Geophysical survey to the Petrified Forest of Sigri in Lesvos Island (North Aegean)


Published: Jan 1, 2001
Keywords:
petrified forest geoelectrical survey magnetic survey radar
Γ. ΒΑΡΓΕΜΕΖΗΣ
Η. ΦΙΚΟΣ
Ι. ΜΕΡΤΖΑΝΙΔΗΣ
Ε. ΖΑΝΑΝΙΡΙ
Ζ. ΡΟΥΜΕΛΙΩΤΗ
Ν. ΖΟΥΡΟΣ
Ε. ΚΟΝΤΗΣ
Η. ΒΑΛΙΑΚΟΣ
Abstract

Remains of fossil plants, which form the famous «Petrified forest of Lesvos», have been found in many localities on the western part of Lesvos Island. The fossilized forest of Lesvos was developed during Late Oligocene to Lower - Middle Miocene, due to the intense volcanic activity in the area (Velitzelos and Zouros, 1997). The products of the volcanic activity had covered the vegetation of the area and the fossilization process took place due to favorable conditions. The fossilized plants in Lesvos are silicified remnants of a sub-tropical forest that existed on the northwest part of the island 20-15 million years ago. In the present study the results of the geophysical survey that has been applied to several locations of the petrified forest are presented. Electrical tomography, magnetic mapping and Ground Penetrating Radar methods of geophysical prospecting have been applied. The surrounding material, which is formed mainly by volcanic ash, contains also volcanic rocks in that size that it could be detected as petrified trunk. So, the effectiveness of the geophysical methods in such an environment has been tested in selected areas where petrified trunks were semi-uncovered. Lied trunks have been successfully detected by the electric tomography in several cases, since the resistivity of the fossilized material is much higher that the resistivity of the volcanic ash. The horizontal mapping of the total magnetic field in the same cases of lied trunks has been also successful since it was combined with the electric tomography and the anomaly were located in the same place and shape. Detection of petrified trunks looks to be uncertain in cases of standing trunks. That, because anomaly of the same pattern could be produced by an intrusion of a rock which the magnetic susceptibility is lower than this of the fossilized material. The same problem has been noticed also to the GPR (Ground Penetrating Radar) data. Several positions to be excavated have been proposed.

Article Details
  • Section
  • Geophysics
Downloads
Download data is not yet available.
References
BARKER R.D. (1992). A simple algorithm for electrical imaging of the subsurface. First Break, 10, 53-63.
ΒΕΛΙΤΖΈΛΟΣ Ε., ΖΟΎΡΟΣ Ν., ΣΕΡΑΪΔΗΣ Π. ΚΑΙ ΚΟΝΤΗΣ E. (1999). Συμβολή στη μελέτη της παλαιοχλωρίδας του απολιθωμένου δάσους της Λέσβου-Δημιουργία του γεωπάρκου Σιγρίου, Δελτίο Ελληνικής Γεωλογικής Εταιρίας τομ. XXXIII, σελ. 89-98.
SAVVAIDIS Α., TSOKAS G., LIRITZIS Y. AND M. APOSTOLOU (1999). The location and mapping of ancient ruins on the castle of Lefkas (Greece) by resistivity and GPR methods, Archaeological Prospection, 6, p63-73.
SHIMA H. (1990). 2-D automatic resistivity inversion technique using alpha centers. Geophysics, 55, 682-694.
TRIPP Α., HOHM-MANN, G. AND SWIFT, C. (1992). 2-D resistivity inversion. Geophysics, 57, 1004-1013.
TSOKAS G.N., GIANNOPOULOS Α., TSOURLOS P., VARGEMEZIS G., TEALBY J.M., SARRIS Α., PAPAZACHOS C.B., AND T. SAVOPOULOU (1994). A large scale geophysical survey in the archaeological site of Europos (northern Greece)Journal of Applied Geophysics 32, p.85-98.
TSOKAS G., PAPAZACHOS C.B., VAFIDIS Α., LOUKOYIANNAKIS M.Z., VARGEMEZIS G. AND K. TZIMEAS (1995). The detection of monumental tombs buried in tumuli by seismic refraction, Geophysics, Vol. 60, No. 6, p. 1735-1742.
TSOURLOS P., SZYMANSKI J., DITTMER J. AND TSOKAS G. (1993). The use of back-projection for fast inversion of 2-D resistivity data. Proceedings of the 2nd congress of the Greek Geophysical Union, Fiorina Greece, 5-7 May, Vol. 1, 71-81.
TSOURLOS P., DITTMER J. AND SZYMANSKI J. (1995). A study of non-linear techniques for the 2-D inversion of earth resistivity data. Expanded abstracts of the 57th meeting of the EAEG: Glasgow, Scotland, 29 May-2June, 1995, P031.
VELITZELOS, E. AND ZOUROS N. (1997). The Petrified Forest of Lesvos-Protected Natural Monument, Proceedings International Symposium on Engineering Geology and the environment, organized by the Greek National Group of IAEG/ATHENS/GREECE/23-27 JUNE 1997, pp3037-3043.
Most read articles by the same author(s)