North Macedonia

North Macedonia is a landlocked country in Southeast Europe, occupying the northern part of the wider historical region of Macedonia on the Balkan Peninsula. It covers about 25,713 km² and has a population of roughly 1.8 million, with Skopje as its capital. Its neighbours are Kosovo and Serbia to the north, Bulgaria to the east, Greece to the south and Albania to the west. Its position at a junction of routes linking Central Europe with the Aegean Sea has long shaped its settlement, trade and political history. The country's official name, the Republic of North Macedonia, dates from February 2019, when constitutional changes implemented the 2018 Prespa Agreement with Greece, which had disputed the earlier name "Macedonia".

The country's physical geography is defined by a rugged frame of mountain ranges, notably the Šar Mountains and Osogovo, which enclose the central valley of the Vardar River, the main axis of the country and its most fertile farmland. Its highest point is Mount Korab at 2,764 m, and its lowest lies near Gevgelija at about 50 m. Three large tectonic lakes, Ohrid, Prespa and Dojran, lie on the southern borders; Lake Ohrid is one of the oldest lakes in the world and is a UNESCO World Heritage Site. Drainage is split among the Aegean, Adriatic and internal systems, and the climate ranges from continental in the interior and mountains to Mediterranean influences in the south.

This entry first treats the country's name, location and territorial extent, then its physical landscape: relief, lakes, drainage, geology and climate. It then covers biodiversity, protected areas, land use, water and environmental pressures, and population and settlement. It closes with regional subdivisions, the historical geography of the wider Macedonian region, transport and strategic position, and the country's political-geographic relations, including its NATO membership and its stalled EU accession.

Name, status and the Prespa Agreement

The state that declared independence from Yugoslavia in 1991 entered international life with a name that its neighbour Greece rejected. The dispute centred on the word "Macedonia," which carried three overlapping meanings: the new republic, the Greek region of Macedonia, and the ancient kingdom of Macedon, whose best-known ruler was Alexander the Great and whose heritage is also claimed in ancient Greek historiography. Athens argued that an unqualified name implied irredentist ambitions on Greek territory and history, and it insisted on a geographical qualifier. The disagreement escalated quickly: in 1994 Greece imposed a trade embargo on the new state, and it blocked recognition and membership in several bodies. The wider naming question, including how the historical region was divided after the Balkan Wars, is treated in the entry on the Macedonian region.

The compromise that allowed the state to join the United Nations in 1993 was a provisional reference, the "former Yugoslav Republic of Macedonia" (usually abbreviated FYROM). Admission was granted under Security Council Resolution 817, which made the provisional name conditional on a settlement of the dispute. The 1995 Interim Accord, signed in New York on 13 September 1995 under UN auspices, did not resolve the name question. Instead, Greece agreed not to obstruct the state's applications to international organisations as long as it used the provisional reference, and the two sides committed to continue negotiations. For more than two decades, the provisional name was used by most international organisations and by many states. Skopje later brought a case against Greece before the International Court of Justice in 2008, arguing that Athens had breached the Interim Accord by blocking its NATO bid, a dispute that shows how the legal framework itself became contested.

The Prespa Agreement was negotiated under UN mediation and signed on 17 June 2018 by the two foreign ministers, Nikola Dimitrov and Nikos Kotzias, at a location near Lake Prespa, which gave the accord its name. Implementation required several steps. A referendum held on 30 September 2018 produced a large majority in favour, but turnout fell below the 50 per cent threshold, so the result was not binding; the Macedonian Assembly instead ratified the agreement and adopted a constitutional amendment on 11 January 2019 with a two-thirds majority. The Greek parliament approved the accord on 25 January 2019. NATO allies had signed the accession protocol for the state earlier in February, and the agreement entered into force on 12 February 2019, when both governments notified the United Nations that their domestic procedures were complete. The constitutional amendments of 2019 formally changed the state's name to the Republic of North Macedonia.

Under the agreement, the new name applies "erga omnes," meaning in all domestic and international relations and in every multilateral forum, so that states that had recognised the country under the old constitutional name were also expected to adopt the new one. The short form is "North Macedonia." The name is rendered in the official languages as Severna Makedonija in Macedonian, Voria Makedonia in Greek and Republika e Maqedonisë së Veriut in Albanian. The agreement keeps the adjectives for citizens and language as "Macedonian," so the nationality and the language are not renamed, a distinction that the agreement uses to limit the scope of the change to the state's name and its official use. The agreement also required that personal documents carrying the old name be replaced within five years of entry into force. Passports bearing the new name began to be issued only from July 2021, after delays linked to political blockades and the COVID-19 pandemic. By early 2024, reports estimated that roughly a third of citizens, around 600,000 people, still lacked passports or identity cards with the new name, and documents bearing the old name ceased to be valid after 12 February 2024.

In relation to history and geography, the agreement's effect is to separate the state's official identity from the contested term while leaving the historical region and the ancient kingdom to historians, archaeologists and neighbouring states. The qualifier "North" marks the state's position within the broader region, but it does not confer any claim to Greek provinces, which is the core of the Greek objection. The Greek side retains the name Macedonia for its own northern region, and the two uses now coexist under the terms of the accord. Debates over the historical legacy of the region continue in scholarship and in public discourse, but the legal naming question is settled by the agreement and its constitutional implementation.

Location, borders and territorial extent

North Macedonia occupies the south-central part of the Balkan Peninsula in southeastern Europe. It is a landlocked country in the south-central Balkans. Its strategic weight comes from its place on the continent's transport network. The Morava and Vardar valleys form a north–south route from the Danube to the Aegean, and older east–west trade paths linked the Black Sea and Istanbul with the Adriatic, crossing this territory at a crucial intersection of communication routes. Three large lakes, Lake Ohrid, Lake Prespa, and Dojran Lake, lie on the southern borders, bisected by the frontiers with Albania and Greece.

Figures for the country's size vary between sources. The total is most often given as 25,713 km^2 (9,928 sq mi), but the split between land and water differs. One source gives a land area of 24,856 km2 and a water area of 857 km², while another gives land 25,433 sq km/ water 280 sq km. Rankings by area also differ, with one source placing the country 148 in the world and another listing it at 145th. In continental terms it is a modest-sized state.

The country has five land neighbours. Kosovo lies to the northwest, Serbia to the north, Bulgaria to the east, Greece to the south and Albania to the west. The Kosovo border is usually given as 159 km long, the Bulgarian border as 148 km long, and the Albanian border as 151 km. The Greek border is the longest, with estimates ranging from 228 km to around 246 kilometers. The Serbian border is the most inconsistently reported. One source gives 62 km for the northern section, another gives 101 km for the stretch in the Preševo area, and a third gives 221 kilometre for the whole. The total boundary length is also reported inconsistently, as 766 km in one source and 838 km in another. The individual figures do not add up to either total, so the segment definitions used by each source should be checked before any single number is relied on.

The country has no coastline, so its access to the sea runs through Greece and, to the west, Albania. The Vardar is the principal link. The Vardar basin comprises two-thirds of the territory of North Macedonia. The river crosses the Greek border near Gevgelija, Polykastro and Axioupoli before emptying into the Thermaic Gulf, west of Thessaloniki, which gives the country its outlet to the Aegean. The valley also carries the transport links. The A1 motorway runs from the Serbian border at Kumanovo to the Greek border at Gevgelija, and the electrified railway from Skopje to Thessaloniki follows the same valley. A proposed Morava-Vardar Canal would link the Danube basin to the Vardar valley and extend the country's waterborne connections to the Mediterranean, though the project remains a proposal.

Mountain frame and the Vardar valley

North Macedonia is mostly mountainous. The average elevation of the terrain is about 850 metres, and roughly four-fifths of the territory consists of hills and mountains. The main ranges fall into two groups. In the north-west, the Šar Mountains run into the West Vardar–Pelagonia range to the south-west and south, forming part of the Dinaric system. In the south-east, the Osogovo–Belasica chain is the western end of the Rila–Rhodope massif. Together these ranges enclose the central lowland and form much of the country's borders.

The Šar Mountains are the largest range in the country, reaching across the Albanian and Kosovo borders. Their highest summit, Titov Vrv, rises to 2,748 metres. The range is considered younger than the Osogovo group and is divided into subgroups around the Vardar, the Pelagonia basin, and the north-west. Its steep flanks and high meadows are typical of a range shaped by recent tectonic uplift and later erosion. The Osogovo massif, by contrast, is an older block of crystalline rock, largely granite, that was lifted and fractured into a horst. Its western slopes are steep and its ridges are cut by deep valleys. The highest peak, Ruen, lies on the border with Bulgaria, and only about 72 percent of the massif's area lies on the North Macedonian side. Its ridges also mark watersheds, including a divide between the Vardar and Struma basins.

The Vardar valley is the country's central lowland. It runs from north-north-west to south-south-east, a direction that follows the major fault lines of the region. The valley owes its shape to the contrast between the rock types on either side, which made the central zone more vulnerable to erosion. The valley floor has deep fluvial deposits and a high water table, which is why its lowland soils are fertile but unsuitable for underground construction. Along this axis lie Skopje, Kumanovo, Veles, and Gevgelija, and the valley carries most of the country's settlement, irrigated farming, and road and rail links. Two basins branch from it. The Pelagonia basin lies in the south-west, where Bitola is located, and the Ovče Pole plain lies to the east of the Vardar's middle course.

The elevation range within the country is among the widest in the Balkans. Mount Korab, at 2,764 metres, is the highest point and forms part of the Korab range along the Albanian border. Its summit is also the highest point of Albania, so it is shared between the two countries. Its flanks include alpine terrain above 2,000 metres. At the other end of the scale, the Vardar near Gevgelija lies at about 50 metres, close to the Greek border. The difference of roughly 2,700 metres between the two points is compressed into a relatively short distance, which is one reason the country's climate and vegetation change so sharply from the valley floor to the high ridges. The Vardar River itself drains the valley toward the Aegean, linking the upland margins to the lowland through a single corridor.

Tectonic lakes of the southwest and south

Three lakes in the southwest and south of the country, Ohrid, Prespa and Dojran, owe their basins to tectonic subsidence rather than to glacial or volcanic processes. Ohrid and Prespa are grouped with other basins that originated from a geotectonic depression 2 to 5 million years ago on the western Dinarides. The area lies in a tectonically active graben system of the Western Macedonian geotectonic zone, which is why the lakes sit in faulted troughs and are linked by underground water pathways.

Lake Ohrid

Ohrid is the largest and deepest of the group. It covers about 358 km², and its maximum depth of 288 metres and mean depth of 155 m make it the deepest lake in the Balkans. Age estimates differ between sources: one puts it at some three to five million years old, while another gives a wider range of 4-10 million years. The lake is shared unevenly, with approximately two thirds of the lake surface area belonging to Macedonia and the remaining third to Albania. Its unique aquatic ecosystem of worldwide importance includes more than 200 endemic species. Water enters mainly from the Sateska River, springs and an underground connection with Prespa, and leaves through the Black Drin. With a water volume of 55.49 km³, its water residence time is about 70 years, a figure linked to the lake's small drainage basin and a Mediterranean-influenced climate (the lake's small drainage basin of 2600 km2 lead to a long hydraulic residence time scale of ~70 years).

Lake Prespa

Prespa lies at a much higher elevation, at 2,800 feet (853 metres) above sea level. Its position is unusual: the tripoint between Albania, North Macedonia and Greece is located on the lake itself, and most of Lake Prespa is in North Macedonia. It is shallow compared with Ohrid. Reported maximum depths range from about 48 to 54 metres, and Prespa has a mean depth of 14 meters. Reported areas also vary, from roughly 250 to 320 km², depending on how the lake's shoreline and sub-basins are measured.

Prespa's hydrology is tied to Ohrid. Because of the karst terrain, a large amount of water of Prespa Lakes seeps into the soil, drains away through a network of underground fissures, and supplies the springs located on the shore of Lake Ohrid. About 20 percent of Ohrid's water drains down from the higher-elevation Prespa through underground karst channels. The link has a cost: Lake Prespa lost 7 percent of its surface area and half of its volume between 1984 and 2020, likely because of increased water withdrawals for agriculture. The two lakes are part of the Ohrid-Prespa Transboundary Biosphere Reserve, added to UNESCO's network in 2014.

Lake Dojran

Dojran is the smallest of the three and lies on the North Macedonia–Greece border. It covers 43.1 km², of which 27.3 km² is in North Macedonia and 15.8 km² is in Greece. Its maximum depth is 10 m, and it sits at 148 m above sea level. The lake is shallow and eutrophic, with extensive Phragmites reedbeds. Its small volume makes it warm in summer; one regional source describes it as the country's warmest and shallowest lake.

Dojran's water budget has been unstable. Heavy overuse of the lake's water for agricultural purposes lowered its level, and due to the high water loss in the period between 1988 – 2000 a charging system was built by transferring water from the basin of the Vardar River to Basin of Dojran Lake. The lake was later designated a Ramsar wetland in 2007.

Shorelines, tourism and water supply

The lakeside settlements are Ohrid and Struga in North Macedonia along with Pogradec in Albania. Ohrid's water supports agriculture, fishing, hydropower and tourism, and the lake is one of the most popular tourist destinations in the Balkans. Prespa developed later: little developed until after 1945, in the 1970s Prespa became a tourist and fishing centre. Dojran's resort towns, Star Dojran (old resort area) and Nov Dojran (newer settlement), depend on a lake whose level and quality are shaped by upstream water abstraction and transfers, so the lakes' value for tourism and water supply is closely tied to how their basins are managed.

Drainage basins and river systems

North Macedonia's rivers drain to three separate outlets: the Aegean, via Greece, and the Adriatic, via Albania, with a few small internal areas. The Aegean system is the largest. A national water-resources report divides the Aegean basin into the Vardar catchment, about 20,525 km², and two right tributaries of the Struma, the Strumica and Lebnica. The report also states that most of the country's water divisions (12 of 16) depend on the Aegean basin.

The Vardar is the main axis of this system. It is 388 km long, of which 76 km lie in Greece, and it drains an area of around 25,000 km². The 25,000 km² figure covers the whole basin, while the in-country share is smaller, which explains the gap between the two numbers. Its springs lie at Vrutok near Gostivar, and it then passes through the Polog valley, the Skopje valley, and the Veles and Tikvesh valleys before crossing into Greece near Gevgelija. The basin takes in about two-thirds of national territory.

The Vardar's largest tributaries are the Bregalnica, the second largest river in North Macedonia, which runs 211.5 km. Its basin covers about 21% of the Vardar watershed within the country. The Crna is another major tributary, a right tributary of the Vardar that runs through much of the south and west of the country. The Treska, 132 km long, joins the Vardar as its right tributary, while the Pčinja has all its major tributaries inside North Macedonia. The Lepenac rises in Kosovo and empties into the Vardar at the northern borough of Skopje.

In the east, the Strumica drains to the Aegean through the Struma. It rises on the Plačkovica mountain in Radoviš municipality and runs south in a deep valley. It runs through the town of Strumica and flows into the river Struma. Estimates of its basin area differ: one source gives 1,535 km² for the Strumica catchment, while another gives around 1,649 km², with smaller portions in Bulgaria and Greece. The Struma itself is much larger, with a drainage area of 17,330 km², of which only 2,365 km² lies in North Macedonia. The Lebnitsa, a right tributary of the Struma that flows through southeastern North Macedonia, is 50 km long.

The Black Drin drains the west of the country. It flows out of Lake Ohrid at Struga. It is 149 km long and its drainage basin covers 3,504 km². Its average discharge is 118 m³/s. After 56 km in North Macedonia, it crosses into Albania west of Debar. It merges with the White Drin at Kukës to form the Drin, which reaches the Adriatic Sea. The lake's own catchment is 2,600 km², and its primary inflows include the Sateska River, springs, and an underground link with Lake Prespa. The Sateska was originally a tributary of the Black Drin, but was re-routed in 1961–1962 into Lake Ohrid. The diversion aimed to reduce sediment entering the Globočica reservoir, to secure hydropower potential on the Black Drin, and to drain the Struga marsh wetlands. The change expanded the lake's catchment by 460 km².

The three basins are linked by how water is used and stored. Groundwater is closely tied to the rivers: karst mountains in the western part of the country, such as Galičica and Jablanica, are significant recharge areas for the largest karst springs. The aquifers are also productive, since the Pelagonija and Strumica basins contain the richest artesian aquifers. Rivers feed farming as well. Seasonal flow is a constraint, as the Marko's River is subject to summer drought and snowmelt in the spring, and therefore experiences a very different flow depending on the season. Its water has great potential for irrigation. Hydropower has also shaped the western basins, since the Sateska diversion was partly meant to strengthen the Black Drin's dam-based generation. The Sateska's diversion also brought pollution, and since the 1960s the river has been a major source of pollution for Lake Ohrid.

Geological origin and tectonic setting

North Macedonia lies in the internal part of the Balkan Peninsula, where the older basement is a stack of tectonic units. Geologists do not agree on how many units to recognise: one scheme lists five major tectonic units, from east to west: the Serbo-Macedonian Massif, the Vardar Zone, the Pelagonian Massif, the Western Macedonian Zone and the Chukali-Krasta Zone, while another counts six major units. The central Vardar Zone and the Pelagonian Massif appear in both schemes and shape most of the country's geology.

The Vardar Zone records an oceanic basin. Its rocks reflect a Triassic–Early Cretaceous ocean that had a protracted and complex subduction history, and closure began in the Late Jurassic. Ophiolites, fragments of oceanic crust and upper mantle, are common within it. The best-known example is the Radusha Massif northwest of Skopje, which covers an area of 60 square kilometers and was mined for chromium for decades. During the Late Cretaceous and Palaeocene, the remaining oceanic crust was consumed and the basement units of most of the country were welded together. Rocks within the Vardar Zone were strongly deformed into narrow NNW trending belts bounded by faults. Geophysical estimates suggest the crust is thinnest here, about 28 km in the Vardar zone, rising to 36–39 km in both the east and west.

The Pelagonian Massif forms a high-grade metamorphic core. Pre-Cenozoic basement tectonic units have a NNW trending structural grain, except in the north-central part of the country, where structures and foliations bend around the north plunging Pelagonian anticlinorium. This curvature shows that the compressional structures of the older orogeny were later bent and offset.

The present landscape owes much to Neogene and later extension. Basins such as Skopje and Tikveš sit in grabens whose faults reused older weaknesses. The NW-trending faults in these grabens lie along the trends of older faults within the NW-trending Vardar zone basement tectonic unit and appear to be reactivated faults controlled by the basement anisotropy. Volcanism accompanied this stage. Late Miocene to Pleistocene volcanism within the Vardar zone covers a large area, has a wide range in composition, and is largely connected to the tectonic evolution of the South Balkan extensional system. Extension moved eastward and N-S extension begins at about the position of the Vardar zone and continues eastward into eastern Macedonia during the Pleistocene.

The tectonic lakes show how this extension works. Lake Ohrid occupies a graben within the South Balkan Extensional Regime. Sedimentation in the Ohrid Basin began in the Late Miocene with the formation of a pull apart basin, controlled by right-lateral strike-slip movements. Subsidence and further extension account for the major dynamic component since the Pliocene-Pleistocene. Vertical displacement between the central and eastern parts of the lake has been estimated at ~0.2 mm a−1. Researchers conclude that there is no indication that a major tectonic event alone caused the formation of Lake Ohrid. Lake Prespa, which lies on the tripoint of North Macedonia, Albania and Greece, is also classed as an ancient tectonic lake, and studies indicate it already existed when Lake Ohrid formed.

Seismic risk is substantial. Lake Ohrid sits in a seismogenic landscape, with many visible traces including fresh fault scarps, displaced sediment and soil sequences, stepped hillsides. The most damaging event in the country's recent past was the 1963 Skopje earthquake. Estimates of its magnitude vary slightly by catalogue, from about 6.0 to 6.1, but it caused severe losses: more than 1,000 deaths and between 3,000 and 4,000 injuries, and about 80 percent of the city was destroyed. Damage was concentrated in poorly designed but recently built office buildings, hotels, and apartment houses in the center of the city.

Karst processes add another layer to the geology. Carbonate rocks in the mountains dissolve over time, creating caves, sinkholes and underground drainage that shape groundwater movement. The lakes are closely tied to this system. Lake Ohrid is mainly fed by karst aquifers, and its main inflows come from underground karstic channels from Lake Prespa carrying minimal sediment.

Climate and regional climatic variation

North Macedonia has no single climate. Its position between the continental interior of the Balkans and the Mediterranean, combined with steep relief, produces several regimes within a short distance. Most sources describe the north and west as relatively close to continental conditions, while the south and east lean towards Mediterranean patterns. Mountains shape this split. The Šar Mountains in the northwest block cold northern air, and ranges to the south restrict the northward movement of hot air, which keeps the interior cooler than its latitude alone would suggest. Along the Vardar valley, a warm wind that arrives from the river's mouth in Greece is credited with milder winters in the lower basin.

The thermal contrast between seasons is strong. At Skopje, the capital at roughly 250 m, the 1991–2020 normals give a mean daily temperature of about 0 °C in January and about 24 °C in July and August. Summer afternoons in the lowlands regularly reach around 32 °C on average, and heat waves can push temperatures past 40 °C. Winter brings cold spells that can drop temperatures to −20 °C or lower. The national extremes recorded to date are about 45.7 °C for the highest and about −31.5 °C for the lowest. Cold winter nights are a regular feature of the basins, and the Skopje airport station has recorded a January minimum of about −25.8 °C. Heat records are also recent: the Skopje Zajcev Rid station reported 42.3 °C in July 2025.

The southern valleys and the Lake Ohrid basin show a clearer Mediterranean character. The Vardar valley experiences hot, dry summers and mild, wet winters, and the sea's influence keeps rainfall moderate there. The Ohrid region is classed as Mediterranean with continental influences. Its mean annual temperature is around 11.5 °C, with winter values typically between 2 and 6 °C and summer values between 10 and 22 °C. The lake itself moderates the local climate through its large thermal capacity, and the nearby Adriatic and local topography also contribute. Regional rainfall in the Ohrid area averages roughly 880 mm a year, with the bulk falling in the cooler half of the year, a pattern typical of Mediterranean rainfall regimes.

Precipitation varies more with location and altitude than temperature does. The western part of the country is the wetter one, with an average of about 730 mm a year and local totals ranging from 400 mm to over 1,000 mm. The lowland stations are drier: published normals for Skopje cluster around 470–490 mm per year, although tables differ on the exact monthly peaks, and most place the heaviest falls in late spring or autumn. Elevation intensifies rainfall in exposed mountain settings, and high ground in the northeast carries snow cover from October into early June. Climate classifications for the country usually separate belts by altitude: sub-Mediterranean conditions up to about 500 m, a warm continental belt roughly between 600 and 900 m, and mountain forest and subalpine climates above about 1,300 m. These boundaries are not fixed, and slope aspect and local weather patterns shift them.

Temperature also falls markedly across short distances within the mountains. The eastern town of Berovo, for example, has a humid continental regime and a much lower mean annual temperature than other places at a similar altitude in the valley, with January means near −10 °C. The overall north-to-south gradient therefore combines latitude, the barrier effect of the ranges, and the cooling effect of elevation, so that a traveller crossing the country can pass from lowland heat to snowy uplands within a few hours' drive.

Biomes, flora and fauna

North Macedonia's vegetation reflects its position where Mediterranean and continental climate influences meet. The northern and western parts of the country are relatively close to a continental climate, and the southern and eastern parts to a Mediterranean climate. Vegetation zones follow altitude. In the mountainous northwest, the lower slopes carry mainly deciduous woodland, while conifers grow at elevations as high as 2,000 metres. Above that, subalpine forests between 1,650 and 2,250 metres are dominated by beech across the country, and in the past they were often converted to pastures for intensive sheep breeding. Cleared forest has also been turned into rough summer pasture. Ancient beech stands are rare, and the largest examples lie on the Korab, Osogovo, Maleshevo and Belasica ranges. Refugial beech forests are remnants of past glaciations, and they developed in deep river gorges at low altitudes with distinctive plant assemblages.

The lowlands have a different character. Grassland steppe occurs in the area around Negotino and Krivolak, where a local endemic plant, Ferulago macedonica, is known from the Macedonian steppe. Dry grasslands near the Bregalnica river and Demir Kapija also support small populations of rare plants. Limestone and gorge habitats add further variety, such as the Matka Canyon near Skopje, where approximately 20% of the 1,000 plant species in the area are endemic or rare.

The flora is large and unusually concentrated in its endemics. At least 3,700 species of vascular plants have been identified, of which 116 are endemic or near-endemic. Strictly endemic species make up a small share of the total, since 3.6% of the vascular flora is endemic, including 114 endemic vascular plant species. The proportion of Balkan endemics is considerably higher, and many species reach the limits of their range within the country, while the diversity of plant communities is also high.

Animal diversity is similarly broad. The country is part of the Mediterranean Basin biodiversity hotspot, and in total it hosts over 16,000 wild species of bacteria, lichens, fungi, moss, plants and animals, more than 800 of which are endemic. Forests support mammals such as bears, wild boars, wolves, foxes, squirrels, chamois and deer. The Eurasian lynx survives, though very rarely, in the mountains of western North Macedonia. Reptiles are also of conservation concern: Hermann's tortoise is now classified as vulnerable, following national assessments supported by an international project.

Lake Ohrid is the centre of the country's aquatic endemism. Of the lake's roughly 1,200 known native species, 212 are endemic, occurring nowhere else. Its fish fauna is the best known. The Ohrid trout is the most celebrated species, and overfishing has reduced its numbers so much that catching it is now illegal on the Macedonian side, though poaching is said to be common. Estimates of fish endemism vary between sources. One analysis states that approximately 40% of the lake's fish species are endemic, while an earlier count listed seven endemic fish species in the lake. The difference partly reflects how species are classified and which groups are counted.

Introduced species are a major pressure on this fauna. The Ohrid trout faces new competition from seven introduced fish species, including rainbow trout. Plants and invertebrates are also affected. Canadian waterweed, the acute pond snail and Prussian carp are now well established and outcompete native invertebrates and fish for food and habitat. The same pattern occurs at the other large lakes. A 2024 inventory of fish species recorded 12 introduced fish species in Prespa Lake, compared with 11 native ones.

The lakes, wetlands and rivers form the core of the country's freshwater life. In the large natural lakes of Prespa, Ohrid and Dojran, about 60 fish species from 15 families have been described, while other species live in rivers and artificial lakes. Lake Dojran is especially notable for species found nowhere else, such as the Dojran bleak and the Dojran roach. Wetlands and ponds in the lowlands provide habitat for amphibians and fish that depend on still or slow water, though many of these species are threatened by drainage, pollution and the spread of non-native fish.

Protected areas and natural heritage

The protected-area system began in 1948, when Pelister became the first national park. Since 1948, when Pelister National Park became the first national park, both the number and total area of protected regions have grown consistently. The country now has four national parks. Pelister, Mavrovo and Galičica date from 1948 to 1958, while the Šar Mountains park was created much later. On June 30, 2021, the Parliament of the Republic of North Macedonia adopted a law proclaiming part of the Shar Mountains a national park, making the area the fourth national park in the country, but also the first to be so designated since the country's independence in 1991.

National parks

Mavrovo is the largest of these parks. Mavrovo National Park is the largest of the four national parks of North Macedonia, within the borders of the municipality of Mavrovo and Rostuše. Its legal status has been tightened over time. It was established in 1949 by a law passed by the National Assembly of the Socialist Republic of Macedonia; later the legislation was changed to enforce a much stricter protection system, dividing the park into three zones: strict nature reserves, managed reserves, and a tourist zone. The recreational zone holds ski facilities around Lake Mavrovo, while the strictly protected core covers areas where human use is excluded. Mavrovo also contains an unusually large chamois population, and their preservation is funded by the revenue generated by the sale of timber gained from salvage logging, a practice that is prohibited in some of the reserves.

Galičica occupies a narrow limestone range between two lakes. Galičica was declared a national park in 1958 and covers roughly 24,000 hectares (about 240 km²) of the mountain range of the same name, in the country's southwestern corner. Figures for its area vary between sources; a national park list gives 227 km². The park's position between Ohrid and Prespa is the reason for its protection, because its wildlife and rare plants are unusually concentrated.

Šar Planina is the most recent addition. The Shar Mountains stretch from Kosovo and northwestern North Macedonia to the northeast of Albania and represent 2% of North Macedonia's land mass. The designation covers territory with a population of 26,000 spread across 30 villages, so it required negotiations with existing concession holders. Those negotiations were still underway in 2022, under the transitional provisions of the park law.

Lake Ohrid and its World Heritage listing

Lake Ohrid is the country's main UNESCO property. In 1979, the Committee decided to inscribe the Ohrid Lake on the World Heritage List under natural criteria. In 1980, this property was extended to include the cultural and historical area, and cultural criteria were added. A later extension in 2019 added the Albanian portion of the lake. The listing is therefore mixed in character. Its natural values rest on the lake's age and endemism: the lake's fish fauna includes 17 native species, of which 10 are endemic, and about 86% of the 50 known species of gastropods are endemic. Its cultural values centre on the town of Ohrid, where over 250 archaeological sites cover a period of more than 5,000 years.

Other protected areas and the national system

Outside the parks, the network includes nature reserves, monuments and other categories. Estimates of the total cover differ according to year and classification. One assessment states that North Macedonia has 68 protected areas, covering 352 135.23 hectares or 13.84% of its territory, and that national parks occupy around 7% of the country's land, natural monuments about 3% and other categories approximately 4%. A different source puts the figure at approximately 9% of the country is designated as protected areas, comprising 86 sites. The legal framework is based on the Law on Nature Protection, and the rest of the protected areas are yet to be reclassified according to the new categorization guidelines from the IUCN. Planned targets are more ambitious: one draft revision seeks to increase protected areas network so that they cover up to 15% of the country territory.

Pressures on protected areas

Tourism, construction and land use change are the most frequently named threats. For Lake Ohrid, a report to the World Heritage Committee notes a negative trend in wintering waterbird populations, driven by habitat loss, shoreline alteration, poaching, and tourism pressure. Illegal construction and pollution are also cited as risks to the lake's standing. On Šar Planina, the new park has faced development pressure, and the mountains are increasingly threatened by exploitation of soil, water, and forests. Management capacity is a further concern. One conservationist has argued that the goal is not just to declare an area, but a lot needs to be invested in management, and that national park efficiency still needs to improve despite foreign donor support. Fire risk also shapes access: Mavrovo has previously required registration or restricted unauthorized forest movement during high fire risk.

Soils, land use and agriculture

Agricultural land covers roughly half of the country, although published shares vary with the data source. One World Bank-based summary gives almost 50 percent, with forests constituting another 45 percent in a USDA report, while CORINE land cover classification figures from 2014 show a lower 36.9 percent. In absolute terms, the USDA counts 1,251,000 hectares of agricultural land in 2023, of which pastures make up 736,000 hectares (59 percent) and the remaining 514,000 hectares are cultivated.

Farmland is heavily fragmented. Over 55 percent of parcels consist of two to five hectares, and fewer than one percent reach 50 hectares or more. The land market is thin, which makes it hard for farms to expand and limits the introduction of modern machinery and better irrigation. Since 2014 the FAO has run consolidation projects that address state-owned land privatisation, abandonment and the development of land markets. Abandonment is itself a major concern: approximately 32 percent of arable agricultural land in the country has been abandoned, a much higher rate than in other European countries. Abandonment is concentrated in smaller rural settlements, where depopulation has been most pronounced.

The Vardar valley is the agricultural core of the country. The Vardar valley is the main economic corridor of North Macedonia, and its alluvial plain is the most intensively cultivated zone. Around Skopje, the large areas are dedicated to the cultivation of vegetables, industrial crops, horticulture, and early vegetable production under greenhouses and plastic tunnels, as well as fruit growing and viticulture. Further south, the Tikveš area is known for vineyards and wine production. Pelagonia, in the southwest, is a major grain region: it contains 25% of arable land and is the leading area for wheat.

Cereals, fruit, vegetables, tobacco and livestock form the core of the farming system. The main field crops are wheat, barley, corn, and rice. Wheat area has stabilized since 2019 at about 70,000 HA, and barley reached 46,000 hectares in 2023. Rice is grown on a small area, yet the country is a net exporter of rice. The country does not produce sufficient quantities of grain and feed crops to meet demand and relies on imports of dairy and meat, with the exception of lamb. Fresh apples are among the leading export products, and livestock farming, especially in its mountainous regions, remains important. Farm structure is mixed: numerous small-scale family farms coexist with large enterprises inherited from the socialist era.

Soil degradation is closely tied to terrain and land management. Steep slopes (≥20°) account for 23% of the total area in the wider Western Balkans study region, and water erosion is quite a present problem, particularly on sloping land. Unplanned deforestation further increases erosion. In the north-western mountains, due to uncontrolled extensive forest exploitation and unsustainable agricultural practices, approximately 58 % of the Lipkovo Municipality is experiencing severe erosion. Urban growth adds another pressure: the greatest soil sealing is observed around the biggest urban areas in North Macedonia, mainly around Skopje. Regional estimates for 2000–2010 identified North Macedonia (589 km²) as land with a trend of degradation.

Policy and monitoring lag behind these pressures. There are no official data for most WB countries as regards areas affected by erosion and no erosion monitoring system in place. A draft law on soil protection was prepared almost a decade ago but has never been adopted, and two attempts at a National Action Plan for Land Degradation and Desertification have not been approved by the government. Irrigation and climate adaptation are now central to the agricultural outlook: the growth potential of most production is highly dependent on reforms in irrigation and the introduction of climate-smart practices, especially as the country has recently suffered through prolonged summer heat and drought waves impacting crop yields.

Water resources and environmental pressures

Surface water and groundwater form two linked systems. Groundwater is formed when precipitation and surface water infiltrate the subsurface and accumulate in aquifers, which lie mostly beneath the floors of the basins and in alluvial plains. The country has documented 4,414 springs with an annual output of about 991.9 million m³, and the west holds most of the largest springs, while the east is much drier and depends more on stored water in reservoirs. Since the 1950s, the state has built more than 300 dams, along with large irrigation systems, to hold water from wet periods for use in dry seasons. Estimates of groundwater's share vary: a 2025 review gives it about 70% of total water supply, while the government's Groundwater Programme states that it provides 77% of drinking water. The same programme says that groundwater management is weak, with limited institutional capacity, sparse monitoring data and an incomplete legal framework.

Water demand is highly variable. The Water Use Index was about 20% in years of intensive use and rose to around 35% in 2012. Drought can lower water tables in both confined and unconfined aquifers across all basins, affecting groundwater salinity, moisture and storage capacity. Because the country's lakes are fed in part by karst springs, the lake and groundwater systems respond to the same dry spells.

Water quality problems are most visible in the lakes and along the rivers. Lake Ohrid, which is oligotrophic, is threatened by nutrient loading. Sewage from settlements has been a major problem: in the lake's catchment, an older government-era assessment found that less than 25% of wastewater was treated, and untreated discharge from Pogradec, on the Albanian shore, was the main source of coliform pollution until 2009. Recent inspections on the Macedonian side report that houses along the shoreline use septic tanks that can seep into the lake, and that stormwater pipes and beach bars also contribute pollution. Fertiliser use in both Albania and North Macedonia was high in the 1990s, at roughly 160–200 kg/ha per year, and irrigation intensifies runoff. Phosphorus transported from the more eutrophic Lake Prespa has also been identified as a potential future threat to Lake Ohrid. Many rivers flow through populated areas with inadequate sewage systems, unauthorised landfills and intensive farming, which raises contamination risks for the towns that depend on them.

Air pollution is most serious in the urban basins, especially Skopje, during the winter heating season. Skopje lies in a valley crossed by the Vardar river, and anticyclonic conditions can create temperature inversions that trap particles near the ground. A 2026 dispersion modelling study of the city found that household heating with biomass is the dominant source of wintertime particulate matter, with PM10 exceeding PM2.5 in contribution. A 2018 household-heating survey by UNDP estimated that heating accounts for about 32% of Skopje's air pollution, and it reported PM10 levels above 14 times the level considered acceptable by health experts. Industrial emissions and traffic add to the load, and similar winter pollution has been recorded in Bitola, Tetovo, Gostivar, Kičevo and Ohrid. Health studies in Skopje have linked increases in PM10 to rising daily hospital admissions for cardiovascular disease.

Climate-related pressures are expected to intensify. Projections for the Vardar catchment suggest that groundwater recharge could fall to about 57.6% of its current level by 2100, and that the annual discharge of the Vardar, Treska and Bregalnica rivers may decline by up to 10% by 2025, 16% by 2050 and 24% by 2100. Warming also threatens Lake Ohrid: one study projected that warmer conditions would significantly reduce the frequency of deep-water mixing, which would affect oxygen supply to the lake's endemic species. Adaptation measures discussed in the country include conjunctive management of surface water and groundwater, and managed aquifer recharge, in which surplus surface water or treated wastewater is stored underground for use during droughts.

Population distribution and settlement pattern

The 2021 census, the first since 2002, recorded 1,836,713 residents, 1-2 roughly 185,800 fewer than two decades earlier. The 1991 population had been just over 2 million. 5-5 Including 260,606 non-residents, the enumerated total reached 2,097,319. 9-2 Estimates of overall density differ by source: one gives about 72 people per square kilometre 13-2, another about 82. 17-2 Either way, the country is sparsely settled, and people cluster in the lowland valleys and basins rather than spreading evenly across the mountains.

Most of the population lives in the Vardar valley and around Skopje. The Skopje Statistical Region had 607,007 inhabitants in 2021, 8-3 which is nearly a third of the national total. 8-4 Beyond the capital, the largest municipalities in 2021 were Kumanovo (98,104), Bitola (85,164) and Tetovo (84,770). 16-5 Ohrid, Prilep and Štip are also significant urban centres, and Ohrid's role is tied to tourism around its lake. The share of people living in towns is reported inconsistently because sources use different definitions and years. One source gives 29.5 percent rural, 42.1 percent in towns and 28.4 percent in cities for 2020. 12-3 Another reports 70.3 percent urban in 2026, 10-4 while a long-run series had 57.33 percent in 2017. 11-5

Rural depopulation is concentrated in the upland municipalities. A study of 37 rural municipalities, covering 34.9 percent of the national territory, 15-3 counted 390,810 people in 2018, a decrease of 3.1 percent since 2005. 15-4 The decline is uneven, however: in 18 municipalities the population grew, and those municipalities held 75.5 percent of the rural population. 15-6 Growth was strongest in rural municipalities close to Skopje, such as Studeničani and Arachinovo. 15-7 Earlier, a large wave of internal migration moved more than 175,000 people from villages into towns and cities, mainly in the decades after the Second World War. 15-1 International emigration has also reduced the population: EU statistics suggest at least 230,000 people moved to EU member states between 1998 and 2011. 5-5 Net migration remained negative in recent years, with about 5,700 more people leaving than arriving in 2026 according to one estimate. 13-5

The ethnic geography of settlement is closely tied to region. Among residents, 58.44 percent identified as Macedonian and 24.3 percent as Albanian in 2021. 9-3 Albanians number 446,245 in the resident population, making them the second-largest group, 2-1 and their settlement is concentrated in the western and north-western parts of the country, with a partial presence in the centre and smaller communities in the south-west. 2-3 Albanians also form a substantial share of Skopje's residents, at 22.8 percent. 9-5 Language patterns follow a similar regional logic: 61.38 percent of the enumerated population gave Macedonian as their mother tongue, and 24.34 percent gave Albanian. 9-4 Turks (3.86 percent) and Roma (2.53 percent) are the other notable groups. 9-3

The 2021 census was contested. The opposition party The Left led a boycott, 1-4 and about 7.2 percent of the population was counted from administrative sources without ethnic or linguistic data. 1-5 Because ethnic shares are politically sensitive, figures based on resident and enumerated populations should be read with their definitions in mind.

Regional geography and historical subregions

Partition and the twentieth-century borders

North Macedonia occupies only part of a wider geographic region that has long been called Macedonia. Under the Ottoman Empire the area was one administrative unit, but its borders were redrawn in 1912–1913. Serbia, Greece, Bulgaria and Montenegro first fought the Ottomans together, then Bulgaria fought its former allies over the spoils in Macedonia, a dispute that became the Balkan Wars of 1912–1913. The Treaty of Bucharest in 1913 gave Greece and Serbia most of the territory, while Bulgaria kept a smaller part, the Pirin area. The Treaty of Versailles in 1919 confirmed this partition among the Kingdom of Serbs, Croats and Slovenes, Bulgaria and Greece. The Serbian share became the Vardar Banovina of the Kingdom of Yugoslavia in 1929, and during World War II it was split between Bulgaria and Italian-occupied Albania.

After 1945 the Serbian share was reconstituted as a republic within Yugoslavia. As one of the six constituent republics of the federal state, it was landlocked and bordered Albania, Greece and Bulgaria, and it shared a northern boundary with Serbia, including the Kosovo province. The republic's borders were thus those of the present state, although the status of the surrounding regions remained a matter of dispute among the Balkan states. The competing historical claims that underlie these disputes are discussed in the Macedonian question entry. Regional names also reflect those divisions: the parts of the wider region in Greece and Bulgaria are often called Aegean and Pirin Macedonia, while the North Macedonian part is commonly called Vardar Macedonia.

Traditional subregions and their physical basis

The country's internal regions follow its river valleys and basins. The Vardar valley is the central axis and is commonly divided into five sections: Polog, the Skopje basin, Veles, Tikveš, and the Gevgelija–Valandovo basin. Polog covers the upper Vardar, with a southern upper part and a northern lower part, and is bounded by the Šar Mountains to the west and Suva Gora to the east. The Skopje basin is separated from Polog, the Kumanovo basin and the Ovče Pole by narrow gorges, which makes these lowlands distinct physical units. Kumanovo lies in the northeast, and Ovče Pole is an open plain to the east of the valley.

Outside the Vardar corridor, the Strumica basin in the southeast is an enclosed unit made up of the Radoviš, Strumica and Petrič basins, framed by the Plačkovica and Ogražden mountains. It opens eastward along the Struma valley toward the Aegean. Pelagonia, in the southwest along the eponymous plain, is the largest of the lowland regions in the west, bordering Greece to the south and Albania to the west. Its fertile plains and the Ohrid and Prespa areas further southwest give the region its agricultural and lacustrine character.

Contrasts between the uplands, the valley and the south

The territory can be read as three broad zones with different geology and relief. The northern and western uplands belong to the Dinaric fold mountains, while the Struma valley in the east is bordered by ranges of the Thracian Massif. Where the Thracian ranges occur, slate, granite and gneiss replace the limestone that dominates elsewhere, which affects soils and drainage. The central Vardar valley is a corridor of lowlands and basins that connects the uplands and supports most settlement and farming. The south-west, with the Pelagonia plain and the Ohrid–Prespa basins, forms a plateau-and-lake landscape that differs in climate and water regime from the northern and central zones.

Transport corridors and strategic position

North Macedonia lies on the line between Central Europe and the Aegean, and two Pan-European corridors cross it. Corridor VIII runs east–west from the Adriatic to the Black Sea, and Corridor X runs north–south from the Serbian frontier to the Greek one. Because both routes converge in the country, its role is mainly that of a transit state, and its transport planning is shaped by how well it connects to these larger networks.

Corridor VIII and Corridor X

Corridor VIII links Albania's Adriatic port of Durrës with Bulgaria's Black Sea port of Varna, and its central section passes through Kičevo, Skopje, Kumanovo, Beljakovce and Kriva Palanka. Its eastern part has been upgraded in stages. A new expressway section between Stracin and Kriva Palanka reduced travel time from about 30 minutes to 10, and the route toward the Bulgarian border was already open in 2020. Future projects named by the government include Gostivar–Bukojčani, Kičevo–Ohrid and Prilep–Bitola. Corridor X enters the country at Tabanovce on the Serbian border and leaves at Gevgelija on the Greek border, carrying traffic between Central Europe and the port of Thessaloniki. The road network totals about 14,182 km, and the two corridors are its principal backbone.

Rail links and their history

The rail system was built on the north–south axis from the late nineteenth century. The Thessaloniki–Skopje line opened in 1873 under Ottoman administration, and the first station on present-day territory, at Veles, dates from the same year. Later lines followed toward Bitola (1894) and Vranje (1889), which connected the region to the wider Central European network. After 1913 the railways were integrated into Serbian administration, and the Veles junction was repeatedly damaged in the wars of the region. The main line from Niš through Kumanovo, Skopje, Veles and Gevgelija remains the central axis, although at the time of some recent travel guides, international services to Belgrade and Thessaloniki had been suspended because of construction works.

The eastern extension of Corridor VIII is the largest unfinished rail project. A 31 km line from Kumanovo to Beljakovce was restored after earlier work, and a further section from Beljakovce to Kriva Palanka was started in 1996 but abandoned in 2004 for lack of money. Contracts were signed in 2022. A 2024 tender covered 23.4 km of new track with 22 tunnels and 52 bridges through difficult mountain terrain, and completion has been projected between 2027 and 2030, although earlier timelines slipped. Financing has come from international lenders: the EBRD provided a €110 million loan for a Corridor VIII section in 2021, and a €560 million package for a later phase was announced in 2023. Officials have also noted that the western section, from Kičevo to the Albanian border, lacks connections, and that Bulgaria has no planned rail link to the country's eastern border.

Airports and border crossings

Skopje International Airport is the main air gateway, and Ohrid St. Paul the Apostle Airport, about 9 km northwest of Ohrid, serves as a second airport mainly for tourists. Both are operated by TAV Macedonia. Together they handled about 3.15 million passengers in 2023, above the 2019 peak of roughly 2.7 million, and Wizz Air carried the largest share of Skopje traffic. The Ohrid runway is about 2,550 m long, which limits it to small and medium aircraft. Road border crossings and rail frontiers with Greece, Serbia, Bulgaria, Kosovo and Albania connect the country to its neighbours, and their capacity affects the flow of goods along both corridors.

Terrain and strategic significance

The Vardar valley provides the main natural route, and motorways run within it along most of the river's length to near Skopje. Away from the valley, the mountains make construction costly. The Kriva Palanka section needed extensive tunnelling and bridging, and the government has also funded slope stabilisation on the express road in the same area. Military planning has added a further dimension: in July 2024, a letter of intent at the NATO summit in Washington committed Italy, Albania, North Macedonia and Bulgaria to harmonised military mobility corridors along Corridor VIII. These projects link the country's infrastructure to regional security and to the economic development of the western Balkans.

Political geography and external relations

North Macedonia is organised into municipalities, and one listing gives 80 opštini (sing. opština: municipalities). The capital, Skopje, is governed as a separate unit. The City of Skopje is an administrative division within the Republic of North Macedonia constituted of 10 municipalities, namely Aerodrom, Butel, Centar, Čair, Gazi Baba, Ǵorče Petrov, Karpoš, Kisela Voda, Saraj and Šuto Orizari. The 2021 census counted 526,502 residents in the City of Skopje area. The Assembly sits in the Centar municipality, which is home to the Assembly of North Macedonia. For statistical purposes, the capital belongs to the Skopje Statistical Region, one of the 8 Statistical Regions, they are for legal and statistical purposes.

The country's foreign policy has been organised around Euro-Atlantic integration. The main obstacle to NATO membership was the naming dispute with Greece, since Athens opposed the use of the name "Macedonia" by its northern neighbour because the Greeks claimed that it related to the Greek heritage associated with Alexander of Macedon. The Greek objection kept the question of membership open until a settlement was reached. Allies signed the accession protocol on 6 February 2019, and the Accession Protocol was subsequently ratified by each of the 29 Allies according to national procedures. The country formally joined on 27 March 2020, when the United States, as a treaty depositary, received The Republic of North Macedonia's instrument of accession to the North Atlantic Treaty, making North Macedonia the 30th NATO Ally. Its armed forces are small; one assessment puts active military strength of approximately 8,000 personnel. The country has also contributed to alliance operations, as the country has provided valuable support to NATO-led operations and missions in Afghanistan and Kosovo. Membership is also read in regional terms: the accession of Northern Macedonia to NATO means a reduction of Russian military influence in the Western Balkans, according to one commentary.

EU membership has proved far harder to reach. The country has been a candidate since 2005, and over 21 years as a candidate — since 2005 — the country has travelled from hope to a systemic deadlock. Talks were formally approved in March 2020, but in November 2020, Bulgaria effectively blocked the official start of North Macedonia's EU accession negotiations. A 2022 compromise, known as the French proposal, unlocked the process. On 16 July 2022, the Assembly of North Macedonia also approved the revised French proposal, allowing accession negotiations to begin. The start of negotiations was officially launched on 19 July 2022. The central dispute concerns constitutional recognition: Sofia made this conditional upon listing Bulgarians among the national minorities in the preamble to the constitution. Skopje has resisted this step, and fears that such a concession would merely prompt further demands from Sofia. Under the government elected in 2024, new PM Mickoski rejects constitutional amendments. In the most recent cycle, not a single negotiating chapter opened, and in November 2025 the EU Enlargement Package set no date for North Macedonia. In September 2026, Bulgarian politicians also tied the case to a criminal trial involving a dual citizen, and Bulgarian members of the European Parliament asked the European Commission to include it in its rule-of-law monitoring of accession process of North Macedonia.

Relations with neighbours are shaped by these same disputes. The name conflict with Greece lasted from independence in 1991, and resulted in a Greek veto against EU and NATO accession talks, which lasted from 2008 to 2019. The 2018 Prespa Agreement ended that standoff, as discussed in the naming section. Relations with Bulgaria remain the most politically sensitive, since Bulgaria, which has been an EU member since 2007, had insisted that North Macedonia formally recognize its language had Bulgarian roots. The EU track also linked the country to Albania. In 2024 Albania "decoupled" from North Macedonia in the accession process, and Bulgaria has argued that Albania should be considered independent from North Macedonia, based on its achievements. The border with Albania and the large Albanian-speaking population in the north and in Skopje make the country's internal politics closely tied to Tirana. Relations with Kosovo, which North Macedonia recognised in 2008, and with Serbia, are shaped by the post-Yugoslav settlement and by the regional legacy of the Yugoslav breakup.

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121. Mavrovo National Park. - Macedonian Encyclopediaen.macedonism.org
122. List of national parks in North Macedoniaen.wikipedia.org
123. Ohrid and its lake, a UNESCO heritage in danger - OBCTbalcanicaucaso.org
124. Report Name:Overview of North Macedonian ...apps.fas.usda.gov
125. Introduction & Objectives North Macedonia - Ecosystem Services Partnershipes-partnership.org
126. Vardar River Travel Guidemacedoniatourism.com
127. Skopje Basinen.wikipedia.org
128. (PDF) Regional specifics of Macedonian agricultureacademia.edu
129. Agriculture in North Macedoniaen.wikipedia.org
130. Cloud-Based Mapping of Soil Erosion Susceptibility for Catchment Prioritisation in the Western Balkans Using a Modified Erosion Potential Methoddoi.org
131. 2021 STATE OF THE ART OF SOIL MANAGEMENT IN THE WESTERN BALKANSseerural.org
132. Building a shield against flooding in vulnerable areas of North Macedoniaunep.org
133. WP1 Analysis of soil erosion state and torrential floods ... - Setofsetof.org
134. North Macedonia - CIF Countriescif.org
135. North Macedonia - Farming, Livestock, Cropsbritannica.com
136. Soil legislation in North Macedoniaseerural.org
137. (PDF) Hydrogeological survey of Groundwater in Macedoniaresearchgate.net
138. Fresh water resources - Macedoniaclimatechangepost.com
139. Water resources usage in Kosovo and North Macedonia:jwld.pl
140. Preliminary Assessment of Hydrological Heritage in North Macedonia: A Novel Contribution to Geodiversity Protectionlink.springer.com
141. Home - Програма за водиprogramazavodi.mk
142. Numerical Modelling of Urban Air Pollution from Residential Heating: A Case Study of Skopjedoi.org
143. Major New Survey of Household Heating Identifies Some Key Causes of Skopje’s Soaring Levels of Pollutionundp.org
144. pmc.ncbi.nlm.nih.govpmc.ncbi.nlm.nih.gov
145. Skopje Among World's Most Polluted Cities: Air Quality Crisis in North Macedoniaocnal.com
146. (PDF) Sensitivity of ancient Lake Ohrid to local anthropogenic impacts and global warmingresearchgate.net
147. (PDF) Evaluation of the Water Quality of the Ohrid Lake (Albanian Part) Compared to the International Standardsresearchgate.net
148. Discussion Paperbg.copernicus.org
149. Sewage and wastewater pollute Lake Ohrid, but its waters remain safe for swimmingmeta.mk
150. graphsearch.epfl.chgraphsearch.epfl.ch
151. 2021 North Macedonia censusen.wikipedia.org
152. Albanians in North Macedoniaen.wikipedia.org
153. Demographics of North Macedoniaen.wikipedia.org
154. North Macedonia Census Reveals Big Drop in Populationbalkaninsight.com
155. North Macedonia, the census does not quell the controversy - OBCTbalcanicaucaso.org
156. Skopje Statistical Regionen.wikipedia.org
157. List of municipalities in North Macedonia by populationen.wikipedia.org
158. North Macedonia Demographics 2026 (Population, Age, Sex, Trends) - Worldometerworldometers.info
159. North Macedonia Population (2026) - Worldometerworldometers.info
160. Macedonia MK: Urban Population: % of Total Populationceicdata.com
161. North Macedonia - Population and Demography Country Profileourworldindata.org
162. (PDF) MIGRATION AS A FACTOR IN THE TRANSFORMATION OF RURAL MUNICIPALITIES - THE CASE OF NORTH MACEDONIAresearchgate.net
163. Exploring North Macedonia's Population Density - Earth Site Educationearth-site.co.uk
164. Macedonian Questionbritannica.com
165. Balkan Warsbritannica.com
166. Macedonia (04/08) - State.gov2009-2017.state.gov
167. The Balkan Wars and the Partition of Macedonia, 1912-1913brewminate.com
168. North Macedonia History • FamilySearchfamilysearch.org
169. Macedonia, Northern Parttib.oeaw.ac.at
170. Pelagonia Statistical Regionen.wikipedia.org
171. Socialist Republic of Macedoniasimple.wikipedia.org
172. Socialist Republic of Macedoniaen.wikipedia.org
173. Breakup of Yugoslaviaen.wikipedia.org
174. New expressway boosts North Macedonia’s connectivitywbif.eu
175. Pan-European Corridor VIIIen.wikipedia.org
176. Road networkroads.org.mk
177. North Macedonia Political Briefing: From Stalled to Strategic: Macedonia’s Bold New Transport..china-cee.eu
178. Progress in the construction of several sections of the Pan-European Railway Corridors VIII and X in North Macedonia, a project supervised by IRD Engineeringirdeng.com
179. North Macedonia and European Transport Corridors - The Western Balkansthewesternbalkans.com
180. Trains in North Macedonia: tickets, routes & rail passeseveryrail.com
181. North Macedonia By Traineurail.com
182. Trains in North Macedoniainterrail.com
183. Veles railway stationen.wikipedia.org
184. economic-geographical characteristics of the rail traffic in ...ojs.ikm.mk
185. Ohrid St. Paul the Apostle Airporten.wikipedia.org
186. 3.15 million passengers in 2023 at Skopje and Ohrid airportsskp.airports.com.mk
187. Republic of North Macedonia Municipalitiesstatoids.com
188. City of Skopje - Wikidatawikidata.org
189. City of Skopje (North Macedonia): City Municipalities - Population Statistics, Charts and Mapcitypopulation.de
190. Centar Municipality, Skopjeen.wikipedia.org
191. Administrative Map of Macedonia - Nations Online Projectnationsonline.org
192. North Macedonia as the 30th NATO memberwarsawinstitute.org
193. Relations with the Republic of North Macedonia (Archived)nato.int
194. North Macedonia Joins the NATO Alliance - United States Department of State2017-2021.state.gov
195. North Macedonia: A New Member State and an Opportunity for NATOrusi.org
196. The Bulgarian Veto: How One EU Member State Blocked the Future of Two Million People — Bulgaria Watchbulgariawatch.fyi
197. Accession of North Macedonia to the European Unionen.wikipedia.org
198. Waiting for Godot: Prospects for resolving the Bulgaria–North Macedonia disputeosw.waw.pl
199. North Macedonia risks new Bulgaria veto?europeanwesternbalkans.com
200. mil 220624 rferl03globalsecurity.org
201. First Intergovernmental Conference with the EU/ Bulgaria does not give up its veto on North Macedonia and requests: To separate the process for Albaniabalkanweb.com
202. mil 210521 rferl02globalsecurity.org
203. Sopi%C5%A1te Municipalityen.wikipedia.org
204. NATO - News: North Macedonia joins NATO as 30th Ally, 27-Mar.-2020nato.int