Turkey is one of the clearest plateau countries on a physical map. Much of Anatolia sits as raised interior land between the Pontic Mountains in the north and the Taurus Mountains in the south. That high interior is not one flat slab. It is a broken set of plateaus, basins, volcanic fields, karst uplands, steppe plains, river valleys, and mountain-rimmed highlands.

The main Turkish plateau regions include the Central Anatolian Plateau, the Eastern Anatolian Plateau, the Erzurum-Kars Plateau, the Southeastern Anatolian plateaus, the Taurus karst plateaus, and the inner western Anatolian uplands. Together, they shape climate, farming, settlement, river flow, road routes, and the way Turkey connects coastal lowlands with high interior terrain.

Major plateau regions in Turkey, with approximate elevation ranges and main landform traits.

Plateau Region	Main Location	Approximate Elevation	Landform Type	Known For
Central Anatolian Plateau	Interior Anatolia; around Ankara, Konya, Kayseri, Nevşehir, Aksaray, Sivas	Often about 900–1,200 m; some uplands rise higher	Orogenic plateau with basins, volcanic fields, and steppe plains	Tuz Gölü Basin, Konya Basin, Cappadocia, Kızılırmak River bends
Eastern Anatolian Plateau	Eastern Turkey; around Erzurum, Kars, Ağrı, Van, Muş, Bitlis	Commonly about 1,500–2,200 m; local surfaces are higher	High tectonic and volcanic plateau	Cold highlands, Lake Van Basin, volcanic mountains, headwaters of major rivers
Erzurum-Kars Plateau	Northeastern Anatolia	Roughly around 2,000–2,500 m in many high surfaces	Volcanic high plateau	Open grasslands, lava-covered terrain, Aras and Kars river systems
Southeastern Anatolian Plateaus	Gaziantep, Kilis, Adıyaman, Şanlıurfa, Mardin, Diyarbakır uplands	Often about 500–1,000 m, with higher limestone ridges in places	Limestone and basalt plateaus on the northern edge of the Arabian Platform	Euphrates and Tigris basins, rolling dry uplands, Mardin-Midyat limestone country
Taurus Karst Plateaus	Southern Turkey; Taşeli, Teke, Lake District, inner Taurus uplands	Often about 1,000–2,000 m depending on the surface	Limestone karst plateau	Dolines, poljes, caves, sinkholes, underground drainage, steep Mediterranean margins
Inner Western Anatolian Uplands	Afyonkarahisar, Kütahya, Uşak, Eskişehir, inner Aegean transition zone	Mostly about 800–1,200 m	Broken plateau and basin terrain	Transition from Aegean grabens to Central Anatolia, volcanic hills, headwater zones
Pontic Highland Plateaus and Yayla Surfaces	Black Sea mountain belt; especially inner and eastern Pontic highlands	Often about 1,500–2,500 m in high pasture zones	Mountain plateau surfaces, benches, and upland pastures	Humid slopes, high meadows, short summer grazing zones, steep river valleys

---

Why Turkey Has So Many Plateaus

Turkey sits where several large landform belts meet. The country is bordered by seas, but much of the land rises quickly inland. Coastal plains are narrow in many places, while the interior stands high, dry, and open.

The Anatolian Plateau is the broad raised heart of this pattern. It is easiest to see on a map as the high interior between the Black Sea mountains and the Taurus range. Yet it is better understood as a mosaic of plateau surfaces, not as a single smooth tableland.

Several processes shaped this terrain:

• Tectonic uplift raised large parts of Anatolia above nearby coastal lowlands.
• Mountain building along the Pontic and Taurus belts created high rims around the interior.
• Volcanism added lava flows, ash deposits, cones, and volcanic plateaus in central and eastern Turkey.
• Karst weathering carved limestone plateaus in the Taurus and southeastern uplands.
• River erosion cut valleys, canyons, and basins into older plateau surfaces.
• Closed basins formed where water collects inland instead of reaching the sea easily.

This mix explains why one Turkish plateau may look like steppe, another like volcanic grassland, and another like limestone country full of sinkholes.

How to Read Turkish Plateaus on a Map

On a physical map of Turkey, plateaus usually appear as broad high zones between darker mountain belts and lower coastal or river plains. The raised interior is clearest in central and eastern Anatolia.

A simple map-reading rule helps: look for wide high land, not just flat land. A plateau can include low hills, basins, volcanic cones, river gorges, salt flats, and dry plains. It does not need to be perfectly level.

The main plateau pattern can be read in three bands:

1. Central interior: broad plateau basins, dry steppe, salt lakes, volcanic fields, and long river bends.
2. Eastern highlands: higher, colder plateaus with volcanoes, lakes, and river headwaters.
3. Southern and southeastern margins: limestone and basalt plateaus that step down toward the Mediterranean, Mesopotamian plains, and Syria.

---

Central Anatolian Plateau

The Central Anatolian Plateau is the main plateau core of Turkey. It covers much of the interior around Ankara, Konya, Kayseri, Nevşehir, Aksaray, Kırşehir, Niğde, Yozgat, and Sivas. It lies between the Pontic Mountains to the north and the Taurus Mountains to the south.

This region is often described as roughly 900 to 1,200 meters above sea level, although uplands, volcanic cones, and mountain margins rise higher. Its surface is broad, dry, and open compared with the coastal belts.

Main Features of the Central Anatolian Plateau

• Large basins: Konya Basin, Tuz Gölü Basin, and smaller interior depressions.
• Steppe landscape: dry grassland, grain fields, grazing land, and open horizons.
• Volcanic areas: Cappadocia, Erciyes, Hasan Dağı, Melendiz, and nearby volcanic terrain.
• Salt and closed drainage: Tuz Gölü and other inland basins show how water can collect without a clear outlet to the sea.
• River corridors: the Kızılırmak, Sakarya, and other rivers cut through or rise near plateau terrain.

The plateau is not a plain. It includes rolling uplands, volcanic ash deposits, eroded valleys, and dry basins. In Cappadocia, soft volcanic tuffs were carved by water, wind, and weathering into valleys, cones, and badland-like slopes.

Climate and Human Use

The Central Anatolian Plateau has a continental and semi-arid climate in many areas. Summers are often hot and dry. Winters can be cold, with snow in higher areas. The mountains around the plateau block some sea moisture, so the interior receives less rainfall than many coastal zones.

This climate helps explain the land use. Wheat, barley, sugar beet, grazing, and dryland farming are common in many parts of central Anatolia. Irrigated farming appears where groundwater, rivers, or basin water allows it.

Eastern Anatolian Plateau

The Eastern Anatolian Plateau is Turkey’s highest large plateau belt. It spreads across the eastern part of the country around Erzurum, Kars, Ağrı, Van, Muş, Bitlis, Bingöl, and nearby provinces. Many surfaces sit around 1,500 to 2,200 meters, with higher volcanic mountains rising above them.

This region forms part of the wider highland system between Anatolia, the Caucasus, the Iranian Plateau, and the northern edge of the Arabian Platform. Its relief is more rugged than central Anatolia, but it still contains broad raised surfaces, high basins, lava plateaus, and mountain-rimmed plains.

What Makes Eastern Anatolia Different

Eastern Anatolia is colder, higher, and more broken than the central plateau. It has volcanic highlands, enclosed basins, and major river headwaters. The land does not feel like one continuous flat surface. It feels like a high plateau system cut by valleys and edged by mountains.

Important landform elements include:

• Lake Van Basin: a high inland basin with a large saline lake and volcanic surroundings.
• Erzurum and Kars uplands: broad high surfaces used for grazing and cold-climate farming.
• Volcanic mountains: Ağrı Dağı, Süphan, Tendürek, Nemrut, and other volcanic forms rise above the plateau belt.
• River sources: the Euphrates headwaters, Aras, Kura, Murat, Karasu, and upper Tigris-related systems connect to eastern uplands.

Climate and Landscape

The Eastern Anatolian Plateau has a harsher continental climate. Winters are long and cold. Snow cover can last for months in high areas. Summers are shorter, but high grasslands and meadows become useful grazing zones.

The landscape includes grassland, volcanic rock, high plains, mountain pastures, lake basins, and deeply cut valleys. In many places, elevation affects daily life as much as latitude does.

Erzurum-Kars Plateau

The Erzurum-Kars Plateau is one of the best-known high plateau areas in northeastern Turkey. It is often linked with elevations around 2,000 meters and higher plateau surfaces near the Erzurum, Kars, Ardahan, and Sarıkamış zones.

The plateau has a strong volcanic character. Lava flows and pyroclastic rocks helped build wide surfaces, while later erosion and river cutting shaped valleys and open basins. This is why the region can look both broad and rugged at the same time.

Landscape Traits

• Open high grasslands shaped by cold climate and short growing seasons.
• Volcanic rock cover across many surfaces.
• River valleys connected with the Aras, Kars, and nearby drainage systems.
• Mountain rims that rise above the plateau and hold snow for long periods.

The Erzurum-Kars Plateau is a good example of a volcanic high plateau. It is not just raised land. It is raised land with a thick volcanic story written into the rock surface.

Southeastern Anatolian Plateaus

Southeastern Turkey has lower plateaus than eastern Anatolia, but they are very important for the country’s landform map. These plateaus stretch across parts of Gaziantep, Kilis, Adıyaman, Şanlıurfa, Mardin, Diyarbakır, Batman, and Siirt.

The region sits near the northern edge of the Arabian Platform and slopes toward the Syrian and Mesopotamian lowlands. Elevations often range from about 500 to 1,000 meters, though limestone ridges and upland shoulders can rise higher.

Main Plateau Areas in the Southeast

• Gaziantep Plateau: a low, rolling plateau around Gaziantep, Kilis, and Adıyaman, with surfaces that step down toward the south and east.
• Şanlıurfa Plateau: broad dry uplands and plains linked with the Euphrates drainage and Harran Plain surroundings.
• Mardin-Midyat Plateau: limestone uplands above the Mesopotamian plain, with slopes, valleys, and stone-built settlements shaped by local rock.
• Diyarbakır-Batman uplands: plateau and basin terrain connected to the upper Tigris system.

These plateaus are warmer and drier than central and eastern Anatolia. They connect upland Anatolia with lower lands to the south. Their rivers, especially the Euphrates and Tigris, give the region strong basin identity.

Why Limestone and Basalt Matter Here

Much of southeastern plateau terrain is shaped by limestone, basalt, or both. Limestone can form dry valleys, springs, caves, and karst features. Basalt flows create dark rocky surfaces and resistant caps. Together, these rocks influence soil, water storage, settlement patterns, and building stone.

Taurus Karst Plateaus

The Taurus Mountains form the southern rim of Anatolia, but they also contain broad karst plateaus. These are not smooth steppe surfaces like central Anatolia. They are limestone uplands shaped by water moving through soluble rock.

Important Taurus plateau areas include the Taşeli Plateau, parts of the Teke Plateau, the Lake District uplands, and inner limestone surfaces behind the Mediterranean coast. Many of these areas sit roughly between 1,000 and 2,000 meters, with local variation.

Typical Karst Plateau Features

• Dolines: closed hollows formed by solution or collapse.
• Poljes: larger flat-floored karst basins that may hold seasonal water or fertile soil.
• Sinkholes: openings where water drains underground.
• Dry valleys: former or seasonal drainage lines on limestone surfaces.
• Caves and springs: signs that water is moving through underground channels.

Karst plateaus can look dry at the surface even when water is active below ground. This makes them different from river-cut plateaus, where surface streams are more visible.

Inner Western Anatolian Uplands

Inner western Anatolia forms a transition zone between the Aegean graben valleys and the central plateau. It includes upland areas around Afyonkarahisar, Kütahya, Uşak, Eskişehir, and nearby districts.

This region is more broken than the Central Anatolian Plateau. It has basins, volcanic hills, ridges, plains, and river headwaters. Elevations commonly sit around 800 to 1,200 meters, but local mountains and volcanic areas rise above that.

Why This Region Matters

The inner western uplands help explain how Turkey shifts from coastal Aegean valleys into inland Anatolia. West-flowing rivers such as the Gediz and Büyük Menderes are linked with the Aegean side, while the Sakarya and Porsuk connect toward the north and interior.

This makes the area a landform bridge: not coastal lowland, not deep central steppe, and not eastern high plateau. It is a mixed upland region where basins and plateau remnants sit close together.

Pontic Highland Plateaus and Yayla Surfaces

The Black Sea region is usually known for steep mountains, wet slopes, forests, and short coastal plains. Yet high plateau-like surfaces and yayla landscapes are common in the Pontic Mountains, especially in the eastern Black Sea highlands.

These areas are different from the Central Anatolian Plateau. They are often narrow, elevated, and close to steep valleys. Many are seasonal pasture lands rather than broad landform plateaus.

How They Differ from Interior Plateaus

Interior plateaus and Black Sea yayla surfaces differ in shape, climate, and land use.

Feature	Interior Plateaus	Pontic Yayla Surfaces
Main setting	Broad inland highlands and basins	High mountain benches, ridges, and pasture surfaces
Climate pattern	Often drier and more continental	More humid on windward Black Sea slopes
Landform shape	Wide plateau floors, basins, and steppe plains	Smaller upland flats near steep valleys
Common use	Grain farming, grazing, settlements, roads	Seasonal grazing, highland villages, summer movement
Common confusion	Called “plateau” in a geomorphic sense	Often called yayla, which may or may not be a true plateau

This distinction matters because English “plateau” and Turkish yayla do not always match. A yayla can be a cultural and seasonal land-use term as much as a landform term.

---

Main Rivers and Basins Linked to Turkish Plateaus

Plateaus shape rivers by setting the height from which water starts moving. In Turkey, many rivers either rise on plateaus, cross plateau basins, or cut down through plateau margins on their way to the sea or neighboring lowlands.

Major river and basin links across Turkish plateau regions.

River or Basin	Plateau Connection	Why It Matters
Kızılırmak	Rises in eastern-central Anatolia and bends through the Central Anatolian Plateau	Shows how long rivers can curve across interior highlands before reaching the Black Sea
Sakarya	Linked with inner western and central Anatolian uplands	Connects plateau basins with northwestern Turkey
Konya Basin	Central Anatolian closed basin	Water collects inland; drainage does not work like a normal river-to-sea system
Tuz Gölü Basin	Central Anatolian interior basin	Salt flats and shallow water reflect dry climate and limited outflow
Euphrates Headwaters	Eastern Anatolian Plateau and mountain basins	High snow-fed uplands supply one of Southwest Asia’s major river systems
Tigris Headwaters	Eastern and southeastern highlands	Links Anatolian uplands with southeastern basins
Aras and Kura Systems	Northeastern high plateaus, including Erzurum-Kars uplands	Drain high volcanic and mountain-rimmed terrain toward the Caucasus region
Lake Van Basin	Eastern Anatolian high plateau	An enclosed high basin where water remains inland instead of flowing to the sea
Göksu and Manavgat Systems	Taurus karst plateaus	Show how rivers can cut deep valleys through limestone uplands toward the Mediterranean

How Turkish Plateaus Formed

Turkish plateaus formed through more than one process. The country’s plateaus are best read as a set of uplifted, folded, volcanic, eroded, and karstified surfaces.

Tectonic Uplift and Mountain Rims

Large parts of Anatolia rose as regional tectonic forces shaped the land between the Pontic Mountains, Taurus Mountains, eastern highlands, and nearby plate boundaries. Uplift gave the interior its height. Mountain rims then helped separate coastal climates from inland climates.

Volcanic Construction

Volcanism is clear in central and eastern Turkey. Cappadocia was shaped by volcanic deposits and later erosion. Eastern Anatolia contains broad lava fields and high volcanic mountains. The Erzurum-Kars Plateau is one of the clearest volcanic plateau areas in the country.

Karst Weathering

Limestone plateaus in the Taurus and southeast developed many karst forms. Rainwater and snowmelt dissolve limestone along cracks, bedding planes, and faults. Over time, this creates dolines, caves, underground routes, springs, and enclosed basins.

Erosion and Basin Cutting

Rivers and seasonal streams cut into plateau surfaces. Some basins stayed closed and became salt flats or inland wetlands. Others were captured by river systems and opened toward the sea. This is why Turkish plateaus contain both dry basins and deep valleys.

Climate Differences Across Turkish Plateau Regions

Elevation changes temperature. Mountain rims change rainfall. Distance from the sea changes seasonality. These three controls explain why Turkey’s plateau climates vary so much.

Climate patterns across Turkey’s main plateau regions.

Region	Typical Climate Pattern	Landscape Result
Central Anatolian Plateau	Continental, often semi-arid; cold winters and dry summers	Steppe, dry farming, salt basins, open grazing land
Eastern Anatolian Plateau	High continental; long cold winters and short summers	High meadows, snow-fed rivers, volcanic uplands, lake basins
Southeastern Plateaus	Hot dry summers, cooler winters, lower average elevation than eastern uplands	Dry limestone and basalt uplands, cereal fields, river-basin farming
Taurus Karst Plateaus	Mediterranean influence on slopes; cooler highland conditions inland	Karst hollows, forests in places, dry summer surfaces, strong spring flow
Pontic Yayla Surfaces	Humid Black Sea influence, especially on north-facing slopes	Meadows, forests, steep valleys, short summer grazing season

The same elevation can feel different in different parts of the country. A 1,500-meter plateau surface in the Taurus, a 1,500-meter basin in eastern Anatolia, and a 1,500-meter Black Sea yayla do not share the same rainfall, vegetation, or farming pattern.

---

Plateau, Plain, Highland, Basin, and Yayla: Common Mix-Ups

Turkish geography uses several terms that can overlap in daily speech. For clear map reading, it helps to separate landform shape from land use.

Terms often confused with plateau in Turkish geography.

Term	Simple Meaning	How It Relates to Plateaus
Plateau	Raised land with a broad surface above nearby lower land	The main geomorphic term for much of interior Anatolia
Plain	Low or level land, often with little local relief	A plain can sit inside a plateau basin, but it is not always a plateau
Highland	General term for elevated terrain	Can include plateaus, mountains, ridges, and basins
Basin	Low area that collects sediment or water relative to nearby land	Many Turkish basins sit inside plateau regions, such as Konya and Tuz Gölü
Yayla	Highland pasture or summer settlement area	May sit on a plateau, but the word also describes seasonal use
Escarpment	Steep slope or edge of raised land	Plateau margins often form escarpments or steep valley sides

Which Turkish Plateaus Are Volcanic?

Some Turkish plateaus are strongly volcanic, but not all of them. Volcanic influence is easiest to see in central and eastern Anatolia.

• Cappadocia and central Anatolia: volcanic ash, tuff, ignimbrite, lava, and later erosion created a famous eroded volcanic landscape.
• Erzurum-Kars Plateau: broad volcanic surfaces and lava fields mark this northeastern high plateau.
• Lake Van region: volcanic mountains and lava fields shape much of the basin edge.
• Southeastern basalt areas: basalt flows appear in parts of the southeast, but limestone is also very important there.

Other plateau regions are mainly shaped by limestone, tectonic uplift, basin formation, or river erosion. The best question is not “Is Turkey’s plateau volcanic?” but which part of Turkey’s plateau system is volcanic.

Why Turkish Plateaus Matter in Geography

Turkish plateaus matter because they control many basic patterns on the map. They affect where people live, where rivers begin, which routes are easier to cross, and how climates change from coast to interior.

They Shape Settlement

Many large towns and cities sit in plateau basins, river corridors, or high plains rather than on rugged mountain slopes. Ankara, Konya, Kayseri, Erzurum, Kars, Van, Şanlıurfa, Mardin, and Afyonkarahisar all show different ways people use elevated terrain.

They Shape Farming and Grazing

Dry central plateaus support grain fields and grazing. Eastern high plateaus support colder-climate grazing and shorter growing seasons. Southeastern plateaus combine dry farming, river-basin agriculture, and limestone upland settlement.

They Shape River Systems

High plateaus feed river headwaters. Closed basins hold salt lakes. Steep margins create deep valleys and gorges. The same raised land that limits rainfall in one basin may supply snowmelt to a river in another.

They Shape Regional Identity

Central Anatolia is known for steppe and broad basins. Eastern Anatolia is known for cold highlands and volcanic mountains. Southeastern Anatolia is known for limestone and basalt uplands above warmer plains. The Taurus plateaus are known for karst, caves, springs, and seasonal highland use.

Simple Regional Breakdown

For a clean mental map, Turkey’s plateau regions can be grouped like this:

• Central plateau core: Central Anatolian Plateau, Konya Basin, Tuz Gölü, Cappadocia, and nearby uplands.
• High eastern plateau belt: Eastern Anatolian Plateau, Lake Van Basin, Erzurum-Kars Plateau, and volcanic highlands.
• Southern karst belt: Taşeli, Teke, Lake District, and inner Taurus limestone plateaus.
• Southeastern step-down plateaus: Gaziantep, Şanlıurfa, Mardin-Midyat, Diyarbakır, and basalt-limestone uplands.
• Western transition uplands: Afyon, Kütahya, Uşak, Eskişehir, and inner Aegean basin-plateau terrain.
• Black Sea highland surfaces: Pontic yayla areas that act as high pasture surfaces rather than one continuous plateau.

This layout avoids a common problem: treating the Anatolian Plateau as one single feature. Turkey’s raised interior is better understood as a connected but varied plateau system.

---

Mini FAQ

What are the main plateaus in Turkey?

The main plateau regions in Turkey are the Central Anatolian Plateau, the Eastern Anatolian Plateau, the Erzurum-Kars Plateau, the Southeastern Anatolian plateaus, the Taurus karst plateaus, the inner western Anatolian uplands, and high Pontic yayla surfaces in the Black Sea mountains.

Is the Anatolian Plateau the same as the Central Anatolian Plateau?

Not exactly. The Anatolian Plateau is often used as a broad term for the raised interior of Anatolia. The Central Anatolian Plateau is the more specific central plateau area around Ankara, Konya, Kayseri, Nevşehir, Aksaray, and nearby provinces.

Which plateau region in Turkey is the highest?

The Eastern Anatolian Plateau is the highest large plateau belt in Turkey. Many surfaces sit around 1,500 to 2,200 meters, and some areas, such as the Erzurum-Kars Plateau, are often linked with even higher plateau surfaces.

Are Turkish plateaus volcanic?

Some Turkish plateaus are volcanic, especially in central and eastern Anatolia. Cappadocia, the Erzurum-Kars Plateau, and the Lake Van region show strong volcanic influence. Other plateau areas, such as the Taurus karst plateaus and Mardin-Midyat uplands, are mainly shaped by limestone, uplift, and erosion.

What is the difference between a plateau and a yayla in Turkey?

A plateau is a raised landform with a broad surface. A yayla is usually a highland pasture or summer settlement area. A yayla may sit on a plateau, but it can also sit on a mountain bench, slope, or upland meadow.

Why do plateaus in Turkey matter for rivers?

Plateaus set the height and slope from which water begins to move. Turkish plateaus feed river headwaters, hold closed basins such as Konya and Tuz Gölü, and help shape major systems such as the Kızılırmak, Sakarya, Euphrates, Tigris, Aras, and Kura.