# Iller-Lech Plateau

The Iller-Lech Plateau (German: Donau-Iller-Lech-Platte), also known as the Upper Swabian Plateau (Oberschwäbische Hochebene), is one of the natural regions of Germany.

## Boundaries

In the northwest the Iller-Lech Plateau borders on the Swabian Jura (unit D60 on the map) and, in the extreme northeast, on the Franconian Jura (unit D61 on the map). The boundary with these two natural regions is roughly formed by the course of the river Danube.
In the east the Iller-Lech Plateau borders on the Lower Bavarian Upland and Isar-Inn Gravel Plateaus (unit D65 on the map). North of Augsburg its eastern boundary runs roughly parallel to state road 2035 (Augsburg-Pöttmes-Neuburg an der Donau), south of Augsburg east of the Lech, roughly between Mering, Geltendorf and Schongau.
To the south the Southern Alpine Foreland (D66 on the map) borders on the Iller-Lech Plateau. The boundary between these two natural regions is partly formed by the terminal moraines of the Würm glaciation.

## Sub-divisions

The sub-divisions are based upon the natural regions of Germany as shown on the BfN's Landscapes in Germany map. In the following table these sub-divisions are described from west to east. For the exact location and boundaries of the individual sub-divisions: see the BfN's map Landscapes in Germany (http://www.bfn.de/geoinfo/landscapes/ Archived 2016-03-03 at the Wayback Machine)

### Sub-divisions in Baden-Württemberg

| Geographical location | Formation | Relief | Soil / Land use | Remarks |
| Danube-Ablach Plateaus |||||
| Region between Danube, Mühlingen, Pfullendorf, Ostrach, Bad Saulgau and Federsee | Old Drift landscape dominated by the Rift and Mindel glaciation of the Rhine Glacier | Gently rolling hill country | Decalcified, waterlogged, brown earth (Parabraunerde) in the valleys to great depth, hence meadow and pasture land Alternation of open landscape in valleys and forested ridges (pine forests) On good soils: arable land | |
| Danube Valley between Mengen and Ulm, Lower Riss Valley |||||
| Danube Valley between Mengen and Ulm, region between Herbertingen and Bad Saulgau, Riss Valley from Schemmerhofen to where it joins the Danube | From Mengen to the narrow gap by the southernmost outliers of the Swabian Jura the floor of the Danube Valley is filled with Würm Ice Age gravels from the Rhine Glacier Beyond this gap the Danube flows through a scoured basin of reed marsh | Flat | Much grassland and arable farming | The Riss valley from the south which merges into the Danube valley is more marshy that the Danube valley |
| Federsee Ried |||||
| The Federsee lies in the middle of this natural region near Bad Buchau | Former tongue-basins (central basin) from the Riss glaciation with the extensive silted-up areas (Verlandungsgebieten) In the south the silted-up areas give way to Young Drift | Flat | On the silted-up areas there is extensive pastureland in places In the transition zone between the silted-up areas and the Young Drift moraines the reeds and wetlands vegetation gives way to stands of coniferous forest | Because the lake has since been filled with sediment and gravel in places, the natural dammed lake was once much large |
| Western Plain of the Lower Riss |||||
| Region between Danube, Riss and, roughly, the B 312 | Tertiary Hill Country, in places however also ice age gravel deposits | Hilly | Agricultural land use predominates because the soils are loamy and fertile | The Bussen is in this region |
| Western and Eastern Riss-Aitrach Plateaus |||||
| Western boundary: Schemmerhofen – Federsee – Bad Waldsee Northern boundary: Schemmerhofen – Ochsenhausen Eastern boundary: Ochsenhausen – Aitrach – Legau Southern boundary: Bad forestsee – Leutkirch im Allgäu Boundary between the Western and Eastern Riss-Aitrach Plateaus: Bad Waldsee - Eberhardzell | Riss glaciation terminal or ground moraine landscape | Undulating | Western part: arable land dominates due to the covering of loess, grassland in the wet valleys Eastern part: much of the landscape is wet or boggy; mainly open landscape with meadows and pastures | The Wurzach Ried is in the east of the Riss-Aitrach Plateau |
| Holzstöcke |||||
| Region between Senden, Aichstetten, Ochsenhausen and Laupheim | Part of the ice-age formed terraced landscape between Riss and Iller Divided by numerous hollows (Muldentäler) and meltwater troughs | Rolling hills | Mostly loam and loess covered, ridges however loam-free, decalcified and therefore forested Rapid alternation of open country (more grassland than arable land) and wooded areas (pine forests) | Landscape still not very dissected |
| Eastern Plain of the Lower Riss |||||
| Region between Neu-Ulm, Senden and Laupheim | Comprises various old gravel terraces along the valleys of the Riss and Danube, formed during the Riss glaciation | | Intensive arable land use | The south is less dissected by valleys than the north |

### Sub-divisions in both Baden-Württemberg and Bavaria

| Geographical location | Formation | Relief | Soil / Land use | Remarks |
| Higher Plains of the Lower Iller Valley (south of Memmingen) and Lower Plains of the Lower Iller Valley (north of Memmingen) |||||
| Iller Valley from Altusried and Dietmannsried to where it joins the Danube at Neu-Ulm | Broad valley filled by large quantities of gravel during and after the ice ages | Flat | The north is used more for arable farming; the south more as grassland | In the southern part the Iller valley, which has cut down to the Tertiary bedrock, crosses the Young and Old Drift deposits In places, continuous alluvial forest, in places still bog |
| Donauried |||||
| Large fen plain by the Danube between Neu-Ulm and Donauwörth | Würm Ice Age formed, partly boggy gravel plain | Flat | Used predominately for grassland and arable land, which has largely displaced the natural reed beds | Many gravel pits |

### Sub-divisions in Bavaria

| Geographical location | Formation | Relief | Soil / Land use | Remarks |
| Upper and Lower Iller-Lech Gravel Plateaus |||||
| Northern boundary: Donauried (Neu-Ulm – Nersingen – Günzburg - Offingen) Western boundary: Iller or Günz Valley in places (Neu-Ulm – Illertissen – Kellmünz an der Iller – Babenhausen – Bad Grönenbach) Southern boundary: Dietmannsried – Obergünzburg – Friesenried Eastern boundary: Mindel between Offingen and Thannhausen – Markt Wald – Bad Wörishofen – Pforzen Boundary roughly between the Upper and Lower Iller-Lech Gravel Plateaus: Babenhausen – Mindelheim – Markt Wald | Gently undulating glacial gravels divided into interfluvial ridges and gravel plateaus by river systems flowing from south to north | Gently undulating | Glacial gravels partly covered by loess Interfluvials: Covered by forest (especially pine forests) River valleys: in the north more arable land, in the south more grassland | Gravel extraction in the Mindel and Günz Valleys Fens were largely drained |
| Stauden Plateau (Stauden) / Zusam Plateau and Stauffenberg Region (Reischenau and Holzwinkel) |||||
| Between Mindel and Flossach Valley in the west (Offingen, Thannhausen and Türkheim) and the Lech and/or Wertach Valley in the east Northern boundary: Offingen – Holzheim – Wertingen – Buttenwiesen Boundary between the Stauden Plateau and Zusam Plateau and Stauffenberg region: Thannhausen – Fischach - Stadtbergen | Region is divided by the Schmutter and Zusam into gently undulating plateaus and flat interfluves Numerous bogs on the valley floors of the partly asymmetrically shaped valleys | Gently undulating | Relatively high proportion of forest and grassland (on the Stauden Plateau higher than in the more northern area of the Zusam Plateau and Stauffenberg region) Pine forests dominated the woodland areas | The Stauden Plateau, Zusam Plateau and Stauffenberg region together form the Augsburg-Westliche Wälder Nature Park |
| Lower and Upper Lech-Wertach Plain |||||
| Northern boundary: near Bobingen Western boundary: Pforzen – Bad Wörishofen – Rammingen – Bobingen Southern boundary: Pforzen – Denklingen Eastern boundary: Denklingen – Untermeitingen – Bobingen Boundary lies roughly between the Upper and Lower Lech-Wertach Plain: Türkheim – Schwabmünchen - Kaufering | Divided into lower terrace landscape by the Rivers Wertach and Gennach Meadows and lower terraces partly waterlogged | Flat | The Brennen are covered by pine forests Intensive agricultural land use (in the south more grassland, in the north more arable land) | There are only a few remnants of the formerly widespread heath landscape Together the Upper and the Lower Lech-Wertach Plains form the Lechfeld (Lech Plateau) |
| Sachsenried and Denklingen Rotwald |||||
| Between Gennach and Lech, south of Denklingen | Dominated by the high terrace gravels of the Lech in the north In the south dominated by Riss Ice Age morainic material, that covers the Tertiary bedrock | Flat to hilly | Pure forest landscape (mainly pine forests) | |
| Lech Valley |||||
| Lech Valley from Schongau to Augsburg and from Augsburg to where it joins the Danube | Extensive deposits of post-glacial gravel between Klosterlechfeld and the confluence with the Danube North of Augsburg: broad U-shaped valley (Kastental) with gravel terraces of different ages; steps between the lower terraces and the loess-covered upper terraces 8 to 10 m high Meadows and lower terraces waterlogged in places | | Mostly used as grassland On the upper terrace chiefly arable farming The further north, the more arable farming predominates | Meadows and lower terraces in places covered by heaths with communities of nutrient-poor, chalk grasses and wasteland plants characteristic of the region Almost continuous belt of alluvial forest along the river |
| Aindlingen Terrace |||||
| Western boundary: Lech Valley Eastern boundary: parallel to state road 2035 (Augsburg-Pöttmes-Neuburg by the Danube) Northern boundary: Danube Valley | High gravel plateau, rising towards the east Divided by deep stream valley that are mostly asymmetrical | Hilly | Thick layer of loess Valley floors mainly covered by grassland Otherwise arable land predominates | |
| Landsberg Plateau |||||
| Western boundary: Mering – Landsberg am Lech – Fuchs Valley Eastern boundary: Mering – Geltendorf – Fuchs Valley | Landscape rising from north to south | Gently undulating | Arable land predominates | Together with the Fürstenfeldbruck hill country forms one of the semi-circular Old Drift moraines in front of the adjoining Ammer-Loisach Hills |