Großensee, Thuringia

Wildeck is a municipality in Hersfeld-Rotenburg district in northeastern Hesse, Germany lying right at the boundary with Thuringia, 54 km southeast of Kassel.

The Hornungskuppe (called the Hornsberg in the Middle Ages) is a wooded hill, 439 m above sea level (NHN), in the Thuringian Zipfel on the border of Hesse and Thuringia in Germany. It is part of the natural region of the Seulingswald. The Hornsberg was mentioned in documents dating to the 12th century in connexion with the eponymous noble family. It belongs to the parish of Widdershausen in the borough of Heringen in the Hessian county of Hersfeld-Rotenburg and the parish of Dankmarshausen in Thuringian Wartburgkreis. The border between the two German states runs over the hill. The Hornungskuppe is (still) used for forestry. The fenced in terrain on which the spoil tip of Monte Kali stands begins on its western slopes. Barely 500 metres to the northeast on a spur of the Hornungskuppe stands Hornsberg Castle.

Monte Kali and Kalimanjaro are local colloquial names for the spoil heap or spoil tip that towers over the town of Heringen, Hesse, Germany. It is one of a number of sites where the K+S chemical company dumps sodium chloride (common table salt), a byproduct of potash mining and processing, a major industry in the area. The names are puns of Kali (shorthand for Kalisalz, German for "potash") on "Monte Carlo" and "Kilimanjaro." The heap lies directly next to the border with the state of Thuringia, and hence next to the former inner German border with what was once East Germany. The heap rises over 250 metres (820 ft) above the surrounding land, its summit reaching 520 metres (1,710 ft) above sea level. According to the Werra Potash Mining Museum in Heringen, Monte Kali has been in operation since 1976; as of August 2016, it covered 98 hectares (240 acres) and contained approximately 201 million tonnes of salt, with another 900 tonnes being added every hour and 7.2 million tonnes a year.

Dankmarshausen is a village and former municipality in the Wartburgkreis district of Thuringia, Germany. Since 1 January 2019, it has been part of the town of Werra-Suhl-Tal.

Heringen (Werra) is a small town in Hersfeld-Rotenburg district in eastern Hesse, Germany lying right at the boundary with Thuringia.

Herfabach is a river located in Hersfeld-Rotenburg, Hesse, Germany. 11.3 kilometres (7.0 mi) in length, it is a west tributary of the Werra. It has a river basin area of 40.011 km ².

Herzberg is a hill of Hesse, Germany.

The Ecker is a 28-kilometre (17 mi), right-hand, southeast tributary of the Oker which runs mainly through the Harz mountains in the German states of Saxony-Anhalt and Lower Saxony.

The Kupferschiefer (German for Copper Shale, also called Copper Slate) or Kupfermergel (Copper Marl), (T1 or Z1) is an extensive and remarkable sedimentary unit in Central Europe. The relatively monotonous succession is typically 30 to 60 centimetres (12 to 24 in) and maximum 2 metres (6.6 ft) thick, but extends over an area of 600,000 square kilometres (230,000 sq mi) across the Southern Permian Basin. The Kupferschiefer can be found in outcrop or in the subsurface straddling six countries, including parts of the southern North Sea. The lateral equivalent outcropping in England is called Marl Slate. Despite its distinctive nature, the Kupferschiefer is not ranked as a formation but is officially declared a sub-unit of the Werra Formation, the lowest formation of the Zechstein Group, overlying the Rotliegend Group. The unit has been dated to 257.3 ± 1.6 Ma, placing it in the Wuchiapingian stage of the Late Permian. The Kupferschiefer comprises black shales, bituminous marls, mudstones and limestones deposited mostly in an open marine setting, with the borders of its extension deposited in a shallow marine environment. At time of deposition, the area what is now northern Europe was covered by an enclosed sea; the Zechstein sea, characterized by anoxic conditions. The Kupferschiefer is renowned for hosting one of the most important copper deposits in the world, which were mined at least since 1199 AD. Other mineral resources found in the unit include zinc, vanadium, lead and silver. The Kupferschiefer is also an important lagerstätte; having provided fossils of early Archosauromorph reptiles, the ancestors to modern crocodiles and extinct dinosaurs, as well as pareiasaurs, many fossil fish, including Coelacanthus granulatus, Dorypterus hoffmanni and Palaeoniscum freieslebeni, flora and other fossils. Famous finds from the unit include Parasaurus geinitzi, Protorosaurus speneri, Weigeltisaurus jaekeli and Glaurung schneideri.

The Richelsdorf Hills (German: Richelsdorfer Gebirge) is the name given to a landscape in the German Central Uplands. The terrain is up to 478.2 m above sea level (NHN) high and forms a landscape characterised by mining (copper shale, cobalt, nickel) in the county of Hersfeld-Rotenburg in East Hesse. Despite its German suffix Gebirge ("hill range") these hills are not a true hill range, but a cultural landscape. Locally this also includes the whole surrounding region in the southeast of the Fulda-Werra Uplands; parts of the county of Werra-Meißner-Kreis to the south and the extreme northwest of the Thuringian county of Wartburgkreis are included.

Dippach is a village and a former municipality in the Wartburgkreis district of Thuringia, Germany. Since 1 January 2019, it is part of the town Werra-Suhl-Tal.

The Weihe Viaduct (German: Weihetalbrücke) is a bridge of the A 4 motorway near Richelsdorf, Germany. It is located in the stretch of the A 4 between Bad Hersfeld (Hesse) and Eisenach (Thuringia), between the exits Wildeck-Obersuhl and Gerstungen. It crosses the valley of the small river Weihe. The bridge was intended to have been built at the beginning of the 1940s, but it wasn't finished then: only a few columns were built. Instead for the motorway a provisional route through the valley was constructed. In the 50 years to follow its construction was cancelled due to its location near the former border between the German Democratic Republic and the Federal Republic of Germany. After the 1990 German reunification, traffic increased considerably, and in 1992 construction of a new bridge was started. One of the old columns was kept as a monument. The new bridge (45 million DM construction costs) was inaugurated in 1994. It is a prestressed concrete bridge of 584 m, which rest on 8 columns.