{ "id": "bahamas", "title": "Bahamas", "lang": "en", "source_lang": "en", "summary": "The Bahamas is a Commonwealth island nation of more than 700 islands and cays in the western Atlantic, southeast of Florida and north of Cuba.", "category": "geography", "subcategory": "", "type": "place", "aliases": [ "The Bahamas", "Commonwealth of The Bahamas" ], "generated_at": "2026-10-09", "model": "pro/claude-haiku-5-5", "url": "https://aiwiki.page/en/bahamas/", "translations": { "zh-Hans": { "url": "https://aiwiki.page/zh/bahamas/", "json": "https://aiwiki.page/zh/bahamas.json" } }, "sections": [ { "heading": "", "text": "The Bahamas, formally the Commonwealth of The Bahamas, is an archipelago of more than 700 islands and cays in the western North Atlantic, southeast of Florida and north of Cuba. Although it sits in the Atlantic rather than the Caribbean Sea proper, it is usually grouped with the Caribbean region. Its land area is only about 13,900 square kilometres, yet its exclusive economic zone covers roughly 655,000 square kilometres, so its maritime extent is far larger than its land suggests.\n\nThe islands are the exposed parts of two submerged carbonate platforms, the Great Bahama Bank and the Little Bahama Bank, which explains the country's low relief, white sand, shallow turquoise waters, reefs, tidal channels and blue holes. Its highest point, on Cat Island, is only 63 metres above sea level. The tropical climate, moderated by the Gulf Stream, supports tourism and rich marine and coastal ecosystems, but it also exposes the country to hurricanes, storm surge, coastal erosion, sea-level rise and saltwater intrusion into its groundwater. These hazards and the lack of permanent rivers make geography central to the country's economy, settlement pattern and environmental policy.\n\nThis entry covers the Bahamas as a geographic system. It begins with location, the geological foundation and the island groups, then examines relief, hydrology, climate and ecosystems. It goes on to human geography, including population distribution, urban growth and land use, followed by the economic geography of tourism and finance, transport and maritime boundaries, natural hazards, conservation, the history of geographic knowledge, and the administrative and political divisions that shape the archipelago." }, { "heading": "Location, Extent and Name", "text": "The Bahamas is an archipelagic state in the western Atlantic Ocean, lying roughly between 21° and 27° N. Its islands run southeast from the coast of Florida toward Cuba and Hispaniola, and the northwestern island of Andros is about 200 km southeast of Florida. The country's official name is the Commonwealth of The Bahamas, and it sits within the wider Caribbean region, although it lies in the Atlantic rather than in the Caribbean Sea itself.\n\nReference figures for the total land area cluster closely. Wikipedia-based geographic data give 13,878 km², while several factbooks report about 13,880 km². The small gap reflects how each compiler measures the land. Such differences arise from decisions about how to treat tidal flats, the many small cays, and the boundary between land and shallow water. A much larger figure appears in the legal calculations used for the archipelagic baseline system. Under that method, the total area is 250,102 km² and the land area is 31,810 km², because most of the underwater banks are counted as land. The difference between these numbers is therefore one of definition, not of survey error.\n\nThe country's maritime zones are much larger than its land. Wikipedia-based data put the exclusive economic zone at 654,715 km², which ranks 41st among the world's EEZs by size. A separate boundary dataset gives a lower figure of about 619,786 km², so the total also depends on the data source used. The Bahamas ratified the United Nations Convention on the Law of the Sea in 1983. Its 1993 domestic legislation sets a 12-nautical-mile territorial sea and a 200-nautical-mile EEZ, both measured from the archipelagic baselines rather than from individual coastlines. The length of the chain is also reported inconsistently. Travel guides describe it as roughly 1,200 km from northwest to southeast, while the more conservative figure of more than 800 km captures the core of the chain.\n\nThe name is most often explained as a derivation from the Spanish phrase baja mar, meaning \"shallow sea\", a reference to the extensive shallow banks around the islands. Tourist guides repeat this account widely. However, the linguist Wolfgang Ahrens of York University argues that it is a folk etymology, that is, a plausible-sounding explanation that was attached to the name after the fact. Another line of explanation links the name to Lucayan. In that account, Bahama was a local term, often glossed as \"large upper middle island\", that originally referred to Grand Bahama alone. Its earliest known appearance is on a map of about 1523, and English usage extended it to the whole archipelago by 1670. A further hypothesis derives the name from Guanahaní, the local name of the island where Columbus first landed in 1492, whose original meaning is no longer known. Isaac Taylor, a toponymist, has proposed a derivation from Bimini, an island that also figures in European legends. None of these explanations has been universally accepted, so the baja mar story should be read as the most familiar account rather than as an established fact." }, { "heading": "Islands, Cays and Island Groups", "text": "The number of Bahamian islands depends on the source and on where each one draws the line between an island and a cay. The government's overview describes a group of about 700 islands and 2,400 cays, and it gives thirty as the number of inhabited islands The group consists of 700 islands and 2,400 cays with an area of 5,358 sq. miles (13,878 sq. km.). Thirty of the islands are inhabited. Other compilations differ. A map site gives 31 inhabited islands But only 31 of them are inhabited., and one travel-industry source gives 26 Andros Island is the largest of the 26 inhabited islands of the Commonwealth of the Bahamas. Most of these differences probably reflect counting rules and the use of different dates, not disagreement about the land itself.\n\nAndros is the largest island and the best example of how fragmented the group is. Its land area is about 5,957 km², and it is 167 kilometres (104 mi) long by 64 km (40 mi) wide at the widest point. For administrative purposes it counts as one island, yet its landmass exceeds the combined area of the other Bahamian islands Politically considered a single island, Andros in total has an area greater than all the other 700 Bahamian islands combined. Its structure is divided. The three main parts are North Andros, Mangrove Cay and South Andros, and the three main islands are separated by bights, estuaries that divide the island from east to west. Some of the channels between them are up to 5 km wide by channels up to 5 km across. Smaller islets and cays fill the gaps, linked by mangrove estuaries and tidal swamplands, so the northern and southern sections are separated by water rather than by a continuous land route.\n\nNew Providence and Grand Bahama are the two principal islands in economic and demographic terms. New Providence is where the capital is located, and New Providence (where the capital, Nassau, is located). Grand Bahama, with Freeport, is the other main urban centre; a Bahamas tourism guide describes the city of Freeport as considered the 2nd city. The two islands carry most of the population. Ninety percent of the total population lives on New Providence, Grand Bahama and Abaco. New Providence has 69.9 percent of the population, Grand Bahama and Abaco with 15.5 percent, and 10.3 percent are scattered on the remaining islands and cays. (The population figures are discussed in a separate section.)\n\nThe remaining islands are usually grouped as the Family Islands, a local term rather than an official administrative category. Other islands, referred to locally as Family Islands, such as Eleuthera, Long Island, Cat Island and an additional four islands are commonly named in this way. Lists differ on membership. One tourism-oriented account names Abaco, Acklins and Crooked Island, Andros, the Berry Islands, the Biminis, Cat Island, Crooked, Eleuthera, the Exumas, Harbour, Inagua, Long Island, Mayaguana, San Salvador, and Spanish Wells. The government's social-services division uses a similar range of places, including Abaco, Acklins, Andros, Berry Islands, Cat Island, Crooked Island, Eleuthera, Exuma, Inagua, Long Island, Mayaguana and San Salvador.\n\nShape and size vary greatly across the group. Some islands are large and multi-part, such as Andros, while others are single cays with little or no permanent settlement. The Exumas illustrate the scattered end of this range, with one travel guide claiming over 365 islands, called cays. The archipelago as a whole spans a long north-west to south-east arc, and The Bahamas is an archipelagic state that extends 760 miles from the coast of Florida on the north-west almost to Haiti on the south-east. Because of this spacing, air links, ferries and boats connect the outer islands to the main centres, and the variation in island size shapes where services, roads and tourism development can be sustained." }, { "heading": "Carbonate Platforms and Geological Foundation", "text": "The islands are the emergent parts of two large submerged carbonate platforms. The northeastern islands rise above sea level from the Little Bahama Bank and the Great Bahama Bank, which are separated by a deep channel, with the Little Bahama Bank lying to the north The northeastern Bahama Islands are isolated landmasses that project above sea level from two large carbonate platforms, Little Bahama Bank and Great Bahama Bank. Little Bahama Bank lies north of the Great Bahama Bank and is separated from it. by a deep channel. Further southeast, the banks give way to smaller, isolated platforms that carry the southeastern islands and cays. The platforms are generally regarded as an outlying part of the North American continental shelf; southeast of Florida, they form submerged limestone plains of nearly 60,000 square miles, and most of that area is covered by only a few feet of clear water Southeast of Florida, outliers of the continental shelf form submerged limestone plains covering nearly 60,000 square miles. These are the Bahamian platforms which, for the most part, are covered by only a few feet of clear sea water.\n\nAlmost all of the bedrock is carbonate rather than igneous rock. Sedimentation began in the Late Triassic and Early Jurassic with a mix of siliciclastic, carbonate and evaporite material, but the bulk of the sedimentary fill from the Jurassic to the present is carbonate The Great Bahamas Bank was initiated by the accumulation of a mix of siliciclastic, carbonate s and evaporite s in the Late Triassic and Early Jurassic but most of the sedimentary fill is from the Jurassic to Holocene is composed of carbonate sediments. Because the archipelago was cut off from the North American landmass, it remained an almost purely carbonate province through the Tertiary As a result of their isolation from the North American landmass, the Bahamas have been an exclusively carbonate province throughout the Tertiary. The contrast with the wider Caribbean is marked: Unlike other Caribbean islands, the Bahama islands largely consist of limestone rather than volcanic rock. The banks have also been tectonically-stable and isostatically-subsiding platforms since the Mesozoic, so the islands owe their existence to accumulation and subsidence rather than to volcanism or uplift.\n\nThe carbonate pile is very thick. One estimate puts the Great Bahama Bank's accumulation at at least 4500 m thick that has been accumulating since Cretaceous time. Subsidence has been persistent. Nearly three miles of carbonate deposits have been laid down in the Bahamas since the early part of the Cretaceous period, indicating that there has been a high sustained rate of deposition. Doubtless this has contributed to the persistent subsidence of the area. The basement beneath the carbonate is thought to be continental in structure, and it may have split from North America during the opening of the Atlantic The crustal block basement underneath the Bank is continental in structure and may have rifted from North America when that continent began to break off from Africa and the Atlantic Ocean originated.. Its margins are not uniform, though. Along the southwestern side, the platform appears to sit on oceanic crust, so the crust beneath the banks varies across the archipelago the northwest Bahamian platform is on the edge of the North American continental crust, while to the southwest it is situated over oceanic crust.\n\nThe sediment itself is largely biological or chemical in origin. On the Great Bahama Bank, abiotic precipitation of aragonite needles and ooids, as well as biogenic contributions from skeletal fragments both contribute to the sediment, and skeletal remains of algae and invertebrates add further material Abundant sediments are also being formed by accumulation of skeletal remains of calcareous algae and invertebrates.. The ooids are concentrated near the margins of the banks, and currents then move them into the interiors Most of this oolitic sand originates within a few hundred meters of the bank margins, but currents distribute the sand into the interior of the bank.. Bank margins are shaped by several interacting factors, including the direction, magnitude, and duration of tidal currents, waves, and storms; the nature and history of sea-level fluctuations; the antecedent (usually bed rock) topography, as well as the biological barriers and sediment supply. The shallow interiors reinforce this dynamic: on the Great Bahama Bank, Water depth on the Great Bahama Bank platform is generally less than 4 fathoms, which keeps the banks exposed to wave action and makes them responsive to storms.\n\nMuch of the visible surface records the Ice Age. The surface geology largely reflects the role of Pleistocene sea-level fluctuations. When sea level fell, the banks were partly exposed and their sediments were altered, and when it rose again, Carbonate dunes are formed during the transgressive phase, where the rising sea level carried sand into new dune ridges. Over time, these ridges and the oolitic sands of the margins were cemented into the Quaternary oolites and eolianites that form much of the present island surface. Rainwater dissolution then acted on this young limestone, producing karst features that now characterize the landscape." }, { "heading": "Relief and Submarine Landforms", "text": "Surface relief\n\nLittle of the archipelago rises far above the sea. Cat Island also has the nation's highest point, Mount Alvernia (formerly known as Como Hill). It rises to 63 metres (207 ft) and is topped by a monastery called The Hermitage. New Providence, which holds Nassau, is much lower, reaching only about 37 metres at its maximum elevation. Because the islands are the emerging tops of the banks, their heights are set by how far those shallow platforms stand above the water, not by high ground within the islands.\n\nThe Tongue of the Ocean\n\nBetween Andros and New Providence lies the Tongue of the Ocean (TOTO), a U-shaped, relatively flat-bottomed depression measuring approximately 30 by 240 kilometres. Its floor deepens northward: its depth varies gradually from 1,100m (3,600ft) in the south to 2,000m (6,600ft) in the north. Dive operators usually describe the depth as about 6,000 feet, which matches the upper end of these survey figures. The trench reaches the open Atlantic only at its northern end, and the surrounding islands, reefs, and shoals form a shelter that isolates it from ocean disturbances, particularly high ambient noise. This quiet setting is one reason the trench is used for acoustic testing.\n\nThe trench belongs to a larger submarine system. This channel and the Providence Channels are the two main branches of the Great Bahama Canyon, a submerged geological feature formed by erosion during periods of lower sea level. Early on, the basin was broad, relatively shallow basins flanked by growing carbonate banks. Afterward, the banks kept pace with sediment accumulation while the basins did not, so the deep form persisted. As the Blake-Bahama platform subsided, sedimentation kept pace with subsidence on the banks, but not in the basins.\n\nThe contrast between bank and trench is abrupt. Off Andros's eastern coast, shallow coral reefs abruptly give way to a vertical drop that descends from roughly 100 feet to depths exceeding 6,000 feet.\n\nBlue holes\n\nThe term blue hole describes a sinkhole that is filled with water, while the entrance to them is located beneath the surface. Such features occur on land and offshore and are a form of karst landscape. Most of the Bahamian blue holes and caves are believed to have formed in the Pleistocene, during the last million years and the ice ages. Fresh water easily dissolves limestone, creating tiny holes throughout. Passages widened over time, and the cycles of lower and higher sea level then played a decisive role. During the Ice Age, the ice caps spread over the world causing the sea water levels to slowly fall. Underground and sea level rose, filling the caves with water and forming what we know today as blue holes.\n\nDepths of more than 200 metres are recorded. Dean's Blue Hole, on Long Island, has a depth of 202 metres (663 ft). Sources disagree on its ranking: one account places it world's third deepest blue hole after the Taam Ja' Blue Hole in the Chetumal Bay and Dragon Hole in the South China Sea. Its origin is also uncertain; it is believed that the blue hole was caused by either a fault in the limestone that allowed a corrosive solution to rise or that a buried cavern collapsed creating a sinkhole.\n\nAndros is often described as the centre of blue hole formation, but counts differ. One tourism source states that Andros has 200 blue holes — the highest concentration on earth. Another gives a breakdown of 175 documented inland blue holes and approximately 50 offshore, a total of around 200. The difference reflects how inland and offshore features are counted and which sites are included." }, { "heading": "Hydrology and Freshwater Resources", "text": "The Bahamas has no permanent rivers, so surface water contributes little to supply. A hydrogeologist's review of national water resources states that all freshwater in the country is groundwater, and there are no rivers. Some islands nonetheless hold ponds, swamps and wetlands, but these are seasonal or localised and do not form a usable regional network.\n\nGroundwater is held in the porous limestone that makes up the islands. Rainfall percolates through the rock and forms a lens of fresh water that floats on denser seawater beneath it, so excessive pumping can draw salt water upward into the wells. The Food and Agriculture Organization identifies fresh groundwater as the primary source of drinking water. Rooftop and cistern collection is marginal by comparison, supplying a meagre three percent or less of the water. Pumping has already caused damage on New Providence, where historic groundwater sources were over-extracted to severe levels of salinization, and some aquifers had not recovered more than eight years later.\n\nDesalination has become the main answer to this shortfall. The hydrogeologist notes that drinking water could only be obtained from wells or from collected rainwater until 1960, when the government began using desalination to supply New Providence. Most freshwater is now provided by desalination through the reverse osmosis process. On New Providence, diesel-operated reverse osmosis plants have served as the primary source of potable water, and an older industry report put their share at about 90% of the water supplied on the most populous island. The cost is substantial: 2003–2004 production figures priced reverse osmosis water at $6.60 per thousand imperial gallons when blended with groundwater, compared with $3 to $4 from New Providence wellfields. Before this, fresh water was barged in from the larger Andros Island for about 40 years, which ultimately became insufficient to meet demand.\n\nWater balance differs sharply between islands. The FAO's renewable freshwater estimates give 155.13 million m³ per year for Grand Bahama and 16.03 million m³ per year for New Providence, and Grand Bahama, Abaco and Andros have enough fresh groundwater reserves to meet their demands, while New Providence and many central and southern islands will depend on desalination. The same report expects that desalination will most likely continue to increase as fresh groundwater availability declines and water demands grow.\n\nUtilities are responding in several ways. The Grand Bahama Utility Company installed a reverse osmosis unit to desalinate groundwater abstracted from Wellfield 6. To counter saltwater intrusion into the freshwater lens, researchers propose managed aquifer recharge, in which excess water from rainfall, surface sources or desalination plants is stored in a suitable aquifer and recovered when demand is higher. Reverse osmosis raises concerns about emissions, and Ocean Thermal Energy Conversion is under consideration to co-generate clean energy alongside drinking water.\n\nShallow banks and tidal channels also constrain movement around the archipelago. Navigation is restricted in many areas, and large vessels can use only a limited number of passages, which shapes where ports and supply routes can be developed." }, { "heading": "Climate and Weather", "text": "Most of the archipelago's districts fall into the Köppen Aw category, a tropical wet-and-dry or savanna type. Most regions (24) in The Bahamas lie in the Tropical wet and dry or savanna climate zone (Köppen: Aw). Other descriptions place the islands in a subtropical marine regime, in which the Gulf Stream softens conditions: warm breezes from the Gulf Stream and the Atlantic Ocean moderate the climate. The two frameworks overlap, and the choice between them mainly reflects whether the classification emphasises latitude or ocean influence. Climate type aside, the weather is governed by two seasons.\n\nThe wet season runs from May to October. During these months, warm, moist tropical air masses dominate, as the Bermuda High brings a southeasterly flow from the deep tropics. The dry season from November to April is shaped by different air. The subtropical high retreats, and drier northeast trade winds, along with occasional westerlies from the North American mainland, reach the islands. Rain in the wet season usually falls in short-lived, fairly intense, but brief thundershowers accompanied by strong gusty winds, followed by a return to clear skies.\n\nAnnual rainfall differs between sources and between stations, so precise totals should be checked against national meteorological records. One widely cited figure is about 1,120 mm, which occurs mostly during the summer months. Another summary gives an annual average of 1,250 millimetres, with some variation among the different islands. Station data show lower totals in places, with one location in the north-west registering approximately 958 mm a year. Temperatures are more uniform. Britannica states that the average temperature varies from the low 70s F during the winter to the low 80s F during the summer. On Grand Bahama, Freeport's summer highs average 31 °C (88 °F), and low temperatures average 26 °C (79 °F).\n\nHurricanes are the most disruptive weather hazard. Tropical cyclones (hurricanes) pose a threat during the period from June to November and have occasionally caused great destruction. Risk is not evenly spread across the season. The Bahamas lies in the heart of the Atlantic hurricane belt, where hurricanes occur throughout August, September and October. Because most islands are low-lying, storm surge and flooding from tropical cyclones present particular dangers, and this exposure is discussed further in the section on natural hazards.\n\nYear-to-year variability is strongly tied to the El Niño–Southern Oscillation. Inter-annual variability in climate is strongly influenced by the El Niño Southern Oscillation (ENSO). The link extends to storms: the occurrence of hurricanes is strongly linked to ENSO, with more frequent hurricane activity associated with La Niña events, and less frequent events in El Niño years. During La Niña episodes, the wet season can turn colder and wetter. These shifts affect tourism, freshwater supply and agriculture, since dry-season droughts already can impact farming and agriculture.\n\nLong-term change is also measurable. Mean annual temperature has increased by around 0.5 °C since 1960, at an average rate of 0.11 °C per decade. By contrast, mean rainfall over The Bahamas has not changed significantly since 1960. Projections for the coming decades point to continued warming, with the mean annual temperature expected to increase by 0.8 to 2.3 °C by the 2060s, which links the climate record to broader climate change concerns." }, { "heading": "Marine Ecosystems, Coral Reefs and Coasts", "text": "The most prominent reef system in the Bahamas is the Andros Barrier Reef, which lies along the eastern coast of Andros, close to the Tongue of the Ocean. Its reported length varies by source: the Bahamas National Trust gives about 124 miles, EBSCO gives about 135 miles, and several tourism sites give about 190 miles. Those figures differ partly because the reef is discontinuous and because measurements follow different boundaries. Sources that rank it generally place it third among the world's barrier reefs, and EBSCO notes that it is the second-largest such complex in the western Atlantic. The ranking is therefore best treated as a commonly repeated claim rather than a precisely measured one.\n\nThe reef is not a single wall but a sequence of linked habitats. Across the marine parks, the Bahamas National Trust describes a progression from sandy bottom to seagrass beds, then hard bottom, patch reefs and the barrier reef itself, before the seafloor drops into deep water. Lagoons and isolated cays sit within this system, so the reef functions as a mosaic rather than a uniform structure. Each zone supports different communities of corals, gorgonians, sponges and algae, and the shallow lagoon-side habitats differ markedly from the exposed outer reef.\n\nReefs, seagrass meadows and mangroves depend on one another and provide shared services. Sources on Caribbean coastal habitats describe reefs as energy absorbers that create calm water where sediment settles in adjacent mangroves and seagrass beds, with wave attenuation reported at up to 97 percent in some locations. Seagrass beds and mangroves in turn trap sediment and nutrients, so the loss of mangroves can increase sedimentation and eutrophication in neighbouring reef and seagrass areas. For the Bahamas, this interdependence means that coastal decisions made far from the reef, such as clearing mangroves for building land, can affect reef health. A survey of the southeastern Bahamas also noted that small islands there often lacked extensive seagrass because of limited shelf area and strong physical exposure.\n\nHuman pressures are concentrated near the coast. Survey work in the southeastern islands identified coastal development, pollution, overfishing and climate change as continuing threats, while also finding the reefs there to be generally in good condition. Tourism growth has increased demand for docks, canals and channels, and the associated dredging releases sediment that can smother corals and seagrass. Removing wetlands and mangroves also reduces the nursery areas used by juveniles of commercially important fish before they move to the offshore reef. Chronic nutrient and sediment runoff can drive algal blooms that compete with corals, linking land use on the islands directly to reef condition.\n\nClimate change adds a second layer of risk. Warm-water events can cause mass coral bleaching and mortality, while ocean acidification lowers the calcification rates of many corals. Hypoxia, or low oxygen, is also emerging as a threat as oceans warm. Seagrass beds face their own problems: rising temperatures, marine heatwaves and sediment smothering reduce the light that meadows need. These findings come mainly from regional and global studies, so applying them to specific Bahamian reefs requires local monitoring data. Regional research shows that reefs, seagrass and mangroves respond to these stresses together, so degradation in one habitat can weaken the others.\n\nProtection in the Andros reef system has focused on the healthiest sections. The government designated the North and South Marine Parks in 2002, covering roughly 8,500 acres of the reef system. These parks protect the main reef, patch reefs, lagoons and isolated cays, and they are presented as a way to balance reef tourism with ecological integrity. Their effectiveness depends on enforcement and on the management of land-based pressures outside park boundaries, which lie beyond the reach of marine zoning alone." }, { "heading": "Terrestrial Ecosystems and Biodiversity", "text": "Andros, the largest island, carries the most varied land cover in the country. Its interior combines wetlands, mangroves, pine woodland and inland blue holes. One blue hole on Central Andros, for example, lies within pine forest growing on a limestone substrate, and sediment cores from such sinkholes preserve pollen and charcoal that record how fire shaped the vegetation over time. Blue hole on Central Andros surrounded by pyric Caribbean pine forest on limestone substrate. Sediments from blue holes provide pollen and charcoal evidence of the historical dynamics of fire-dependent pine forest vegetation. Pine woodland is the dominant land class on Andros, covering roughly one-third of the total terrestrial area, and the island holds a major share of the national total: Andros contains 55 percent of the country's pine forests.\n\nPine Forests and Wetlands\n\nCaribbean pine (Pinus caribaea var. bahamensis) is the defining tree of the northern islands. Pineland vegetation is confined to Grand Bahama, Abaco, Andros and New Providence, and across the whole country pine forests comprise 23 percent of the terrestrial ecosystems. The trees tolerate sandy, saline soils, but their shallow yet strong root systems are an adaptation to frequent hurricanes. Fire is a maintaining process rather than a disturbance to be avoided: without naturally occurring fire, succession to a broadleaf forest would occur. Ridges are often covered by coppice, and the pine understory includes shrubs such as poisonwood and the endemic five-finger palm. Wetlands are equally widespread, and almost every island contains some wetland habitat, with the great majority comprised of shallow brackish to saline lagoons, mangrove swamps, coastal flats, and inter-tidal mudflats. Forest patches on Andros are not highly isolated, since most were close to other patches of pine. Remote-sensing work also found that a global forest-loss product overstated clearance there, and that understory fires were often mistaken for deforestation.\n\nEndemism and Notable Species\n\nThe archipelago's biota contains a high proportion of endemic taxa, though the figures differ by group and source. A biodiversity profile lists Reptiles 48 ... Endemic 25 ... % Endemic 52.1%, while its own mammal row gives a much lower endemic share, so the group-level counts should be checked against the original tables. For plants, one secondary source reports that over 1,350 species of flowering plants and ferns have been described in The Bahamas, with around 9% of them being endemic to the region. The most prominent bird is the Bahama oriole (Icterus northropi), which is a Critically Endangered species endemic to The Bahamas and currently found only on the Andros island complex. Earlier research estimated fewer than 300 individuals remaining in the global population. Observers have recorded birds nesting deep in pine forest, not only in coconut palms near settlements, which matters for population estimates and conservation planning.\n\nThreats and Protection\n\nHabitat loss and invasive species are the main pressures on terrestrial biodiversity. One analysis lists habitat destruction, habitat fragmentation, pollution, the introduction of invasive alien species, and over-harvesting as the principal human-related threats. Invasive species are a particular problem inside protected areas: the Bahamas National Trust reports that national parks across The Bahamas are being impacted by invasive animals like wild hogs, feral cats, rats, and raccoons; and by invasive plants, especially the likes of casuarinas, brazilian pepper, scaevola, and melaleuca. Casuarina, for instance, outcompetes native vegetation and creates monocultures. Melaleuca also invades wetlands and dries them out reducing their ability to provide habitat for migrating birds and waterfowl. The national protected area system, which includes National Parks, Natural Monuments, Nature Reserves, Wildlife Sanctuaries, and Marine Reserves, therefore depends on invasive species management as much as on boundary designation. Control is harder on small islands, where a single introduced predator or weed can spread across a whole habitat." }, { "heading": "Population Distribution and Settlement", "text": "Estimates of the Bahamian population for 2025 vary by source. One series based on UN data puts it at 403,033 people at mid year, while the total population of the Bahamas stood at 412,640 people in 2025, a figure attributed to the IMF. The most recent full enumeration, the 2022 census, counted 192,544 males and 206,770 females, for a total of 399,314, up from 351,461 in 2010. Because the census is a count rather than a projection, it provides the firmest basis for analysing where people live.\n\nSettlement is strongly concentrated in two islands. New Providence with 296,522 persons accounted for 74.26% of the population. Grand Bahama is second, but its share has fallen: Grand Bahama's count of 47,475 persons accounted for 11.89% of the population, a decline of 2.73 percentage points, from 14.62% in 2010. Grand Bahama's absolute population also shrank, by 3,893 souls in 2022 from the preceding census in 2010. Taken together, these two islands hold roughly 86 per cent of residents, which leaves the remaining islands with a much smaller share.\n\nNassau, the capital, sits on New Providence and is the country's largest city. It is commonly defined as a primate city, dwarfing all other towns in the country, and it serves as the centre of commerce, education, law, administration, and media of the country. Freeport, on Grand Bahama, is the main urban centre of that island. The overall population is highly urban: in the country's own time series, the urban share had reached about 83 per cent by 2021.\n\nThe Family Islands hold a much smaller but not negligible population. Taken collectively, they showed a change in population from 53,764 in 2010 to 55,317 in 2022, an increase of 2.89 percent. Growth was uneven, and several islands, including Acklins, Andros, the Berry Islands, Bimini, Cat Island, Eleuthera, Exuma, Harbour Island, and Spanish Wells, recorded gains over that period. Abaco, a larger Family Island, had 16,587 in 2022 after losing residents since 2010. Only about thirty islands are inhabited, and on many of the outer islands settlement is small and dispersed, with livelihoods tied to fishing, farming and tourism.\n\nDispersed settlement creates practical difficulties for public services. Schools, clinics, hospitals and utilities must be provided on islands that are often far apart and reachable only by air or sea, so the cost per resident of delivering services is higher on outer islands than in Nassau or Freeport. Staffing remote schools and clinics, and maintaining supply links during storms, are recurring challenges for the government." }, { "heading": "Urban Growth and Land Use", "text": "Most urban expansion in the Bahamas happens on New Providence, where Nassau has grown from a small colonial port into the country's dominant city. Between 1989 and 2020 the city's population rose by about 1.5 percent a year, from roughly 139,000 to 225,000. Its urban extent grew by about 1.9 percent annually over recent decades, and the built-up area is now 1.8 times its 1989 size. Because land was consumed faster than people arrived, the city became much less compact. Its density of 19 inhabitants per hectare ranked 35th in a 70-city regional sample for 2010–2020, down from 7th in 1989–2000. The result is a sprawling urban pattern in a city that remains sparsely populated for its area.\n\nGrand Bahama, centred on Freeport, shows a different pressure. Its property market has drawn buyers from Nassau, and in 2024 a local broker reported that real estate values were around one-third of comparable properties in Nassau, which prompted buyers to act before prices rose. Such claims come from individual market participants rather than systematic statistics, so they indicate direction more than scale. Freeport's industrial base and port facilities give it a role in the economy that also shapes where housing and workplaces are built.\n\nLand-use projections for New Providence highlight the scale of the challenge. A growth study covering the island reported that the urban footprint increased from 36% in 2014 to 70% under the business-as-usual scenario. Its alternative \"intelligent\" scenario aims for a forecasted footprint of 54% by 2045, which would still accommodate about 367,500 residents. Under that scenario an estimated 98,979 new housing units will be required. The study's land-cover analysis relied on satellite imagery, and the gap between the two scenarios indicates how much planning choices affect the loss of wetlands and other natural systems. Resorts, marinas and reclaimed coastal land compete for the same limited shoreline, so decisions about tourism development and residential building are closely linked.\n\nHousing affordability is the most politically visible dimension of this growth. A March 2026 study by the Inter-American Development Bank found that growth in the affordable housing stock fell by 8,571 units between 2010 and 2022, compared with the decade from 2000 to 2010. The Minister of Housing and Land Reform said in 2024 that the country faced a shortage of some 12,000 housing units. The same study found that the median dwelling age in 2022 was more than 35 years, and that over 40 percent of homes predate 1990. It also linked owner-driven construction with limited regulatory oversight to faster deterioration of the existing stock. Many households have responded by sharing homes. Multi-family households are growing in number, which the IDB attributes at least partly to affordability pressures and describes as a coping mechanism.\n\nThese pressures featured prominently in the May 2026 election. Concerns about affordability, poor wage growth, and rising housing costs were top of mind for voters. Both main parties pledged to use private developers and capital to build more homes. The Progressive Liberal Party's platform included affordable housing subdivisions across the Family Islands, a national rental registry with minimum habitability standards, and an expanded rent-to-own programme. The government's budget removed value-added tax on the purchase price for first-time buyers. In early October 2026, the Ministry of Housing and Land Reform began public consultations in Nassau, Abaco and Freeport under its SHOUT programme, which focuses on affordable housing pipelines and land ownership reform.\n\nRapid, uneven building also raises issues of quality, drainage and exposure to climate risk. Some residents expand homes or add rental units without obtaining building permits and/or in violation of zoning regulations, which complicates oversight of informal settlements and substandard housing on low-lying land. Dense paved areas and limited vegetation in Nassau and Freeport can intensify urban heat, while poor drainage increases flooding during heavy rain and storms. These problems connect urban planning to climate adaptation, since the same low elevation that makes land attractive for development also exposes it to rising seas and informal settlement risks." }, { "heading": "Economic Geography: Tourism and Financial Services", "text": "The Bahamian economy rests mainly on two pillars, tourism and financial services. Because the archipelago has few natural resources and a limited industrial base, both sectors earn most of the foreign exchange that pays for imports, which include much of the country's food and fuel. Agriculture and manufacturing are small by comparison. Sources put their combined share of output at roughly 7 to 10 percent. The World Bank classifies the Bahamas as a developed economy, and its per capita GDP is the second highest in the English-speaking Caribbean.\n\nTourism\n\nEstimates of tourism's share of GDP vary widely, and the gap mostly reflects definition. Some official and secondary sources put the direct share near half of output, while others use broader measures. A U.S. State Department investment climate report for 2023 gives 70 percent for \"tourism and related services,\" and the economic data service Economy.com gives a range of 75 to 80 percent. A tourism statistics website citing the World Travel & Tourism Council gives a much lower figure of about 24 percent for direct contribution in 2023. The distinction between direct, indirect and induced effects therefore has to be made explicit before any single number is used. Employment figures are more consistent: tourism directly or indirectly supports about half of the labour force.\n\nThe sector depends heavily on the United States. Over 80 percent of visitors come from the U.S., so tourism revenue tracks American income and travel patterns. Visitor arrivals are split between two forms. Stopover visitors stay in hotels and resorts, while cruise passengers arrive by ship and spend shorter periods ashore. Official figures cited by the Bahamian mission to the United Nations in Geneva record an average of about 1.4 million stopover visitors and 4.6 million cruise visitors a year, with a record 7.2 million arrivals in 2019.\n\nGeographically, cruise traffic concentrates in the ports of Nassau on New Providence and Freeport on Grand Bahama, where most large resorts and the principal airports are also located. Nature-based tourism, diving and marine recreation draw more visitors to the Exuma Cays and other outer islands, although those areas have far less accommodation and infrastructure. The sector is also exposed to shocks. Hurricane Dorian disrupted travel in 2019, and the COVID-19 pandemic led S&P to forecast a 16 percent contraction in GDP for 2020.\n\nFinancial Services\n\nFinancial services form the second-largest sector. The Central Bank of The Bahamas estimates that the sector accounts for roughly 10 to 15 percent of GDP, and it employs a substantial number of skilled workers. Its effects extend to construction, real estate and wholesale and retail trade. The sector is divided into a domestic side, which is more retail and labour-intensive, and an international side, which serves high-net-worth clients and employs more specialised, higher-paid staff. The international side includes Bahamian-incorporated institutions and foreign banks, as well as trust companies, insurers, investment funds and corporate service providers. Sources disagree on the number of licensed institutions. One source cites more than 200 licensed banks and trust companies, while another gives about 400 banks registered in the country.\n\nThe sector is concentrated in Nassau, which is both the capital and the main financial centre. Its position as an offshore financial centre links the economy to international regulation and capital flows. Global regulatory standards have increased compliance costs, and the Central Bank's 2021 survey reported headwinds from these standards and from pressure to consolidate balance sheets and operations. International bodies have also criticised the jurisdiction. The European Union has listed the Bahamas among several Caribbean \"uncooperative jurisdictions,\" and the Financial Action Task Force has pressed the country on compliance. These pressures have affected some international business.\n\nTourism and finance therefore depend on different things. Tourism relies on the natural landscape, the cruise schedule, air and sea access, and American demand, while finance relies on Nassau's legal and professional infrastructure and on international regulatory acceptance. Both are concentrated on a small number of islands, and the outer islands depend mostly on tourism and small-scale fishing. Tourism and financial services therefore shape where wealth, jobs and public investment are concentrated, as well as how exposed the country is to hurricanes and to changes in external demand." }, { "heading": "Transport, Infrastructure and Maritime Boundaries", "text": "Because the islands are separated by open water and lack land links, movement between them depends mainly on aircraft and boats. Air travel is the main form of inter-island movement. Nassau and Freeport host the principal international airports, and many overseas visitors arrive on connecting flights from North American hubs. The islands' biggest airports are Nassau's Lynden Pindling International Airport (LPIA), Grand Bahama International Airport (FPO) and Exuma International Airport (GGT). The national carrier, Bahamasair, runs scheduled services between Nassau and the Family Islands, while smaller Nassau-based operators offer charter flights to the Out Islands. Most Family Island travellers fly through Nassau or take ferries and boats to the more remote destinations. The Nassau airport was expanded in 2011 and now includes a separate terminal for domestic and Out Island flights. The airport underwent major expansion in 2011 and now includes a dedicated U.S. departures terminal, plus a domestic and international terminal for flights to the Out Islands, Canada, the U.K., and the Caribbean.\n\nSea links fill the gaps left by air services. Ferry and water-taxi services are concentrated between New Providence and the Out Islands, and boat travel can be the only way to reach some of the smaller islands. The country does not have a large ferry network. Regular ferries run from the United States to Bimini and Grand Bahama, and these are the busiest routes. Fast passenger and freight services operate from Nassau to several Family Islands, and the largest of these operators has run inter-island services since 1999. Slower mailboats, which depart from Potter's Cay in Nassau, carry cargo and mail to remote communities. Their sailings are cheaper but often late, and even ferries from Florida have to cross the Gulf Stream to reach the islands, and when winds blow in from the north, high-speed sailings are frequently cancelled at the last minute for safety.\n\nPorts handle most of the country's cargo and cruise traffic. The Bahamas has about 10 ports, most of them being cruise ports, but it also has two important container ports of the Caribbean. The Freeport Container Port on Grand Bahama opened in 1997 and is owned by Hutchison Port Holdings. It has three berths and a draft depth of 16.1 metres. Beyond containers, it handles non-containerised heavy cargo, cold storage and ship repair, and it serves as a transhipment point linked to markets on the U.S. East Coast, Central and South America and the Caribbean. After Hurricane Dorian, operations there were limited by a lack of electricity and personnel, which illustrates how dependent port functions are on reliable power. Cruise infrastructure is concentrated in Nassau and Freeport. The Lucayan Harbour Cruise Facility in Freeport and Nassau harbour's Prince George Wharf are built specifically to handle multiple modern cruise ships at one time.\n\nMaritime boundaries are shaped by the country's status as an archipelagic state under the United Nations Convention on the Law of the Sea (UNCLOS). The convention allows such a state to draw straight baselines that join the outermost points of its islands and dry reefs, and these lines serve as the reference for measuring its territorial sea and exclusive economic zone. The Bahamas has a water-to-land ratio greater than 9 to 1, and is therefore unable to enclose the entire archipelago within a single series of straight baselines. Domestic legislation implements these rules. The country's Act No. 37 of 1993 governs the territorial sea, archipelagic waters, internal waters and the exclusive economic zone. The baseline coordinates were set out in a 2008 order, and those baselines constitute the outer limits of the archipelagic waters and the inner limits of the territorial sea. The Bahamas then deposited the coordinate list with the United Nations in December 2008.\n\nBoundary arrangements with neighbours follow the same technical logic. A maritime boundary agreement with Cuba was signed in October 2011, and the geodetic median line was calculated between The Bahamas' archipelagic baseline and the Territorial Sea baseline model of Cuba. The agreement entered into force in March 2012. Infrastructure such as power generation, water supply and telecommunications must serve a dispersed population and an exposed coastline, which is why the reliance on ports, airports and small boats remains central to how the country connects its islands." }, { "heading": "Natural Hazards and Climate Vulnerability", "text": "The archipelago's main natural hazards come from its low relief and its exposure to Atlantic storms. Hurricane Dorian, which struck in September 2019, shows how these hazards combine. As the Category 5 hurricane crossed the islands, its forward speed slowed and it stayed nearly stationary over Grand Bahama for roughly 36 hours. In parts of the affected islands, the eyewall brought wind gusts of up to 220 miles per hour and a storm surge of more than 6 metres. Flooding from the surge and from heavy rain (about a metre of rain fell over most of the northern Bahamas) compounded the wind damage.\n\nThe damage was shaped as much by construction and siting as by the storm's intensity. The Inter-American Development Bank estimated the total cost at about $3.4 billion, equal to one-quarter of The Bahamas' GDP. The same assessment found that inadequate construction and infrastructure located in vulnerable areas exacerbated the storm's impacts. The Red Cross estimated that more than 13,000 houses, about 45 percent of the homes on Grand Bahama and Abaco, were believed to have been severely damaged or destroyed. The building code had been revised over time, with a 2003 edition that increased design wind speeds and made hurricane shutters mandatory, yet Dorian's winds and surge exceeded the design requirements of the Bahamian Building Code. Commentators have also noted that code provisions rarely extend to withstand both the strong winds and the extended duration of a storm like Dorian, so the stall itself was a design problem as well as a meteorological one.\n\nSea-level rise adds a slower but cumulative pressure. Because the land is so low, projected rises of 1, 2 and 3 metres could eliminate about 6%, 12% and 22% of the national territory, respectively, according to one study. Projections for the end of the century, as summarised by a Berkeley case study, anticipate a sea-level rise of 56.17 cm, which is well above the global average of 40.73 cm. The most acute threat to water supply is saltwater intrusion. The archipelago's fragile freshwater lenses and limited, sandy soils are vulnerable to salinisation, and on Grand Bahama, where approximately 20 % of the land surface is lower than 1 m above sea level, the island's groundwater is the only source of potable water. Dorian's storm surge inundated more than half of the island and caused seawater intrusion into the freshwater lenses. Degradation of coral reefs, which normally absorb wave energy before it reaches shore, further reduces natural protection, and it also affects fisheries and the tourism sector that depends on the coast.\n\nAdaptation efforts combine engineering, planning and institutional change, though their effectiveness is debated. Seawalls are a common response to shoreline retreat on small islands, but research on island coasts has found that seawalls have failed to resolve coastal erosion in rural islands and can create unanticipated problems, including aggravated erosion. The same research identifies soft-engineering and nature-based solutions as alternatives, and relocation to safer areas as a longer-term option. For water security, proposed measures include halophyte restoration, organic soil amendments, aquifer recharge, and soil flushing, along with identifying wellfields in elevated areas on the island to reduce saltwater intrusion from over-wash. Policy work has focused on the building code: a government minister has said that the building code must be revisited and homes designed to sustain the impact of stronger storms. Financing for these measures has come partly through the Inter-American Development Bank's Climate-Resilient Coastal Management and Infrastructure Program, which included a contract for upgrading the building code with coastal infrastructure design guidance. Early warning also matters: before Dorian, evacuation orders for low-lying areas were issued the day before the storm, but many people ignored the warnings." }, { "heading": "Conservation and Resource Management", "text": "Conservation in the Bahamas is organised largely around the Bahamas National Trust (BNT), a statutory body that advises the government on conservation matters and manages national parks. The Trust was created by legislation in 1959, and its governing council includes government, private-sector and scientific representatives. The BNT now oversees a national parks system of 25 protected areas covering more than 700,000 acres on land and at sea.\n\nThe system's founding case is the Exuma Cays Land and Sea Park. The park was established in 1958, and it is usually described as the first land and sea park in the world. It covers about 176 square miles (roughly 460 km²) of cays, reefs, seagrass beds, mangroves and blue holes. Its waters have been a no-take zone since the mid-1980s, when the BNT designated the park as a protected replenishment zone. Sources give slightly different dates for this change, with some citing 1985 and others 1986. The protected waters have allowed commercially important species such as queen conch, Nassau grouper and spiny lobster to maintain breeding populations, and there is evidence that adult fish are restocking areas outside the park boundaries. Sources differ on the \"first\" claim: some call it the first marine protected area in the world, while others describe it as the first in the Caribbean. The park is widely cited as a model for integrated land-and-sea management elsewhere.\n\nProtection has since expanded beyond the Exumas. The West Side National Park on Andros, established in 2002 and enlarged in 2012, covers the western half of the island and its surrounding waters. Marine work has also continued through partnerships. The Nature Conservancy has worked with the BNT and the government to develop ecosystem-wide zoning plans for five marine protected areas, and the Bahamas made a regional commitment under the Caribbean Challenge to protect 20 percent of its marine and coastal habitat. The BNT's protected-area network is therefore closely linked to the country's marine ecology, which in turn supports the national economy.\n\nNatural landscapes also underpin the tourism sector. Boat tours, snorkelling, diving and wildlife watching in the Exumas and on Andros depend on intact reefs, clear water and visible wildlife such as turtles and iguanas. Visitors thus have a direct economic stake in conservation, and tourism revenue can strengthen support for park management. At the same time, the presence of many visitors can add pressure on fragile shorelines, which makes managing visitor activity part of the conservation agenda.\n\nResource extraction is another area where protection and use must be reconciled. On Great Inagua, the Morton Salt Company acquired an existing salt operation in 1954, and it has since run a large solar evaporation facility that uses wind and sun to concentrate seawater into brine and then into salt. Sources differ on the scale of production, with some reporting about one million pounds per year and others about one million tons. The evaporation ponds also support a food chain of algae and brine shrimp that sustains the West Indian flamingo. Inagua National Park, established in 1965, protects what is described as the largest breeding colony of these birds in the world. Flamingos had been heavily hunted on the island about a century ago, and the BNT later took over responsibility for their protection. The salt works and the national park therefore share the same landscape, and their coexistence reflects a practical balance between industry and habitat.\n\nFisheries, salt production and tourism all draw on the same shallow banks and reefs. Land-use decisions on Andros, the Exumas and other islands therefore involve trade-offs between development pressure and the protection of habitats that underpin fishing and tourism. Managing these trade-offs requires coordination among the BNT, government agencies and private operators, and the outcome depends heavily on enforcement, scientific monitoring and the zoning of protected waters." }, { "heading": "Geographic Exploration and Knowledge", "text": "Written European knowledge of the archipelago begins with Christopher Columbus's 1492 voyage. Sailing from Spain with three ships, he sought a direct route to Asia, and on 12 October his fleet reached land in the Bahamas. The Lucayan name for the island was Guanahani; the Spanish called it San Salvador. The island was renamed officially in the mid-1920s, with sources giving either 1925 or 1926, when it was previously known as Watling Island.\n\nThe identity of that first landfall remains open. Several Bahamian islands have been proposed as Guanahani, including Sanama Cay, Rum Cay, Grand Turk Island and the Plana Cays, but the most popular theory points to San Salvador. Historians have also weighed the Turks and Caicos as an alternative. In 1942 the naval historian Samuel Eliot Morison identified Watling Island as the landfall, and that view shaped later scholarship. Some researchers have since reexamined the question with archaeology and reconstructed sailing routes, and a 1987 field team tested alternative candidates on Long Island, which it considered the third island Columbus visited. Because the surviving journal does not give modern coordinates, the debate has not been resolved.\n\nThe people who met Columbus were Lucayans, a branch of the Taíno. Arawakan-speaking Taíno people reached the islands from other parts of the Caribbean, with estimates for arrival ranging from about 500 to 800 AD. They spread through the archipelago over roughly 800 years, from an initial settlement on Great Inagua, and population density was highest in the south-central islands and declined toward the north, reflecting the shorter period of occupation in the northern islands. Their settlements focused on coasts and resources. Archaeological sites on Eleuthera, San Salvador, New Providence and other islands show adaptation to beaches, mangroves, reefs, tidal flats and caves. The Lucayans used dugout canoes to move between islands and to sustain trade networks. A 2020 study of skulls found that Lucayan remains are related to groups from Hispaniola and Jamaica rather than to Cuban inhabitants.\n\nSpanish contact quickly reshaped this geography of knowledge. Columbus took several Lucayans as slaves, and later colonizers continued the practice. Historical accounts record a 1509 authorization to obtain workers from the Bahamas, and Lucayans were then transported to Hispaniola and other Spanish-controlled areas. Their swimming and diving skills made them especially valuable to slave traders, and some were sent to pearl-diving work around Cubagua. The loss of population also erased much of the local knowledge that European navigators might otherwise have recorded.\n\nLater charting of the banks, channels and island groups was carried out by British colonial administrators and then by scientific surveyors, and the resulting maps gradually replaced the fragmentary sketches of early voyages. Modern research has added a different kind of archive. The Bahamian blue hole, the Florida sinkhole and the Mexican cenote are all descriptions of identical karst features that arise from the same physical process, and their floors record past environments. The seafloor at the base of a blue hole works like a calendar of storms, because sediment builds up over time in much the way that an ice core or tree ring accumulates. Ordinary currents carry fine sand grains into the hole, while violent hurricanes deliver coarser grains. Cores from Hine's Hole, a site near the Cay Sal Bank, were drilled 18 metres into the sediment, recovering a record of the past 540 years of deposition. Comparison with the modern storm record led researchers to conclude that the hole captured every Category 2 or stronger hurricane within 75 kilometres, and over the last 170 years there have been about five hurricanes per century on average. Cores from South Andros reach further back: one 59-foot-long continuous core records encounters with tropical cyclones going back 1,500 years. Fragments of mangrove trees within the storm layers were radiocarbon dated to date each event. Work on Abaco has also reconstructed environmental change: during the Holocene, rising coastal aquifer levels and relative sea-level rise controlled the depositional environments inside one blue hole. Such studies require multiple cores, since lateral facies changes cannot be characterised from a single core." }, { "heading": "Administrative and Political Geography", "text": "The Bahamas is a parliamentary democracy modelled on the Westminster system, in which the prime minister is the leader of the party controlling the majority of the House of Assembly seats. The Crown is represented by Monarch Charles III, with Cynthia A. Pratt serving as Governor-General. The lower house, the House of Assembly, has 41 members, each elected from one constituency for a five-year term elected from individual constituencies for five-year terms. Because a party needs 21 seats needed for a majority, the allocation of seats across islands directly shapes which party can form a government.\n\nEach constituency returns one member through a first-past-the-post vote using the first-past-the-post voting system. The current map was set by the House of Assembly Revision of Boundaries and Re-distribution of Seats Order, 2026, which came into force on 16 January 2026 but could not affect an election until the Governor-General proclaimed a date Provided that in accordance with the proviso of Article 70(7) of the Constitution, this Order shall not affect any election to the House of Assembly. The order allocates the 41 seats unevenly across the islands: 25 to New Providence, five to Grand Bahama and 11 to the other Family Islands. The boundaries commission's report reached Parliament on 8 January 2026 and confirmed the two new seats. St James draws on voters who had lived in Killarney, Golden Isles, Tall Pines and Southern Shores, while the Berry Islands were detached from the North Andros and Berry Islands seat so that they could join Bimini. The commission justified the changes by pointing to electorate size, noting that Killarney had more than 7,000 registered voters and West Grand Bahama and Bimini had 6,070. Representation therefore follows the number of voters rather than land area. The Bimini and Berry Islands seat had an electorate of 2,253 (2025), while St James had 5,149 (2025).\n\nThe 2026 general election was held on 12 May 2026 under these boundaries. Parliament had been dissolved on 8 April, before the regular end of the term, and the election was held on 12 May 2026 to elect all 41 members. The governing Progressive Liberal Party won 33 seats, while the opposition Free National Movement took eight returned to government with 33 of the 41 seats. Opposition leader Michael Pintard accepted defeat about four hours after polling stations closed conceded the election four hours after the polls closed. Philip Davis took the oath as prime minister at Government House on 14 May 2026 Davis was sworn in as prime minister at Government House on 14 May 2026. The PLP's success marks the first back-to-back general-election win by a Bahamian party since 1997 the first back-to-back general-election victory by a Bahamian party since 1997.\n\nSmall constituencies can produce narrow margins and decisive local results. In the new St James seat, Owen Wells took 1,620 or 46.4 percent of the votes in a multi-candidate contest. In the Bimini and Berry Islands seat, Randy Rolle won with 51.9 percent or 946 of the 1,821 votes.\n\nAdministrative geography is layered on top of the island structure. Constituencies are grouped into island-based districts, and each district corresponds to one or more islands. Fort Charlotte, for instance, is classed as part of the New Providence district and elects one Member of Parliament using the first-past-the-post voting system, having been created in 1967. The Senate, the upper chamber, has Members: 16 and complements the elected lower house in the legislative process." } ], "links": [ "caribbean", "sea-level-rise", "karst", "climate", "el-nino-southern-oscillation", "climate-change", "invasive-species", "urbanization", "city", "wetland", "adaptation", "financial-market", "government" ], "sources": [ { "title": "Geography of the Bahamas", "url": "https://en.wikipedia.org/wiki/Geography_of_the_Bahamas" }, { "title": "The Bahamas", "url": "https://en.wikipedia.org/wiki/The_Bahamas" }, { "title": "LIS No. 128 - The Bahamas", "url": "https://www.state.gov/wp-content/uploads/2019/12/LIS-128.pdf" }, { "title": "Bahamas EEZ (0-200NM)", "url": "https://map.navigatormap.org/site-detail?site_id=6031" }, { "title": "Geography of Bahamas - Confidus Solutions", "url": "https://www.confiduss.com/en/jurisdictions/bahamas/geography/" }, { "title": "Bahamas Country Information", "url": "https://www.aardy.com/blog/bahamas-country-information/" }, { "title": "Geography of the Bahamas: Unique Islands and Landscapes", "url": "https://www.jarniascyril.com/expatriation/guide-to-settling-in-the-bahamas-for-expats/geography-country-bahamas/" }, { "title": "Bahamas - Etymology, Origin & Meaning of the Name", "url": "https://www.etymonline.com/word/Bahamas" }, { "title": "Overview Of The Bahamas", "url": "https://www.bahamas.gov.bs/overview-of-the-bahamas" }, { "title": "Map of the Bahamas - Islands and Cays - GIS Geography", "url": "https://gisgeography.com/bahamas-map/" }, { "title": "Andros Island Information", "url": "https://bamsi-handbook.cleancatalog.net/andros-island-information" }, { "title": "Andros, The Bahamas", "url": "https://en.wikipedia.org/wiki/Andros,_The_Bahamas" }, { "title": "Andros Island is divided into three large, inhabited cays (North...", "url": "https://www.researchgate.net/figure/Andros-Island-is-divided-into-three-large-inhabited-cays-North-Andros-Mangrove-Cay_fig1_317802306" }, { "title": "Bahamas at a glance", "url": "https://www.fao.org/jamaica-bahamas-and-belize/fao-in-jamaica-bahamas-and-belize/bahamas-at-a-glance/en/" }, { "title": "About The Bahamas", "url": "https://www.thebahamaschamber.com/visit-the-bahamas" }, { "title": "The Abaco Islands, of the Family Islands of the Bahama Islands -", "url": "https://hsjchronicle.com/the-abaco-islands/" }, { "title": "9 great options for a Bahama family vacation", "url": "https://www.vrbo.com/vacation-ideas/families/family-destination-guides/caribbean/bahamas-family-vacation" }, { "title": "How Many Islands Are In The Bahamas?", "url": "https://www.worldatlas.com/islands/how-many-islands-are-in-the-bahamas.html" }, { "title": "Lucayan Archipelago", "url": "https://en.wikipedia.org/wiki/Lucayan_Archipelago" }, { "title": "Family Islands Division", "url": "https://www.moss.gov.bs/family-islands-division" }, { "title": "Bahamas", "url": "https://www.mindat.org/loc-159602.html" }, { "title": "THE BAHAMA BANKS: A \"LIVING\" FOSSIL-ENVIRONMENT LOUIS S. KORNICKER", "url": "https://repository.si.edu/bitstream/handle/10088/8544/iz-Kornicker-1963c.pdf?sequence=1" }, { "title": "Geological Studies on the Great Bahama Bank", "url": "https://pubs.geoscienceworld.org/sepm/books/book/1120/chapter/10552644/Geological-Studies-on-the-Great-Bahama-Bank" }, { "title": "Bahamas - SEPM Strata", "url": "http://www.sepmstrata.org/page.aspx?pageid=51" }, { "title": "Geology of the Bahamas: Subsurface Geology of the Bahamas Banks - ScienceDirect", "url": "https://www.sciencedirect.com/science/chapter/bookseries/abs/pii/S0070457104800256" }, { "title": "The Geology of the Bahama Islands - Donald Scarinci", "url": "https://donaldscarinci.com/geology-bahama-islands/" }, { "title": "plate c-16 great bahama bank", "url": "http://geoinfo.amu.edu.pl/wpk/geos/geo_6/geo_plate_c-16.html" }, { "title": "Bahama Banks — Grokipedia", "url": "https://grokipedia.com/page/Bahama_Banks" }, { "title": "Shallow Carbonate-Bank-Margin Growth and Structure, Little Bahama Bank, Bahamas1", "url": "https://pubs.geoscienceworld.org/aapg/aapgbull/article-abstract/61/3/376/104346/Shallow-Carbonate-Bank-Margin-Growth-and-Structure" }, { "title": "Geology of the Bahamas Final Paper", "url": "http://jrscience.wcp.muohio.edu/fieldcourses06/PapersMarineEcologyArticles/GeologyoftheBahamasFinalP.html" }, { "title": "Cat Island, Bahamas", "url": "https://en.wikipedia.org/wiki/Cat_Island,_Bahamas" }, { "title": "Tongue of the Ocean", "url": "https://en.wikipedia.org/wiki/Tongue_of_the_Ocean" }, { "title": "Diving the Tongue of the Ocean in Andros: World-Class Vertical Wall Diving", "url": "https://discoverbahamas.com/directory/diving-the-tongue-of-the-ocean-in-andros-world-class-vertical-wall-diving-article-1004.aspx" }, { "title": "Trips Places Foods Stories Newsletters", "url": "https://www.atlasobscura.com:443/places/deans-blue-hole" }, { "title": "OTHER NAMES Sink holes, Ocean holes, Boiling holes FORMATION AND DESCRIPTION", "url": "https://bnt.bs/storage/2019/06/blueholes.pdf" }, { "title": "Dean%27s Blue Hole", "url": "https://en.wikipedia.org/wiki/Dean%27s_Blue_Hole" }, { "title": "The Blue Holes of the Bahamas: Andros, Dean's Blue Hole, and the Lusca Legend", "url": "https://thingstodoinbahama.com/island-life/blue-holes-bahamas-andros-deans-guide" }, { "title": "Mount Alvernia", "url": "https://en.wikipedia.org/wiki/Mount_Alvernia" }, { "title": "Conditions - Stuart Coves - Bahamas Dive Shop & Tours", "url": "https://stuartcove.com/underwater-hollywood/conditions/" }, { "title": "Richard Cant PhD Hydrogeologist The Water Resources of The Bahamas", "url": "https://wsc.com.bs/wp-content/uploads/2020/01/The-Water-Resources-of-The-Bahamas-1.pdf" }, { "title": "Country profile", "url": "https://openknowledge.fao.org/server/api/core/bitstreams/6566540e-2b59-41c7-8135-8c6c7c07f9f4/content" }, { "title": "Hydrologist Urges Meaningful Action to Preserve Natural Freshwater Resources - University of The Bahamas", "url": "https://www.ub.edu.bs/hydrologist-urges-meaningful-action-preserve-natural-freshwater-resources/" }, { "title": "(PDF) Interventions and solutions for water supply on small islands: The case of New Providence, The Bahamas", "url": "https://www.researchgate.net/publication/364061037_Interventions_and_solutions_for_water_supply_on_small_islands_The_case_of_New_Providence_The_Bahamas" }, { "title": "Sun, Sand & (No) Water", "url": "https://www.wwdmag.com/wastewater-treatment/article/10926230/sun-sand-no-water" }, { "title": "(PDF) Water Resources - Challenges for Groundwater Management & Climate Change in the Caribbean", "url": "https://www.researchgate.net/publication/345507790_Water_Resources_-_Challenges_for_Groundwater_Management_Climate_Change_in_the_Caribbean_Commonwealth_of_The_Bahamas_Havana_Cuba_2018" }, { "title": "Climate change resilience of freshwater supply on small islands: Research gaps and strategies for a case study in Grand Bahama - ScienceDirect", "url": "https://www.sciencedirect.com/science/article/pii/S2214581825002551" }, { "title": "The Bahamas Climate Zone, Weather By Month and Historical Data", "url": "https://weatherandclimate.com/the-bahamas" }, { "title": "Blue Green Atlas - The Climate of the Bahamas", "url": "https://bluegreenatlas.com/climate/bahamas_climate.html" }, { "title": "The Bahamas - Tropical, Islands, Caribbean", "url": "https://www.britannica.com/place/The-Bahamas/Climate" }, { "title": "Grand Bahama", "url": "https://en.wikipedia.org/wiki/Grand_Bahama" }, { "title": "UNDP Climate Change Country Profiles The Bahamas", "url": "https://research.fit.edu/media/site-specific/researchfitedu/coast-climate-adaptation-library/latin-america-and-caribbean/bahamas-bermuda-turks-amp-caicos/McSweeney-et-al.--Bahamas-UNDP-CC-Profile..pdf" }, { "title": "The Bahamas Climate: Weather The Bahamas & Temperature By Month", "url": "https://en.climate-data.org/north-america/the-bahamas-15/" }, { "title": "North & South Marine Parks - Bahamas National Trust", "url": "https://bnt.bs/explore/andros/northsouthmarinepark/" }, { "title": "Andros Barrier Reef", "url": "https://www.ebsco.com/research-starters/zoology/andros-barrier-reef" }, { "title": "Southeastern Bahamas Coral Reef & Island Survey", "url": "https://www.agrra.org/wp-content/uploads/2019/01/SE-Bahamas-Coral-Reef-and-Island-Survey-Final-REA-Report-9-24-13.pdf" }, { "title": "(PDF) The functional value of Caribbean coral reef, seagrass and mangrove habitats to ecosystem processes", "url": "https://www.academia.edu/4421121/The_functional_value_of_Caribbean_coral_reef_seagrass_and_mangrove_habitats_to_ecosystem_processes" }, { "title": "For a World Without Boundaries: Connectivity Between Marine Tropical Ecosystems in Times of Change", "url": "https://link.springer.com/chapter/10.1007/978-3-319-93284-2_9" }, { "title": "Sentinels for future coral reef conditions: assessment of environmental variability and water quality in semi-enclosed inland bays in the southern Caribbean", "url": "https://www.biorxiv.org/content/10.1101/2023.10.04.560694.full.pdf" }, { "title": "Fire Management Assessment of the Caribbean Pine (Pinus caribea)", "url": "https://research.fs.usda.gov/treesearch/download/21640.pdf" }, { "title": "Comparing global and local maps of the Caribbean pine forests of Andros, home of the critically endangered Bahama Oriole - PubMed", "url": "https://pubmed.ncbi.nlm.nih.gov/34791534/" }, { "title": "Bahamian Pineyards", "url": "https://www.oneearth.org/ecoregions/bahamian-pineyards/" }, { "title": "Bahamas Biodiversity and Nature Conservation", "url": "https://biodb.com/region/bahamas/" }, { "title": "Bahamas Biodiversity: Animal and Plant Species and What Is Under Threat", "url": "https://constructive-voices.com/bahamas-biodiversity/" }, { "title": "New documentation of pine forest nesting by the Critically Endangered Bahama Oriole (Icterus northropi)", "url": "https://jco.birdscaribbean.org/index.php/jco/article/view/472" }, { "title": "Cultivating Critical Collaboration for Invasive Alien Species Management", "url": "https://bnt.bs/news/cultivating-critical-collaboration-for-invasive-alien-species-management/" }, { "title": "Bahamas Invasive Species Field Guide", "url": "https://caribbeaninvasives.org/wp-content/uploads/2014/05/Bahamas-IS-Field-Guide-print-version.pdf" }, { "title": "Ecosystems of The Bahamas PINE FOREST SCIENTIFIC NAMES", "url": "https://bnt.bs/storage/2019/06/pineforest.pdf" }, { "title": "Pine Forests", "url": "https://www.friendsoftheenvironment.org/pine-forests" }, { "title": "Bahamas Population (2026) - Worldometer", "url": "https://srv1.worldometers.info/world-population/bahamas-population/" }, { "title": "Total population Bahamas| Statista", "url": "https://www.statista.com/statistics/578553/total-population-of-the-bahamas/" }, { "title": "Population up", "url": "https://www.thenassauguardian.com/home/population-up/article_6fb60271-32d3-5bfc-a936-5d40d9c7ce65.html" }, { "title": "2022 Census of Population and Housing", "url": "https://cdn.bahamas.gov.bs/tenant/tenantbnsi/documents/All%20Documents/2022CENSUSPRELIMINARYRESULTSFINALApril122023-20240606015028.pdf" }, { "title": "The Bahamas, by the numbers, pt. 2", "url": "https://www.thenassauguardian.com/opinion/columnists/the-bahamas-by-the-numbers-pt-2/article_372f9c76-630a-11ef-9a5f-5f85420e29eb.html" }, { "title": "Nassau, Bahamas", "url": "https://en.wikipedia.org/wiki/Nassau,_Bahamas" }, { "title": "Bahamas demographics 2025 - StatisticsTimes.com", "url": "https://statisticstimes.com/demographics/country/bahamas-demographics.php" }, { "title": "Unpacking Housing Affordability in The Bahamas Robin Rajack Jose Luis Saboin", "url": "https://publications.iadb.org/publications/english/document/Unpacking-Housing-Affordability-in-The-Bahamas.pdf" }, { "title": "Freeport real estate sees 25% surge before market ‘explodes’", "url": "https://www.tribune242.com/news/2024/apr/03/freeport-real-estate-sees-25-surge-market-explodes/" }, { "title": "(PDF) The New Providence (The Bahamas) Nassau Urban Growth Study", "url": "https://www.academia.edu/100913647/The_New_Providence_The_Bahamas_Nassau_Urban_Growth_Study?uc-sb-sw=1946327" }, { "title": "Housing grows ‘1.5 times slower’ over vacancy and disrepair woes", "url": "https://www.tribune242.com/news/2026/jun/01/housing-grows-15-times-slower-over-vacancy-and-disrepair-woes/" }, { "title": "Voters head to the polls in the Bahamas for high-stakes snap election", "url": "https://www.aljazeera.com/news/2026/5/12/voters-head-to-the-polls-in-the-bahamas-for-high-stakes-snap-election" }, { "title": "Budget hailed for targeting ‘Bahamian housing’s DNA’", "url": "https://www.tribune242.com/news/2026/jun/02/budget-hailed-for-targeting-bahamian-housings-dna/" }, { "title": "Party Platforms", "url": "https://www.bahamas2026.com/platforms" }, { "title": "Public consultations and stakeholder sessions regarding national land legislation and housing opportunities are taking place in Nassau, Abaco, and Freeport - ZNS BAHAMAS", "url": "https://znsbahamas.com/public-consultations-and-stakeholder-sessions-regarding-national-land-legislation-and-housing-opportunities-are-taking-place-in-nassau-abaco-and-freeport/" }, { "title": "Economy of the Bahamas", "url": "https://en.wikipedia.org/wiki/Economy_of_the_Bahamas" }, { "title": "Bahamas", "url": "https://www.economy.com/bahamas/indicators" }, { "title": "The Bahamas - United States Department of State", "url": "https://www.state.gov/reports/2023-investment-climate-statements/the-bahamas" }, { "title": "Bahamas, The - United States Department of State", "url": "https://www.state.gov/reports/2020-investment-climate-statements/bahamas" }, { "title": "The Bahamas - Economy", "url": "https://www.globalsecurity.org/military/world/caribbean/bs-economy.htm" }, { "title": "How Many Tourists Visit the Bahamas Each Year? [Bahamas Tourism Statistics] - hotelagio.com", "url": "https://hotelagio.com/bahamas-tourism-statistics/" }, { "title": "The Bahamian Economy - Permanent Mission of The Bahamas to the United Nations in Geneva", "url": "https://www.bahamasmission.ch/the-bahamian-economy/" }, { "title": "Financial services account for 15 percent of GDP says Bahamas Central Bank", "url": "https://www.caribbeannationalweekly.com/posts/financial-services-account-for-15-percent-of-gdp-says-bahamas-central-bank" }, { "title": "Gross Economic Contribution of the Financial Sector in The Bahamas (2021)", "url": "https://www.centralbankbahamas.com/viewPDF/documents/2022-06-16-11-19-22-Gross-Economic-Contribution-of-The-Financial-Sector-in-The-Bahamas-2021.pdf" }, { "title": "Banking - The Bahamas Guide", "url": "https://thebahamasguide.com/business-investment/banking/" }, { "title": "Listen to this article:", "url": "https://rethinkq.adp.com/money-matters-bahamas" }, { "title": "Bahamas Transportation", "url": "https://travel.usnews.com/Bahamas/Getting_Around/" }, { "title": "Transportation in the Bahamas", "url": "https://www.coldwellbankerbahamas.com/page-bahamas-real-estate---bahamas-luxury-homes,-islands-and-rentals---transportation-in-the-bahamas-54.html" }, { "title": "Getting Here & Getting Around", "url": "https://www.outislandlifebahamas.com/getting-here-getting-around" }, { "title": "Transport in the Bahamas", "url": "https://en.wikipedia.org/wiki/Transport_in_the_Bahamas" }, { "title": "Bahamas Ferry Map and Routes", "url": "https://ferrygogo.com/bahamas/" }, { "title": "6 Major Ports in the Bahamas", "url": "https://www.marineinsight.com/know-more/major-ports-in-the-bahamas/" }, { "title": "Freeport Container Port", "url": "https://en.wikipedia.org/wiki/Freeport_Container_Port" }, { "title": "Freeport Harbor in Bahamas open for limited operations - FreightWaves", "url": "https://www.freightwaves.com/news/freeport-harbor-in-bahamas-open-for-limited-operations" }, { "title": "Archipelagic Waters - Oxford Public International Law", "url": "https://opil.ouplaw.com/display/10.1093/law:epil/9780199231690/law-9780199231690-e1140?d=%2F10.1093%2Flaw%3Aepil%2F9780199231690%2Flaw-9780199231690-e1140&p=emailAiZrX6nem1ihE&print=" }, { "title": "BAHAMAS", "url": "https://www.un.org/depts/los/LEGISLATIONANDTREATIES/STATEFILES/BHS.htm" }, { "title": "Archipelagic Waters and Maritime Jurisdiction (Archipelagic Baselines) Order (Cap. 282).", "url": "https://www.fao.org/faolex/results/details/en/c/LEX-FAOC112161/" }, { "title": "Bahamas and Cuba define boundary with LOTS", "url": "https://www.teledynecaris.com/en/news/newsroom/227/" }, { "title": "Delimitation of The Maritime Boundary Between the ...", "url": "https://www.un.org/depts/los/nippon/unnff_programme_home/fellows_pages/fellows_papers/turnquest_0506_bahamas.pdf" }, { "title": "Archipelagic States and the Law of the Sea", "url": "https://medium.com/@arabaman69/archipelagic-states-and-the-law-of-the-sea-474d3b171107" }, { "title": "Bahamas Airports Guide 2026: Nassau, Grand Bahama & Out Island Transfers", "url": "https://www.secretflying.com/guides/bahamas/airports/" }, { "title": "Bahamas Ferries Ltd.", "url": "https://bahamasferries.com/" }, { "title": "Northern Bahamas devastated by major Hurricane Dorian", "url": "https://www.preventionweb.net/news/northern-bahamas-devastated-major-hurricane-dorian" }, { "title": "Hurricane Dorian: September 2019", "url": "https://courses.ems.psu.edu/earth107/book/export/html/1606" }, { "title": "The facts: Hurricane Dorian’s devastating effect on The Bahamas - Bahamas", "url": "https://reliefweb.int/report/bahamas/facts-hurricane-dorian-s-devastating-effect-bahamas" }, { "title": "IDB", "url": "https://www.iadb.org/en/news/damages-and-other-impacts-bahamas-hurricane-dorian-estimated-34-billion-report" }, { "title": "hurricane dorian bahamas destruction revealed", "url": "https://www.foxnews.com/world/hurricane-dorian-bahamas-destruction-revealed" }, { "title": "Op-Ed: Hurricane Dorian", "url": "https://ewnews.com/op-ed-hurricane-dorian-a-reset-part-3/" }, { "title": "The Bahamas at risk: Material stocks, sea‐level rise, and the implications for development - Martin del Campo - 2023 - Journal of Industrial Ecology - Wiley Online Library", "url": "https://onlinelibrary.wiley.com/doi/full/10.1111/jiec.13402" }, { "title": "Bahamas Case Study", "url": "https://belonging.berkeley.edu/climatedisplacement/case-studies/bahamas" }, { "title": "Building climate resilience in The Bahamas: A framework for enhancing soil and water resource management amidst saltwater intrusion", "url": "https://cob.journals.publicknowledgeproject.org/index.php/files/article/view/603" }, { "title": "Seawalls as maladaptations along island coasts - ScienceDirect", "url": "https://www.sciencedirect.com/science/article/abs/pii/S0964569121000399" }, { "title": "Environment minister: Building codes must be revisited", "url": "https://ewnews.com/environment-minister-building-codes-must-be-revisited" }, { "title": "Notice of Award - The Bahamas Building Code Upgrade incorporating Coastal Infrastructure Design", "url": "https://bahamas.gov.bs/notices/notice-of-award-the-bahamas-building-code-upgrade-incorporating-coastal-infrastructure-design-guidance" }, { "title": "Hurricane Dorian: What You Need To Know", "url": "https://www.projecthope.org/news-stories/responses/hurricane-dorian-what-you-need-to-know/" }, { "title": "Hurricane Dorian Relief", "url": "https://www.directrelief.org/emergency/hurricane-dorian/" }, { "title": "Exuma Cays Land & Sea Park - Bahamas National Trust", "url": "https://bnt.bs/explore/exuma/exuma-cays-land-sea-park/" }, { "title": "Exuma Cays Land and Sea Park in The Bahamas", "url": "https://www.nature.org/en-us/get-involved/how-to-help/places-we-protect/bahamas-exuma-cays-land-and-sea/" }, { "title": "Exuma Turtle Project, The Bahamas - Sea Turtle Conservancy", "url": "https://conserveturtles.org/project/exumas-turtle-project/" }, { "title": "Bahamas National Trust", "url": "https://en.wikipedia.org/wiki/Bahamas_National_Trust" }, { "title": "Review of Exuma Cays Land & Sea Park", "url": "https://www.afar.com/places/exuma-cays-land-and-sea-park" }, { "title": "Exuma Cays Land and Sea Park", "url": "https://en.wikipedia.org/wiki/Exuma_Cays_Land_and_Sea_Park" }, { "title": "Marine Managed Areas in The Bahamas", "url": "https://www.nature.org/en-us/about-us/where-we-work/caribbean/bahamas/stories-in-the-bahamas/marine-managed-areas/" }, { "title": "Bahamas - Protected - Marine Planning", "url": "https://marineplanning.org/wp-content/uploads/2019/07/Bahamas-Protected_MPA-Management-Guidance_Final-Report_rev.March2019.pdf" }, { "title": "West Side National Park", "url": "https://en.wikipedia.org/wiki/West_Side_National_Park" }, { "title": "Inagua Morton Salt Factory", "url": "https://www.bahamas.com/plan-your-trip/things-to-do/morton-salt-factory" }, { "title": "Morton Salt, Campbells, and Flamingos in the Bahamas. — Elaine A. Powers, Author", "url": "https://elaineapowers.com/morton-salt-campbells-and-flamingos-in-the-bahamas/" }, { "title": "How Morton Salt Helped Bahamas Flamingos", "url": "https://thepopularflamingo.com/blogs/posts/morton-salt-flamingos" }, { "title": "Inagua - The Bahamas Guide", "url": "https://thebahamasguide.com/islands/inagua/" }, { "title": "Great Inagua, Bahamas", "url": "https://sailabacos.com/bahamas/cays/great-inagua" }, { "title": "History of the Bahamas", "url": "https://en.wikipedia.org/wiki/History_of_the_Bahamas" }, { "title": "Columbus Makes Landfall in the Caribbean", "url": "https://education.nationalgeographic.org/resource/columbus-makes-landfall-caribbean/" }, { "title": "Looking for Columbus", "url": "https://www.usni.org/magazines/naval-history-magazine/1988/september/looking-columbus" }, { "title": "Lucayan people", "url": "https://en.wikipedia.org/wiki/Lucayan_people" }, { "title": "Lucayan People of The Bahamas: Indigenous History, Culture, Archaeology & Legacy", "url": "https://discoverbahamas.com/directory/lucayan-people-the-indigenous-history-of-the-bahamas-article-1369.aspx" }, { "title": "The Rich Past of the Lucayan People: Lucayans in the Bahamas - Only By Land", "url": "https://onlybyland.com/lucayan-people/" }, { "title": "Faces Divulge the Origins of Caribbean Prehistoric Inhabitants", "url": "https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6954214/" }, { "title": "Holocene sedimentation in a blue hole surrounded by carbonate tidal flats in The Bahamas: Autogenic versus allogenic processes - ScienceDirect", "url": "https://www.sciencedirect.com/science/article/abs/pii/S0025322719301811" }, { "title": "Blue Holes Show Hurricane Activity in the Bahamas Is at a Centuries-Long Low", "url": "https://www.smithsonianmag.com/science-nature/blue-holes-show-hurricane-activity-in-the-bahamas-is-at-a-centuries-long-low-180980235/" }, { "title": "Blue Holes Show Hurricane Activity in the Bahamas Is at a Centuries-Long Low", "url": "https://hakaimagazine.com/news/blue-holes-show-hurricane-activity-in-the-bahamas-is-at-a-centuries-long-low/" }, { "title": "Blue holes hide the ghosts of ancient Caribbean hurricanes", "url": "https://www.nationalgeographic.com/science/article/ghosts-ancient-hurricanes-caribbean-blue-holes" }, { "title": "Where Did Columbus Land?", "url": "https://www.britannica.com/topic/Where-Did-Columbus-Land" }, { "title": "Christopher Columbus - Explorer, Voyages, New World", "url": "https://www.britannica.com/biography/Christopher-Columbus/The-first-voyage" }, { "title": "Parliament of the Bahamas", "url": "https://en.wikipedia.org/wiki/Parliament_of_the_Bahamas" }, { "title": "15th Bahamian Parliament", "url": "https://en.wikipedia.org/wiki/15th_Bahamian_Parliament" }, { "title": "Parliament of the Bahamas", "url": "https://en.wikipedia.org/wiki/Bahamas_House_of_Assembly" }, { "title": "2026 Bahamian general election", "url": "https://en.wikipedia.org/wiki/2026_Bahamian_general_election" }, { "title": "Bimini and Berry Islands", "url": "https://en.wikipedia.org/wiki/Bimini_and_Berry_Islands" }, { "title": "EXTRAORDINARY OFFICIAL GAZETTE THE BAHAMAS PUBLISHED BY AUTHORITY NASSAU", "url": "https://laws.bahamas.gov.bs/cms/images/LEGISLATION/SUBORDINATE/2026/2026-0005/2026-0005_1.pdf" }, { "title": "St James (Bahamas Parliament constituency)", "url": "https://en.wikipedia.org/wiki/St_James_(Bahamas_Parliament_constituency)" }, { "title": "Progressive Liberal Party", "url": "https://en.wikipedia.org/wiki/Progressive_Liberal_Party" }, { "title": "The election results: An analysis", "url": "https://www.thenassauguardian.com/news/the-election-results-an-analysis/article_8c8fa01a-3dd3-4406-ae7f-a7bdcff3ac67.html" }, { "title": "Fort Charlotte (Bahamas Parliament constituency)", "url": "https://en.wikipedia.org/wiki/Fort_Charlotte_(Bahamas_Parliament_constituency)" }, { "title": "Philip Davis and Progressive Liberal Party win general election in Bahamas", "url": "https://www.aljazeera.com/news/2026/5/13/philip-davis-and-progressive-liberal-party-win-general-election-in-bahamas" }, { "title": "House Speaker announces major boundary changes, two new parl", "url": "https://www.bahamas.gov.bs/news-press-release/house-speaker-announces-major-boundary-changes-two-new-parliamentary-seats" } ], "license": "https://creativecommons.org/licenses/by/4.0/" }