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Bilstein-Höhlen

The road cutting between Oberbrombach and Bilstein shows the transition from the upper Hobräck beds through the Grenzkalk to the Mühlenberg beds and includes two caves, the Bilstein Höhle and the Bilsteiner Zwergenlabyrinth.

Overath

The road cutting between Oberbrombach and Bilstein shows the transition from the upper Hobräck beds through the Grenzkalk to the Mühlenberg beds and includes two caves, the Bilstein Höhle and the Bilsteiner Zwergenlabyrinth.

Characteristics

  • Type: Cave
  • Municipality: Overath
  • Record updated:

Caves are protected biotopes (§30 BNatSchG). Caves used by bats as winter quarters must not be entered from 1 October to 31 March (§39(6) BNatSchG), except show caves and their developed parts.

Location

The road cutting lies between Oberbrombach and Bilstein. The two caves, the Bilstein Höhle and the Bilsteiner Zwergenlabyrinth, lie in the area of the middle quarry above the road.

Map

Approximate position

Entrances

Always verify coordinates and access conditions before setting out.

  1. Bilstein-Höhlen

    50.982497, 7.254321
Download all entrances as GPX

Description

Morphology

Bilstein-Höhle: location: R 2588220, H 5650425; passage length: 10.5 m, height difference: 4 m. Bilsteiner Zwergenlabyrinth: location: R 2588190, H 5650325; passage length: 30.5 m, height difference: 3 m.

Other details

The road cutting between Oberbrombach and Bilstein shows excellently the transition from the upper Hobräck beds through the Grenzkalk to the Mühlenberg beds. The outcrop also shows the facies change of the former limestone reefs. At the bottom are fine sandstones with clayey-silty lenses and layers as well as sedimentary structures. These are unconformably overlain by an alternating sequence of biostromal reef limestones with marl and claystone layers. The limestones are partly fossil-bearing. Several normal faults dipping 55° to the north are also exposed. Above the Grenzkalk, the Mühlenberg beds are exposed along the path above the road and in two old quarries. Here there are calcareous rock layers with crinoid debris, shell and brachiopod layers, which can locally thicken into smaller limestone lenses. These then often also contain stromatoporoids and corals. On the bedding planes of the sandstones there are plant fragments, trace fossils, ripple marks and slump bodies. In the large quarry at the northern end of the profile, the succession of the upper Hobräck beds and their sedimentary structures can be studied particularly well on a high rock face. The geotope also includes 2 caves, the Bilstein Höhle and the Bilsteiner Zwergenlabyrinth.

History

Among other things, a pot-base sherd from the Iron Age was found there. Both caves were discovered in the year 2001 by the Arbeitskreis Kluterthöhle (AKKH).

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Source: Geotopkataster Nordrhein-Westfalen (Geologischer Dienst NRW) (ogc-api.nrw.de), modified. Data licence Germany – attribution – version 2.0 (dl-de/by-2-0), https://www.govdata.de/dl-de/by-2-0 Geowissenschaftliche Daten: INSP-GeotopeinNRW @ Geologischer Dienst NRW · data as of 2026