Brohltal

Niederzissen is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany.

The Bausenberg is a cinder cone hill, 339.8 m above sea level (NN), in the East Eifel in the county of Ahrweiler in the German state of Rhineland-Palatinate.

Oberzissen is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany.

Waldorf is a municipality belonging to the Verbandsgemeinde Bad Breisig in the district of Ahrweiler, in Rhineland-Palatinate, Germany. In 2020 Waldorf had 866 inhabitants.

Galenberg is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany.

Niederdürenbach is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany.

Wehr is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany. Wehr is a small village off Bundesautobahn 61.

Schloss Allner is a fifteenth-century castle in Rhein-Sieg-Kreis, North Rhine-Westphalia, Germany. It is located on the southern slope of the Nutscheid Ridge, on the north bank of the River Sieg, and just northeast of the Allner See. It lies to the northeast of the town of Hennef, east of the district of Allner. During its history it has served as a residence, a municipal seat and an orphanage. During World War II it was the scene of an unsuccessful attempt by the Wehrmacht to halt the advancing Allied forces from crossing the Sieg and entering the Ruhr Valley.

Glees is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany. It lies near the Maria Laach Abbey.

Dedenbach is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany.

Brenk is a municipality in the district of Ahrweiler, in Rhineland-Palatinate, Germany.

The Veitskopf is a hill, 428 m above sea level (NHN), in the Eifel mountains of Germany. It is located in the county of Ahrweiler in the state of Rhineland-Palatinate. It rises north of the lake of Laacher See in the area of the village of Wassenach. The Veitskopf is the cinder cone of a volcano that erupted during the Quaternary period. Because there are no reference strata, its age cannot be accurately estimated. The Veitskopf produced three lava flows, of which the first and easily the largest spread out northwards from the crater rim in the west. Because the neighbouring valley, the Gleeser Tal, was formed after the eruption of the Veitskopf, this lava flow stands above the present valley and forms the so-called Mauerley. The two lava streams that run in a southerly direction are nowhere near as large and were first identified from magnetic surveys because they were covered by a layer of pumice. At the top of the Veitskopf is the Lydia Tower which enables an all-round view that includes the Laacher See, the Brohltal valley and even the Siebengebirge hills.