Upper Inn Valley

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Upper Inn Valley
The Upper Inn Valley near Zams / Landeck

The Upper Inn Valley near Zams / Landeck

location Tyrol , Austria
Waters Inn
Mountains Northern Limestone Alps , Central Alps
Geographical location 47 ° 13 '  N , 10 ° 43'  E Coordinates: 47 ° 13 '  N , 10 ° 43'  E
Oberinntal (Tyrol)
Upper Inn Valley
height 600 to  800  m above sea level A.
length 90 km
climate inner alpine valley climate
Template: Infobox Glacier / Maintenance / Image description missing
View of the Upper Inn Valley in west direction near Zirl
The Upper Inn Valley with Zams around 1900

The upper part of the Tyrolean Inn Valley is referred to as the Oberinntal , also known as the Tiroler Oberinntal .

geography

The Upper Inn Valley stretches from the border with the Swiss Engadin to the confluence of the Melach a few kilometers west of Innsbruck . The area between the border and Landeck is called the Upper Court . The Oberinntal is part of the Tyrolean Oberland .

The valley is (excluding the Upper Court) around 90 km long and surrounded by mountains up to 3000 m high. It separates the Northern Limestone Alps from the higher Central Alps to the south . In contrast to the Lower Inn Valley , the Upper Inn Valley is narrower and in some places formed by gorges, for example near Zams and Roppen , or forms a landslide landscape at the entrance to the Ötztal . From Silz the valley floor is wider. The valley is partly accompanied by low mountain range terraces, including the Mieminger Plateau as the largest . The largest side valleys are the Pitztal and Ötztal from the south and the Stanzer and Gurgltal from the west and north.

The border between the Upper and Lower Inn Valley at the (old) Melach estuary near Zirl and the Meilbrünnl opposite the Inn near the Martinswand represents the old regional court boundary between Sonnenburg and Hörtenberg .

climate

Protected by the high mountain ranges, the Upper Inn Valley has a typical inner-Alpine valley climate. There is less rainfall than in the north or south alpine congestion areas , lots of sun in winter, little fog and wind. To the west and north of Landeck there is an abrupt transition to the high- precipitation reservoirs of the Arlberg area and the Lechtal Alps . On the other hand, precipitation decreases even further towards the south towards the main Alpine ridge (Ötztal, Upper Court). The mean annual precipitation for the years 1971-2000 in Haiming is 716.7 mm, in Imst 788.9 mm, in Landeck 753.6 mm and in Prutz 633.6 mm.

Monthly average temperatures and precipitation for Landeck ( 785  m above sea level )
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Max. Temperature ( ° C ) 2.6 6.0 11.0 14.5 19.8 22.3 24.6 24.1 20.4 15.2 7.1 2.7 O 14.2
Min. Temperature (° C) -4.1 -3.3 -0.1 2.7 7.1 9.8 11.8 11.8 8.8 4.6 -0.4 -3.1 O 3.8
Temperature (° C) -1.4 0.3 4.2 7.6 12.7 15.3 17.4 16.8 13.2 8.5 2.5 -0.6 O 8.1
Precipitation ( mm ) 43.5 44.3 43.1 37.0 59.3 94.8 106.0 107.1 67.3 46.4 54.9 49.9 Σ 753.6
Hours of sunshine ( h / d ) 2.3 3.7 4.8 4.9 5.9 5.4 6.2 6.2 5.3 4.3 2.5 1.4 O 4.4
T
e
m
p
e
r
a
t
u
r
2.6
-4.1
6.0
-3.3
11.0
-0.1
14.5
2.7
19.8
7.1
22.3
9.8
24.6
11.8
24.1
11.8
20.4
8.8
15.2
4.6
7.1
-0.4
2.7
-3.1
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
N
i
e
d
e
r
s
c
h
l
a
g
43.5
44.3
43.1
37.0
59.3
94.8
106.0
107.1
67.3
46.4
54.9
49.9
  Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Source:

population

The town centers are mostly elevated on the alluvial cones of the brooks or on the low mountain range terraces. Meanwhile, the valley floor is also increasingly being used for settlements and, above all, for businesses. The largest towns and regional centers are the third largest municipality in Tyrol, Telfs (16,046 inhabitants), Imst (10,765), Zirl (8110) and Landeck (7633).

The form of the farms in the Upper Inn Valley is Rhaetian , in contrast to the Bavarian court forms of the Lower Inn Valley. The southern Bavarian dialects show individual characteristics of Alemannic , especially in the west .

Economy and Transport

Upper Inn Valley junction of the Inntal motorway, Inn, Arlberg railway and north portal of the Landeck tunnel

There are several commercial locations in the Upper Inn Valley, but many residents still commute. Landeck, Imst and Telfs used to be centers of the textile industry. There are good conditions for agriculture in the wider valley sections and on the low mountain ranges. Due to the previously common real division , the corridor is more structured than in the Lower Inn Valley. In contrast to the side valleys, tourism only plays a minor role.

The Upper Inn Valley is an important traffic axis, the Arlberg Railway , the Inntal A12 motorway  and the Tiroler Straße run here . In addition to the east-west traffic from Innsbruck towards Arlberg , the north-south traffic across the Alps from the Fernpass to Reschen , like the ancient Via Claudia Augusta , also uses part of the valley.

panorama

View from the east of the Oberinntal and the Mieminger Plateau between the Northern Sellrainer Mountains (left) and the Mieminger chain (right)

Web links

Commons : Oberinntal  - Collection of images, videos and audio files

Individual evidence

  1. ^ A b Central Institute for Meteorology and Geodynamics: Climate data from Austria 1971–2000
  2. ^ Land Tirol: Planning associations Landeck and surroundings , Imst and surroundings , Inntal - Mieminger Plateau , Telfs and surroundings - Salzstraße