Abstract

The Benedictine Convent of Saint John at Müstair is a UNESCO World Heritage Site located in the eastern part of Switzerland close to South Tyrol’s border (Italy). Known as a well-preserved Carolingian building complex housing Carolingian and Romanesque frescoes, the convent has received much academic attention. However, all research activities so far have been concentrated on the area enclosed by the convent’s walls, even though the neighbouring fields to the east and south are also part of the convent’s property. This paper reports on the archaeological magnetic and ground-penetrating radar surveys of these areas, executed as part of a pilot project exploring the convent’s immediate environment. At present, these fields are used for agriculture and located on a massive alluvial fan of the mountain stream Valgarola. Dense geophysical sampling revealed an intricate network of distributary channels with stream and mudflow deposits, constituting a natural border of the convent’s territory. In addition to different field systems, a newly discovered broad pathway appears to be an original Roman road. Numerous structural elements, mapped within the convent’s walls, could be attributed to specific building phases. Over 40 large and deep burial shafts, arranged in three rows, were discovered outside the convent’s burial ground. Their specific design and arrangement are characteristic of early medieval burials, such as those of the 6th century Lombards on the edge of the eastern Alps.

Highlights

  • The Benedictine Convent of Saint John at Müstair (Canton of Grisons, Switzerland) was built around AD 775 during the reign of Charlemagne and is presently located near the border of South Tyrol (Italy)

  • In survey area 1, the GPR data reveal large meandering reflective structures with different sizes and shapes. They start at a depth of 50 cm beneath the present surface and can be traced further downward in the data. These reflecting structures, which widen as they deepen, could be fluviatile deposits connected to the alluvial fan of the Valgarola mountain stream, which flows into the Rom river near the convent (Figure 2)

  • (see the upper right inset of Figure 5). These findings show how the inhabitants reshaped the landscape around the Convent of Saint John and regulated the natural water flows for their specific needs

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Summary

Introduction

The Benedictine Convent of Saint John at Müstair (Canton of Grisons, Switzerland) was built around AD 775 during the reign of Charlemagne and is presently located near the border of South Tyrol (Italy). These scholars examined and documented the convent buildings, which led to discovering its Carolingian and Romanesque wall paintings. These well-preserved frescoes were the main argument to date the original building complex to the Carolingian period. They secured a UNESCO World Heritage Site label in 1983 [1]. Significant restoration and renovation activities started in 1964, which lead to the creation of the “Pro Kloster St. Johann in Müstair” foundation.

Panoramic
The depicts the the main main river river Rom
(4). Background
Geophysical
Data Processing
Results and Discussion
Natural Fluvial Features
These structures mustwere be drainage channorth of the convent
Overview of the known historical structures and prospection additions area
Herb Garden
Building Structures Connected to the Convent
Carolingian and Undated Building Southern Structures
Around
Overview
Burial Grounds
The Nun Graves
Row Graves
Conclusions and Outlook
Full Text
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