Hostname: page-component-5db58dd55d-smskv Total loading time: 0 Render date: 2026-06-02T02:32:59.902Z Has data issue: false hasContentIssue false

The LIEPPEC Project: using lidar for the study of long term landscape change

Published online by Cambridge University Press:  22 April 2026

Catherine Fruchart*
Affiliation:
MSHE Ledoux, Université de Franche-Comté, 30-32 rue Mégevand, Besançon 25030, France
Clément Laplaige*
Affiliation:
MSHE Ledoux, Université de Franche-Comté, 30-32 rue Mégevand, Besançon 25030, France
Rachel Opitz*
Affiliation:
Laboratoire Chrono-Environnement, Université de Franche-Comté, 16 route de Gray, Besançon 25030, France
Laure Nuninger*
Affiliation:
Laboratoire Chrono-Environnement - UMR 6249, CNRS, 30-32 rue Mégevand, Besançon 25030, France

Abstract

Information

Type
Project Gallery
Copyright
Copyright © The Author(s), [2011]. Published by Cambridge University Press on behalf of Antiquity Publications Ltd.
Figure 0

Figure 1. The location of Besançon and Mandeure-Mathay.

Figure 1

Figure 2. The Besançon and Mandeure-Mathay lidar surveys cover 140km2 and 81km2 respectively. Data was collected at a planimetric resolution of eight points per m2, with four returns per pulse.

Figure 2

Figure 3. Field systems north of Besançon in the Forêt de Chailluz are characterised by a combination of low linear stone mounds and natural terraces or cuttings forming boundaries and stone piles within fields.

Figure 3

Figure 4. Lime kilns are often found alongside small quarries, pits and charcoal burning platforms.

Figure 4

Figure 5. Examples of the remains found by the LIEPPEC project include: A-B) amorphous raised mounds interpreted as habitation sites; C-E the remains of buildings and enclosures, tentatively dated to the Gallo-Roman Period based on metal and ceramic objects found through prospection (1: linear mound forming an enclosure; 2: amorphous flat area probably representing a primary building — NB the number is placed immediately to the right of the flat area); F) ecclesiastical site with good morphological definition of the main building.

Figure 5

Figure 6. The magnetometry results: A) DTM of the medieval fortified Chamabon site with topographic features marked; B) results of the magnetometry survey draped over the terrain model; C) the principle anomalies visible in the magnetometry survey; D) a synthetic map showing both topographic and magnetic anomalies. Topographic anomalies 1, 2, and 3 correspond to magnetic anomalies.