- Iller-Lech Plateau
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The Iller-Lech Plateau (German: Donau-Iller-Lech-Platte), also known as the Upper Swabian Plateau (Oberschwäbische Hochebene)[1], is one of the natural regions of Germany.
Contents
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 Uplands 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/)
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 southermost 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 ares 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 hills, 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
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 Wertach and Gennach rivers
- 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 Hills forms one of the semi-circular Old Drift moraines in front of the adjoining Ammer-Loisach Hills
See also
Sources
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- Natural regions of Germany
- Bavarian Alpine Foreland
- Riedel
- Bayernviewer at the Bavarian Measurement Office: http://www.geodaten.bayern.de/BayernViewer/index.cgi
- Map of the BfN's Landscapes in Germany: http://www.bfn.de/geoinfo/landscapes/ and the information pages of the individual sub-divisions of the Iller-Lech Plateau
References
- ^ Kutt Schrem, Gesellschaft Oberschwaben für Geschichte und Kultur e.V. (ed.): Pfullendorff, ein Reichs-Statt in Ober-Schwaben gelegen. Tettnang 6 October 2011.
Categories:- Swabia
- Geography of Bavaria
- Geography of Baden-Württemberg
- Natural regions of Germany
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