The Geoenvironmental dimension of Greek Mythology


ΗΛΙΑΣ Δ. ΜΑΡΙΟΛΑΚΟΣ
Abstract

Native civilizations, as that of the ancient Greeks, are directly connected to the geological and the physicogeographical regime of the regional area in which they have been developed, and mainly to its geoenvironmental evolution since the last glacial period (18,000 BP). Volcanoes, earthquakes and mineral resources, as building materials, the underground water and the various minerals, consist the so called geological regime. Soil, climate, relief, shorelines and coastal areas belong to the physicogeographical regime of an area. The regional territory, where the prehistorical and historical ancient Hellenic civilization has been developed is the Hellenic Peninsula, Aegean Sea and the coasts of Minor Asia, from the geotectonic point of view, composing the Hellenic Arc which is characterized by intense tectonic, seismic and volcanic activity. The main factor contributing to the evolution of the Hellenic civilization is the climate and its fluctuations, mainly during the last 18,000 years, and most essentially the impact of these changes in the displacement of the shorelines and the coastal areas in general. It is widely known that climate changes periodically and that the main reasons for this periodicity are astronomical (Milankowitch theory). Thus, during Quaternary, several successive glacial and interglacial periods have been observed due to the increasing and decreasing of the solar radiation that earth receives. The last glacial period ends approximately 18,000 years BP, since, for the same astronomical reasons, earth's mean temperature abruptly increased. Due to this increase, huge volume of glaciers started to melt resulting to the release of large water quantities, which until that time were trapped within the glaciers, resulting in the gradual rise of the global sea level that, around 18,000 years BP, was about 125 m. lower than today. This rise caused successively transgression of all areas that nowadays constitutes the seafloor of Aegean Sea until a depth around 125 m. This transgression happened within a few thousands of years, namely between 18,000 and 6,000 years BP approximately. Therefore, prehistoric man who inhabited the area of the Aegean Sea, though until 18,000 years BP was living for tens of thousands of years in a geoenvironment unfavourable but more or less stable, following 18,000 BP and due to the increase of the mean temperature of the earth's atmosphere, he witnessed cosmogony changes. These especially concern the change of the coastal scene, since year after year, slowly but steadily, coastal areas are being submerged, featuring high mean velocities that under certain conditions should exceed 5 m per year. Together with these shoreline displacements if one takes also into account seismicity, volcanic activity and the related phenomena (tsunamis, abrupt uplift or subsidence of the coastal areas caused by earthquakes, landslides, rockfalls, etc.), the physicogeological scenery should have been a nightmare. The third generation of the Gods must have been originated during this period. This generation is the result of the union of Gaia (Earth), the Big Mother of all, and Ouranos (Heaven), namely Titans, Ekatoncheires, Cyclops and Giants, who might represent the destructive natural powers that terrify man and move the earth under his feet. What else than volcanoes might Giants represent, when, according to the Hellenic Mythology ".... they (the giants) breathed fire from their mouth ...." "...they were crying out wildly....", "they were shooting rocks and blazing trees in the sky "! ? Yet, Paleolithic and Mesolithic man needs to create more gods who will protect him from all these natural disasters. So, he originates the fourth generation that comes out of the union of the Titan Kronos and the Titanide Rhea. In this generation belong some of the great gods, such as Hera, Demeter, Estia, Hades, Poseidon and Zeus. The favorable climate ensures the basic nutrition species that man needs, either he is a food collector or he is a food producer, and especially without any particular effort. This means that it allows prehistoric man to have enough free time. Especially after his inhabitance in towns, he may be continuously mobile in the open space and he may communicate with other men having free time as well. In order to attitude within his small society, he has to learn to discuss, to argue, to oppose, to agree or to disagree with his co-speakers. Yet, all these constitute the basic substantial features of Democracy. All these physicogeographical and geological changes of the mythological and the prehistorical, in general, era, that have determined directly or indirectly all partial settings and the evolution of the civilization itself, should be promoted in such a way that the relationship between physicogeographical environment and civilization should be primarily introduced.

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ALLEN Η., 1990: A postglacial record from the Kopais basin, Greece.- In; Man's Role in the Shaping of the Eastern Mediterranean Landscape, Ed. Bottema, G. Entjes-Nieborg and W. Van Zeist. Balkema, Rotterdam.
BERGER Α., 1988: Milankowitch theory and climate.- Review of Geophysics, 26(4), pp. 624-657.
CHRISTARAS Β., MARIOLAKOS I., FOUNTOULIS I., ATHANASIAS S. & DIMITRIOU Α., 1997: Geotechnical input for the protection of some Macedonian tombs in Northern Greece. In Proceed, of IV th Intern. Symposium on the conservation of monuments in the Mediterranean basin, (Rhodes, 6-11 May, 1997), ν.Ι,ρρ. 125-132.
CURTIUS E., 1892: Die Deichbauten der Minyer.- Sitzungsbericht der Berliner Akademie der Wissensch., Philosophisch-Historische Klasse, V. 55, pp. 1181-1193.
ΓΡΑΜΜΕΝΟΣ Α., 1997: Νεολιθική Μακεδονία.- Υπουργείο Πολιτισμού TATI, 283 σελ., Αθήνα.
DAWSON A.G., 1992: Ice Age Earth: Late Quaternary Geology and Climate.- Routledge, 293 p, London.
DUFF D., 1993: Holme's principles of physical Geology - Chapman & Hall, 791 p.
ΔΙΟΔΩΡΟΣ ΣΙΚΕΛΙΩΤΗΣ, 1997: Βιβλιοθήκης Ιστορικής, Βίβλος Πέμπτη.- Οι Έλληνες, Κάκτος, Τ. 405, Αθήνα.
ΘΕΟΧΑΡΗΣ Δ., 1993: Νεολιθικός Πολιτισμός.- Μορφ. Ιορ. Εθν. Τραπέζης, 193 σελ.
FAIRBRIDGE R.W., 1983: Isostasy and Eustasy.- In D.E. Smith and A.G.Dawson (eds): Shorelines and Isostasy, pp. 3-28, Academic Press, London.
GREENBERG GARY, 1996: To Μυστήριο του Μωύσή. Ο μύθος της Βίβλου.- Εκδόσεις Ενάλιος (Μετάφρ. Δ. Μήλα), σελ. 543, Αθήνα 1999 (The Moses Mystery / The Bible Myth.- Citadel Press Book/Carol Publishing Group, 1996).
GUIOT J., PONS Α., BEAULIEU L. & REILLE M., 1989: A 140.000 year continental climate reconstruction from two European pollen records.- Nature, 338, pp. 309-13.
JACOBSEN T, 1976: 17.000 Years of Greek Prehistory.- Scientific American, 234 (1976).
JINSUN JL, NICOLE PETIT-MAIRE & ZHONGWEI YAN., 1993: The last 1000 Years climatic change in arid Asia and Africa.- Global and Planetary Change, 7, pp. 203-210.
IMBRIE J. & IMBRIE K.P, 1979: Ice Ages: solving the mystery.- Macmillan, 229 p., London.
IS AR A. S. & BRUINS H.J., 1983: Special climatological conditions in the desserts of Sinai and the Negev during the latest Pleistocene.- Paleo 3, Elsevier Science Publishers, 43, pp. 63-72, Amsterdam.
KAKRIDIS J., 1986: Greek Mythology. - Ekdotiki Athinon, v. 4 (in greek).
KENNEY I., 1935: The ancient drainage of the Kopais.- Annals of Archeology and Anthropology, University of Liverpool, v. 22, pp. 63-72.
KNAUSS J., 1984: Die Wasserbauten der Minyer in der Kopais - Die aelteste Flussregulierung Europas (Kopais 1).- Wasserbau und Wasserwirtschaft, Nr. 50. Technische Universitaet Muenchen.
KNAUSS J., 1987: Die Melioration des Kopaisbeckens durch die Minyer im 2 Jt. v. Chr. - Wasserbau und Siedlungsbedingungen im Altertum (Kopais 2). - Wasserbau und Wasserwirtschaft, Nr. 57. Technische Universitaet Muenchen.
KNAUSS J., 1996: Argolische Studien: Alte Strassen - Alte Wasserbauten.- Wasserbau und Wasserwirtschaft, - Nr. 77, Technische Universitaet Muenchen.
ΚΟΪΔΑΚΗ Κ, (Μητροπολίτου Κίτρους), 1939: Γεωλογία και Αγία Γραφή.- Έκδοση εφημερίδος «Μακεδόνικος Αγων», Κατερίνη.
KOKKOROS Ρ êâé KANELLIS Α., 1960: Découverte d' un crane d' homme paléolithique dans la péninsule Chalcidique.- L' Anthropologie, 64.
KOMMHTA ΣΤΕΦΑΝΟΥ, 1827: Ελληνική Μυθολογία.- Έκδοση ΕΚΑΤΗ (Επανεκτύπωση), 594 σελ., Αθήνα 1996.
KRAFT J.C. et al., 1977: Palaeogeographic reconstructions of coastal Aegean archaeological sites.- Science, 195, pp. 941-7.
KRAFT J. C. et al., 1985: Geological studies of coastal change applied to archaeological settings.- In: Archaeological Geology, Ed. G RAPP and J.A.GIFFORD, Yale University Press.
KRAFT, J. C, RAPP, G, SZEMLER, G.J., TZIAVOS, C, and KÄSE, E.W., 1987: The Pass at Thermopylae, Greece: Jour, of Field Archaeology, v. 14, pp. 181-198.
LEHMANN H., 1937: Landeskunde der Ebene von Argos und ihrer Randgebiete (Argolis I).- Deutsches Archaeol. Inst., Athen.
ΜΑΡΙΟΛΑΚΟΣ Η., 1975: Σκέψεις και απόψεις προβλημάτων της γεωλογικής και τεκτονικής δομής της Πελοποννήσου -Ann. Geol. Pays Hellen., XXVII, pp.215-313.
MARIOLAKOS I. & STIROS S., 1987: Quaternary deformation of the Isthmus and Gulf of Corinthos (Greece) - Geology, 15: pp. 225-8
ΜΑΡΙΟΛΑΚΟΣ Η., ΛΕΚΚΑΣ Σ., ΔΑΝΑΜΟΣ Γ., ΛΟΓΟΣ Ε. & ΦΟΥΝΤΟ ΥΛΗΣ L, 1991: Γεωλογικές, Νεοτεκτονικές και Γεωτεχνικές συνθήκες στον αρχαιολογικό χώρο του Μυστρά (Ν. Πελοπόννησος) - Γ Συνέδριο Γεωλογία και Περιβάλλον, Πάτρα, (υπό εκτύπωση).
MARIOLAKOS I., LOGOS Ε., LOZIOS S. & NASOPOULOU S., 1991: Technicogeological observations in the ancient Delphi area (Greece) - In "Natural hazards and engineering geology. Prevention and control of landslides and other mass movements". Eds.: Almeida - Texeira M.E., Fantechi R., Oliveira R., Gomes Coelho Α., Commiss, of the Europ. Commun., pp.273-283.
MARIOLAKOS I., FOUNTOULIS I. & KRANIS H., 1997: Introduction to the Geology of Sterea Hellas, Hellenic Territory: Current geodynamic regime, Neoteconics of Corinthiakos Gulf, Delphi, Minyan Ancient Flood Prevention works. In: Boat and field trip guide of the Th International Symposium Engineering Geology and the Environment I AEG (Editors: I. Mariolakos and Fountoulis, Geology and Tectonics, P. Marinos, G. Tsiambaos and M. Kakavas: Engineering Geology and Geotechnical Engineering, Hydrogeology), 60 p.
ΜΑΡΙΟΛΑΚΟΣ Η., ΛΕΚΚΑΣ Σ., ΑΛΕΞΟΠΟΥΛΟΣ Α., ΦΟΥΝΤΟΥΛΗΣ Ι. & ΔΑΝΑΜΟΣ Γ., 1998: Γεωλογικές, νεοτεκτονικές και γεωτεχνικές συνθήκες στον αρχαιολογικό χώρο του κάστρου Παλαιόχωρας Κυθήρων - Πρακτικά 8"ν Συνεδρίου της Ελλ. Γεωλ. Ετ., Μαϊος 1998, Πάτρα, Δελτ. Ελλ. Γεωλ. Ετ., ΧΧΧΙΙ/4, σελ. 121-129.
MARIOLAKOS Ι., 1998: The geomythological geotope of Lerni Springs (Argolis, Greece) - Geologica Balcanica, 28, 3-4, pp.101-108.
ΜΑΡΙΟΛΑΚΟΣ Η., 1999: Συμβολή των γεωτόπων στην ιστορία και την περιβαλλοντική ευαισθητοποίηση. Τριήμερο για τη Διατήρηση της Γεωλογικής-Γεωμορφολογικής Κληρονομιάς, Σύρος, 12-14 Ιουλίου 1996, ΙΓΜΕ, σελ. 45-59.
ΜΑΡΙΟΛΑΚΟΣ Η., 1999: Το Νερό, ο Ανθρωπος και ο Ελληνικός Πολιτισμός - Πρακτικά Συμποσίου «Το Αθάνατο Νερό», 18-21 Νοεμβρίου 1999, Ευρωπαϊκές Ημέρες Πολιτιστικής Κληρονομιάς, Αθήνα (υπό εκτύπωση).
ΜΑΡΙΟΛΑΚΟΣ Η., ΧΡΗΣΤΑΡΑΣ Β., ΦΟΥΝΤΟΥΛΗΣ Ι, ΔΗΜΗΤΡΙΟΥ Α., ΑΘΑΝΑΣΙΑΣ Σ., ΛΕΜΟΝΗ Ε. & ΧΑΤΖΗΑΓΓΕΛΗ Μ., 1999: Προτεινόμενες διαδικασίες αποστράγγισης των Μακεδόνικων Τάφων στα Λευκάδια Ν. Ημαθίας, 5" Υδρογεωλογικό Συνέδριο Ελληνικής Επιτροπής Υδρογεωλογίας της Ελλην. Γεωλ. Ετ., Λευκωσία (υπό εκτύπωση).
ΜΑΡΙΟΛΑΚΟΣ Η. & ΘΕΟΧΑΡΗΣ Δ., 2001: Μετατοπίσεις των ακτογραμμών στο Σαρωνικό κατά τα τελευταία 18.000 χρόνια και η Κυχρεία Παλαιολίμνη, Πρακτικά 9ου Συνεδρίου της Ελλ. Γεωλ. Ετ., Σεπτέμβριος 2001, Αθήνα, Δελτ. Ελλ. Γεωλ. Ετ., XXXIV/1, σελ. 405-413.
ΜΑΡΙΟΛΟΠΟΥΛΟΣ Η, 1938: Το κλίμα της Ελλάδος, 370 σ., Αθήνα
MARTINSON D., PISIAS N.G., HAYS J.D., IMBRIE J., MOORE T.C., SHACKLETON H.J. & JR., 1987: Age dating and the orbital theory of the Ice Ages: development of a high-resolution 0-300.000-year chronostratigraphy.- Quaternary Research, 27, pp. 1-29.
MILANKOWITCH M., 1941 : Kanon der Erdbestrahlung und seine Anwendung auf dem Eiszeitenproblem.- Royal Serbian Sciences, Spec. Pubi. 132, Section of Mathematical and Natural Sciences, v. 33, 633 p., Belgrade.
MILOJCIC V., BOESSNECK J., JUNG D. & SCHNEIDER H, 1965: Palaeolithikum urn Larissa in Thessalien.- B.A.M., I., Bonn.
MINOY - ΜΙΝΟΠΟΥΛΟΥ Δ., 2000: Η Ανάδυση ενός Πολιτισμού μέσα από ένα Ηφαίστειο. - Γεωτουριστικά - Γεωπολιτιστικά Μονοπάτια και Γεωμυθότοποι, ΓΕΩΤΕΕ, Αθήνα, 1-4 Ιουνίου 2000 (υπό εκτύπωση).
MOERNER Ν.- Α., 1971: Eustatic changes during the last 20.000 years and a method of separating the isostatic and eustatic factors in an uplifted area.- Palaeogeography, Palaeoclimatology, Palaeoecology, 19, pp. 63-65.
MOERNER Ν.- Α., 1976: Eustasy and geoid.- Journal of Geology, 88, pp. 123-151.
MOERNER N.A., 1976: Eustasy and geoid changes.- Journal of Geology, 84, pp. 123-152.
NEEV D., & EMERY K.O., 1995: The Destruction of Sodom, Gomorrah and Jericho. Geological, Climatological and Archaeological Background.- Oxford University Press, 175 p., N. York.
OTA Y., 1987: Sea-level changes during the Holocene: the Northwest Pacific- In R.Y.N. Devoy (Eds): Sea Surface Studies -A Global View, pp. 348-374, Room Helm. Ltd, London.
PAEPE R., 1986: Landscape changes in Greece as a result of changing climate during the Quaternary.- In: Desertification in Europe, Eds.: R. FAÎTECHI and N. MARGARIS, D. Riedl Pub. Co.
PAEPE R., HATZIOTIS M.E., THOREZ J., OVERLOOP v. E. & DEMAREE G.,1982: Climatic indexes on the basis of sedimentation parameters in geological and archaeological sections.-Palaeoclimatic Research and Models, Eds.: A. GHAZI, EEC, pp. 129-138.
PAEPE R. and MARIOLAKOS L, 1984: Paleoclimatic reconstruction in Belgium and in Greece based on Quaternary lithostratigraphic sequences.- Proc. E.C. Climatology Programe Symposium, Sophia Antipolis, France, 2-5 October 1984.
PAEPE R., & OVERLOOP v.E., 1989: River and soils cyclicities interfering with sea level changes.- In: Greenhouse Effect, Sea Level and Drought, Eds.: R. PAEPE, et al., NATO ASI Series, Series C, V. 325, pp. 253-280.
ΠΑΠΑΔΟΠΟΥΛΟΥ - ΒΡΥΩΝΗ Κ., 1990: Γεωμορφολογική μελέτη της περιοχής Κωπαϊδας, Διόακτορική Διατριβή, Γεωλογικό Τμήμα Παν/μίαν Αθηνών, 140 σελ., Αθήνα.
PHILIPPSON Α., 1892: Der Peloponnes.- Berlin.
PIRAZZOLI P.A., 1986: The early byzantine tectonic paroxysm. - Ζ. Geomorph. Ν.E, Suppl., 62, pp.31-49, Berlin.
PIRAZZOLI P.A., 1987: Sea-level changes in the Mediterranean.- In M.YTOOLEY and I. SHENNAN (eds). Sea Level Changes, pp. 152-181, Basil Blackwell, Oxford.
POPE K. & VAN ANDEL, Tj. H., 1984: Late Quaternary alluviation's and soil formation in the southern Argolid: its history, causes and archaeological implications.- Journal of Archaeological Science, 11, pp. 281-306.
POUQUEVILLE F.-C.-H.-L.-, 1820: Voyage dans la Grèce.- Peloponnes. (Greek translation N. Molfeta), 478 p., Athens, 1997.
RANKE-GRAVES R. von, 1955: Griechische Mythologie. Quellen und Deutung, Rowolts Deutsche Enzyclopadie, 2, pp. 80- 116.
RAPP G. & GIFFORD J.A., 1982: Troy. The Archaeological Geology.- Supplementary Monograph 4, University of Cincinnati, Princeton University Press.
RYAN W., & PITMAN W., 1999: Noah's flood. The new scientific discoveries about the event that changed history.- Simon & Schuster, 337 p., Sydney.
ROBERTS N., 1989: The Holocene: An Environmental History.- Basil Blackwell, 227 p., Oxford.
SCHNEIDER H, 1968: Zur quartargeologischen Etwicklungsgeschichte Thessaliens (Griechenland), Beitr.Ur-u. Fruhgesch. Archaol. d. Mittelmerr. - Kulturraumes (BAM), 6,. Bonn.
SCHWARZBACH M., 1974: Das Klima der Vorzeit: Eine Einfuhrung in die Palaoklimatologie.- Ferd. Enke Verlag, 380 p., Stuttgart.
ΣΠΥΡΟΠΟΥΛΟΣ Θ., 1973: Εισαγωγή εις την μελέτην του Κωπαϊδικοΰ χώρου.- AAA, 6, 201 σελ.
ΣΠΥΡΟΠΟΥΛΟΣ Π., 1997: Χρονικό των σεισμών της Ελλάδος από την αρχαιότητα μέχρι σήμερα - Εκδ. Δωδώνη, 453 σελ.
STRUCK Α., 1912: Zur Landeskunde von Griechenland, Frankfurt a.IQ.
TZIAVOS C, 1977: Sedimentology, Ecology, and Paleogeography of the Sperchios Valley and Maliakos Gulf, Greece, Ms. Thesis, University of Delaware, 119 p.
TZIAVOS C, ANAGNOSTOU C, and PAVLAKIS P., 1986. Search for Archaeological Sites in the Strymon delta (Greece), utilizing Geological and Geophycical Methods, Intern. Symposium on Archaeometry, Athens.
THIEDE J., 1974: A Glacial Mediterranean - Nature, 276, pp. 680-683.
VAN ANDEL TH., 1998: Middle and upper Paleolithic environments and the calibration of l4C dates beyond 10.000 BP- ANTIQUITY, 72, pp. 26-33.
VITA-FINZI C, 1969: The Mediterranean Valleys.- Cambridge University Press.
ΧΡΗΣΤΑΡΑΣ Β., ΜΑΡΙΟΛΑΚΟΣ Η., ΦΟΥΝΤΟ ΥΛΗΣ Ι., ΑΘΑΝΑΣΙΑΣ Σ. & ΔΗΜΗΤΡΙΟΥ Α., 1998: Γεω-περιβαλλοντικές επιδράσεις στους Μακεδόνικους Τάφους των Λευκαδιών Ν. Ημαθίας - Πρακτικά Συνεδρίου «Τεχνολογία Περιβάλλοντος για τον 21° αιώνα», TEE, Ι, σελ. 359-366, Θεσ/νίκη.
YONEKURA Κ. & ΟΤΑ Υ, 1986: Sea-level changes and tectonics in the Late Quaternary.- Recent Progress of Natural Sciences in Japan, 11, Quaternary Research, Science Council of Japan, pp. 16-34.
ZANGGER E., 1991: Prehistoric Coastal Environments in Greece: The vanished Landscapes of Dimini Bay and Lake Lerna.- J. Field Α., 18 (1991) pp. 1-15.
ZANGGER E., 1993: The Geoarchaeology of the Argolida (Argolis II) - Deutsches Archaeol. Inst. Athen.
ZERVAS S., 1965: Hydrogeological study of the water resources of Argolis plain - Hellenic Ministry of Agriculture, Athens, (Report in greek).