A map of Greece outlines a highly fragmented, peninsular Mediterranean country situated at the crossroads of Europe, Asia, and Africa in Southeastern Europe. Occupying the southern tip of the Balkan Peninsula, Greece is bordered by Albania, North Macedonia, and Bulgaria to the north, and Turkey to the northeast. The national territory is defined by an extensive coastline stretching across 13,676 kilometers, flanked by the Ionian Sea to the west, the Mediterranean Sea to the south, and the Aegean Sea to the east. The country comprises a mountainous continental mainland, the distinct Peloponnese peninsula connected via the narrow Isthmus of Corinth, and an expansive network of thousands of islands scattered across the Mediterranean basin.
In this definitive geographic guide, you will gain an elite-level understanding of the map of Greece, its administrative divisions, and its intricate physical landscapes. We will survey the core continental areas, trace the distinct borders of the nine historical geographic regions, and break down the complex island groups that dominate the maritime charts. Additionally, you will discover practical navigation strategies for planning land or sea routes, evaluate regional transportation corridors, and test your knowledge with a comprehensive frequently asked questions section. Whether you are an academic researcher, a student of classical antiquity, or a traveler mapping out a Mediterranean voyage, this guide provides an authoritative reference.
Macro-Geographic Location and Borders
On a global political map, Greece occupies a highly strategic geopolitical position at the southern edge of the Balkan landmass, forming the easternmost maritime gateway of the European Union. The country lies approximately between latitudes 34° and 42° N, and longitudes 19° and 30° E. This coordinates set places Greece at a critical historical crossroads where major overland trading paths and maritime shipping lanes converge. The sovereign territory encompasses 131,957 square kilometers, combining a rocky continental landmass with a vast maritime exclusive economic zone that touches multiple maritime basins.
Greece shares precise international land borders with four distinct sovereign states along its rugged northern frontier, totaling approximately 1,228 kilometers of land boundaries. Its westernmost land border is shared with Albania, extending across 282 kilometers through the mountainous Epirus hinterland down to the Ionian coast. To the north, Greece shares a 246-kilometer border with North Macedonia, running through deep river valleys and tectonic lakes. The longest northern land border is shared with Bulgaria, tracking along 494 kilometers of the high Rhodope mountain crests, while the northeastern border with Turkey follows the natural course of the Evros River for 206 kilometers.
The Nine Geographic Regions
The internal map of Greece is traditionally divided into nine distinct historical-geographic regions, which reflect the country’s ancient tribal divisions, Byzantine administrative boundaries, and modern cultural identities. These regions should not be confused with the contemporary peripheries utilized for European Union administrative funding; instead, they represent the timeless geographic blocks that have defined Greek statehood since the 19th century.
[ MAP OF GREECE: TOPOGRAPHIC PROFILE ]
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[Macedonia & Thrace] [Epirus & Thessaly] [Central Greece] [The Peloponnese] [Island Groups]
(High northern (Rugged peaks & (Attica, Athens & (Southern historic (Aegean, Ionian
continental basins) agricultural plains) cultural heart) peninsula matrix) & Crete blocks)
Macedonia
Macedonia stands as the largest geographic region of Greece, dominating the northern third of the national map. This vast territory is defined by fertile river basins, including the Axiós and Strymónas valleys, and is bordered by high alpine ranges that separate Greece from its northern neighbors. The regional economy is anchored by Thessaloniki, a historic port city that serves as the second-largest urban center on the map of Greece. Topographically, western Macedonia features rugged, landlocked highlands, whereas central and eastern Macedonia slope gently toward the Thermaic and Strymonic Gulfs.
Thrace
Situated in the far northeastern corner of the map, Western Thrace forms the land bridge connecting Europe directly to the Anatolian landmass of Asia. This region is geographically isolated from western Greece by the Nestos River and bounded to the east by the wide Evros River floodplain along the Turkish border. The landscape alternates between the dense forests of the southern Rhodope Mountains and a fertile coastal plain facing the North Aegean Sea. Thrace contains a unique cultural tapestry, with historic towns like Komotini and Alexandroupoli serving as vital trade hubs and transit points for international energy pipelines.
Epirus
Epirus occupies the northwestern corner of the Greek mainland, nestled tightly between the high Pindus mountain range and the clear waters of the Ionian Sea. It represents the most mountainous and heavily forested region on the map of Greece, characterized by deep limestone canyons, rushing rivers, and high alpine plateaus. The capital city, Ioannina, sits along the shores of Lake Pamvotis, surrounded by historic stone-built villages that were isolated from the rest of Greece for centuries due to the harsh terrain. Epirus receives the highest annual rainfall in the country, which feeds major river systems like the Achelous and Louros.
Thessaly
Thessaly forms the central core of continental Greece, framed by the Pindus Mountains to the west, Mount Olympus to the north, and the Aegean Sea to the east. The defining geographic feature of Thessaly is its massive, flat central plain, which acts as the primary agricultural breadbasket for the Greek nation, producing grain, cotton, and livestock. This region is divided into northern and southern basins, which are drained by the Pineios River through the narrow Vale of Tempe. Rising abruptly from the flat northwestern plain are the striking sandstone pillars of Meteora, which support ancient monastic communities.
Central Greece
Central Greece, traditionally known in Greek as Sterea Ellada, covers the southern expansion of the continental mainland directly north of the Peloponnese. This region functions as the administrative and historical heart of the modern Greek state, housing the sprawling metropolitan area of Athens within the Attica peninsula. The geography of Central Greece is highly complex, featuring high peaks like Mount Parnassus, deep gulfs, and the elongated island of Euboea, which runs parallel to the mainland coast. This region controls critical transit routes, including the historic mountain pass of Thermopylae and the modern Boeotian highway network.
The Peloponnese
The Peloponnese is a large peninsula that forms the southernmost tip of the Greek mainland, shaped like a giant, four-fingered leaf extending into the Mediterranean Sea. It is technically an island today, separated from Central Greece by the artificial Corinth Canal, which was cut through the narrow Isthmus of Corinth in 1893. The interior of the Peloponnese is a rugged maze of high limestone mountains, including the Taygetos range, which yield to fertile coastal valleys famed for olive and citrus cultivation. The regional map is dotted with world-renowned archaeological sites like Mycenae, Olympia, and Sparta.
The Ionian Islands
The Ionian Islands, collectively known in Greek tradition as the Heptanese (the Seven Islands), form a distinct maritime chain running down the western coast of Greece. Unlike the dry, wind-swept islands of the Aegean Sea, the Ionian group benefits from high rainfall, resulting in lush green pine forests and extensive olive groves. The main islands include Corfu in the north, Paxos, Lefkada, Ithaca, Kefalonia, and Zakynthos, with Cythera situated far to the south off the tip of the Peloponnese. These islands have a unique architectural and cultural identity shaped by centuries of Venetian, French, and British rule.
The Aegean Islands
The Aegean Islands encompass a vast, dense archipelago of thousands of islands scattered across the Aegean Sea between the Greek mainland and Turkey. This maritime region is traditionally subdivided into several distinct clusters based on their geographic location and geological origins: the Cyclades, the Dodecanese, the Sporades, the Saronic Islands, and the North Aegean group. These islands are generally characterized by a dry Mediterranean climate, steep rocky coastlines, and traditional white-washed villages designed to deflect the intense summer sun. The Aegean archipelago forms a crucial bridge for migratory birds and marine life crossing the Mediterranean basin.
Crete
Crete stands as the largest island in Greece and the fifth-largest in the entire Mediterranean Sea, forming a long, narrow southern border for the Aegean basin. Stretching 260 kilometers from west to east, the map of Crete is defined by a massive backbone of four high mountain ranges, including the White Mountains and Mount Ida. These rugged highlands are carved by deep gorges, such as the famous Samaria Gorge, which drop down to fertile northern coastal plains and isolated southern shores. Crete possesses its own distinct cultural, linguistic, and culinary identity, supported by major urban centers like Heraklion and Chania.
Physical Topography and Mountain Chains
The physical map of Greece is dominated by a highly rugged, alpine topography, with mountains covering approximately 80% of the total national territory. This makes Greece one of the most mountainous nations in Europe, featuring a complex geological structure shaped by the ongoing collision of the African and Eurasian tectonic plates. This tectonic activity has created a highly fractured landscape of steep ridges, deep fault valleys, and underground cave systems, while leaving the country prone to frequent seismic activity along its coastal fault lines.
The primary mountain system of the country is the Pindus range, often called the “spine of Greece,” which extends from the Albanian border down through Epirus and Thessaly into Central Greece. The Pindus range is a direct geological extension of the Dinaric Alps, characterized by sharp limestone peaks, dense fir forests, and deep river canyons like the Vikos Gorge. South of the mainland, the Pindus system continues underwater, reemerging to form the rugged mountains of the Peloponnese, the island of Crete, and the underwater ridges of the southern Aegean Sea.
Standing isolated from the central Pindus spine along the border of Macedonia and Thessaly is Mount Olympus, the highest and most famous mountain peak on the map of Greece. Rising abruptly from the Gulf of Thermaos to an elevation of 2,917 meters at its highest peak, Mytikas, Olympus features steep glaciated valleys, high alpine meadows, and volatile weather patterns that inspired ancient Greek mythologists to crown it as the home of the gods. Other prominent mountain peaks include Mount Parnassus in Central Greece (2,457 meters), Mount Taygetos in the Peloponnese (2,404 meters), and Mount Ida on Crete (2,456 meters).
Intricate Coastline and Hydrology
With a total length of 13,676 kilometers, the coastline of Greece is exceptionally long relative to the country’s modest land area, ranking as the eleventh-longest coastline in the world. This high length-to-area ratio is caused by extreme geographical fragmentation, with thousands of deep bays, gulfs, peninsulas, and capes carving the shoreline into an intricate zigzag pattern. No point on the mainland of Greece is located more than 85 kilometers away from the sea, a geographic reality that has bound the history, economy, and culture of the Greek people to maritime pursuits for millennia.
The maritime territory of Greece is divided into several major gulfs and semi-enclosed seas that branch off from the main Mediterranean basin. The largest internal waterway is the Gulf of Corinth, a deep tectonic rift valley that separates the northern mainland from the Peloponnese, connected to the Ionian Sea in the west via the Rio-Antirrio strait. Along the eastern coast, the Aegean Sea is carved into several smaller sub-basins, including the Thermaic Gulf in the north, the Saronic Gulf near Athens, and the deep Sea of Crete to the south, which features depths exceeding 3,000 meters along the Hellenic Trench.
Because the Greek landscape is narrow and mountainous, the country’s river systems are relatively short, fast-flowing, and prone to extreme seasonal changes in water volume. The longest river contained entirely within Greek territory is the Aliakmon, which flows for 297 kilometers from the northern Pindus Mountains into the Thermaic Gulf. Other major river systems, such as the Evros, Strymónas, and Axiós, originate deep within the central Balkan Peninsula and flow southward through Greece to empty into the Aegean Sea. Natural lakes are concentrated in the northern lowlands, with Lake Trichonida in western Greece ranking as the largest natural freshwater basin, covering 98 square kilometers.
Detailed Study of Greek Island Groups
The thousands of islands scattered across the territorial waters of Greece are organized into six primary geographic clusters, plus the independent large island of Crete. These island groups are defined by their unique geological histories, climate profiles, architectural styles, and historic maritime trade patterns.
The Cyclades
The Cyclades form a central circular archipelago in the heart of the Aegean Sea, comprising roughly 220 major islands that encircle the sacred ancient islet of Delos. This group includes some of the world’s most famous tourism destinations, notably Santorini, Mykonos, Naxos, Paros, and Milos. Geologically, the Cyclades are the exposed peaks of an underwater mountain range, with Santorini forming the volatile southern rim of an active volcanic caldera. The islands are globally renowned for their uniform Cycladic architecture, featuring cubic white-washed houses, blue-domed churches, and stone windmills built to withstand the fierce summer Meltemi winds.
The Dodecanese
The Dodecanese cluster consists of 12 principal islands and scores of smaller islets situated in the southeastern Aegean Sea, hugging the southwestern coastline of Turkey. The largest and historically most dominant island in this group is Rhodes, complemented by significant destinations like Kos, Patmos, Leros, and Karpathos. Because of their frontier location along the border between Western Europe and the Ottoman world, the Dodecanese showcase a unique blend of architectural styles, including medieval castles, Ottoman mosques, and Italian rationalist buildings from the early 20th century. The islands feature a warm, semi-arid climate with some of the longest sun exposure periods in Europe.
The Sporades
The Sporades are located off the eastern coast of the Greek mainland, directly north of Euboea, and comprise 24 islands, of which only four are permanently inhabited: Skiathos, Skopelos, Alonnisos, and Skyros. Unlike the dry, rocky landscapes of the southern Aegean, the Sporades are covered in dense Mediterranean pine forests that extend all the way down to the water’s edge. The surrounding maritime waters are exceptionally clean and protected, forming the core of the National Marine Park of Alonnisos, which protects the largest remaining population of the critically endangered Mediterranean monk seal.
The Saronic Islands
The Saronic Islands are nestled within the protected waters of the Saronic and Argolic Gulfs, situated close to the metropolitan coastline of Athens and the Attica peninsula. This cluster includes the historic islands of Salamis, Aegina, Agistri, Poros, Hydra, and Spetses, along with the adjacent Peloponnesian coastal strip. Due to their close proximity to the capital, these islands have served as strategic maritime centers since antiquity; Salamis was the site of the famous naval battle against the Persian Empire in 480 BCE. The islands feature distinct architectural identities, with Hydra and Spetses showcasing preserved stone mansions built by wealthy 18th-century shipping merchant families.
The North Aegean Islands
The North Aegean Islands form a loose, geographically dispersed chain of large, isolated islands situated in the northern and northeastern reaches of the Aegean Sea, running along the maritime border with Turkey. The primary islands in this group include Lesbos, Chios, Samos, Thasos, Samothrace, and Lemnos. Unlike the smaller, clustered archipelagos to the south, these islands are characterized by large land areas, high mountain peaks, and rich agricultural economies that produce unique commodities like the mastic resin of Chios and the sweet Muscat wine of Samos. Samothrace features Mount Saos, which rises 1,611 meters straight out of the sea.
National Reference Matrix
This reference matrix provides accurate data for the key geographic points, high peaks, and maritime zones that define the cartography of Greece.
| Geographic Feature | Type | Key Location / Region | Maximum Elevation / Length | Notable Geological Attribute |
| Mount Olympus | Mountain Peak | Border of Macedonia / Thessaly | 2,917 meters | Highest peak in Greece (Mytikas summit). |
| Pindus Range | Mountain Range | Continental Spine (Epirus to Central) | ~160 kilometers length | Core geological framework of mainland Greece. |
| Aliakmon | River System | Western & Central Macedonia | 297 kilometers | Longest river running entirely within Greece. |
| Evros | Border River | Western Thrace / Turkish Frontier | 480 kilometers total | Forms the natural international boundary line. |
| Lake Trichonida | Freshwater Lake | Aetolia-Acarnania (West Greece) | 98 square kilometers | Largest natural freshwater basin in Greece. |
| Samaria Gorge | Canyon System | Chania Region (Western Crete) | 16 kilometers length | One of the longest canyons in Europe. |
| Hellenic Trench | Ocean Trench | Southern Ionian / Sea of Crete | 5,267 meters depth | Deepest point in the entire Mediterranean Sea. |
Administrative Divisions and Peripheries
The modern administrative map of Greece is organized according to the Kallikratis reform, a major legislative reorganization that took effect on January 1, 2011. This system streamlined the country’s local government by replacing older prefectures with a highly efficient, multi-tier administrative hierarchy. Today, Greece is divided into 13 distinct administrative Peripheries (Regions), which are further subdivided into 74 Peripheral Modules and 332 localized Municipalities. Each periphery is led by an elected Regional Governor and a Regional Council responsible for localized economic development, infrastructure projects, and environmental management.
The 13 Peripheries of Greece cover both mainland and island territories, organizing the country into distinct economic and planning units. The mainland is covered by the peripheries of Western Macedonia, Central Macedonia, Eastern Macedonia and Thrace, Epirus, Thessaly, Central Greece, Western Greece, Attica, and the Peloponnese. The maritime islands are split into four dedicated peripheries: the Ionian Islands, the North Aegean, the South Aegean (which combines the Cyclades and Dodecanese clusters), and the independent island periphery of Crete. Attica is by far the most populous periphery, housing over one-third of the nation’s total population within the Athens urban area.
Standing completely outside this standard administrative structure is the monastic community of Mount Athos, situated on the easternmost prong of the Chalcidice peninsula in Central Macedonia. Known officially as the “Autonomous Monastic State of the Holy Mountain,” this ancient religious enclave has enjoyed complete self-governance since the Byzantine era, a status explicitly protected by modern international treaties and the Greek Constitution. Mount Athos operates under its own spiritual charter, led by a Holy Community of representatives from its 20 sovereign Eastern Orthodox monasteries, and maintains a strict century-old ban on entry for women and female domesticated animals.
Transportation Corridors and Navigation
The complex topography of the Greek map has required the development of an advanced multimodal transportation network designed to connect isolated mountain communities and distant island archipelagos to the main economic centers. The backbone of mainland transport is the Egnatia Odos highway, a massive engineering project completed in 2009 that spans 670 kilometers across northern Greece from the port of Igoumenitsa on the Ionian Sea to the Turkish border in Thrace. This modern toll highway follows the path of the ancient Roman Via Egnatia, utilizing 73 advanced tunnels and 177 bridges to cross the high Pindus and Rhodope mountain chains.
Connecting northern and southern Greece is the PATHE motorway network, an acronym for Patras-Athens-Thessaloniki-Evzonoi. This north-south highway corridor runs along the eastern coast of the mainland, linking the country’s largest urban areas and industrial zones before reaching the main border crossing into North Macedonia. For rail transport, the Hellenic Railways Organisation (OSE) operates a modernized main line connecting Athens and Thessaloniki, utilizing high-speed passenger trains that travel between the two cities in under four hours through advanced mountain tunnels beneath Mount Othrys.
For maritime transport, the port of Piraeus, located just southwest of Athens, serves as the primary maritime gateway for the map of Greece and ranks as one of the largest passenger ports in Europe. From Piraeus, a vast network of commercial ferry lines spreads out across the Aegean Sea, operating high-speed catamarans and large roll-on/roll-off vehicle ferries that keep island communities connected year-round. Air transport is managed through a network of 45 airports, anchored by Athens International Airport (AIA “Eleftherios Venizelos”), which coordinates international arrivals with domestic flights to specialized island airstrips equipped with short runways designed for challenging island terrain.
Practical Information and Planning
Entry Gateways and Pricing
For international travelers and geographers planning an overland or maritime expedition across the map of Greece, understanding entry logistics and associated costs is essential:
Principal Airports: Most long-haul international visitors arrive at Athens International Airport (ATH) or Thessaloniki Airport (SKG). Round-trip international flights from major European capitals range from €80 to €350 depending on the season, while domestic flights connecting Athens to islands like Santorini or Rhodes typically cost between €40 and €150.
Maritime Ferry Corridors: Ferries depart daily from the main ports of Piraeus, Rafina, and Lavrio. Standard economy ferry tickets from Piraeus to the central Cyclades (e.g., Paros or Naxos) cost approximately €40 to €60 one-way on conventional ships, whereas high-speed catamaran tickets cost between €70 and €90 one-way.
Mainland Toll Highways: Driving across the main continental motorways (Egnatia Odos or PATHE) involves passing several automated toll plazas. Total toll costs for a passenger car traveling from Athens to Thessaloniki total roughly €30, with fuel costs adding an additional €70 to €90 based on regional European fuel pricing.
Rules for Safe Navigation
Navigating through the diverse terrains of the Greek mainland and island archipelagos requires adhering to strict safety guidelines and transport regulations:
International Driving Permits: Visitors holding non-EU driver’s licenses must secure an International Driving Permit (IDP) alongside their domestic license before renting a vehicle. Local car rental rates range from €25 per day in winter to over €80 per day during the peak summer tourist rush.
Island Nautical Regulations: Renting a small motorized boat under 30 horsepower does not require a formal marine license on most Greek islands, but operators must stay within 1-2 nautical miles of the shore. Chartering larger sailing yachts requires a certified skipper or a verified International Certificate of Competence (ICC).
Mountain Hiking Protocol: When exploring wilderness trails in the Pindus range or climbing Mount Olympus, hikers must stick to marked European long-distance paths (E4 trail network). Mountain weather can change abruptly, making it vital to check forecasts from the Hellenic National Meteorological Service (HNMS) before setting out.
Seasonal Climatic Mapping
The climate map of Greece is divided into three distinct regional weather zones that are heavily influenced by the country’s rugged topography and surrounding seas. The coastal mainland and most island groups experience a classic Mediterranean climate, characterized by mild, wet winters and hot, dry summers with prolonged sun exposure. During July and August, the Aegean Sea experiences the Meltemi, a powerful, dry northern wind that blows continuously for days, providing natural cooling for the islands but occasionally disrupting local ferry schedules and creating challenging conditions for amateur sailors.
In contrast, the high interior peaks of the Pindus range and Mount Olympus fall within an Alpine climate zone. These mountain areas experience harsh, cold winters with heavy snowfall that feeds several popular ski resorts, including Mount Parnassus and Velouxi, which stay active from December through April. Summers in the alpine zone are brief and cool, with regular afternoon thunderstorms. Finally, the lowlands of interior Macedonia and Thrace feature a Temperate Continental climate, showing much larger temperature swings between winter and summer, along with higher humidity and more frequent rainfall than the coastal regions down south.
Frequently Asked Questions
What are the main seas surrounding the map of Greece?
The map of Greece is surrounded by three primary branches of the Mediterranean Sea: the Ionian Sea to the west, the Mediterranean Sea proper to the south, and the Aegean Sea to the east. Additionally, the southern section of the Aegean between Crete and the Cyclades is known as the Sea of Crete.
How many islands are included on the map of Greece?
The territorial waters of Greece contain between 1,200 and 6,000 islands and islets depending on the minimum size threshold used for counting. Of these thousands of islands, only 227 are permanently inhabited by residents, with a mere 53 islands supporting populations of over 1,000 people.
What is the longest river shown on the map of Greece?
The longest river contained entirely within Greek territory is the Aliakmon, which flows for 297 kilometers from the northern Pindus Mountains to empty into the Thermaic Gulf. However, the longest river that passes through Greece is the Maritsa (known in Greek as the Evros), which flows for 480 kilometers total, originating in Bulgaria before forming the border between Greece and Turkey.
Where is the deepest point on the map of Greece?
The deepest point on the map of Greece—and the entire Mediterranean Sea—is Calypso Deep, located in the Ionian Sea southwest of the Peloponnese along the Hellenic Trench. Calypso Deep reaches a maximum depth of 5,267 meters ($17,280\text{ feet}$) below sea level, where the African tectonic plate dives beneath the Eurasian plate.
Why is Crete separated from the rest of the Greek island groups?
Crete is classified as its own independent geographic region because of its exceptional size, distinct geological history, and unique cultural identity. Measuring 260 kilometers long, Crete is the largest island in Greece and forms a natural southern border for the entire Aegean basin, separating it from the open Libyan Sea.
What is the Corinth Canal on the map of Greece?
The Corinth Canal is an artificial waterway cut through the narrow Isthmus of Corinth in 1893, separating the Peloponnese peninsula from the central Greek mainland. The canal measures 6.4 kilometers long and only 21.4 meters wide, creating a vital maritime shortcut that allows small commercial ships and yachts to transit between the Gulf of Corinth and the Saronic Gulf.
What is the highest mountain peak on the map of Greece?
The highest mountain peak in Greece is Mount Olympus, situated on the border between the regions of Macedonia and Thessaly. Its highest summit, Mytikas, reaches an elevation of 2,917 meters ($9,570\text{ feet}$) above sea level, featuring steep cliffs and alpine valleys that inspired ancient Greek storytellers to declare it the home of the Olympian gods.
How are the Greek islands divided into groups?
The Greek islands are organized into six distinct geographic clusters based on their location and geological history: the Cyclades (central Aegean circle), the Dodecanese (southeastern frontier), the Sporades (forested eastern group), the Saronic Islands (protected coastal bays), the Ionian Islands (lush western chain), and the North Aegean Islands, along with the independent island of Crete.
Which administrative periphery has the largest population on the map?
The periphery of Attica has by far the largest population on the map of Greece, housing over 3.8 million residents. This single periphery contains the entire Athens metropolitan area, concentrating more than one-third of the nation’s total population within a compact peninsula in Central Greece.
What is the special status of Mount Athos on the map?
Mount Athos, located on the easternmost prong of the Chalcidice peninsula in northern Greece, is an autonomous monastic state that enjoys complete self-governance under the spiritual authority of the Ecumenical Patriarchate of Constantinople. The enclave has its own entry permits and maintains a strict, centuries-old legal ban prohibiting women and female animals from entering its territory.
What highway connects western and eastern northern Greece?
The primary transport corridor across northern Greece is the Egnatia Odos highway (A2), a modern toll motorway that stretches 670 kilometers from the Ionian port of Igoumenitsa to the Turkish border at Evros. This major highway runs across the regions of Epirus, Macedonia, and Thrace, utilizing a vast network of tunnels to cut through the Pindus range.
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