The Eifel is a hilly region in Germany. It occupies parts of southwestern North Rhine-Westphalia and northwestern Rhineland-Palatinate.
The Eifel is bordered by the Moselle River in the south and the Rhine in the east. In the north it is continued by the hills of the High Venn (Hohes Venn), in the west by the Ardennes. (Ardennes and Eifel are actually the same geological region. They are a single volcanic field.)
In the Tertiary the Eifel was a site of extensive volcanic activity. Some of the hills are volcanoes. The lakes of the regions are former volcanic craters (maars). The last eruptions took place around 10 000 years ago. The Eifel is a hotspot volcano. Research has shown that the Mantle plume is still active; the Eifel region is rising by 1-2 mm per year. Historically, the Eifel volcanoes had inactive phases of 10 000 to 20 000 years between active phases, suggesting there is a possibility of future eruptions.
There are several distinct hill chains within the Eifel.
Since 2004 about 110 km² of the Eifel are protected as the Eifel National Park.
An interesting archeological feature of the region is the Eifel aqueduct, one of the longest aqueducts of the Roman empire, providing the city of Cologne with water...