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Founding
Founding of Oppidum du Fossé des Pandours
2nd-century BC Celtic urban center
- 2nd century – 2nd century BCE
- Europe
Founding
2nd-century BC Celtic urban center
Fetching the article from Wikipedia…
The Oppidum du Fossé des Pandours is an urban center of the Celtic people known as the Mediomatrici. It was established near the Saverne Pass, within the territory of the modern communes of Saverne and Ottersthal (Bas-Rhin). It is the largest oppidum in the region of Alsace.
The territory of the Mediomatrici is home to several oppida. Although the Fossé des Pandours has yet to be fully excavated, several factors indicate that it was the largest oppidum of the Mediomatrici in Alsace, at least until the arrival of Ariovistus in the region. The Fossé des Pandours is one of two known archaeological sites at the Saverne Pass, the other being the Gallo-Roman station of Uspann. A Gallo-Roman necropolis was also discovered to the west of the oppidum.
The site's name originated in the 18th century when it was used to refer to the Pandours of Baron von Trenck during the War of the Austrian Succession (1740–1744). This conflict originated from opposition to the Pragmatic Sanction, a decree issued by Emperor Charles VI of the Holy Roman Empire that bequeathed the hereditary territories of the House of Habsburg to his daughter, Maria Theresa of Austria. In 1744, these mercenaries, serving under the command of Maria Theresa, successfully occupied Saverne.
The Vosges Mountains constitute a substantial barrier between the Lorraine Plateau (part of the eastern Paris Basin) and the Rhine Plain. The most accessible crossing points are the Saverne Pass (417 m) in the north and the Belfort Gap (345 m) in the south. The intervening valleys are precipitous, rendering the establishment of cart roads a challenging endeavor.
The Saverne Pass occupies a central position in the strategic west-east axis that connects central Gaul (comprising the territories of the Carnutes, Senones, Tricasses, and Remi) with the Rhine Valley.
The topography of the Saverne area is typified by elevated terrain and a rugged landscape. This is situated within a distinctive geological zone, the Saverne Fault Field, which forms part of the Rhine Graben. This geomorphological feature is responsible for the distinctive rolling topography of the pre-Vosgian hills.
The oppidum consists of three summits: Barbarakopf, Baerenkupfel, and Koepfel, which extend southward to another Vosgian summit, Kaestenberg.
The Mediomatrici were one of the Celtic peoples who settled in the area between the Rhine and the Pyrenees from the 6th century BC onwards. This region, which the Romans later named Gaul, was occupied by the Mediomatrici between the Meuse and the Rhine, from Argonne to the Black Forest. Their capital was the oppidum of Divodurum, which is now known as the Sainte-Croix district in Metz.
The territory of the Mediomatrici exercised control over a trade route between Gaul and Germania, which included the Saverne Pass. In the 2nd century BC, they constructed a fortress at this location, presumably to monitor the pass and take advantage of a rocky promontory overlooking the site.
This settlement of the Mediomatrici was one their oppida, at about 77 miles from Divodurum Mediomatricorum, their capital. Their territory, spanning approximately 250 km, encompassed at least eight oppida situated along river and road routes. The Fossé des Pandours, due to its considerable size, represents one of the largest oppidum in this area.
The term "oppidum" described fortified Celtic settlements that often served as important economic and political centers. While the early protohistoric settlements were relatively small, those constructed during the Gallic period were significantly larger. During the transition between the 3rd and 2nd centuries BC, settlements in the Celtic world, particularly those located along trade routes, experienced a period of growth, with notable developments in Gaul during the 2nd and 1st centuries BC. These settlements are regarded as the "first cities north of the Alps."
The Fossé des Pandours oppidum was probably created ex nihilo, as no evidence of previous Gallic occupation has been found. It dates from the end of the 2nd century BC, with the murus gallicus and other elements discovered dating from this period. It was occupied until the beginning of the Common Era. The excavations suggest a single construction phase following a coherent and planned program. The oppidum covers 170 hectares and is considered by Heitz to be "one of the largest in independent Gaul".
The site is a promontory fort. Part of the oppidum is naturally defended by cliffs, but additional fortifications were necessary, leading to the construction of the "Fossé des Pandours", a 600-meter-long and 10-meter-high fortification. The main rampart was complemented by a perimeter wall of about 7 kilometers. This fortification system is typical of the Oppida of the late La Tène period.
The fortress at the Saverne Pass lost its importance after Ariovistus invaded the region (c. 70 BC) and Julius Caesar's establishment of the Triboci on the Rhine plain (after 58 BC), although the site remained under the control of the Mediomatrici until Augustus reorganized Gaul. A possible sign of the site's decline is the lack of restoration of the murus gallicus, which normally requires repair or rebuilding every 30 years. The site probably lost its rank after the Gallic Wars.
Archaeologists have found artifacts from the late La Tène period on the Baerenkupfel. This Baerenkupel wall was built later, during a phase of settlement contraction to the two peaks of Barbarakopf and Baerenkupfel, leaving Koepfel outside the main enclosure.
According to Fichtl, the capital of the Mediomatrici shifted westwards from the middle of the 1st century BC. In Roman Gaul, the main axis of circulation became the Rhône-Saône-Moselle line, and the strongholds on this axis were strengthened, while those on the old west-east axis declined. However, this hypothesis is very controversial and is not accepted by many scientists.
The site remained occupied throughout the 1st century, but no longer had a significant political or economic role.
It was crossed by the Roman road from Strasbourg to Metz and a road relay (at the site of Uspann) was set up to provide travelers with fresh horses. The exact size of the site is unknown as it was partially destroyed during 18th-century road works and partial excavations. The Uspann site was abandoned in the late 2nd or early 3rd century.
A necropolis and sandstone quarries bear witness to the continued occupation and exploitation of the site. The sandstone quarry may have been in use during the Gallic period, but there is no evidence of this. The necropolis, dating from the second half of the 2nd and early 3rd centuries, yielded 17 burials and a house-shaped stele. In the Celtic world, necropolises were located outside oppida and along roads, similar to the Roman civilization.
Restorations and modifications may have taken place in the 9th and 10th centuries; in particular, the two sections of the wall between Baerenkupfel and Koepfel are thought to date from this period, according to the Mérimée database. Fichtl does not give a date.
The construction of the royal road from Paris to Strasbourg between 1730 and 1737 led to the destruction of about 150 meters of the rampart.
During the War of the Austrian Succession (1740–1744), mercenaries in the service of Austria under Maria Theresa - Hungarians or Croats, according to Heitz - occupied the site for a time in 1744 and gave it their name, Pandours. They also left other traces of their stay, including place names and legends.
Despite being identified by Forrer as early as 1926, the site was "long neglected." The site was ultimately incorporated into the supplementary inventory in 1989.
The initial archaeological works date from the early 20th century, yet they remained superficial. The second half of the century saw a greater level of activity, with intermittent excavations of the Uspann road station from 1949 to 1993 and excavations of Gallo-Roman tombs in 1980.
Excavations of the oppidum commenced in 1995 as part of a field school directed by the archaeology department of the University of Strasbourg. The Fossé des Pandours wall was excavated between 1995 and 1999, and the Barbarakopf habitation was excavated in 2000 and 2001, uncovering a craft area. After the 2003 publication, excavations continued, and various operations benefited from skidding work or the creation of forest tracks.
In addition to utilizing topography, Oppida constructed supplementary defensive structures for their late fortifications. The Oppidum covers an area of 160 to 165 hectares. To address the absence of uninterrupted natural protection, in addition to the 600-meter-long barrier rampart that obstructs access from the north via the Lorraine plateau, ramparts were constructed, collectively measuring approximately 7 kilometers in length and encompassing the entire site.
The archaeological excavations yielded a murus gallicus from the La Tène period, specifically period D1, dated to approximately 100 BC. This was based on the findings from the 1995 and 1996 excavation campaigns. A single construction phase has been identified, accompanied by substantial preliminary earthworks. Such buildings were pervasive throughout Gaul and were chronicled by Caesar in Commentaries on the Gallic War. The ramparts are described as "wood architecture", not dry stone, wherein the stones had no structural function and served merely as cladding.
The beams were embedded in sand and fastened with iron, and the entire structure was faced with pink sandstone. The rampart, measuring approximately 12 to 13 meters in width at its base, was faced with sandstone, which was preserved at a height of 1 meter. This refined facing is a distinctive feature of the Alsace site, as stones are typically laid in dry-stone construction and are not carved. The stones forming the base of the structure were larger than those used in the upper levels. An internal framework provided stability to the wall and situated behind the rampart was an earth embankment and a filled-in ditch. The preceding earthworks were extensive, with beams measuring 2 to 4 meters in length, fitted with nails measuring 0.16 to 0.32 meters in length, and stones filling the gaps. The intersecting beams provided lateral stability to the wall, with a height of approximately 60 to 70 cm at the base and reaching up to 5 to 6 meters, with the beams spaced 1.50 to 1.60 m apart. The pink sandstone cladding protected the wooden structure, although the ends of the perpendicular beams were initially visible. The rear of the rampart featured a ramp.
The exterior of the fortification was equipped with a 12-meter glacis, which preceded a ditch measuring between four and seven meters in width. The interior of the fortress featured a 10-meter-wide sand embankment. The murus gallicus structure was approximately 40 meters in width and 10 meters in height. The structure bears a resemblance to that of the wall at Alesia. Excavations conducted in the Barbarakopf region have revealed that the clay soil was reinforced with stones to support the weight of the rampart, indicating the involvement of "significant earthworks." Excavations on the northern slope of Kaestenberg have uncovered a rampart, despite its poor condition, measuring approximately 1.50 m in width. The sand fill has been observed to include beams fastened with nails, suggesting that these additions were introduced to stabilize the rampart.
Three additional ramparts are present on the site. Two modest, parallel inner ramparts were identified, situated between the heights of Baerenkupfel and Koepfel. However, these are not from the Gallic period, according to Fichtl. While the precise date is not specified, it is evident that this is a later construction, postdating the 3rd century.
The Baerenkupfel rampart was partially excavated. The posts were spaced at intervals of between four and five meters, and horizontal beams were probably used to supplement them, in contrast to the other ramparts. Furthermore, this rampart was devoid of embankments. The structure of the rampart was relatively simple, consisting of a ramp constructed of sand layers, with stones at the front measuring approximately one meter in width and a stone facing, and unaligned stone slabs at the rear.
The wall elements of the Fossé des Pandours exhibit a number of shared characteristics. Archaeological excavations have revealed that the bases of the facing were not designed with a focus on achieving horizontality. Instead, the facing was carefully cut on its front side.
Text from the Wikipedia article “Oppidum du Fossé des Pandours”, available under CC BY-SA 4.0.