Crooked Steyr

from Wikipedia, the free encyclopedia
Crooked Steyr
The Krumme Steyr flows into the Steyr (right)

The Krumme Steyr flows into the Steyr (right)

Data
location Upper Austria
River system Danube
Drain over Steyr  → Enns  → Danube  → Black Sea
source on the eastern slope of the Great Priel
47 ° 42 ′ 50 ″  N , 14 ° 5 ′ 27 ″  E
Source height approx.  1360  m above sea level A.
muzzle southwest of Hinterstoder in the Steyr coordinates: 47 ° 41 '23 "  N , 14 ° 8' 3"  E 47 ° 41 '23 "  N , 14 ° 8' 3"  E
Mouth height approx.  610  m above sea level A.
Height difference approx. 750 m
Bottom slope approx. 14%
length approx. 5.3 km
Catchment area 20.66 km²
Discharge at the Polsterlucke
A Eo gauge : 15.6 km²
Location: 1.85 km above the mouth
NNQ (January 8, 2006)
MNQ 1976–2010
MQ 1976–2010
Mq 1976–2010
MHQ 1976–2010
HHQ (July 19, 1997)
0 l / s
10 l / s
2.31 m³ / s
148.1 l / (s km²)
21.1 m³ / s
36.8 m³ / s
Communities Hinterstoder

The Krumme Steyr is a 5 km long left tributary of the Steyr in the Totes Gebirge  in Upper Austria .

course

The Krumme Steyr rises between Unterer and Oberer Salmeralm on the eastern slope of the Great Priel  in the Dead Mountains. It initially flows steeply over steps and waterfalls south into the valley and then turns east on the wide valley floor. In the cushioned gap, it feeds the artificially created Schiederweiher via a ditch , which flows below into the Krumme Steyr. About 300 m further on, the river flows into the Steyr from the left.

Catchment area and water supply

The catchment area of the Krummen Steyr measures 20.7 km² and extends over around 1900 meters in altitude to the Großer Priel ( 2515  m above sea level ). The mean discharge at the Polsterlucke gauge is 2.31 m³ / s. The extremely high discharge of 148 l / s · km² can be explained by the fact that it is a karst area and the actual underground catchment area is considerably larger than that corresponding to the surface relief. The strong fluctuation in runoff with precipitation and snowmelt in spring can also be attributed to the location in the karst. The month with the most discharge is June with an average discharge of 6.70 m³ / s, more than fifty times the month with the lowest discharge, February (0.13 m³ / s).

nature

The entire course of the Krummen Steyr is very close to nature. Wide relocation stretches, on which the gravel beds fall completely dry at low tide, alternate with calmly flowing deep sections. The bank areas consist of various ecologically valuable grassland areas, which are characterized by the gravel soil and flooding.

Web links

Commons : Krumme Steyr  - Collection of pictures, videos and audio files

Individual evidence

  1. a b c Digital Upper Austrian Room Information System (DORIS)
  2. Federal Ministry of Agriculture, Forestry, Environment and Water Management (ed.): List of areas of the Austrian river basins. Enns area. In: Hydrographischer Dienst in Österreich (Hrsg.): Contributions to the Hydrographie Österreichs. Issue No. 61, Vienna 2011, p. 51 ( PDF on bmnt.gv.at ).
  3. a b Federal Ministry of Agriculture, Forestry, Environment and Water Management (Ed.): Hydrographisches Jahrbuch von Österreich 2010. 118th volume. Vienna 2012, p. OG 199, PDF (12.6 MB) on bmlrt.gv.at (2010 yearbook)
  4. ^ Office of Upper Austria. Provincial government (ed.): Mapping of natural areas in Upper Austria. Biotope mapping community Hinterstoder south-east and center. Final report. Kirchdorf an der Krems 2007, p. 66, PDF (9.5 MB) on ZOBODAT