Bavarian Forest
You can help expand this article with text translated from the corresponding article in German. (April 2019) Click [show] for important translation instructions.
|
Bavarian Forest | |
---|---|
Highest point | |
Peak | Großer Arber (Great Arber) |
Elevation | 4,776 ft (1,456 m) |
Naming | |
Native name | Bayerischer Wald (German) |
Geography | |
Country | Germany |
Region | Bavaria |
Parent range | Central Uplands Bohemian Massif |
Geology | |
Orogeny | Variscan |
Type of rock | Metamorphic Gneiss and Granite rocks |
The Bavarian Forest (German: ⓘ or Bayerwald; Bavarian: Boarischa Woid) is a wooded, low-mountain region in Bavaria, Germany that is about 100 kilometres long. It runs along the Czech border and is continued on the Czech side by the Bohemian Forest (Czech: Šumava). Most of the Bavarian Forest lies within the province of Lower Bavaria, but the northern part lies within Upper Palatinate. In the south it reaches the border with Upper Austria.
Geologically and
The highest mountain in the region is the
Overview
Together with the adjacent Upper Palatine Forest on the far side of the Cham-Furth Depression, and the Neuburg Forest south of Passau, the Bavarian Forest forms the largest contiguous area of woodland in Bavaria and, together with the Bohemian Forest and the Sauwald (its southeastern continuation towards Upper Austria), it forms one of the largest contiguous forests in Europe.
The Bavarian Forest is drained mainly by the
The highest mountains of the Bavarian Forest are the
In older cartographic and lexical works, the term "Bavarian Forest" refers only to the mountainous region of the
Tourism is important to the Bavarian Forest. Sharing the natural environment are walkers, the forestry industry and several ski resorts. Furthermore, the Bavarian Forest is known for its glassblowing in the area of Zwiesel and is also known in the field of geoscience as a result of the fundamental station of Wettzell at Bad Kötzting.
Geomorphology
The heart of the Bavarian Forest (in its broader sense) is divided into the Rear or High Bavarian Forest (Hinterer Bayerischer Wald) in the centre of the Bohemian Forest, the Regen valley and the Anterior Bavarian Forest (Vorderer Bayerischer Wald). In addition, there are the foothills of the two main ridges to the southeast and those of the Anterior Bavarian Forest to the northwest. Almost all of the crest-like mountain ridges run from northwest to southeast; apart from that the most important local landscapes are generally characterised by their natural regional and geomorphological nature:[3][4][5][6][7][8]
High Bavarian Forest and Regen valley
The centre of the Bohemian Forest lies between
However, the highest peaks of the low mountain range are found on a second ridgeline, southwest of the main ridge, and which also runs from northwest to southeast. The
The
To the southwest of this third ridge are the rolling hills or direction.
Anterior Bavarian Forest or Danube Hills
To the south-west of the Regen depression is the Anterior Bavarian Forest (also called the Danube Hills), which is up to 1,121 m high. Its crest also runs roughly south-eastwards, but is clearly divided into individual ridges, each of which runs in a different direction.
In the far northwest are the Elisabethszell Mountains near the village of Elisabethszell, the line of which runs away to the southeast. At the Hadriwa they reach a height of 922 m. Immediately to the east are the Hirschenstein Mountains which are similarly oriented. Beginning at the Zeller Höhe (850 m), the northernmost mountain of the Anterior Bavarian Forest overall, this range climbs to 1,092 m) at the Hirschenstein. Southeast of the Hirschenstein lie the Vogelsangwald woods and the Vogelsang (1,022 m), which comprises only one ridge; it runs from north to south. On the northern extension of this ridge in the Regen valley lies the Hornbergwald forest, which reaches 844 m at the Abendberg and thus clearly towers above the floor of the basin.
Immediately east of the Vogelsang is the Grafling Saddle (Graflinger Paßsenke), which follows the valleys of the Kollbach and Teisnach rivers from Gotteszell in the north to Grafling in the south. It is the most prominent gap in the Anterior Bavarian Forest and is crossed by the Bundesstraße 11 which climbs up to a height of 583.7 m.[3] Immediately to the east of the pass are the Riegel Mountains (Riegelbergen) with the Einödriegel (1,121 m) to the north and the Breitenauriegel (1,116 m) to the south of the highest point of the Anterior Bavarian Forest. South of it and separated by the state road, St 2135, is a chain of summits, the Hausstein Mountains (Haussteinberge) and Leopoldswald, running eastwards. The Hausstein reaches a height of 917 m, the Fürberg in the far east climbing to 880 m.
The most southerly mountain range, the Sonnenwald, is also a chain of individual peaks running from west to east; it is only connected to the Leopoldswald southwest of the Fürberg by a narrow ridge. In its western half, the Brotjacklriegel reaches 1,011 m, in the east the Aschenstein climbs to a height of 944 m. Even the mountains at the western and eastern ends of the mountain chain rise clearly above the 800 m line. To the south of the Brotjacklriegel, the isolated Stierberg (716 m), southwest of Zenting, bounds the Lallinger Winkel (see below) markedly in the east. It is usually considered part of the Passau Vorwald (see below).[10]
Falkensteiner Vorwald
The westernmost part of the Bavarian Forest is the
Between
The western part of the Vorwald transition in the south and on this side of the Regen into the Jurassic rocks of the Franconian Jura; Regenstauf being located at the boundary between the rock formations. Below Nittenau, the Regen breaks through the Vorwald impressively in a 90° bend and various smaller loops. The main summit in this high-relief part of the landscape, is the Jugendberg (611 m) immediately southwest of Nittenau, but more spectacular are the slopes of the 664 m high Gailenberg above the bend in the Regen. On the right-hand, western side of the Regen the Schwarzberg reaches at height of 538 m immediately east of Maxhütte-Haidhof.
In the north of the western part of the Falkensteiner Vorwald there is a second, somewhat less prominent Regen water gap : the Reichenbach Regen valley (Reichenbach Regental) which begins at the bend in the Regen below Roding, runs through
Southeastern Bavarian Forest
To the southeast and adjacent to the Regen Depression and Anterior Bavarian Forest is the Passauer Vorwald and, beyond it, the
Geological structure
The Bavarian Forest is continued, initially northwest, then northeast, by the Upper Palatine Forest, Fichtel Mountains, Ore Mountains and Sudetes. Geologically, as the southwestern edge of the Bohemian Massif, it is indistinguishable from the Bohemian Forest on the other side of the Czech border and from the Sauwald on Austrian soil. Together with the Upper Palatinate Forest it forms the main unit group known as the Upper Palatine-Bavarian Forest.
For the sake of simplicity, a distinction is not made between the Bohemian Forest (originally the Inner Bavarian Forest) and the Bavarian Forest. Instead, the common local name of "Bavarian Forest" is used for the entire area of the low mountain range on the German side, as the term "Bohemian Forest" has become synonymous with the areas in the
The Bavarian Forest is the rump of a
An important line that divides the Bavarian Forest into two parts is the approximately 150-kilometre-long fault line of the
Between Regensburg and Passau, there is a marked difference in height between the forested mountains to the northeast and the Danube plain ("Gäuboden") to the southwest. This dividing line between the Tertiary Hill Country and the Bavarian Forest is marked by the Danube Edge Fault (Donaurandbruch), a geological disruption between the sunken crystalline basement, lying beneath the Tertiary and Quaternary deposits of the molasse basin, and the still visible part northwest of this line, which belongs to the Bavarian Forest.
Quite striking too, is the difference in height between the Danube Plain, 300 to 350 m, and the highest peaks of the Anterior Forest, such as the Einödriegel at 1,121 m}, a difference of 800 metres in height over only a few kilometres of horizontal distance. Due to the uplift of the Bavarian Forest, which also affected the Neuburg Forest and the Sauwald, there was an antecedent incision of the rivers Inn and Danube into this area of the crystalline basement which led to the formation of a narrow valley zone from Pleinting down the Danube into Austria and south of Passau, where the Inn has formed a deeply incised riverbed.
Ice-Age landforms
Whilst the
In particular, those regions of the High Bavarian Forest were covered by snow and ice fields during the
banks.The toe of the glacier, for example near the Grosser Arbersee, was located at a height of 850 metres, the snout of the northern glacier down to the small Arbersee at a height of about 830 metres. Accordingly, there was a considerable difference in height of more than 600 metres from the summit regions to the terminal moraines. Other glacial tongues flowed down from the Grosser Rachel. Here too, there are cirques and caroids, which suggest ice-age glaciation.
Places of interest
Amongst the places of interest in the Bavarian Forest are:
Nature
Observation towers
|
Culture
|
Mountains
The following is a list of the mountains in the Bavarian Forest, sorted alphabetically with heights given in metres (m) above sea level (NN):
|
|
|
See also
References
- ^ Bavarian Forest delights with nature's elegant artistry
- ^ Rafferty, John P (ed.). Forests and Grasslands, New York: Britannica, 2011, p. 119.
- ^ Handbuch der naturräumlichen Gliederung Deutschlands. Bundesanstalt für Landeskunde, Remagen/Bad Godesberg, 1953–1962 (9 issues in 8 books, updated map, 1:1,000,000 scale with major units, 1960).
- Die naturräumlichen Einheiten auf Blatt 164 Regensburg. Bundesanstalt für Landeskunde, Bad Godesberg, 1981. → Online map(pdf; 4.8 MB)
- Die naturräumlichen Einheiten auf Blatt 165/166 Cham. Bundesanstalt für Landeskunde, Bad Godesberg, 1973. → Online map(pdf; 4.4 MB)
- Die naturräumlichen Einheiten auf Blatt 174 Straubing. Bundesanstalt für Landeskunde, Bad Godesberg, 1967. → Online map(pdf; 4.3 MB)
- Die naturräumlichen Einheiten auf Blatt 175 Passau. Bundesanstalt für Landeskunde, Bad Godesberg, 1971. → Online map(pdf; 4.7 MB)
- Federal Agency for Nature Conservation
- ^ The text part of the Handbook of the Natural Region Divisions of Germany explicitly allocates the Zeller Valley and the Weigelsberg-Kronberg ridge to the High Bavarian Forest. In the associated maps from 1954 and 1960, on the other hand, only those areas beyond the Black Regen are counted as being in the High Bavarian Forest, while the Weigelsberg and Kronberg are counted as part of the "Regen valley", while the Zeller Valley is again counted as High Bavarian Forest. Different again is the detailed division shown on Sheet 165 - Cham, which counts the Kronberg as part of the High Bavarian Forest, but assigns the Weigelsberg and Zeller Valley to the Regen Valley. For simplicity's sake, we follow the text of the manual here.
- ^ Sheet 174 Straubing, under the name Ranfelser Bergland, counts the Stierberg and its environs as part of the High Bavarian Forest; however, the cartography of the handbook and the common opinion see it differently.