The tower's current incline of 4.93 degrees exceeds Pisa's 3.99 degrees.
The base of the tower rests on unstable gypsum, which dissolves in water and creates massive sinkholes.
The tower was part of the Oberkirche, which had to be demolished in 1982 due to irreparable structural damage.
It is often referred to as the 'Oberkirchturm' by local residents.
Regular laser monitoring is used to track the tower's movement in real-time.
The Leaning Tower of Bad Frankenhausen, known as the Oberkirche tower, features a greater incline than the Leaning Tower of Pisa. It is the bell tower of the former Upper Church and currently leans at an angle of 4.93 degrees. The tilt resulted from the dissolution of subterranean gypsum layers caused by groundwater, a geological process active since the 14th century. The tower was decommissioned as a religious site in the 1960s due to structural instability and safety concerns. Extensive engineering stabilization efforts have been implemented to prevent further collapse. The structure stands on the edge of the Kyffhäuser mountain range. It serves as a visual marker for the local salt-mining and geological history of the region.
From the street level on Oberkirchgasse, capturing the contrast between the tilted tower and the straight vertical lines of adjacent buildings.
Check the official website for current stabilization status before visiting, as access to the interior can be restricted.
Wear comfortable walking shoes to navigate the sloping terrain surrounding the base.
Do not attempt to climb the tower if signs indicate the interior is closed for structural safety reasons.
The site is subject to periodic closures for geological surveys and structural maintenance; verify status on the official website.
