ΓΕΩΚΛΗΡΟΝΟΜΙΑ/ΜΕΤΑΛΛΕΥΤΙΚΗ ΠΕΡΙΗΓΗΣΗΓΕΩΛΟΓΙΑ/ΚΟΙΤΑΣΜΑΤΟΛΟΓΙΑΜΕΤΑΛΛΕΥΤΙΚΟ ΛΑΥΡΙΟ

The Lavrion Mines: A Unique Site of Geological and Mineralogical Heritage

Lavrion belongs to the world mineralogical, geological, mining, and archaeological heritage and can be considered as a mineralogical-petrological treasure trove. The geotouristic development of Lavrion combined with the foundation of a new Mineralogy Museum ensures the preservation of the geological heritage and also offers the opportunity for sustainable development.
The unique geological, mineralogical, and educational (mining, archaeological, and environmental) features suggest that it is highly suitable to be developed as a future UNESCO Global Geopark. Field photos showing typical lithologies and tectonic features in the Lavrion area.
Field photos showing various mineralization styles at Lavrion
Field and underground photos showing evidence of ancient and modern mining activity, ore dressing, and metallurgical facilities at Lavrion.

The Lavrion area corresponds to the western part of the Attic-Cycladic metamorphic belt, in the back-arc region of the active Hellenic subduction zone. Between the Eocene and the Miocene, metamorphic rocks (mainly marbles and schists) underwent several stages of metamorphism and deformation due to collision and collapse of the Cycladic belt. Exhumation during the Miocene was accommodated by the movement of a large-scale detachment fault system, which also enhanced emplacement of magmatic rocks, leading to the formation of the famous Lavrion silver deposits.

Supergene oxidation, secondary (and primary) minerals at Lavrion.
List of the 23 type locality (TL) minerals from Lavrion area (data from mindat.org page of Branko Rieck- https://www.mindat.org/loc-1942.html   and related articles).

The area around the mines shows the stacking of nappes, with ore deposition mainly localized within the marbles, at marble-schist contacts, below, within, or above the detachment. The Lavrion deposit comprises five genetically-related but different styles of mineralization, a feature never observed in another ore deposit elsewhere, containing the highest number of different elements of any known mining district. The local geology, tectonic, and magmatic activity were fundamental factors in determining how and when the mineralization formed.

Other key factors, such as the rise and the fall of sea level, which resulted from climate change over the last million years, were also of major importance for the subsequent surface oxidation at Lavrion that created an unmatched diversity of secondary minerals. As a result, the Lavrion deposit contains 638 minerals of which Lavrion is type-locality for 23 of them, which is nearly 12% of all known species. Apart from being famous for its silver exploitation, this mining district contains more minerals than any other district on Earth.

Lavrion belongs to the world mineralogical, geological, mining, and archaeological heritage and can be considered as a mineralogical-petrological treasure trove. The geotouristic development of Lavrion combined with the foundation of a new Mineralogy Museum ensures the preservation of the geological heritage and also offers the opportunity for sustainable development.

This district should become part of the Global Network of Natural Geoparks, following a policy which enhances the natural mineral wealth so as to protect and promote it for educational, research, and social purposes.

See the full paper in the attached file.

Keywords: Lavrion; Attica; minerals; ore deposits; geoheritage; cultural heritage; geotope

Σχετικά Άρθρα