Abstract
Four Monasteries have been investigated as pilot monuments in the area of Mount Athos. In the present research the geotechnical conditions of the Monasteries foundation area are studied, regarding the description and the classification of the rock mass and the analysis of the rock slope stability. The area is very fractured and traversed by joints of various directions (mainly NNW, NNE and SSW). These discontinuities can generate unstable geotechnical conditions in the rock mass especially at the slopes of the construction areas.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Barton N, Choubey V (1977) The shear strength of rock joints in theory and practice. Rock Mech 6:1–54
Christaras B, Pavlidis S, Dimitriou A (1994) Slope stability investigation in relation to the neotectonic conditions along the south-western coast of Mount Athos (N. Greece). The case of Symonos Petra Monastery. Proceedings of the 7th Int. Congr. I.A.E.G., pp 1577–1583
Christaras B, Dimitriou A, Mazzini E (1995) Rockmass quality at the foundation area of the Simonos Petra Monastery, in Mount Athos, Greece. La Citta Fragile in Italy, 1° Convegno del Gruppo Nazionale di Geologia Applicata con la participatione della IAEG. Giardini Naxos (ME), pp 191–196
Dimitriou A, Christaras B, Dimopoulos G, Pavlides Sp (1997) Geotechnical aspects at four Monasteries in Mount Athos (N. Greece). A first approach of the stability conditions of the geological formations at their foundation sites. Int. Symp. of IAEG, Engin. Geol. and Env., Athens, Balkema Publ., pp 3113–3122
Hocking G (1976) A method for distinguishing between single and double plane sliding of tetrahedral wedges. Int J Rock Mech Min 13:225–226
Hoek E, Bray JW (1981) Rock slope engineering. Inst. Mining and Metal., London, pp 1–358
Kadas S (1989) Agion Oros. Ekdotiki Athinon, Athens
Kockel F, Mollat H (1977) Erläuterungen zur geologischen Karte der Chalkidiki und angrenzender Gebiete 1:100000 (Nord-Griechenland). Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover
Markland JT (1972) A useful technique for estimating the stability of rock slopes when the rigid wedge sliding type of failure is expected. Imperial College Rock Mech Research Report 19:1–10
Mercier JL, Sorel D, Simeakis K (1987) Changes in the state of stress in the overriding plate of a subduction zone. The Aegean Arc from Pliocene to Present. Ann Tectonicae 1:20–39
Papazachos B, Papazachou K (1989) Earthquakes of Greece. Ziti, Thessaloniki, pp 1–356
Pavlides S, Kilias A (1987) Neotectonic and active faults along the Serbomacedonian Zone (SE Chalkidiki, Northern Greece). Ann Tectonicae 1:97–104
Pavlides S, Mountrakis D, Kilias A, Tranos M (1990) The role of strikeslip movements in the extensional area of Northern Aegean (Greece). A case of transtensional tectonics. In: Boccaletti M, Nur A (eds) Active and recent strike-slip tectonics. Ann Tectonicae 4(2):196–211
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2005 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Christaras, B., Dimitriou, A., Dimopoulos, G., Pavlides, S., Marinos, P. (2005). World Heritage “Monasteries of Mount Athos” at Rock Slide Risk, in Greece. In: Sassa, K., Fukuoka, H., Wang, F., Wang, G. (eds) Landslides. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-28680-2_30
Download citation
DOI: https://doi.org/10.1007/3-540-28680-2_30
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-28664-6
Online ISBN: 978-3-540-28680-6
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)