Örtze
Sign in to saveÖrtze () is a river of Lower Saxony, Germany. The Örtze rises north of Munster in the Große Heide (in the Raubkammer federal forest) and, after , joins the Aller southeast of Winsen.
Key facts
- River<! de:Template:Infobox Fluss >.name
- Örtze
- River<! de:Template:Infobox Fluss >.image
- ÖrtzeHermbg.jpg
- River<! de:Template:Infobox Fluss >.image_caption
- The Örtze near Hermannsburg
- River<! de:Template:Infobox Fluss >.subdivision_type1
- Country
- River<! de:Template:Infobox Fluss >.subdivision_name1
- Germany
- River<! de:Template:Infobox Fluss >.subdivision_type2
- State
- River<! de:Template:Infobox Fluss >.subdivision_name2
- Lower Saxony
- River<! de:Template:Infobox Fluss >.length
- (with Aue and Wietze )
- River<! de:Template:Infobox Fluss >.source1_location
- north of Munster in the Große Heide (Bundesforst Raubkammer)
- River<! de:Template:Infobox Fluss >.mouth_location
- into the Aller southeast of Winsen
- River<! de:Template:Infobox Fluss >.tributaries_right
- Ilster, Wietze, Brunau, Brandenbach, Hasselbach, Mühlenbach
- River<! de:Template:Infobox Fluss >.tributaries_left
- Kleine Örtze, Schmarbeck and Sothrieth (discharge as the Landwehrbach into the Örtze), Weesener Bach, Angelbach
- River<! de:Template:Infobox Fluss >.custom_label
- References
via Wikipedia infobox
Wikidata facts
- Instance of
- river
- Country
- Germany
- Located in
- Lower Saxony
- Image
- ÖrtzeHermbg.jpg
Show 3 more facts
- P403
- Aller
- P974
- Brunau
- P8168
- Marlene Fuchs
via Wikidata · CC0
Article
12 sectionsContents
- Source and course
- Fauna and flora
- Boating on the Örtze
- In literature
- Meadow irrigation
- Timber rafting
- History
- Technology
- See also
- References
- Sources
- External links
Örtze () is a river of Lower Saxony, Germany. The Örtze rises north of Munster in the Große Heide (in the Raubkammer federal forest) and, after , joins the Aller southeast of Winsen.
== Source and course == The Örtze valley is an old glacial valley. It was formed during the Saale glaciation about 230,000 to 130,000 years ago by the drainage of meltwater from the ice sheet which cut deep into the plateaus of the southern Lüneburg Heath. The upper Örtze has incised its own, much smaller valley into the sandur beds and the roughly wide, flat glacial valley floor.