological section above. In some cases, administrative boundaries combine parts of multiple natural atolls or separate sections of a single natural atoll into different administrative units, a distinction that should not be treated as interchangeable with natural atoll geography.

Within each administrative division, individual islands function as the basic units of local governance, with inhabited islands typically administered through island-level councils. This administrative framework governs matters such as local infrastructure, land use, and municipal services, operating within the broader national government structure based in Malé.

Historical Geography

The historical geographic development of Maldives has been shaped consistently by its maritime location. Early settlement of the islands is understood to have involved seafaring peoples arriving from the surrounding Indian Ocean region, drawn by the reef and lagoon resources that could support small communities.

Over subsequent centuries, the archipelago’s position along Indian Ocean trade routes connected it to broader networks of maritime commerce linking South Asia, the Arabian Peninsula, and East Africa. Historical accounts describe Maldives as a source of goods such as cowrie shells and coir rope, traded outward through these networks. The introduction of Islam represented a significant historical geographic development, reshaping social and cultural organization across the islands and linking Maldives more closely to Islamic trading networks across the Indian Ocean.

During the colonial era, Maldives maintained a distinct political status relative to some neighboring territories, eventually developing into a fully independent, modern state in the second half of the twentieth century. Since independence, geographic development has centered on strengthening inter-island connectivity, expanding the capital region, and building the infrastructure necessary to support both a dispersed population and a growing tourism economy.

Fisheries and Marine Resource Geography

Fisheries hold longstanding geographic and economic importance in Maldives. Tuna fishing, in particular, has historically formed a central pillar of the fishing economy, supported by the country’s location along productive open-ocean waters where tuna populations migrate seasonally. Traditional pole-and-line fishing techniques remain culturally significant and continue alongside more modern commercial fishing operations.

Reef fisheries provide an additional, more localized source of food and income for island communities, drawing on the biodiversity supported by surrounding coral reef systems. Ocean conditions, including seasonal current patterns and water temperature, directly influence where and when fish stocks are most abundant, shaping the rhythms of fishing activity across different atolls.

The cultural and economic importance of fishing in Maldives is substantial, though sustainable management of these resources is an ongoing consideration given increasing pressure from expanding fishing effort and broader environmental change affecting fish populations and reef health.

Agriculture and Food Production

Agricultural geography in Maldives is severely constrained by the physical characteristics of its islands. Limited land area, sandy and nutrient-poor soils, restricted freshwater availability, and salinity all limit the scale and diversity of crop cultivation possible on most islands. High population density on inhabited islands further limits the land available for farming relative to housing and other uses.

Where cultivation does occur, it is generally limited to crops tolerant of these conditions, including coconut palms and certain fruits and vegetables grown on a small scale, often supplemented by imported soil or controlled growing environments on some islands. Given these constraints, Maldives depends heavily on food imports to meet national consumption needs, a dependence directly linked to the physical limitations of its island geography and a central factor in the country’s food security considerations.

Economy and Economic Geography

The Maldivian economy is structured around a relatively small number of key sectors shaped directly by the country’s island geography. Tourism represents the largest single contributor to the national economy, supported by the resort-island development model described in more detail below. Fisheries remain an important traditional sector, alongside transport and maritime services necessary to connect the dispersed archipelago. Construction activity, closely tied to land reclamation and tourism infrastructure development, and a range of trade and service-sector activities round out the broader economic structure.

Tourism development is geographically concentrated on specific islands designated and developed for resort use, often located near attractive reef and lagoon environments, while other islands remain reserved for local communities, fishing, or conservation. Malé functions as the country’s principal economic and administrative center, hosting the main port, government institutions, and a concentration of commercial activity that draws economic linkages from across the archipelago.

The dispersed island structure imposes distinctive economic costs. Transporting goods, delivering services, and maintaining infrastructure across many small, separated islands requires more extensive shipping, aviation, and logistics networks than would be needed in a geographically consolidated country of similar population size, contributing to higher per-capita costs for infrastructure and service delivery.

Tourism and Island Development

Tourism in Maldives follows a distinctive geographic model built around dedicated resort islands, many of which are developed exclusively for this purpose rather than shared with residential communities. This model relies directly on the physical assets of the surrounding environment, including coral reefs, clear lagoon waters, sandy beaches, and high marine biodiversity, all of which depend on the health of the reef and lagoon systems described earlier in this article.

Access to resort islands typically depends on a combination of transportation modes suited to the archipelago’s fragmented geography, including domestic flights, seaplane transfers, and boat transport connecting islands to the main international gateway near Malé. The scale of island development required to support resort infrastructure, including accommodation, water and waste treatment facilities, and staff housing, places direct environmental pressure on small island ecosystems, particularly regarding wastewater management, solid waste disposal, coastal modification for erosion control or land expansion, and freshwater demand from desalination and other supply systems.

Transportation and Regional Connectivity

Transportation geography in Maldives is shaped fundamentally by the fragmented, dispersed nature of the archipelago. Domestic aviation, including both fixed-wing aircraft and seaplanes, connects the capital region to outer atolls and resort islands where boat travel alone would be impractical for longer distances. Boats remain essential for shorter inter-island trips, ranging from small local ferries to speedboats used for faster transfers, particularly for tourism-related transport.

Velana International Airport, located near Malé, functions as the country’s principal international gateway, connecting Maldives to destinations across South Asia, the wider Indian Ocean region, and beyond. A network of harbors and smaller domestic airports across various atolls supports onward travel to more distant island communities. This layered transportation system, combining air and maritime links, is necessary precisely because no single mode could adequately connect a country composed of hundreds of separated islands spread across a long ocean expanse. Regional connectivity extends this network outward, linking Maldives with India, Sri Lanka, and broader Indian Ocean shipping and aviation routes.

Energy Geography and Infrastructure

Electricity generation in Maldives has historically depended heavily on imported fossil fuels, particularly diesel, transported to individual islands for local power generation. This reliance reflects the practical difficulty of building a unified national electricity grid across a widely dispersed archipelago, where undersea cabling between distant islands is often impractical or prohibitively costly.

In recent years, solar energy has emerged as a growing component of the national energy mix, offering a renewable alternative suited to the country’s abundant sunlight and reducing dependence on fuel imports. Battery storage systems have been introduced on some islands to help manage the intermittency of solar generation. Nonetheless, the challenge of supplying reliable electricity across many small, isolated islands remains significant, and renewable energy expansion must contend with limited land area for solar installations and the logistical difficulty of distributing power equipment across a fragmented geography.

Natural Hazards and Environmental Challenges

Maldives faces a distinctive set of natural hazards linked directly to its low elevation and small island morphology. Coastal flooding and storm surges pose recurring risks, capable of inundating low-lying areas even during moderate weather events given the minimal elevation separating land from sea level. Extreme wave events and swells generated by distant storm systems can also affect shorelines, contributing to coastal erosion on exposed islands.

Heavy rainfall events can cause localized flooding on islands with limited natural drainage capacity, while periods of low rainfall can create freshwater stress given the limited storage capacity of island groundwater lenses. Marine heat stress represents an additional hazard, capable of triggering coral bleaching events that weaken reef structures and reduce their capacity to protect islands from wave energy. Because reefs function as a primary natural buffer against coastal erosion and storm damage, any degradation of reef health carries direct consequences for coastal hazard exposure.

Climate Change, Sea-Level Rise, and Environmental Change

Maldives is widely recognized as particularly exposed to the effects of climate change and sea-level rise, a consequence directly linked to its extremely low elevation and small island morphology. Observed changes documented by international climate research include measured increases in sea level across the Indian Ocean basin and rising sea surface temperatures, both of which carry direct implications for a country where even small elevation changes affect large proportions of habitable land.

Scientific projections indicate continued sea-level rise over coming decades, though the precise magnitude and pace remain subject to ongoing research and depend heavily on future global greenhouse gas emissions trajectories. Potential impacts under these projections include increased frequency of coastal flooding, accelerated shoreline erosion, greater risk of saltwater intrusion into groundwater lenses, and continued pressure on coral reef systems from ocean warming and acidification. Changes in rainfall patterns and extreme weather events could further affect freshwater security, fisheries productivity, and tourism infrastructure.

It is important to distinguish between what has been directly observed and what remains a scientific projection subject to uncertainty. While Maldives faces genuine and well-documented exposure to these environmental changes, credible scientific assessments describe a range of possible future scenarios rather than a single certain outcome, and adaptation measures can meaningfully influence how these risks unfold over time.

Conservation and Environmental Management

Environmental management in Maldives centers substantially on protecting the coral reef and marine ecosystems that underpin both the natural environment and the economy. Marine protected areas have been established in various locations to limit fishing pressure and other disturbances in ecologically significant reef zones. Reef conservation efforts, including monitoring of coral health and, in some cases, coral restoration projects, aim to support reef resilience in the face of warming ocean temperatures.

Waste management presents a persistent challenge given the limited land area available for disposal facilities across a dispersed archipelago, prompting efforts to improve recycling, waste consolidation, and treatment capacity. Coastal protection measures, including engineered structures and reef-based approaches, aim to reduce erosion and flooding risk on vulnerable islands. Sustainable fisheries management seeks to balance continued economic reliance on fishing with the long-term health of fish stocks, while climate adaptation planning and freshwater management initiatives address the broader environmental pressures described in earlier sections. Coordinating these efforts across a highly dispersed set of islands, each with its own local conditions and infrastructure needs, remains a significant practical challenge for environmental governance in Maldives.

Regional Geographic Importance

Within the Indian Ocean and South Asian region, Maldives holds geographic significance stemming from its central oceanic location along established maritime routes. Its coral-atoll geography and associated marine biodiversity make it a notable example within global discussions of reef ecosystems, atoll formation, and small island environmental management. Its fisheries and tourism sectors connect it to broader regional and global economic networks, while its transportation links tie it into wider Indian Ocean air and maritime connectivity. Environmentally, Maldives is frequently referenced in international discussions of sea-level rise and small island vulnerability, reflecting the distinctive physical characteristics detailed throughout this article.

Key Geographic Facts

Geographic Fact	Information
Official Name	Republic of Maldives
Capital	Malé
Region	South Asia / Indian Ocean
Total Area	Land area of approximately 298 sq km, surrounded by a much larger maritime exclusive economic zone
Land Area	Approximately 298 sq km
Geographic Setting	Coral atoll archipelago
Number of Atolls	Approximately 26 natural coral atolls; administrative atolls are grouped differently for governance purposes
Number of Islands	Approximately 1,192 coral islands (figures vary depending on counting method and definition of an island)
Highest Natural Elevation	Approximately 5.1 meters, on Vaadhoo Island, Addu Atoll
Major Ocean	Indian Ocean
Major Seas/Water Bodies	Laccadive Sea (northern waters), Arabian Sea (regional context)
Climate	Tropical maritime, monsoon-influenced
Population	Approximately 515,000–521,000 (2022 census)
Population Density	High at the national level due to concentration in Malé; varies greatly by island (2022 census)
Official Language	Dhivehi
Administrative Divisions	Malé (capital) and a number of administrative atolls/cities
Major Economic Sectors	Tourism, fisheries, transport and maritime services, construction, trade
Major Natural Resources	Fisheries (notably tuna), coral reefs
Major Marine Ecosystems	Coral reefs, atoll lagoons, seagrass meadows, limited mangrove stands
Major Environmental Challenges	Sea-level rise, coastal erosion, coral bleaching, freshwater scarcity, waste management
Currency	Maldivian Rufiyaa