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Geological Formation

Ahr Valley

Valleys

The Ahr Valley is named for the Ahr, a left tributary of the Rhine in Germany, and begins at the Ahr spring in Blankenheim in the county of Euskirchen before running generally eastward. It enters the county of Ahrweiler in the state of Rhineland-Palatinate at its southernmost point, and bends northeast through the collective municipality of Adenau before reaching Altenahr, where it resumes its west-to-east course, interrupted by meanders. From Altenahr, in the section known touristically as the Ahrtal, the valley is characterized by vineyards on south-facing slopes and a picturesque rocky landscape, where the river has carved a gorge some 300 meters deep through the Ahr Hills. The valley continues past Bad Neuenahr-Ahrweiler before the Ahr discharges into the Rhine south of Remagen, in the borough of Sinzig. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Ahr Valley

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Ahr Valley
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Ahr Valley
Sources
Ahr Valley (Wikipedia)
Lead section
Quote, Lead section
The Ahr valley (German: Ahrtal, pronounced [ˈaːɐ̯taːl]) is named after the Ahr, a left tributary of the Rhine in Germany.
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Wikidata: Ahr Valley
Wikidata Q402908, class allow-list match (w-wdresolver-0926)View the Source
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