East Sauerland mountain range

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East Sauerland mountain range
surface approx. 785 km²
Systematics according to Handbook of the natural spatial structure of Germany
Greater region 1st order Low mountain range threshold
Greater region 2nd order Rhenish Slate Mountains
Main unit group 33 →
Süderbergland
Natural space 332
East Sauerland mountain range
Geographical location
Coordinates 51 ° 9 '53.1 "  N , 8 ° 44' 20.5"  E Coordinates: 51 ° 9 '53.1 "  N , 8 ° 44' 20.5"  E
East Sauerland mountain range (North Rhine-Westphalia)
East Sauerland mountain range
Location Eastern Sauerland mountain range
state North Rhine-Westphalia , Hesse
Country Germany

The Eastern Sauerland mountain range is a major natural spatial unit in eastern North Rhine-Westphalia and north-western Hesse. The landscape bears the code number 332 within the main unit group 33 ( Süderbergland ) and covers the (northern) Rothaargebirge (main unit 333) to the east to the West Hessian mountains (main unit group 34). To the north it borders on the Paderborn plateau (362) in the Upper Weserbergland (main unit group 36), to the south with the Gladenbacher Bergland (320) on part of the natural Westerwald (Main unit group 32).

The East Sauerland mountain range is bounded roughly to the northwest by the Rhine-Weser watershed between the towns of Brilon (west) and Marsberg (east), and to the south by the upper reaches of the Lahn between Biedenkopf and Sterzhausen .

Adjacent natural areas

To the north is the Paderborn plateau (main unit 362), to the northeast the Egge Mountains (363) - both parts of the Lower Saxony mountainous region . On the other hand, three parts of the West Hessian mountainous region border to the east , namely the Waldecker Tafel (340) in the north , the Kellerwald (344) in the middle and the Burgwald (345) in the south . These landscapes differ significantly from the Rothaargebirge bordering to the west (with the Hochsauerland), to which the west of the (historical) Upland also belongs, while the east is part of the mountain range.

Natural characteristics

The landscapes surrounding the edge of the mountain differ significantly in terms of their geological structure and the clearly deviating landscape reliefs ( geomorphology ) as well as their respective climatic conditions.

geology

While the East Sauerland mountain range, just like the Rothaar Mountains adjoining it to the west, originates from the earlier Paleozoic era , the landscapes adjoining it to the east are attributed to the much more recent Hessian Bruchschollentafelland, the formation of which mainly took place in the Mesozoic Era.

The East Sauerland main saddle is built from rocks from the Devonian and Carboniferous . This sequence of partly strongly folded, Middle Paleozoic rocks (Upper Devonian and Lower Carboniferous slate, pebble slate, limestone and sandstone, partly with interposed tufa layers) plunge into the northeast under the late Paleozoic-early Mesozoic clays, carbonates and sandstones of the Waldeck Upland.

In contrast, the characteristic rocks of the Hessian Bruchschollentafelland region to the east (shell limestone, red sandstone, marl, gypsum and claystone) come from the Triassic and Jurassic ages .

The Kellerwald plays a special role here, as it comes from the Paleozoic Era - like the Rothaargebirge and Ostrand - and, in terms of rock structure, can also be assigned to the Rhenish Slate Mountains , on the other hand it is clearly located on the West Hessian Bruchscholle, from which it protrudes like a clump.

climate

Since the eastern edge of the Sauerland is in the rain shadow of the Rothaargebirge, the annual precipitation is halved from west to east from up to 1200 mm to barely more than 600 mm, while the mean daytime temperature is around 2 ° C from 6 to 7 ° C to 8 to 9 ° C increases.

Soil and vegetation

Soil conditions and use of the Eastern Sauerland mountain range are diverse and range from mixed forest landscapes ( bagpipe foreheads , Waldstruth ) to well-developed agricultural landscapes ( Medebacher Bucht , Upland ) to areas in the north where the mining of mineral resources plays a major role ( Marsberg copper slate , Ore mining in lead washing ).

Rivers

Although the Rhine-Weser watershed crosses the East Sauerland mountain range twice, this takes place in distinctly peripheral locations in the north and south, so that almost the entire area drains east to the Weser via Eder and Diemel .

Together with the abundance of precipitation in the Rothaargebirge, the low water storage capacity of the slate rocks on the edge of the mountain leads to a high risk of flooding, which has given rise to the construction of the Diemel Reservoir in the north and the Edertal Reservoir (east on the other side, in the northern Kellerwald).

Natural structure

The Süderbergland is structured as follows:

View from the Christenberg in the Burgwald to the Wetschaft depression and the bagpipe behind it, along with foreheads (332.0) with a mountain of coal (583 m, half right, two-peaked), bagpipe (673.5 m, right of center, very wide, with a transmission mast), splendor of the groves (631 m, left of it in the background), Hassenroth (622 m, middle, dome) and Arennest (592 m, second half left)
Meadow and field landscape of the Sachsenberg Leimestruth (332.31) on the Eder - Nuhne water divide between Sachsenberg and Viermünden . In the front background, across the Eder valley, the Hessensteiner Wald (332.32), in the far background the Hohe Lohr in the Kellerwald .
The Orke's entry valley into Örksche Schweiz (332.33) near Dalwigksthal ; above in the background Lichtenfels Castle
The valley of the Wild Aa in the Aarstruth (332.34) on the road Auf der Aar between Goddelsheim and Medebach ; View diagonally upstream to the northeast
  • (to 33 Süderbergland )
    • 332 East Sauerland mountain range - approx. 785 km²
      • 332.0 Bagpipe Vorhöhen (with Wollenberg ) - 66.54 km², all in HE
      • 332.1 Hinterland Ederbergland - approx. 141.35 km²
      • 332.2 Frankenberger Grund - 35.43 km², completely in HE
      • 332.3 Waldstruth - approx. 162.33 km²
      • 332.4 Medebacher Bucht - approx. 113 km², of which 20.13 km² in HE
        • 332.40 Medebach Inclined Plane - completely in NW
        • 332.41 Hallenberger Hügelland - almost completely in NW; only 0.79 km² in HE
        • 332.42 Münder Grund - 26.34 km² in HE
      • 332.5 Grafschafter Bergland - approx. 90.82 km²
      • 332.6 (Vorupländer) Adorfer Bay - 83.63 km²
        • 332.60 Flechtdorfer Höckerflur - 44.84 km², all in HE
        • 332.61 Vorpländer hill country - 24.63 km², practically entirely in HE
        • 332.62 Adorfer Grund - 14.16 km², all in HE
      • 332.7 Diemel-Bergland - approx. 92 km²

Individual evidence

  1. s. structure
  2. ^ A b E. Meynen and J. Schmithüsen : Handbook of the natural spatial structure of Germany - Federal Institute for Regional Studies, Remagen / Bad Godesberg 1953–1962 (9 deliveries in 8 books, updated map 1: 1,000,000 with main units 1960)
  3. Martin Bürgener: Geographical Land Survey: The natural spatial units on sheet 111 Arolsen (Martin Bürgener 1963) and sheet 125 Marburg (Gerhard Sandner 1960) - Federal Institute for Regional Studies, Bad Godesberg →  online map
  4. a b c d e f g h i j k l m n o p q r s t u v Map and legend of the natural areas of Hesse (online copy of Die Naturraum Hessens , Otto Klausing 1988) in the Hesse State Office's Environmental Atlas for Environment and geology
  5. a b c d e measurement in TIM online
  6. The prefix “Sachsenberger” comes from Klausing (1988). Bürgener (1963) only writes about “Leimestruth”.
  7. About 8 km² of this can also be interpreted as part of the Goddelsheimer Feld (cannot be delimited in lines; geomorphologically flowing), of which about 2 km² Heimbachtal plus peripheral hills.
  8. a b Landscape profiles of the Federal Agency for Nature Conservation ( information )
  9. On most of the official maps this summit is not marked with an altitude and you can only see the 535 line. The 543 m are explicitly recorded in the background maps of the Hessen Environmental Atlas and the Hessen ERRL.

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