Krummennaab

The German Continental Deep Drilling Programme (German: Kontinentales Tiefbohrprogramm der Bundesrepublik Deutschland, lit. 'Continental deep-drilling program of the Federal Republic of Germany'), abbreviated as the KTB borehole, was a scientific drilling project carried out from 1987 to 1995 near Windischeschenbach, Bavaria. The main super-deep borehole reached a depth of 9,101 m (29,859 feet) in the Earth's continental crust. The Federal Ministry of Research funded the project with 528 million DM (270 million euros). The (Lower Saxony) LBEG mining office (State Office for Mining, Energy and Geology) took the project lead. After the drilling project ended, the German Research Centre for Geosciences used the borehole to install a seismic deep observatory (Tiefenobservatorium) which was active from 1996 to 2001. The derrick used at the site, one of the largest in the world, remains in place and has become a tourist attraction. The two boreholes were kept open for further scientific research and for in-situ testing of equipment and devices.

Erbendorf (German pronunciation: [ˈɛʁbm̩ˌdɔʁf] ) is a town in the Upper Palatinate (Oberpfalz) region of Germany. As of December, 2006, the town has a population of 5,341. The following villages are incorporated into the town: Aschenhof, Birkenreuth, Boxdorf, Eppenhof, Frodersreuth, Glashütte, Gössenreuth, Gramlhof, Grötschenreuth, Hauxdorf, Inglashof, Napfberg, Neuenreuth, Pfaben, Plärn, Schadenreuth, Siegritz, Steinbach, Straßenschacht, Thann, Wäldern, Wetzldorf, and Wildenreuth.

Kirchendemenreuth is a municipality in the district of Neustadt an der Waldnaab in Bavaria, Germany. It includes the village (Dorf) of Steinreuth.

Friedenfels is a municipality in the district of Tirschenreuth in Bavaria, Germany.

The Fichtelnaab is a river, 47.5 kilometres long, in Upper Franconia and the Upper Palatinate, Bavaria, Germany. It rises in the Fichtel Mountains and flows into the Waldnaab near Windischeschenbach.

Windischeschenbach is a town in the district of Neustadt an der Waldnaab, in Bavaria, Germany. It is situated 14 km (8.7 mi) north of Weiden in der Oberpfalz. The German Continental Deep Drilling Programme, which reached a super-deep maximum depth of 9,101 metres (29,859 ft), is located near Windischeschenbach. Windischeschenbach is generally considered the centre of Zoigl beer.

The Parkstein, also called the Hoher Parkstein and Basaltkegel Hoher Parkstein is a well-known local hill and tourist destination in the Steinwald Mountains of central Germany. It lies 10 kilometres (6.2 mi) northwest of Weiden in der Oberpfalz in the district of Neustadt a.d.Waldnaab and is one of the most popular walking and daytripper destinations in North Upper Palatinate. Around the volcanically-formed hill, which is 595 metres (1,952 ft) above sea level (N.N.), is the village of the same name, Parkstein. At one time a castle (Parkstein Castle) stood on the summit. The Parkstein is famous for its impressive basalt outcrop. This basalt formation consists of pentagonal and hexagonal columns, up to one metre high, whose shafts extend into the earth to a depth of up to 30 metres. It is part of an old stream of lava that has been exposed at the surface after the softer rock above it had been weathered away over the course of millions of years. The wall of basalt measures 38 metres. Alexander von Humboldt viewed the Parkstein as the "most beautiful basalt cone in Europe". In 2004 it was entered by the Free State of Bavaria as No. 20 on the list of the 100 "most beautiful geotopes in Bavaria".

At 946 metres (3,104 ft), the Platte is the highest mountain in the Steinwald, a forest in the Fichtel mountain range in central Germany. The Platte is a popular walking destination, not least because of the Upper Palatinate Tower, which is located on its summit. It is climbable and offers good views of the surrounding region.

The Upper Palatinate Tower (German: Oberpfalzturm) is an observation tower on the 946 metres (3,104 ft) high Platte mountain, the highest peak in the Steinwald and in Northern Upper Palatinate in southern Germany. The first solid observation tower was built in 1971–1972 by the Steinwald Nature Park Authority from Steinwald spruce trees. Due to dilapidation it had to be demolished on 1 April 1998. The engineer, Ferdinand Lehner, from Tirschenreuth was then given the contract to design and build a new tower. On 10 September 2000 the new observation tower was opened. It is 35 metres (115 ft) high and was made of larch plywood. The contract was let by the town of Erbendorf. The total cost of construction came to about DM 400,000 and was supported by grants from the European Union, the Free State of Bavaria, the district of Tirschenreuth and the surrounding towns and villages. From the observation platform there are views of the Fichtel Mountains, the Karlovy Vary Region, the Stiftland and over the Upper Palatine Forest.

The Steinwald is a mountain range up to 946 m above sea level (NN) in southern Germany and, at the same time, a nature park (Steinwald Nature Park) founded in 1970 with an area of 246 square kilometres (95 sq mi) in the province of Upper Palatinate, in North Bavaria.

Parkstein (Northern Bavarian: Parkstoa) is a municipality in the district of Neustadt an der Waldnaab in Bavaria in Germany. In 2020, it counted approximately 2,300 inhabitants. The origins of its castle, built atop a conical shaped mountain, also called the Parkstein, date back to around the year 1000. A first written account of its existence can be traced back to the year 1053 in the documentations of the monks of Niederalteich of the Reichstag in Merseburg. Parkstein was chartered in 1435.Most likely in November 1796, Alexander von Humboldt called the 24-million-year-old basalt formation the most beautiful he had encountered in Europe. According to the Bavarian State Geology Office, during the Cenozoic, from Paleocene to the Pliocene epochs, a number of active volcanoes produced liquid magma in Northern Bavaria, mostly due to the continental collision of Europe and Africa. As a result, not only the Alps but a number of fissures and cracks began to form throughout central Europe where magma could rise. Most of the Parkstein's magma cooled below the surface, leading to the crystalline column formation that is now exposed as a result of erosion.

The Dürrschweinnaab is a river of Bavaria, Germany. It is a right tributary of the Sauerbach river (Naab basin) in Upper Palatinate. It arises at Großenbühl (448 m) from the confluence of the Lohbach and the Schwarzenmoosbach, northeast of Parkstein.