Developing a Biotic River Typology and Defining Reference Conditions in the Rivers of Greece: a Spatially- Based Approach

Total Page:16

File Type:pdf, Size:1020Kb

Developing a Biotic River Typology and Defining Reference Conditions in the Rivers of Greece: a Spatially- Based Approach Developing a biotic river typology and defining reference conditions in the rivers of Greece: a spatially- based approach A.N. Economou, S. Zogaris, S. Giakoumi, R. Barbieri & D. Petridis Abstract Developing a biotic river typology and reference conditions are vital components of ecological assessment using fish. In Greece, due to the absence of systematic monitoring data, fish sampling data from previous ichthyological surveys conducted primarily in the southern and western parts of the Hellenic Western Balkan ecoregion (Illies' ecoregion 6) were utilised. These surveys were undertaken for the purpose of fish conservation and were not designed with the prospect of ecological assessments. As a consequence, the sampling methodologies, the site selection criteria, the analytical procedures and the recorded parameters were not in line with the requirements of the WFD. A brief synopsis of the main environmental features of the Greek rivers which indicate a remarkable environmental heterogeneity is presented. Greece is a geographically fragmented mountainous country with a large number of medium and small sized rivers. Most rivers run through narrow mountain valleys that descend abruptly to the coast. Usually a mountain river becomes a lowland river very near its estuary. As a result many small and medium sized rivers have a flashy and erosive behavior and suffer from the lack of lowland riverine habitat. Lowland rivers are usually small; large floodplain rivers are very few, almost wholly restricted to northern Greece. Precipitation is irregularly distributed and hydrology varies remarkably among basins. Semi-arid regions and areas with seasonally arid conditions exist in parts of the south and southeast where localized karstic springs play an important role in enabling perennial water flows. Hence, hydrology, river geomorphology, biogeography and climatic conditions vary remarkably among basins and longitudinally along river courses. The major degradation types and their impacts on fish communities are reviewed. Throughout most of Greece, major impacts have resulted from water abstraction, which most often takes place mainly during the summer, and therefore coincides with the summer drought. The impacts of hydroelectric dams and other water exploitation practices and the operation of dams as reservoirs are ranked as next in importance, followed by reclamation and river management works, pollution, river bed substrate exploitation and the drainage of lakes and wetlands associated with rivers. Generally, streams and small rivers have been affected more adversely due to severe water abstraction (tapping of springs for domestic use and irrigation use) and their inability to buffer the harmful effects of pollutants in the way that large rivers can. The distributional patterns of 59 native freshwater species were used to investigate biogeographical relationships among river basins in the Hellenic part of ecoregion 6. For the purpose of this analysis the results of previous ichthyological investigations conducted by the NCMR were primarily utilised, however unpublished information on fish distribution was also used here to investigate biogeographical relationships. This analysis corroborates recent biogeographical proposals, but goes further in hypothesizing new biogeographical divisions in western and southern Greece. Paucity of data from some areas, taxonomic problems still evident in some taxa and a confusing pattern of faunal affinities and divergences make the use of the overall similarity of ichthyofaunas among drainage basins difficult to complete over the entire ecoregion. The results of statistical analysis on current fish distribution and fish community structure, supported by geological data and phylogenetic evidence, propose that the Greek part of Ecoregion 6 may be preliminarily divided into 5 freshwater fish subecoregions: (a) Macedonia- Thessalia, (b) Adriatic, (c) Ionian, (d) Evrotas and (e) Attiki-Beotia. Despite broad similarities, the rivers within the subecoregions Attiki-Beotia and Ionian show distinctive regions, which necessitate a further subdivision into “fish districts” for the interpretive purposes of this regionalization exercise. Linking ichthyological communities in reference sites with abiotic variables was proved to be a task beyond the abilities of the available dataset. Of the problems encountered, the most important concern the calibrated reference sites, some of which are poorly selected and not representative, others have sampling effect problems, and other sites proved to be more impacted than the screening process may have shown. Further complexities arise from the high degree of endemism and disjunct geographical distributions, which generate the need for a high level of typological discrimination. The extensive hydrological 1 fragmentation and a great diversity of factors affecting the fish communities in Greek rivers, requires us to set reference conditions in a large number of strata. It is postulated that specifically designed research is necessary to arrive at a biologically meaningful typology scheme. Despite these difficulties, using available data and statistical analysis we identified some abiotic variables as potentially important for predicting community types; of which the most important in a nationwide scale seem to be basin size, altitude (a surrogate of temperature) and discharge (some other variables appear to be locally important also). Scarcity of appropriate data has prevented us to statistically justify the specific prominence of these variables and the significance of other abiotic variables, or to set biologically defensible boundaries among abiotic types. A preliminary top-down river biotic typology for the Peloponnesian part of the Ionian subecoregion, using combinations of these three variables only, is presented. During the work of WP3 candidate metrics were selected on the basis of knowledge of the fish fauna and of the aquatic systems of Greece, and the theoretical expectations for each metric were delineated. A general difficulty for establishing metrics for the development of a biologically-based multimetric index for ecological assessment in small rivers is that species richness is low and the fish communities in these rivers are dominated by tolerant species with wide ecological requirements. Multimetric approaches such as the IBI, using lots of metrics may not provide reliable assessment of ecological quality, because by adding a metric that is not biologically relevant or sensitive to the prevailing pressures less weight is given to more relevant metrics. We suggest that appropriate methods for the Greek low speciesrich rivers should rely on a limited number of metrics. For the case of flow regime disturbances the methods could include metrics for total fish abundance and biomass, abundance or proportion of sensitive species to flow reduction, and longevity or proportion of large age (size) groups, which seem to be intolerant to reduced flow. A short discussion is presented of the problems associated with the setting of reference conditions and building a multimetric index for ecological assessment using spatial methods in Greece. 2 1. Introduction An analysis of the available ichthyological data was made with the objective to define a fish-based river typology and to identify reference conditions for FAME. The analysis was based on the following: (a) the results of previous ichthyological investigations conducted by the NCMR - Institute of Inland Waters – and (b) on published and unpublished fish data and biogeographical research. The NCMR’s field investigations concentrated on the southern and western portion of the Hellenic Western Balkan ecoregion (Illies' ecoregion 6), however sporadic data from the eastern portion are also available (Appendix 1, Map 1). The investigations were undertaken mainly for the purposes of endemic fish surveys and conservation assessments and they were not designed with the prospect of river ecological status assessments. As a consequence, the sampling methodologies, the site selection criteria, the analytical procedures and the recorded environmental and abiotic parameters were not in line with the requirements of the WFD, or adequate for the development of a multimetric index. The aims of this report are the following: 1. A synopsis of the characteristics of Greek rivers and a brief description of degradation types in the scope of developing a spatially-based approach using a multimetric index for ecological assessment, 2. Initial development of a fish-based typology which centers on: The definition of biogeographically-relevant subecoregions (regionalization) Linking ichthyological communities in reference (plus calibrated reference) sites with important abiotic variables Provisional establishment of an abiotic typology for a portion of Peloponnese based on system B using the top-down approach. The data available were not adequate (a) to develop a biotic typology and to link biotic river types with abiotic variables, nor to perform comparisons with typologies based on systems A and B, (b) to set reference conditions and develop a rating system. Scarcity of data from other Balkan counties also prevented an expansion of our analyses to the whole ecoregion 6. 2. Methods 2.1. Data utilised The NCMR dataset contains site-specific data from about 600 samples taken from 48 rivers of western Greece, the Peloponnese and the Island of Rhodes (most of these data have been stored in a PARADOX database). The usefulness of these data
Recommended publications
  • The Mt. Lykaion Excavation and Survey Project Survey and Excavation Lykaion Mt
    excavating at the Birthplace of Zeus The Mt. Lykaion Excavation and Survey Project by david gilman romano and mary e. voyatzis www.penn.museum/expedition 9 Village of Ano Karyes on the eastern slopes of Mt. Lykaion. The Sanctuary of Zeus is above the village and beyond view of this photograph. in the 3rd century BCE, the Greek poet Callimachus wrote a Hymn to Zeus asking the ancient and most powerful Greek god whether he was born in Arcadia on Mt. Lykaion or in Crete on Mt. Ida. My soul is all in doubt, since debated is his birth. O Zeus, some say that you were born on the hills of Ida; others, O Zeus, say in Arcadia; did these or those, O Father lie? “Cretans are ever liars.” These two traditions relating to the birthplace of Zeus were clearly known in antiquity and have been transmitted to the modern day. It was one of the first matters that the village leaders in Ano Karyes brought to our attention when we arrived there in 2003. We came to discuss logistical support for our proposed project to initiate a new excavation and survey project at the nearby Sanctuary of Zeus. Situated high on the eastern slopes of Mt. Lykaion, Ano Karyes, with a winter population of 22, would become our base of operations, and the village leaders representing the Cultural Society of Ano Karyes would become our friends and collaborators in this endeavor. We were asked very directly if we could prove that Zeus was born on Mt. Lykaion. In addition, village leaders raised another historical matter related to the ancient reference by Pliny, a 1st century CE author, who wrote that the athletic festival at Mt.
    [Show full text]
  • Business Concept “Fish & Nature”
    BUSINESS CONCEPT “FISH & NATURE” Marina Ross - 2014 PRODUCT PLACES FOR RECREATIONAL FISHING BUSINESS PACKAGE MARINE SPORT FISHING LAND SERVICES FRESHWATER EQUIPMENT SPORT FISHING SUPPORT LEGAL SUPPORT FISHING + FACILITIES DEFINITIONS PLACES FOR RECREATIONAL FISHING BUSINESS PACKAGE MARINE SPORT FISHING LAND SERVICES FRESHWATER EQUIPMENT SPORT FISHING SUPPORT LEGAL SUPPORT FISHING + FACILITIES PLACES FOR RECREATIONAL FISHING PRODUCT MARINE SPORT FISHING MARINE BUSINESS SECTION FRESHWATER SPORT FISHING FRESHWATER BUSINESS SECTION BUSINESS PACKAGE PACKAGE OF ASSETS AND SERVICES SERVICES SERVICES PROVIDED FOR CLIENTS RENDERING PROFESSIONAL SUPPORT TO FISHING SUPPORT MAINTAIN SAFE SPORT FISHING RENDERING PROFESSIONAL SUPPORT TO LEGAL SUPPORT MAINTAIN LEGAL SPORT FISHING LAND LAND LEASED FOR ORGANIZING BUSINESS EQUIPMENT AND FACILITIES PROVIDED EQUIPMENT + FACILITIES FOR CLIENTS SUBJECTS TO DEVELOP 1. LAND AND LOCATIONS 2. LEGISLATION AND TAXATION 3. EQUIPMENT AND FACILITIES 4. MANAGEMENT AND FISHING SUPPORT 5. POSSIBLE INVESTOR LAND AND LOCATIONS LAND AND LOCATIONS LAND AND LOCATIONS List of rivers of Greece This is a list of rivers that are at least partially in Greece. The rivers flowing into the sea are sorted along the coast. Rivers flowing into other rivers are listed by the rivers they flow into. The confluence is given in parentheses. Adriatic Sea Aoos/Vjosë (near Novoselë, Albania) Drino (in Tepelenë, Albania) Sarantaporos (near Çarshovë, Albania) Ionian Sea Rivers in this section are sorted north (Albanian border) to south (Cape Malea).
    [Show full text]
  • Flora and Vegetation of Mt Likeo (Peloponnisos, Greece)
    Fl. Medit. 23: 15-47 doi: 10.7320/FlMedit23.015 Version of Record published online on 30 December 2013 Evagelos Baliousis Flora and vegetation of Mt Likeo (Peloponnisos, Greece) Abstract Baliousis, E.: Flora and vegetation of Mt Likeo (Peloponnisos, Greece). — Fl. Medit. 23: 15- 47. 2013. — ISSN: 1120-4052 printed, 2240-4538 online. The current investigation presents 701 specific and infraspecific taxa of the vascular flora of Mt Likeo, SW Peloponnisos. From these, 543 are reported from the mountain for the first time, 41 are Greek and 23 Balkan endemics. For each taxon, local distribution and habitat types are pre- sented. Trifolium strictum seems to be a first record for Peloponnisos. Some of the new records concern rare taxa in Greece, in Peloponnisos or regional endemics, which are, therefore, choro- logically significant, such as Arenaria guicciardii, Cota brachmannii, Thlaspi graecum, Alkanna methanaea, Campanula topaliana subsp. cordifolia, Sedum laconicum subsp. laconicum, Achillea grandifolia, Scrophularia scopolii. The main vegetation types are also briefly described. Key words: biodiversity, adventive plants, phytogeography. Introduction Mt Likeo or Diaforti is located in Peloponnisos and belongs to the homonymous unit according to the phytogeographical division in “Flora Hellenica” (Strid & Tan 1997). It is situated in the southwestern part of Peloponnisos between the Megalopolis basin and the town of Zaharo. It lies NNE of the Messinian peninsula and administratively belongs to the prefectures of Messenia, Arkadia and Ilia. Its name is correlated with ancient Greek history as it was regarded from the ancient arkades as the place of birth of Zeus and thus their holy mountain. The highest peaks of Mt Likeo (Fig.
    [Show full text]
  • An Allied History of the Peloponnesian League: Elis, Tegea, and Mantinea
    An Allied History of the Peloponnesian League: Elis, Tegea, and Mantinea By James Alexander Caprio B.A. Hamilton College, 1994 M.A. Tufts University, 1997 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES (Department of Classical, Near Eastern, and Religious Studies) THE UNIVERSITY OF BRITISH COLUMBIA January, 2005 © James A. Caprio, 2005 Abstract Elis, Tegea, and Mantinea became members of the Peloponnesian League at its inception in 506, although each had concluded an alliance with Sparta much earlier. The initial arrangement between each city-state and Sparta was reciprocal and membership in the League did not interfere with their individual development. By the fifth century, Elis, Mantinea, and Tegea had created their own symmachies and were continuing to expand within the Peloponnesos. Eventually, the prosperity and growth of these regional symmachies were seen by Sparta as hazardous to its security. Hostilities erupted when Sparta interfered with the intent to dismantle these leagues. Although the dissolution of the allied leagues became an essential factor in the preservation of Sparta's security, it also engendered a rift between its oldest and most important allies. This ultimately contributed to the demise of Spartan power in 371 and the termination of the Peloponnesian League soon thereafter. 11 TABLE OF CONTENTS Abstract ii Table of Contents iii List of Maps iv List of Abbreviations v Acknowledgements viii Introduction • 1 Chapter One: Elis 20 Chapter Two: Tegea and southern Arkadia 107 Chapter Three: Mantinea and northern Arkadia 181 Conclusion 231 Bibliography , 234 iii Maps Map 1: Elis 21 Map 2: Tegean Territory 108 Map 3: The Peloponnesos 109 Map 4: Phigalia 117 Map 5: Mantinea and Tegea 182 Map 6: Mantinea and its environs 182 Abbreviations Amit, Poleis M.
    [Show full text]
  • Neotectonic Folds in the Central-Western Peloponnese, Greece
    Z. dt. Ges. Geowiss., 159/3, p. 485–494, 12 figs., Stuttgart, September 2008 Article Neotectonic folds in the central-western Peloponnese, Greece Ioannis Fountoulis & Ilias Mariolakos* Fountoulis, I. & Mariolakos, I. (2008): Neotectonic folds in the central-western Peloponnese, Greece. [Neotektonische Fal- tung auf der mittleren West-Peloponnes, Griechenland.] – Z. dt. Ges. Geowiss., 159: 485–494, Stuttgart. Abstract: The western Peloponnese, being very close to the Hellenic Trench, is one of the most active areas in Greece. The study area is located at the central western part of Peloponnese and it is developed in a NNW–SSE direction along 45 km, parallel to the Ionian Trench, which occurs at a distance of only 30–40 km to the west. Based on the morphotectonic studies of the neotectonic macrostructures of the central-western Peloponnese in many scales, it was concluded that the main neo- tectonic mega-structure is the “Megalopolis–Lykaeon–Minthi–Tetrazio Composite Morphotectonic Structure” (MELYMITE CMS) (1st order structure). The neotectonic deformation is expressed not only by faults, but also by folds which in some cases are the principal structures of the neotectonic deformation. Neotectonic folds occur in the Alpine formations as well as in the post-Alpine ones in various scales. The folds, and the ductile deformation in general, are not easily observed on the surface because of the intense presence of brittle tectonics. A rotational couple stress-fi eld could satisfactory incorporate and explain the brittle-ductile neotectonic structures of the area. Kurzfassung: Die westliche Peloponnes, recht nahe dem Hellenischen Graben gelegen, ist eines der tektonisch aktivsten Gebiete Griechenlands.
    [Show full text]
  • Field Trip Guide: Formalization of Neotectonic Maps (Post Congress Excursion of the 8Th Congr
    ΔΗΜΟΣΙΕΥΣΗ Νο 48 MARIOLAKOS, I., FOUNTOULIS, I., KRANIS, H., (1998). - Field Trip Guide: Formalization of Neotectonic Maps (Post congress excursion of the 8th Congr. Geol. Soc. Greece), 74 p. International Union for Quaternary Research Neotectonics Commission Working Group I International Workshop: Formalization of Neotectonic Maps Patra, Greece, 29 May - 2 June, 1998 Organizing Committee Dr. Ilias Mariolakos, Professor, University of Athens Dr Pablo Silva, Assoc. Professor, Universidad de Salamanca Dr Spyros Lekkas, Assoc. Professor, University of Athens Dr Ioannis Fountoulis, Lecturer, University of Athens DrS Haris Kranis, M.Sc., University of Athens DrS Sophia Nassopoulou, University of Athens DrS Dimitris Theocharis, University of Athens DrS Ioannis Badekas, University of Athens The organizing Committee would like to thank the following for their contribution to the Workshop: Dioryga Corinthou, SA. Earthquake Planning & Protection Organization (EPPO) Gefyra, SA. Geological Society of Greece Ministry of Culture Ministry of Development - General Secretariat for Research & Technology (GSRT) University of Athens ` Field Trip: Formalization of Neotectonic Maps Peloponnessos - Sterea Hellas 30 May - 2 June 1998 Post-Congress excursion of the 8th International Congress of the Geological Society of Greece Excursion Leader: Prof. Ilias Mariolakos Field guide compilation: Prof. Ilias Mariolakos Lecturer I. Fountoulis H. Kranis, M.Sc. Contents FOREWORD...........................................................................................................................1
    [Show full text]
  • Back Matter (PDF)
    Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. Acidere Formation 205 Catalina-Rincon Mountains Permo-Triassic evolution 36 Acigo¨l Fault 199 (Arizona, USA) 4 magmatism 39–44 acoustic fluidization 17 Central Anatolide Crystalline Complex metamorphism 36–39 Aegean extensional province 198 sedimentary basins and tectonic map 198 Central Finland Granitoid Complex 229 volcanics 44–47 tectonic setting 197–198, 200 crust detail 242, 245, 246 map 35 Aegean Sea structure interpretation 237, 238 numerical analysis of geological geodynamics 181–183 Central Volcanic Region (New Zealand) evolution geological map 140 74, 79, 81–83 model set-up 47–49 tectonic map 170, 181 chlorite, and fault strength 15 thermomechanics 50–52 Agridi Fault 126, 127, 129, 130, 131 clays, reactions and fault strength 15 numerical and natural data compared Akrata Fault 129 Coastal Fault System 141, 144, 145 52–53 Alasehir detachment 199, 205 collisional modelling 225–226 magmatism 58–64 Alasehir graben 215, 217 continental back-arc systems 73 metamorphism 53–58 Alasehir granitoid 199, 202 conceptual model 74 sedimentary basins and Alpine orogeny 34–36 studies in New Zealand, extension in volcanics 64 Amonton’s Law 11–12, 17 relation to local variables Evciler granitoid 199 Amorgos detachment crustal structure 78–81 Evia 140, 141 geological setting 171–173 extension and arc migration 78 exhumation, factors affecting 179 map 170 extension–rotation relations 78 extension timing of detachment geodetic strain estimates 76–77 and isostasy
    [Show full text]
  • Structural Cross Sections Through the Corinth-Patras Detachment Fault-System in Northern Peloponnesus (Aegean Arc, Greece) N
    Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, Τομ. XXXIV/1, 235-241, 2001 Bulletin of the Geological Society of Greece, Vol. XXXIV/1, 235-241, 2001 Πρακτικά 9ου Διεθνούς Συνεδρίου, Αθήνα, Σεπτέμβριος 2001 Proceedings of the 9th International Congress, Athens, September 2001 STRUCTURAL CROSS SECTIONS THROUGH THE CORINTH-PATRAS DETACHMENT FAULT-SYSTEM IN NORTHERN PELOPONNESUS (AEGEAN ARC, GREECE) N. FLOTTÉ1 & D. SOREL1 ABSTRACT Structural mapping in northern Peloponnesus reveals the emergence of an E-W striking, more than 70km long, low angle detachment fault dipping to the north beneath the Gulf of Corinth. This paper describes four north-south structural cross-sections in northern Peloponnesus. Structural and sedimentological field observa­ tions show that in the studied area the normal faults of northern Peloponnesus branch at depth on this major low angle north-dipping brittle detachment. The southern part of the detachment and the related normal faults are now inactive. To the north, the active Helike and Aigion normal faults are connected at depth with the seismically active northern part of the detachment beneath the Gulf of Corinth. KEY WORDS: rifting, Corinth Gulf, Peloponnesus, detachment normal fault, Pleistocene INTRODUCTION : GEODYNAMIC SETTING AND STRUCTURAL FRAME Some 130 km long and 5 to 20 km wide, the Corinth-Patras rift is the major active transverse structure of the Aegean Arc (Fig. 1). Fault kinematics (Sibrier, 1977), earthquakes focal mechanisms (e.g. Hatzfeld et al, 1996), and satellite geodesy (Clarke et al, 1998) indicate a N0° to 20°E direction of extension. The extension rate increases toward the west (Le Pichon et al., 1994; Clarke et al., 1998): from 0.5cm/yr near Corinth, it reaches 1.5cm/yr near Aigion.
    [Show full text]
  • Download the Course Outline
    Competence Level: N144: Rift Systems, Faulting and 5 Days Skilled Fault-Controlled Sedimentary Architecture: Gulf of Corinth Field Course (Greece) Classroom Elements Instructor(s): Mary Ford and Ed Williams Low Physical Demand Summary This course evaluates rift stratigraphy and structure, the geometry and kinematics of a normal fault network and the facies of selected Gilbert-type fan deltas. Participants will examine fluvial successions, fan deltas and turbidites deposited in an active rift; the controlling factors in delta construction and distribution; geometry, connectivity and growth of a normal fault network; the interaction of surface processes and tectonics in active rifts. This course will primarily be of use in exploration but is also applicable to reservoirs and oil fields in extensional settings during appraisal, development and production. Learning Outcomes Participants will learn to: 1. Assess the tectonic setting and evolution of the Corinth Rift; evaluate the rapidity and scale of the rifting processes compared with other rift systems. 2. Evaluate the geometry, kinematics and evolution of a normal fault system. 3. Understand the evolution of rift stratigraphic architecture in time and space. 4. Assess geometry and sediment infill of an individual fault block. 5. Construct a cross-section through part of the rift. Calculate the heave and throw of faults, individually and cumulatively. 6. Compare and contrast fault block stratal and structural geometries, including syn-sedimentary block tilting and folding. 7. Evaluate the role of inherited palaeotopography in rift basins. 8. Examine a detailed case history of relay ramp evolution and assess its influence on sedimentary input and the location of deltas.
    [Show full text]
  • The 92Nd Annual Meeting of the Archaeological Institute of America Source: American Journal of Archaeology, Vol
    The 92nd Annual Meeting of the Archaeological Institute of America Source: American Journal of Archaeology, Vol. 95, No. 2 (Apr., 1991), pp. 285-339 Published by: Archaeological Institute of America Stable URL: http://www.jstor.org/stable/505727 Accessed: 30-05-2015 14:01 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://www.jstor.org/page/ info/about/policies/terms.jsp JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Archaeological Institute of America is collaborating with JSTOR to digitize, preserve and extend access to American Journal of Archaeology. http://www.jstor.org This content downloaded from 134.153.184.170 on Sat, 30 May 2015 14:01:56 UTC All use subject to JSTOR Terms and Conditions The 92nd Annual Meeting of the Archaeological Institute of America The 92nd Annual Meeting of the Archaeological Institute of America was held in conjunction with the 122nd Annual Meeting of the American Philological Association in San Francisco, California, on 27-30 December 1990. On 28 December Martha Sharp Joukowsky, President of the Archaeological Institute of America, presented the Institute's 26th annual Gold Medal for Distinguished Archaeological Achievement to John W. Hayes. George F. Bass, Vice-President of the Institute, presented the 1 1th annual Pomerance Award of the Archaeological Institute of America for Scientific Contributions to Archaeology to Robert H.
    [Show full text]
  • List of Rivers of Greece
    Sl. No River Name Location (City / Region ) Draining Into Region Location 1 Aoos/Vjosë Near Novoselë, Albania Adriatic Sea 2 Drino In Tepelenë, Albania Adriatic Sea 3 Sarantaporos Near Çarshovë, Albania Adriatic Sea 4 Voidomatis Near Konitsa Adriatic Sea 5 Pavla/Pavllë Near Vrinë, Albania Ionian Sea Epirus & Central Greece 6 Thyamis Near Igoumenitsa Ionian Sea Epirus & Central Greece 7 Tyria Near Vrosina Ionian Sea Epirus & Central Greece 8 Acheron Near Parga Ionian Sea Epirus & Central Greece 9 Louros Near Preveza Ionian Sea Epirus & Central Greece 10 Arachthos In Kommeno Ionian Sea Epirus & Central Greece 11 Acheloos Near Astakos Ionian Sea Epirus & Central Greece 12 Megdovas Near Fragkista Ionian Sea Epirus & Central Greece 13 Agrafiotis Near Fragkista Ionian Sea Epirus & Central Greece 14 Granitsiotis Near Granitsa Ionian Sea Epirus & Central Greece 15 Evinos Near Missolonghi Ionian Sea Epirus & Central Greece 16 Mornos Near Nafpaktos Ionian Sea Epirus & Central Greece 17 Pleistos Near Kirra Ionian Sea Epirus & Central Greece 18 Elissonas In Dimini Ionian Sea Peloponnese 19 Fonissa Near Xylokastro Ionian Sea Peloponnese 20 Zacholitikos In Derveni Ionian Sea Peloponnese 21 Krios In Aigeira Ionian Sea Peloponnese 22 Krathis Near Akrata Ionian Sea Peloponnese 23 Vouraikos Near Diakopto Ionian Sea Peloponnese 24 Selinountas Near Aigio Ionian Sea Peloponnese 25 Volinaios In Psathopyrgos Ionian Sea Peloponnese 26 Charadros In Patras Ionian Sea Peloponnese 27 Glafkos In Patras Ionian Sea Peloponnese 28 Peiros In Dymi Ionian Sea Peloponnese
    [Show full text]
  • Rifting and Shallow-Dipping Detachments, Clues from the Corinth
    Rifting and shallow-dipping detachments, clues from the Corinth Rift and the Aegean Laurent Jolivet, Loic Labrousse, Philippe Agard, Olivier Lacombe, Vivien Bailly, Emmanuel Lecomte, Frédéric Mouthereau, Caroline Mehl To cite this version: Laurent Jolivet, Loic Labrousse, Philippe Agard, Olivier Lacombe, Vivien Bailly, et al.. Rifting and shallow-dipping detachments, clues from the Corinth Rift and the Aegean. Tectonophysics, Elsevier, 2010, 483 (3-4), pp.287-304. 10.1016/j.tecto.2009.11.001. insu-00448474 HAL Id: insu-00448474 https://hal-insu.archives-ouvertes.fr/insu-00448474 Submitted on 19 Jan 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Rifting and shallow-dipping detachments, clues from the Corinth Rift and the Aegean Laurent Jolivet 1,2, Loïc Labrousse 1, Philippe Agard 1, Olivier Lacombe 1, Vivien Bailly 1, Emmanuel Lecomte 1, Frédéric Mouthereau 1, Caroline Mehl 3 1 ISTEP, UPMC-Paris6, UMR 7193, T 46-00 E1, 4 Place Jussieu, 75252 Paris cedex 05 2 Now at: ISTO, UMR 6113, Université d'Orléans 1A, Rue de la Férollerie, 45071 Orléans Cedex 2, France 3 Ecole des Mines de Paris, Centre de Géosciences, 35 rue Saint Honoré, 77300 Fontainebleau France Keywords: Aegean, Corinth, rifting, post-orogenic extension, detachment, Phyllite-Quartzite Abstract : The Corinth Rift is superimposed on the Hellenic nappe stack that formed at the expense of the Apulian continental crust above the subducting African slab.
    [Show full text]