Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 Research history  





2 Limes  





3 Footnotes and references  





4 Literature  














Lautertal Limes






Deutsch
Français
 

Edit links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 


The Lautertal Limes (in German also: SibyllenspurorSybillenspur) is a Roman limes section of the early 2nd century which is located between the River Neckar and the Swabian Jura. It extends for a distance of 23 kilometres (14 mi), running, straight as a die, from the present-day municipality of Köngen on the Neckar (Lat: Grinario) in the northwest to Donnstetten (Lat: Clarenna) in the Swabian Jura to the southeast.[citation needed]

Research history

[edit]

The 600-metre long crop mark in the form of a long strip, known in German as the Sibyllenspur, in the Lauter valley between Dettingen and Owen under Teck has been known about for a long time.[1] It was interpreted differently in the past, and there is even a legend according to which it was the track of a cart belonging to a sibyl. Soil scientists and geologists thought the strip of land might be a geological discontinuity or an old processional way or a road. The first investigations were carried out in 1976 by soil scientist and geologist, Siegfried Müller, in collaboration with the Schwäbischer Albverein. The results of this study revealed an archaeological site consisting of a straight ditch system, which was classified as Roman as the result of the discover of sherds. The Kirchheim local historian, Eugen Schweitzer, brought to the table the thesis that the Sibyllenspur was a limes and thus part of the great European network of Roman centuriation.[2]

In the dry summer of July 1976, aerial archaeology by Walter Sölter discovered the fortlet on the hill of Hasenhäuslesberg near Donnstetten. This find reinforced the theory of a Roman limes between Köngen and Donnstetten. This was finally confirmed that same year by the then archaeological monument conservationist of the administrative region of Stuttgart, Dieter Planck, who also evaluated the 1976 aerial photographs by Alfred Brugger. However, the thesis of the centuriation network was not able to be proven archaeologically. In 1978 the Sibyllenspur was first named by Eugen Schweitzer as the Limes in the Lautertal, connecting the Neckar Limes from the Roman fort of Köngen to the Alb Limes at Donnstetten Roman Fort.[3] Subsequent studies showed that the "Lautertal Limes" consisted of a palisade and three parallel ditches. Unlike the Upper Germanic-Rhaetian Limes, which was protected by two ditches, the ditches here run on the outside of the palisade.

Aerial photographs by Alfred Brugger uncovered another Roman fort behind the limesatDettingen unter Teck. Subsequent archaeological finds by the Landesdenkmalamt Baden-Württemberg in 1982 showed that the archaeological find was a Roman military camp intended for the direct protection of the Lautertal Limes.

Limes

[edit]
Scale drawing representing an artist's impression of the limes defences in the Lautertal

An excavation by the Landesdenkmalamt Baden-Württemberg in 1982 uncovered the following: the Sibyllenspur comprises three parallel ditches, the outer one in the northeast being a 3.20-metre-wide and 1.60-metre-deep V-shaped ditch. To the southwest, at a distance of 6 metres, is a 2.60-metre-wide and 1.4-metre-deep V-shaped ditch (2) and, behind it, 1.5 metres away, is a 70-cm-wide and 1.10-metre-deep U-shaped ditch (3), into which the wooden posts of a palisade were driven. This presented a wooden obstacle on the enemy side; against which on the inside was probably an earthen bank (vallum). The excavation confirmed the presence of the Roman fortlet, seen on the aerial photograph taken by Dieter Planck, behind the ditches.

During these excavations, two fragments of terra sigillata vessels were found in the ditch. The sigillata were able to be dated to around 120 to 130 AD, based on the manufacturer's seal by the potter, Satto, who worked at the terra sigillata pottery in Chémery-lès-Faulquemont (historically German: Schemmerich) near Faulquemont (German: Falkenberg) in Gallia Belgica. These artefacts classify the Sibyllenspur with its V-shaped ditches and the wood and earth rampart as the long-sought connection between the Domitian Neckar Limes and the Alb Limes.[4]

Footnotes and references

[edit]
  1. ^ Filtzinger, Aalen pp.32ff.
  • ^ Planck 2005; Schweitzer 1983
  • ^ Schweitzer based his thinking on research by Siegfried Müller in 1976
  • ^ Handbuch der Baden-Württembergischen Geschichte. 1. Allgemeine Geschichte. Teil 1 Von der Urzeit bis zum Ende der Staufer, Klett-Cotta, 2001, p. 20.
  • Literature

    [edit]

    Monographies

    Articles


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Lautertal_Limes&oldid=1217570270"

    Categories: 
    Roman frontiers
    Heritage sites in Baden-Württemberg
    Reutlingen (district)
    Esslingen (district)
    Roman fortifications in Germania Superior
    Hidden categories: 
    Articles with short description
    Short description is different from Wikidata
    All articles with unsourced statements
    Articles with unsourced statements from April 2023
     



    This page was last edited on 6 April 2024, at 16:36 (UTC).

    Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Mobile view



    Wikimedia Foundation
    Powered by MediaWiki