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Germany

North Rhine-Westphalia

Düsseldorf District

Regierungsbezirk Düsseldorf

Die Roos (Rhine Oxbow Lake)

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Places to see

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Germany

North Rhine-Westphalia

Düsseldorf District

Regierungsbezirk Düsseldorf

Die Roos (Rhine Oxbow Lake)

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Die Roos (Rhine Oxbow Lake)

Recommended by 69 hikers out of 76

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Location: Regierungsbezirk Düsseldorf, Düsseldorf District, North Rhine-Westphalia, Germany

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Best Hikes to Die Roos (Rhine Oxbow Lake)

5.0

(7)

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1. Die Roos (Rhine Oxbow Lake) – View of the Rhine Bend loop from Eisenbahnsiedlung

6.52km

01:39

10m

Easy hike. Great for any fitness level. Easily-accessible paths. Suitable for all skill levels.

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Easy

5.0

(8)

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2. Die Roos (Rhine Oxbow Lake) – View of the Rhine Bend loop from Krefeld-Hohenbudberg Chempark

6.98km

01:47

20m

Easy hike. Great for any fitness level. Easily-accessible paths. Suitable for all skill levels.

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Easy

5.0

(5)

hikers

3. Die Roos (Rhine Oxbow Lake) – View of the Rhine Bend loop from Krefeld-Uerdingen

10.6km

02:43

50m

Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

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Moderate

Tips

PfotenTrio🐕🐶⭐🐕

November 1, 2018

A very beautiful and idyllic landscape. Beautiful dog round to relax.

Translated by Google •

January 30, 2022

further information e.g. here:
de.wikipedia.org/wiki/Naturreservation_Rheinaue_Friemersheim

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PeterH65 (a.k.a. "Waldorf")

January 22, 2024

>

"In the cold times, ice shaped the Lower Rhine, either through glaciers or a frozen subsoil (permafrost). At the same time, the sedimentation of moraines took place, which gave the flat Lower Rhine landscape at least a certain relief. The flowing waters at that time had different dynamics, depending on the Season and climatic phase are related to the water availability and the load with sediments. Rivers and streams were characterized by an overgrown runoff. In the last Vistula glaciation, the low terrace was created by filling up.

10,000 years ago, drainage patterns changed because the climate transitioned to our current warm period, the Holocene. The drainage was now more linear and the rivers formed the meanders that are still typical today. In doing so, they cut into the lower terrace. Smaller rivers and streams eventually silted up or became bogs.

However, the main receiving water, the Rhine, continued to deepen; At the same time, its (periodically flooded) floodplains and oxbow lakes emerged - such as the early Holocene "Die Roos", which was still a fully "functional" tributary of the Rhine in the middle of the 19th century.

The oxbow “Die Roos” lies largely in the west of the Rheinaue Friemersheim nature reserve. The area is, among other things, a refuge for insects (dragonflies). The use of parts of the water for fishing is being discussed critically, among other things in view of the seasonal water levels."

(Kai-William Boldt, Rhenish Association for Monument Preservation and Landscape Protection e.V. / LVR Department of Regional Cultural Work, Department of Landscape Cultural Preservation, 2016)

kuladig.de/Objectansicht/KLD-254808

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Elevation 20 m

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Friday 28 November

9°C

7°C

100 %

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Max wind speed: 14.0 km/h

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Location: Regierungsbezirk Düsseldorf, Düsseldorf District, North Rhine-Westphalia, Germany

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Die Roos (Rhine Oxbow Lake)

1. Die Roos (Rhine Oxbow Lake) – View of the Rhine Bend loop from Eisenbahnsiedlung

2. Die Roos (Rhine Oxbow Lake) – View of the Rhine Bend loop from Krefeld-Hohenbudberg Chempark

3. Die Roos (Rhine Oxbow Lake) – View of the Rhine Bend loop from Krefeld-Uerdingen

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