Europe’s major plateau regions are not all wide, empty, flat surfaces. Many are old uplands, dissected massifs, glacial forelands, volcanic highlands, limestone tablelands, and rolling river divides. They sit between mountain belts, plains, basins, coastlands, and river systems, so their geography is often more varied than the word plateau suggests.
The largest and best-known European plateau regions include the Meseta Central in Spain, the Massif Central in France, the Bohemian Massif in Central Europe, the Swiss Plateau, the Central German and Rhenish Uplands, the Scandinavian uplands, and the broad East European uplands linked with the Volga, Don, Dnieper and Dniester river basins.
| Plateau Region | Main Location | Approximate Elevation Pattern | Landform Type | Main Rivers or Basins | Known For |
|---|---|---|---|---|---|
| Meseta Central | Central Spain, with western links toward Portugal | Often around 600–700 m above sea level | High interior plateau and basin system | Duero, Tagus and Guadiana basins | Spain’s broad interior tableland and high central plains |
| Massif Central | South-central France | Many plateau surfaces around 600–900 m, with higher volcanic peaks | Old massif, volcanic upland and dissected plateau region | Loire, Dordogne, Allier, Tarn and Rhône-edge drainage | Volcanic landforms, old crystalline rocks and high rural plateaus |
| Bohemian Massif | Czech Republic, with edges in Germany, Austria and Poland | Varied uplands, basins and rim mountains | Dissected plateau and old shield-like massif | Elbe, Vltava, Morava and Oder-related drainage | Central Europe’s enclosed plateau-basin landscape |
| Central German and Rhenish Uplands | Germany, Belgium, Luxembourg and nearby borderlands | Mostly low to moderate uplands; many areas below 900 m | Dissected plateaus, forested massifs and river-cut uplands | Rhine, Moselle, Ruhr, Main and Weser systems | River valleys, wooded plateaus, escarpments and old massif terrain |
| Swiss Plateau | Between the Jura Mountains and the Alps in Switzerland | Commonly around 400–700 m, with local variation | Glacially shaped foreland plateau | Aare, Reuss, Limmat, Rhine and lake basins | Rolling hills, lakes, cities and the main Swiss lowland corridor |
| Scandinavian Uplands and Northern Plateaus | Norway, Sweden and northern Fennoscandia | Highly varied; lower northern plateaus and higher mountain-edge surfaces | Glaciated uplands, fjell surfaces and old highland plateaus | Rivers draining to the North Sea, Norwegian Sea, Baltic Sea and Arctic Ocean | Glacial valleys, lakes, fjords, tundra-like highlands and hard-rock terrain |
| East European Uplands | European Russia and parts of Ukraine | Mostly low to moderate uplands, often a few hundred metres high | Rolling uplands within the East European Plain | Volga, Don, Dnieper, Oka, Dniester and Southern Bug systems | Broad river divides, loess-covered surfaces and steppe-forest transitions |
| Dinaric and Karst Plateau Belts | Slovenia, Croatia, Bosnia and Herzegovina, Montenegro and nearby areas | Varied limestone plateaus, basins and mountain-edge surfaces | Karst plateau and limestone highland terrain | Adriatic, Sava, Neretva and underground karst drainage | Caves, sinkholes, dry valleys, poljes and broken limestone tablelands |
Geography Note: In Europe, many plateau regions are called uplands, massifs, mesetas, tablelands or highlands. The names differ by language and region, but the landform idea is often similar: raised ground with broad surfaces, cut by rivers, valleys, basins or escarpments.
What Makes a European Plateau Different?
A European plateau is usually a raised landform that stands above nearby plains, basins or coastlands. It may look fairly level from a regional map, but on the ground it can include hills, valleys, gorges, volcanic cones, river terraces, forests, farms and towns.
Europe’s plateaus are often older and more dissected than the huge high plateaus of Asia, Africa or North America. Many formed from ancient rocks that were lifted, worn down, broken by faults, covered by lava, shaped by ice, or cut by rivers over long periods.
This is why a plateau in Europe may not look perfectly flat. It may look like a high rolling country rather than a table.
Common Traits of European Plateaus
- They often sit between mountain ranges and lowland plains.
- They can act as river divides, sending water into different basins.
- Many are old crystalline or limestone regions, later cut by erosion.
- Some contain volcanic landforms, lava plateaus or extinct volcanic cones.
- Glaciers shaped several northern and Alpine-edge plateau landscapes.
- Elevation affects climate, farming, settlement and transport routes.
Why Europe Has Many Uplands Instead of One Huge Plateau
Europe is a small, heavily broken continent with peninsulas, inland seas, old mountain roots, young mountain belts and large plains placed close together. This creates many regional plateau systems rather than one single raised block.
The result is a patchwork: the Spanish Meseta, the French Massif Central, the Bohemian basin, the Swiss foreland, the Scandinavian hard-rock uplands and the broad East European rolling highlands all belong to different geologic stories.
Major Plateau Regions in Europe
Meseta Central, Spain
The Meseta Central is one of Europe’s clearest examples of a large interior plateau. It covers much of central Spain and gives the Iberian Peninsula its high, dry, elevated core. Madrid sits within this broader plateau region.
The Meseta is often described as having an average elevation around 600–700 m, though the surface is not uniform. It is divided into northern and southern sections by the Central System mountain range. The northern part is generally higher, while the southern part lies somewhat lower.
The plateau is surrounded or bordered by important mountain systems, including the Cantabrian Mountains to the north, the Iberian System to the east, the Sierra Morena to the south, and older highlands toward the west.
Rivers and Basins of the Meseta
The Meseta helps organize some of Iberia’s major river basins. The Duero drains much of the northern plateau. The Tagus crosses the central plateau system. The Guadiana is linked with the southern Meseta and nearby lowland transitions.
This makes the Meseta more than a high plain. It is a drainage platform that sends water westward toward the Atlantic and shapes farming, settlement and regional movement across central Spain.
Landscape and Climate
The Meseta has a strong interior climate pattern. Summers can be hot, winters can be cold for its latitude, and rainfall varies by region and elevation. The high plateau position helps explain why central Spain feels different from nearby coastal areas.
Wide plains, cereal fields, dry basins, river valleys and mountain rims all belong to the Meseta’s geography.
Massif Central, France
The Massif Central covers a large part of south-central France. It is not one flat plateau. It is a broad highland region made of old rocks, dissected plateaus, volcanic areas, deep river valleys and higher summits.
Many plateau surfaces sit roughly between 600 and 900 m, while volcanic peaks rise higher. The Puy de Sancy, in the Auvergne area, reaches about 1,885 m, making it the highest point of the region.
The Massif Central borders or overlooks several major French lowland and basin areas, including the Aquitaine Basin, the Paris Basin, the Rhône-Saône corridor and Mediterranean-facing lowlands.
Volcanic Origin and Old Rock Structure
The Massif Central is known for its volcanic landscapes, especially in Auvergne. Some areas include extinct cones, lava plateaus and volcanic domes. Other areas are older crystalline uplands that were lifted and worn down over time.
This mix gives the region a layered landform pattern: old plateau surfaces, younger volcanic forms, steep river valleys and basin edges.
Rivers and Drainage
The Massif Central sends rivers in several directions. The Loire rises in the region and flows north and west. Rivers such as the Allier, Dordogne, Tarn and Lot also cut through or near the uplands.
Because of this, the Massif Central acts as a water source, a high divide and a landform barrier inside France.
Bohemian Massif and Bohemian Plateau, Central Europe
The Bohemian Massif is a large old highland block in Central Europe. It occupies much of the Czech Republic and reaches into Germany, Austria and Poland. Its inner area is often described as the Bohemian Plateau or Bohemian Basin, ringed by mountains and highlands.
This region is a good example of a European plateau that is not open and flat. It is a dissected upland-basin system, with rim mountains, river valleys, rolling surfaces and old crystalline rocks.
The surrounding highland rim includes areas such as the Bohemian Forest, Ore Mountains and Sudeten-related uplands. These ranges help define the basin-like shape of Bohemia.
Rivers and Basins
The Vltava and Elbe are central to the drainage of Bohemia. Water moves from the plateau-basin interior toward lower river corridors, while nearby uplands also connect with the Morava, Oder and Danube-related systems.
This makes the Bohemian Massif one of Europe’s most useful map examples for seeing how a plateau can be enclosed by mountains yet drained by major rivers.
How It Differs from the Meseta
The Meseta is a broad interior plateau across much of central Spain. The Bohemian Massif is more like an old raised block and enclosed basin with a mountain rim. Both are plateau-like regions, but their shape, climate, river patterns and surrounding landforms differ.
Central German and Rhenish Uplands
The Central German Uplands form a belt of massifs, plateaus, basins and forested highlands across Germany and nearby borderlands. The Rhenish Uplands, Eifel, Hunsrück, Sauerland, Harz-related areas and other uplands belong to this wider central belt.
These are not high mountains by Alpine standards. Many areas are low to moderate in elevation, with several plateau surfaces, rounded summits and steep river valleys. The landscape is often dissected, meaning rivers have cut into older upland surfaces.
Rhine, Moselle and River-Cut Plateaus
The Rhine and its tributaries help define this region. The Moselle, Ruhr, Main and other rivers cut valleys through uplands and connect plateau surfaces with lowland corridors.
On a map, the region looks like a chain of wooded uplands placed between the North German Plain and the Alpine foreland. On the ground, it includes ridges, river gorges, volcanic areas, sandstone plateaus and basin floors.
Map Note: A plateau does not need to be the highest land in a country. In Germany, many plateau-like regions are better read as uplands cut by rivers. Look for broad raised surfaces first, then check how rivers have carved them.
Swiss Plateau
The Swiss Plateau, also known as the Mittelland, lies between the Jura Mountains to the northwest and the Alps to the south and southeast. It is one of Europe’s best examples of a settled foreland plateau.
Its elevation is often around 400–700 m, with rolling hills, lake basins, towns, farms and transport corridors. Unlike the rugged Alps beside it, the Swiss Plateau is lower, smoother and easier to cross.
A Plateau Between Two Mountain Systems
The Swiss Plateau is shaped by its position. The Jura rises on one side. The Alps rise much higher on the other. Between them sits a belt of rolling land formed by sedimentary basins, river action and past glaciation.
Glaciers helped shape many of the lakes and valley forms in and around this region. The Aare, Reuss, Limmat and Rhine-related drainage systems connect the plateau with Switzerland’s larger river network.
Why It Matters
The Swiss Plateau holds many of Switzerland’s main cities, routes and agricultural zones. This is a reminder that plateaus are not always remote. Some are dense settlement corridors because they offer gentler land between harder mountain terrain.
Scandinavian Uplands and Northern Plateaus
Northern Europe includes several plateau-like upland regions across Norway, Sweden and northern Fennoscandia. These landscapes are strongly shaped by old hard rocks, glaciation, lakes, fjords, river valleys and high latitude climate.
The Scandinavian Mountains form the main western spine, but broad upland surfaces, fjell areas and lower plateaus spread across parts of Norway and Sweden. The Finnmark Plateau in northern Norway is one named example, often described as a broad upland surface around a few hundred metres above sea level.
Glacial Shape and Hard-Rock Terrain
Ice has strongly shaped northern plateau landscapes. Glaciers smoothed hard-rock surfaces, cut valleys, left lakes and opened routes for rivers. In Norway, the contrast between high inland surfaces and steep fjord-cut coasts is especially clear.
In Sweden, large northern uplands include rounded hills, forests, lakes and river valleys draining toward the Gulf of Bothnia and the Baltic Sea. Farther north, colder climates and tundra-like vegetation appear on exposed high surfaces.
Why They Look Different from Southern European Plateaus
Scandinavian plateau regions often feel more open, glacial and lake-rich than the Meseta or Massif Central. Their climate is colder, their bedrock is older in many areas, and their surface has been strongly worked by ice.
East European Uplands
The East European Plain is mostly low and broad, but it contains several important upland and plateau-like regions. These include the Central Russian Upland, the Volga Upland, the Volyn-Podilsk Upland, the Dnieper Upland and related raised surfaces.
These uplands are not very high compared with the Alps or the Caucasus. Many elevations are only a few hundred metres above sea level. Even so, they matter because they divide major river basins and shape the flow of water across eastern Europe.
Central Russian Upland and Volga Upland
The Central Russian Upland stretches across part of European Russia between the Oka and Donets river areas. Its maximum elevation is only about 290 m, yet it forms a clear raised zone within the wider Russian Plain.
Farther east, the Volga Upland rises near the Volga River. It helps separate drainage areas and creates a more broken edge along parts of the river system. In a lowland continent-scale plain, even modest uplands can guide rivers and settlement patterns.
Volyn-Podilsk and Dnieper Uplands
The Volyn-Podilsk Upland and Dnieper Upland are linked with western and central Ukraine’s raised terrain. Their surfaces include rolling plains, river valleys, ravines and canyon-like cuts in some areas.
They help explain why eastern Europe is not just one flat plain. It contains low plateaus and river-divide uplands that become clear when reading drainage maps.
Dinaric and Karst Plateau Belts
The Dinaric region of southeastern Europe includes limestone mountains, basins and karst plateaus stretching through parts of Slovenia, Croatia, Bosnia and Herzegovina, Montenegro and nearby areas. This is not one single plateau, but a belt of karst highlands and tableland surfaces.
Karst plateaus form where limestone and similar rocks dissolve through water action. The result can include caves, sinkholes, disappearing streams, dry valleys, springs and enclosed basins called poljes.
Why Karst Plateaus Are Special
Many plateaus drain through visible rivers. Karst plateaus may also drain underground. A stream can vanish into limestone, move through caves and reappear at a spring lower down.
This makes the Dinaric karst one of Europe’s best examples of how geology controls surface water. The plateau may look dry on top, while much of the water is moving beneath the ground.
Icelandic Interior Highlands
Iceland’s interior highlands add a volcanic island example to Europe’s plateau geography. The interior includes lava fields, volcanic deserts, ice caps, highland routes, glacial rivers and broad raised surfaces.
Unlike the old crystalline uplands of Central Europe, Iceland’s highlands are tied to active volcanic and tectonic processes. Lava, ash, glaciers and meltwater all help shape the land.
This region shows another European plateau pattern: a volcanic highland where elevation, ice and young rocks work together.
How European Plateaus Formed
Europe’s plateau regions formed through several processes. Some are ancient rock masses lifted and worn down. Some are volcanic. Some are glacial forelands. Others are limestone surfaces shaped by dissolving rock and underground water.
| Formation Process | How It Works | European Examples |
|---|---|---|
| Old Massif Uplift and Erosion | Ancient rock blocks are raised, worn down and cut by rivers over long time spans. | Massif Central, Bohemian Massif, Central German Uplands |
| Interior Basin and Plateau Development | A broad elevated region develops inside or between mountain systems and drains through major river basins. | Meseta Central |
| Volcanic Activity | Lava, ash and volcanic cones build or cover raised surfaces. | Auvergne in the Massif Central, Icelandic Interior Highlands |
| Glacial Shaping | Ice smooths bedrock, cuts valleys, leaves lakes and reshapes plateau margins. | Swiss Plateau, Scandinavian uplands, Icelandic highlands |
| Karst Solution | Water dissolves limestone, creating caves, sinkholes, dry valleys and underground drainage. | Dinaric Karst, Karst Plateau region near Slovenia and Italy |
| River Incision | Rivers cut valleys, ravines and gorges into broad raised surfaces. | Rhenish Uplands, Dnieper Upland, Volyn-Podilsk Upland |
Old Rocks and Dissected Surfaces
Many European plateaus are old landforms. Their rocks may be much older than the present landscape. Over time, uplift raised these areas, while erosion cut valleys into them.
This creates dissected plateaus: land that may have once had broader, smoother surfaces but is now broken by river valleys, ravines, hills and escarpments.
Volcanic Plateaus and Highland Lava Landscapes
Volcanic activity adds another pattern. The Massif Central includes volcanic areas within an older highland region. Iceland’s highlands are younger and more active in geologic terms, with lava fields and glacial rivers shaping much of the interior.
Volcanic plateaus often have dark rock, poor or thin soils in some areas, distinct cones or domes, and drainage shaped by lava surfaces.
Karst Plateaus
Karst plateaus form when water dissolves limestone and related rocks. Surface rivers may be short, broken or absent because water can enter cracks and move underground.
This creates one of Europe’s most useful landform lessons: a plateau can be shaped as much by hidden drainage as by visible rivers.
How Plateaus Shape European Rivers and Basins
Plateaus often work as high starting points or dividing surfaces for river systems. Even a low plateau can decide whether water flows toward the Atlantic, Mediterranean, Baltic, Black Sea, North Sea or Caspian-related basins.
River Divides
A river divide is a raised area that separates drainage basins. The Meseta Central divides major Iberian river systems. The Massif Central sends water toward different parts of France. East European uplands separate the Volga, Don, Dnieper and other river systems.
In simple terms: water leaves plateaus in different directions.
Escarpments and Valley Edges
Some plateau margins end in escarpments, steep slopes or broken edges. Rivers may cut through these margins, creating gorges and narrow valleys. This is common in dissected uplands such as the Rhenish region and parts of eastern Europe.
Lakes and Glacial Drainage
The Swiss Plateau and Scandinavian uplands show how glaciers can change plateau drainage. Ice deepened basins, left lakes and guided river courses. This is why many northern and Alpine-edge plateau regions have lake-rich landscapes.
Elevation Note: A plateau does not need extreme height to shape drainage. In eastern Europe, low uplands only a few hundred metres high can still separate large river basins because the surrounding plains are also low.
Climate and Landscape Patterns on European Plateaus
Elevation changes climate. A plateau is usually cooler than nearby lowlands at the same latitude. It may also receive more rain if moist air is forced upward, or less rain if it sits behind a mountain barrier.
Dry Interior Plateaus
The Meseta Central shows how distance from the sea, elevation and surrounding mountains can produce a strong interior climate. Summers can be hot, winters can feel cold, and rainfall is lower than in many coastal or mountain-edge regions.
Wet and Forested Uplands
The Massif Central, Central German Uplands and parts of the Rhenish region include wetter, greener plateau landscapes. Forests, pasture, river valleys and upland farming are common in many places.
Cold Northern Plateaus
Scandinavian plateau regions have colder conditions, especially with higher elevation and latitude. Snow, lakes, conifer forests, bogs and tundra-like surfaces appear in different zones.
Karst Plateaus and Thin Soils
Limestone plateaus often have thin soils, rocky surfaces and special drainage. In karst areas, water may be present underground even where the surface looks dry.
European Plateaus by Broad Region
Western and Southwestern Europe
- Meseta Central: Spain’s large interior plateau, linked with the Duero, Tagus and Guadiana basins.
- Massif Central: France’s large highland and plateau region with volcanic areas and river-cut valleys.
- Rhenish Uplands: A dissected plateau and highland area cut by the Rhine and its tributaries.
Central Europe
- Bohemian Massif: A large old upland block with an enclosed plateau-basin pattern.
- Central German Uplands: A belt of low mountains, forested plateaus and river valleys.
- Swiss Plateau: A rolling foreland plateau between the Jura and the Alps.
Northern Europe
- Scandinavian Uplands: Glaciated hard-rock highlands with lakes, valleys and mountain-edge plateau surfaces.
- Finnmark Plateau: A northern Norwegian plateau landscape with low relief compared with the main Scandinavian Mountains.
- Icelandic Interior Highlands: Volcanic highlands shaped by lava, ice and meltwater.
Eastern Europe
- Central Russian Upland: A low but broad upland dividing river systems in European Russia.
- Volga Upland: A raised region near the Volga River with dissected slopes and river-valley edges.
- Dnieper and Volyn-Podilsk Uplands: Rolling uplands and plateau-like surfaces linked with Dnieper, Dniester and Southern Bug drainage.
Southeastern Europe
- Dinaric Karst Plateaus: Limestone highlands with caves, sinkholes, poljes and underground drainage.
- Balkan Upland Basins: Raised basins and mountain-edge plateaus appear in several inland parts of the Balkan Peninsula.
Plateau, Upland, Highland and Mountain: Common Mix-Ups
European geography uses several overlapping terms. A plateau can be part of an upland. A highland may include plateaus and mountains. A massif may contain plateau surfaces, ridges and valleys.
| Term | Simple Meaning | How It Appears in Europe | Example |
|---|---|---|---|
| Plateau | Raised land with a broad, fairly level surface | May be flat, rolling or cut by rivers | Meseta Central |
| Upland | Higher land compared with nearby lowlands | Often rounded, forested or dissected | Central German Uplands |
| Highland | Broad elevated region, often rougher than a plain | Can include hills, mountains, plateaus and valleys | Scandinavian uplands |
| Massif | Large block of old rock forming a mountain or upland region | May contain plateau surfaces and basin interiors | Massif Central, Bohemian Massif |
| Mountain Range | Line or group of high, steep landforms | Often borders or cuts across plateaus | Alps, Pyrenees, Carpathians |
| Basin | Lower area where sediment or water collects | Can sit inside or beside a plateau region | Bohemian Basin, Aquitaine Basin edge |
A Simple Rule for Reading the Difference
If the land is broad and raised, think plateau. If it is raised but more broken and uneven, think upland. If it is very high and steep, think mountain. If it is an old rock block with several landforms inside it, think massif.
Many European regions fit more than one term.
How to Read European Plateaus on a Map
A physical map can make Europe’s plateau regions much easier to understand. The trick is to look beyond the names and read the shape of the land.
Look for Broad Raised Areas
Plateaus usually appear as larger areas of higher elevation, not narrow ridges. The Meseta Central, Massif Central and Bohemian Massif stand out because they cover broad regions rather than single peaks.
Check the River Direction
Rivers show how a plateau works. If water flows away in several directions, the region may act as a divide. If rivers cut deep valleys into the land, the plateau is probably dissected.
Find the Edges
Plateaus often have edges: escarpments, mountain rims, basin margins or steep river valleys. The edge can be more dramatic than the surface.
Compare Nearby Lowlands
A plateau is defined partly by contrast. The Swiss Plateau is not high compared with the Alps, but it is still a raised and distinct foreland region between mountain systems. The East European uplands are low in absolute height, but they rise above nearby plains enough to guide rivers.
Watch for Local Names
European plateau regions may appear under local or regional names. Meseta, Mittelland, upland, massif, plateau, karst and highland may point to plateau-like terrain depending on the region.
Why Plateaus Matter in European Geography
Plateaus shape more than relief. They affect where people live, where roads and railways pass, where rivers begin, where farming works best and where regional climates differ from nearby lowlands.
They Shape Settlement
Some plateaus are sparsely populated because of cold, dryness, thin soils or rough terrain. Others, such as the Swiss Plateau, support dense settlement because they offer usable land between mountains.
They Shape Farming and Land Use
Plateau farming depends on soil, rainfall, slope and temperature. The Meseta supports large dryland farming zones. The Massif Central includes pasture and upland agriculture. Karst plateaus may have thin soils and scattered fertile basins.
They Shape Travel Routes
Transport often follows plateau corridors, river valleys and basin edges. Uplands can slow movement, but they can also provide passes, rolling routes and safer ground above flood-prone lowlands.
They Shape Regional Identity
Many European plateau regions have strong local landscapes: Castilian tablelands, Auvergne volcanic uplands, Bohemian basin country, Swiss Mittelland towns, Scandinavian fjell surfaces and Dinaric karst fields. Geography gives each region a clear physical setting.
Mini FAQ
What are the main plateau regions in Europe?
The main plateau and upland regions in Europe include the Meseta Central in Spain, the Massif Central in France, the Bohemian Massif in Central Europe, the Swiss Plateau, the Central German and Rhenish Uplands, the Scandinavian uplands, the East European uplands and the Dinaric karst plateau belts.
Is Europe mostly plateau or plain?
Europe is a mix of plains, mountains, uplands, basins and plateaus. The North European Plain and East European Plain cover large areas, but many plateau and upland regions break up the continent, especially in Iberia, France, Central Europe, Scandinavia and eastern Europe.
What is the largest plateau in Europe?
The Meseta Central is often treated as one of Europe’s largest and clearest plateau regions. It covers much of central Spain and forms the high interior core of the Iberian Peninsula.
Why are many European plateaus called uplands or massifs?
Many European plateaus are old, dissected and uneven rather than perfectly flat. Because of that, regional geography often uses names such as upland, highland or massif. These terms can describe plateau-like terrain that has been cut by rivers, shaped by ice or bordered by mountains.
Which European plateau is volcanic?
The Massif Central in France includes well-known volcanic areas, especially in Auvergne. Iceland’s interior highlands also include volcanic plateau landscapes shaped by lava, ash, glaciers and meltwater.
How do European plateaus affect rivers?
European plateaus often act as river divides. They guide water toward different basins, such as the Atlantic, North Sea, Baltic Sea, Mediterranean, Black Sea or Caspian-related drainage. Rivers also cut valleys, gorges and ravines into many plateau surfaces.
Is the Swiss Plateau a mountain plateau?
The Swiss Plateau is not a high mountain plateau like the Tibetan Plateau. It is a lower foreland plateau between the Jura Mountains and the Alps. It has rolling hills, lakes, river valleys, cities and farmland.
What is a karst plateau in Europe?
A karst plateau is a limestone plateau shaped by dissolving rock and underground drainage. In Europe, the Dinaric karst region includes caves, sinkholes, dry valleys, poljes and springs across parts of southeastern Europe.