Geoarchaeology is the application of geological knowledge to archaeological sites. The Geoarchaeology Work Group in Mainz focuses primarily on the ancient culture of the Mediterranean region, particularly the Roman period. We specialize in researching ancient water supply systems such as aqueducts and the application of geological methods in antiquity. Our main task is the investigation of calcareous deposits in ancient aqueducts, water mills, lifting installations, and baths using fabric analysis and geochemical procedures. From these deposits, we obtain information about ancient water management, societal changes, the environment and climate of antiquity, as well as earthquakes. In addition to this core area, we research the use of building stones and quarrying operations in antiquity, the properties of Roman concrete, and attempt to reconstruct the understanding of geology and engineering among prospectors, architects, and engineers of antiquity.
- Hygienic conditions in Pompeii’s early baths were poor Calcareous deposits in wells, pipes, and bathing facilities provide insights into Pompeii’s ancient water supply
- The water management of ancient Arles Using carbonate fragments, researchers from Mainz, Oxford, and Innsbruck have deciphered the complex history of the aqueduct system of Arles
- Unknown microorganisms used marble and limestone as habitat Unusual structures are noticeable in the rock of desert regions, whose origin has not been clarified
- Carbonate layers open a view into the Roman era Researchers reconstruct the developmental history of the water mills of Barbegal through carbonate deposits
- Regular cleaning secured water supply via the Roman aqueduct of Divona Calcareous deposits in the water channel were systematically removed / Maintenance in accordance with Roman recommendations
- The aqueduct of Constantinople: How the longest water channel of antiquity was maintained Double water channels possibly served to maintain the facility during ongoing operation
- Material loss in the production of marble slabs was possibly lower in the Roman Imperial period than today Analysis of wall cladding from the 2nd century provides new insights into marble extraction and processing
We use other laboratories for our research work
Next class in Mainz will be from 17.2.2026 to 26.2.2026
It is possible to participate in only Part I (17th-21st of February) or Part II (23rd-26th of February) of the Microtectonics Masterclass, but we recommend joining both since they are complimentary. We invite participants external to the University of Mainz to join us for the classes, for a fee detailed below.
If you want to register, or have any questions, please send an e-mail to Friedrich Hawemann.
We offer two linked practical Masterclasses in Microtectonics at the University of Mainz, Germany. These courses should interest students, postdocs and professionals who wish to learn about the deformation of rocks on the microscopic scale.
Masterclass Microtectonics
Part I: Delivered by Prof. Virginia Toy and Dr. Friedrich Hawemann, which is entitled “Fault Rocks and Fault Mechanisms Revisited” will focus on how fault zone processes can be inferred from their textural record. The class will examine the set of thin sections and samples of fault rocks (mylonites, cataclasites, pseudotachylytes) from the Outer Hebrides Fault Zone (Scotland) that inspired Sibson (1977) to develop his widely-cited classification of fault rocks, and from New Zealand’s Alpine Fault Zone where he next applied this classification. Additionally, a set of exercises will examine microstructural datasets from both Outer Hebrides and Alpine Fault Zone samples acquired using advanced analytical tools, including SEM (EBSD, BSE-imaging), TEM, and synchrotron-CT. These exercises will demonstrate how to quantify the 2D and 3D arrangement and shapes of fault rock grains and particles, their textures, their crystallographic orientations, and the nature of porosity. The implications for fault rheology will be explored.
Part II: Delivered by Prof. Cees Passchier, teaches how deformation mechanisms can be inferred from the microstructures visible in thin sections. It is based on the book “Microtectonics” by Passchier and Trouw (2005), and the superb Microtectonics Collection of 300 selected thin sections that are the source of figures in that book will be examined during the course. The main topics, which are treated through an alternation of lectures and microscopy practicals, are: Principles of microtectonic analysis, overprinting relations, deformation phases and tectonic phases, flow and deformation, intracrystalline deformation, foliations and lineations, shear zones, veins and fringes, porphyroblasts, metamorphic reaction rims.