Published 2009 | Version v1
Miscellaneous

Application of a terrain model in the interpretation and evaluation of a magnetic survey carried out for archaeological purposes in Porolissum, Romania

  • 1. Eoetvoes Lorand University, Budapest (Hungary). Department of Geophysics and Space Science
  • 2. Babes-Bolyai University, Cluj-Napoca (Romania). Department of Archeology and History of Ancient Times
  • 3. Eoetvoes Lorand University, Budapest (Hungary). PhD School of Historical Sciences
  • 4. Hungarian Academy of Sciences, Eoetvoes Lorand University, Budapest (Hungary). Research Group of Geology, Geophysics and Space Science
  • 5. Museum of History and Arts, Zalau (Romania)

Description

Complete text of publication follows. Presently, both geophysical surveying and archaeological excavation requires precise determination of local coordinates and occasionally, the creation of a Digital Terrain Map. Besides topography implies essential information for archaeology in itself, combination of topography with geophysical data is able to give further knowledge about the archaeological objects. We carried out a high-resolution magnetic survey over the Roman-age ruins of the ancient town, Porolissum located in NW Romania. We surveyed an area of 100 m x 120 m with grid spacing of 0.5 m and we measured the total magnetic field and its vertical gradient. In this case study we present how joint application of magnetic and geodetic data can be used for topographic correction and interpretation of the magnetic anomaly map. Magnetic topographic correction is defined here as the removal of disturbing magnetic signals caused by the topography. In this procedure the induced magnetic field is calculated using the geomagnetic field of the Earth and the magnetic susceptibility of the soil. The induced magnetic field is subtracted from the measured data. We also investigate the magnitude of the induced field considering three different susceptibility values (0.0035, 0.005 and 0.01 SI) of the soil. In the correction the remanent magnetization of the soil is neglected. The correction was made for both the total field and the gradient. With the help of the topographic correction the obtained anomaly maps contain more details and they are easier to interpret. The corrected magnetic gradient map shows streets and foundations of houses like a present day city map. In some places two generations of houses built on top of each other's foundation can be recognized as the walls of different ages have different directions. The magnetic maps proved to be very useful in reconstructing the structure of the ancient city.

Part of:
International Association of Geomagnetism and Aeronomy IAGA 11. Scientific Assembly

Additional details

Identifiers

Publishing Information

Publisher
Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences
Imprint Place
Sopron (Hungary)
Imprint Title
International Association of Geomagnetism and Aeronomy IAGA 11. Scientific Assembly
Imprint Pagination
[1212 p.]
Journal Page Range
[1 p.]
Report number
INIS-HU--010

Conference

Title
International Association of Geomagnetism and Aeronomy IAGA 11. Scientific Assembly
Dates
23-30 Aug 2009
Place
Sopron (Hungary)

INIS

Country of Publication
Hungary
Country of Input or Organization
Hungary
INIS RN
41072796
Subject category
S58: GEOSCIENCES;
Resource subtype / Literary indicator
Conference, Non-conventional Literature
Descriptors DEI
ARCHAEOLOGY; EXCAVATION; MAGNETIC FIELDS; MAPS; ROMANIA; TOPOGRAPHY
Descriptors DEC
DEVELOPING COUNTRIES; EASTERN EUROPE; EUROPE

Optional Information