Skip to main content

Advertisement

Log in

Geoarchaeological observations in the wider area of Nemea using airphotos and GIS

  • Research Article
  • Published:
Earth Science Informatics Aims and scope Submit manuscript

Abstract

The northeastern part of the Peloponnese is tectonically active and it is the object of study of many geomorphologists since it provides information for the evolution of the terrain, comparable with other similar areas. The study area in this paper is a small segment of northeastern Peloponnese, where we try to understand the evolution of the relief using geomorphological and archaeological data. We study the flow of the river systems Asopos and Nemeas - which are in the wider area of the Nemea archaeological site - in order to understand how the evolution of these rivers in time affected the overall image of the area. In order to access our goal, aerial photographs and GIS analysis were used. The geomorphological and tectonic analysis of the area and the development and evolution of settlements therein (based on archaeological studies) gave us clues regarding the shape of the terrain over time. The main factors affecting the shape of the terrain (intense tectonic activity and headward erosion) were not adequate reasons - in our case - to effect immediate abandonment of the area (since, in the human timescale, they are fairly slow processes). Their effect, however, is evident over time, in the form of gradual abandonment of sites, movement of settlements or the creation of new settlements.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10

Similar content being viewed by others

References

  • Armijo R, Meyer B, King GCP, Rigo A, Papanastasiou D (1996) Quaternary evolution of the Corinth rift and its implications for the late Cenozoic evolution of the Aegean. Geophys J Int 126:11–53

    Article  Google Scholar 

  • Bengtson H (1991) History of Acient Greece (from the beginning to roman Empire) Translated by A. Gavrili. (in Greek)

  • Bettis EA III, Mandel RD (2002) The effects of temporal and spatial patterns of Holocene erosion and alluviation on the archaeological record of the central and eastern great plains, U.S.A. Geoarchaeology 17:121–154

    Article  Google Scholar 

  • Doutsos T, Piper WJD (1990) Listric faulting, sedimentation, and morphological evolution of the quaternary eastern Corinth rift, Greece: first stages of continental rifting. Geol Soc Am Bull 102:812–829

    Article  Google Scholar 

  • Guccione MJ (2008) Impact of the alluvial style on the geoarcheology of stream valleys. Geomorph 101:378–401

    Article  Google Scholar 

  • Guccione MJ, Sierzchula MC, Lafferty RH III, Kelley D (1998) Site preservation along an active meandering and avulsing river: the Red river, Arkansas. Geoarchaeology 13:475–500

    Article  Google Scholar 

  • Herz N, Garrison GE (1998) Geological methods for archaeology. Oxford University Press, USA, pp 3–14

    Google Scholar 

  • Hudson PF (2004) The geomorphic context of prehistoric huastec floodplain environments: panuco basin, Mexico. J Archaeol Sci 31:653–668

    Article  Google Scholar 

  • Kelletat D, Kowalcczyk G, Schroeder D, Winter K (1976) A synoptic view on the neotektonic development of the Peloponnesian coastal regions. Z Dtsch Geol Ges 127:447–465

    Google Scholar 

  • Lymperis E, Papatheodorou G, Chassiotis T, Ferendinos I (1998) Marine faults in the active tectonic graben of the Corinthian gulf. Four typical examples of modern tectonic control of morphology and sedimentary processes below sea level. Bull Greek Geol Soc XXXII(2):223–234, in Greek

    Google Scholar 

  • Miller St, Bravo J, Kraynak L, Landon M, Marchand J (2005) Nemea Museum and Archaeological Site. Athens. (in Greek)

  • Papanikolaou D (1986) Geology of Greece. University of Athens, Greece

    Google Scholar 

  • Pavlopoulos A, Parcharidis I, Gatsis I (1999) Relationship of geological structure and land cover in the area of Corinth (NE Peloponnese) by applying remote sensing techniques and GIS. 5th Panhellenic Geographical Conference, pp. 229–238. (in Greek)

  • Sakellariou M, Faraklas N (1971) Corinthia - Cleonaea. Ancient Greek Settlements XI

  • Seger M, Alexander J (1993) Distribution of plio - Pleistocene and modern coarse - grained deltas south of the gulf of Corinth, Greece. Spec Publs Int Ass Sediment 20:37–48

    Google Scholar 

  • Siart C, Hecht S, Holzhauer I, Altherr R, Meyer HP, Schukraft G, Eitel B, Bubenzer O, Panagiotopoulos D (2010) Karst depressions as geoarchaeological archives: the palaeoenvironmental reconstruction of zominthos (Central Crete), based on geophysical prospection, sedimentological investigations and GIS. Quat Int 216:75–92

    Article  Google Scholar 

  • Stiros CS (1988) Model for the Peloponnesian (C. Greece) uplift. J Geodyn 9:199–214

    Article  Google Scholar 

  • Zelilidis A (2000) Drainage evolution in a rifted basin, Corinth graben, Greece. Geomorphology 35:69–85

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Konstantina Mexia.

Additional information

Communicated by: Konstantinos Nikolakopoulus

Published in the Special Issue Remote Sensing and Geology “Surveying the GEOsphere” with Guest Editors Dr. Konstantinos Nikolakopoulus, Dr. Cornelia Glaesser and Dr. Nilanchal Patel

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Mexia, K. Geoarchaeological observations in the wider area of Nemea using airphotos and GIS. Earth Sci Inform 8, 269–278 (2015). https://doi.org/10.1007/s12145-014-0190-2

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12145-014-0190-2

Keywords

Navigation