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Germany
Rhineland-Palatinate
Rhein-Hunsrück-Kreis
Morshausen

Theresia Mine Tunnel

Theresia Mine Tunnel

Recommended by 63 hikers out of 67

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    Best Hikes to Theresia Mine Tunnel

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    1. Baybach Valley Trail – Baybach Valley Trail loop from Morshausen

    14.7km

    04:13

    350m

    350m

    Intermediate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

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    Intermediate

    Intermediate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

    Intermediate

    Expert hike. Very good fitness required. Sure-footedness, sturdy shoes and alpine experience required.

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    Tips

    December 17, 2019

    One of the many mine tunnels in the Hunsrück, which were driven into the rock for ore, gemstone or slate quarrying. Most are closed by bars and serve as sheltered sleeping places for bats.

    Translated by Google •

      March 4, 2021

      Tunnel of the former "Theresia" ore mine.

      In the period from 1859 to 1886, lead, silver, copper and zinc ores were mined here by a mining company from Bendorf. The ore veins led into the mountain 250 meters with a width of up to 15 meters. (Source: From mill to mill)

      Translated by Google •

        August 24, 2021

        Theresia ore mine

        From 1859 to 1886, lead, silver, copper and zinc ore were mined from the spoil dump of the lower tunnel sole of the former "Erzgrube Theresia" and transported to St.Goar-Fellen for smelting. The upper tunnel sole reached about 20m into the mountain, the deep tunnel bottom, from the Baybachtal, approx. 250 m. The passages in the mountain followed the ore veins and were in places 10 to 15 meters wide. Because of "impossibility" and inefficiency, the operators stopped mining ore after only 27 years During the Second World War, many Morshausen citizens sought protection in the abandoned tunnels from the artillery fire of the advancing American troops

        Murscher ores and their origin

        Around 400 million years ago, the rocks were sediment from the seabed. The layers of different materials (sand and clay) deposited and solidified over millions of years. During the mountain formation 400-200 million years ago, the solid layers were folded into a mountain range by the continental shifts. This folding resulted in deep cracks and cavities. Hot, highly mineralized water made its way up along this path, and over time various minerals crystallized from the water and filled the cavities. The minerals include iron, zinc and lead ores, which were mined as ore veins in the period from 1859 to 1886. Source: Text information board

        Translated by Google •

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          Elevation 170 m

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          Wednesday 8 October

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          Location: Morshausen, Rhein-Hunsrück-Kreis, Rhineland-Palatinate, Germany

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