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Journal articles on the topic 'Argolis'

Author: Grafiati

Published: 4 June 2021

Last updated: 17 June 2025

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1

Vassilopoulou, S. "MORPHOTECTONIC ANALYSIS OF SOUTHERN ARGOLIS PENINSULA (GREECE) BASED ON GROUND AND SATELLITE DATA BY GIS DEVELOPMENT." Bulletin of the Geological Society of Greece 43, no. 1 (2017): 516. http://dx.doi.org/10.12681/bgsg.11202.

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Southern Argolis Peninsula is an interesting Geological and Geomorphological area due to the variety of the geological structures and the interchange on the terrain. Ground and remote sensing data, relating to geology and tectonics, were compiled with terrain analysis data in a GIS data base, in order to perform morpho-tectonic analysis in the Southern Argolis Peninsula. Terrain analysis data were automatically produced by the specific software “PROANA” (based on ArcGIS). The main direction of Southern Argolis Terrain is E-W. The same direction is observed from the rose-diagrams of morphological discontinuities. The hydrographic network has a NW-SE main direction. The depositional planation surfaces (0-5%) that are located near the coast are related with neotectonic faults. The direction of the Faulting Zones is mainly ESE-WNW and E-W. The most active tectonic structures were observed to the southern and south-western area of Southern Argolis Peninsula, towards Kranidi and Argolikos Gulf.

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2

Whitley, James, Sophia Germanidou, Dusanka Urem-Kotsou, et al. "Argolis." Archaeological Reports 53 (November 2007): 18–23. http://dx.doi.org/10.1017/s0570608400000089.

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3

Mitropapas, A., I. Koumantakis, E. Vasileiou, M. Perdikaki, and A. Kallioras. "OVEREXPLOITATION OF GROUNDWATER RESOURCES IN THE COASTAL AQUIFER SYSTEM OF ARGOLIS." Bulletin of the Geological Society of Greece 50, no. 2 (2017): 865. http://dx.doi.org/10.12681/bgsg.11792.

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Intense abstraction of groundwater resources in the coastal aquifer system of Argolis is investigated since the late 1950’s. The increasing water demands due to the agricultural development of the area (mainly citrus trees) during the last years, in combination with the touristic growth, has led to the overexploitation of groundwater resources of the coastal aquifer system of Argolis. This paper presents the piezometric conditions in the plain of Argos during the period between 1986 and 2014, analysing the fluctuations of groundwater levels and highlighting the problem of seawater intrusion in the study area. In October 2014, measurements were made in app. 160 wells and drills which are located within the boundaries of the granular aquifer of the study area. Selected piezometric maps are presented, which demonstrate the problem of overexploitation of groundwater in the plain of Argos.

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4

Chen, Zhuo, Michael D. Webb, and Wanzhi Cai. "A Revision of the Genus Argolis (Hemiptera: Reduviidae: Stenopodainae) from Asia." Insects 14, no. 8 (2023): 680. http://dx.doi.org/10.3390/insects14080680.

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The assassin bug genus Argolis Stål, 1861 (Hemiptera: Reduviidae: Stenopodainae) has a disjunct distribution in Sub-Saharan Africa and Asia. In the present study, the Asian species of Argolis are revised. Two species are recognized, redescribed, and illustrated, with the following new subjective synonyms and new combination proposed: Argolis Stål, 1861 = Bardesanes Distant, 1909, syn. nov. = Neoklugia Distant, 1919, syn. nov.; A. farinator (Reuter, 1882) = N. typica Distant, 1919, syn. nov. = B. sericenotatus Livingstone & Ravichandran, 1989, syn. nov.; A. signata (Distant, 1909), comb. nov. (transferred from Bardesanes) = Caunus noctulus Hsiao, 1977, syn. nov. Lectotypes for C. farinator, B. signatus, and N. typica are designated. A key to separate the two Asian species of Argolis is provided. The sexual dimorphism, systematic relationships, and distribution of Argolis are discussed. Argolis is newly recorded from Laos, Pakistan, and Vietnam.

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5

SWANSON, DANIEL R. "Status of the name Argolis in Insecta." Zootaxa 4471, no. 1 (2018): 179. http://dx.doi.org/10.11646/zootaxa.4471.1.9.

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The purpose of the present notice is to identify and clarify a case of mistaken homonymy surrounding the name Argolis, pertaining to Lepidoptera, Hemiptera, and Coleoptera. It is here demonstrated that “Argolis” (Boisduval 1836: 2) is an incorrect original spelling of Ergolis Boisduval, 1836 (Lepidoptera: Nymphalidae); therefore, Argolis Stål, 1861 (Hemiptera: Reduviidae) is the valid senior synonym of Caunus Stål, 1865, while Argolis Chapuis, 1874 (Coleoptera: Chrysomelidae) remains a junior homonym. The following details summarize the situation:

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6

Mitrakou, K., I. Mitrakos, G. C. Michalopoulos, et al. "Bacterial Resistance in Argolis, Greece." International Journal of Infectious Diseases 12 (December 2008): e400. http://dx.doi.org/10.1016/j.ijid.2008.05.1054.

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7

Fossey, John M. "The cults of Artemis in Argolis." Euphrosyne 15 (January 1987): 71–88. http://dx.doi.org/10.1484/j.euphr.5.126636.

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8

VASSILIOU, Anastasia. "Middle Byzantine chafing dishes from Argolis." Δελτίον Χριστιανικής Αρχαιολογικής Εταιρείας 37 (October 25, 2016): 251. http://dx.doi.org/10.12681/dchae.10702.

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Τα αυτοθερμαινόμενα σκεύη, γνωστά στην ελληνική βιβλιογραφία ως «σαλτσάρια», συνιστούν ένα σύνθετο σκεύος της μεσοβυζαντινής περιόδου. Εμφανίζονται τόσο σε λευκό όσο και σε ερυθρό πηλό, με κυρίαρχη την παράκτια και αστική διασπορά στο χώρο της κεντρικής και ανατολικής Μεσογείου. Στην Αργολίδα και κυρίως στο Άργος, έχουν έως τώρα καταγραφεί 53 δείγματα που στην πλειονότητά τους φέρουν ομοιότητες με αντίστοιχα δείγματα από την Κόρινθο, την Αθήνα και τη Θήβα και θα μπορούσαν να χρονολογηθούν, βάσει παραλλήλων, κυρίως στον 10ο-11ο αιώνα. Θα απευθύνονταν πιθανώς σε μέλη της τοπικής ελίτ, συνιστώντας μια μαρτυρία για πιο «εξελιγμένες» διατροφικές συνήθειες στη βυζαντινή περιφέρεια.

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9

Senowbari-Daryan, Baba. "Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece." Acta Palaeontologica Romaniae 10, no. 1-2 (2014): 1–2. https://doi.org/10.5281/zenodo.13189667.

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10

Yioutsos, Nektarios-Peter. "The last occupation of Asine in Argolis." Opuscula. Annual of the Swedish Institutes at Athens and Rome 10 (November 2017): 164–89. http://dx.doi.org/10.30549/opathrom-10-08.

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Kastraki Hill on the eastern Argolic Gulf, with visible remains of impressive fortifications, has been identified since the mid-19th century as the position occupied by the acropolis of ancient Asine. The first systematic excavations were carried out by the Swedish Institute in the 1920s and revealed the continuous habitation of the site from the Early Helladic period (3rd millennium BC) up to the late 4th-early 5th century AD. Many additions and repairs on the acropolis were made during the Byzantine period and the 2nd Venetian Occupation of the Peloponnese (1686–1715). However, the most destructive interventions in the area are the works carried out by the Italians during World War II. Fearing an invasion of the Allies on this side of the Peloponnese, the Italians fortified the acropolis by making additions to the ancient walls and constructing auxiliary buildings, pillboxes, observation posts and trenches around the rocky outcrop using materials from buildings of the Lower Town. Their departure after the war revealed the extent of the destruction of the antiquities. During the past few decades we have seen interest in approaching sites of recent conflict using archaeological methods that could help researchers understand these transformations of matter in a deeper way. Such is the case of Asine, a palimpsest landscape with archaeological and historical remains of human activity extending from prehistoric to modern European times. This article will attempt to reveal this hidden side of contemporary history and offer a glimpse into the lives of the last inhabitants of the ancient city.

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11

Senowbari-Daryan, Baba, Dionissios Matarangas, and Myrsini Vartis-Matarangas. "Norian-Rhaetian reefs in Argolis Peninsula, Greece." Facies 34, no. 1 (1996): 77–82. http://dx.doi.org/10.1007/bf02546157.

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12

Mitrakou, K., I. Mitrakos, G. C. Michalopoulos, P. Papageorgiou, M. Vossou, and F. Rozi. "Analysis of Blood Cultures in Argolis Greece." International Journal of Infectious Diseases 12 (December 2008): e213. http://dx.doi.org/10.1016/j.ijid.2008.05.530.

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13

Argyriadis, I., M. Midoun, and P. Ntontos. "A NEW INTERPRETATION OF THE STRUCTURE OF INTERNAL HELLENIDES." Bulletin of the Geological Society of Greece 43, no. 1 (2017): 264. http://dx.doi.org/10.12681/bgsg.11179.

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This study is based on some new observations made from Southern and Central Evia, Argolis and North-central part of Pindos. Our observations lead us to adopt a simplified view of the paleogeography of Greek mainland just before the Alpine orogeny. The subsequent varied tectonic units originate mainly from the following paleogeographic areas:• A carbonate Arab-African shelf margin which displays several lateral transitions, ridges and basins. In the Greek mainland this margin is represented by the Preapulian, Ionian, GavrovoTripolis, Parnassos zones, Olympus platform and probably the Kavala and Thassos Marbles.• A transition zone from the shelf units to the Tethys ophiolites (Pindos Zone, Styra, Argolis and Hydra, Eretrias new unit).• Tethys ophiolites, which might represent an “ocean” fault zone or subduction of lithosphere along a weak zone.• An Hercynian continental mass (Servomacedonian).

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14

Zananiri, I., E. Chiotis, P. Tsombos, V. Hademenos, and A. Zervakou. "GEOARCHAEOLOGICAL STUDIES IN URBAN AND SUBURBAN AREAS OF THE ARGOLIS PREFECTURE." Bulletin of the Geological Society of Greece 43, no. 3 (2017): 1539. http://dx.doi.org/10.12681/bgsg.11328.

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The application of earth science principles and techniques to the understanding of the archaeo-logical record has become a common practice, while reducing the archaeological risk is possible by clarifying areas of archaeological potential at an early stage. Towards this scope non-invasive geophysical magnetometry surveys were carried out at the city of Argos, successfully locating areas of interest for future excavations. Geoarchaeology studies in the Argolis Prefecture also involved the spatial location of the archaeological protection zones in the city of Nafplio, by combining data from the Official Government Gazettes, aerial photographs and high-resolution satellite images. Another study dealt with the palaeogeographic evolution of the broader Palea Epidavros area; fieldwork comprised electric resistivity soundings, total field magnetic measurements and two research boreholes at different altitudes. Finally, geoarchaeological research was employed to locate rocks suitable for the restoration of the Grave Circle A of Mycenae. The data management and cartographic representation was performed, in all cases, using Geographic Information Systems, where a geographic database was created, including all available information: local geology, topographic features, satellite images and archaeological data.

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15

Bandini, Alexandre N., Peter O. Baumgartner, and Michéle Caron. "Turonian Radiolarians from Karnezeika, Argolis Peninsula, Peloponnesus (Greece)." Eclogae Geologicae Helvetiae 99, S1 (2006): S1—S20. http://dx.doi.org/10.1007/s00015-006-0605-2.

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16

Mariolakos, Ilias. "The Geomythological geotope of Lerni Springs (Argolis, Greece)." Geologica Balcanica 28, no. 3-4 (1998): 101–8. http://dx.doi.org/10.52321/geolbalc.28.3-4.101.

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17

Weber-Pallez, Clémence. "Argos, l’Empire romain et les historiens aujourd’hui : déconstruire les représentations, reconstruire l’histoire argienne." Revue des Études Grecques 134, no. 2 (2021): 317–60. http://dx.doi.org/10.3406/reg.2021.8709.

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This article examines the dangers of anachronism in the use of late sources to reconstruct the history of Argos in the Archaic, Classical and Hellenistic periods. Three traditional historiographical objects – the Argolid region, the Argolic shield and the destruction of Mycenae in 468 BC – are analyzed as representations. Through the identification of the producers of these representations, from their creation to their impact on current research, we attempt to draw a new history of Argos that steers away from the stereotypes conveyed by imperial period sources.

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18

Mitropoulos, D., and I. Zananiri. "UPPER QUATERNARY EVOLUTION OF THE NORTHERN ARGOLIS GULF, NAFPLIO AREA." Bulletin of the Geological Society of Greece 43, no. 3 (2017): 1474. http://dx.doi.org/10.12681/bgsg.11322.

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The recent palaeogeographic history of the Gulf of Argolis was studied by means of marine geophysical surveys and sediment sampling for subsequent laboratory analyses. Data interpretation suggests a relatively smooth seafloor gradient, characterized by an amphitheatrical pattern of the sea bottom. Prominent beetling features comprise the Bourtzi islet near Nafplio coast, small ridges in the southern margin of the studied area, and several conical ridges in the central part of the gulf. Four unconformities were identified, defining four different sedimentary units. Granulometry measurements allowed the mapping of present-day seafloor sediment distribution, where fine sediments prevail; the only exception was observed at the eastern coastal areas, where sand con-tent reaches 70%. Contouring of granulometry statistical parameters highlights a NW towards SE transfer of fine-grain sediments. Finally, taking into account the results of the present study and all available information for the broader area, a model for the Upper Quaternary palaeogeographic evolution of the Argolis Gulf was constructed.

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19

Dimou, D., J. Drossopoulou, E. Moschos, C. Varveri, and F. Bem. "First Report of Citrus tristeza virus in Greece." Plant Disease 86, no. 3 (2002): 329. http://dx.doi.org/10.1094/pdis.2002.86.3.329b.

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Large-scale surveys of Citrus spp. for the presence of Citrus tristeza virus (CTV) by the Ministry of Agriculture in Greece began in 1995. Over 26,000 trees have been tested by enzyme-linked immunosorbent assay and immunoprinting (2). In summer 2000, the first CTV-infected sweet orange cv. Lane Late tree grafted on CTV-tolerant Carrizo citrange was found in Argolis County, Peloponnese. This tree belonged to a batch of CAC propagation material (20 trees) illegally introduced from Spain in 1994, which was subsequently traced and found to be infected (45%). A follow-up search of trees grafted with the above material was undertaken in the two concerned regions (Argolis and Chania-Crete), and more than 3,500 trees have been removed. Extensive surveys continue to identify and destroy new infections. Few cases (15 of 16,800) of natural transmission to cultivars other than cv. Lane Late have been found. All of these have been close to the initially infected trees in the Argolis area. Surveys in spring 2001 were extended to certified propagation material of Clemenpons mandarin on Carrizo citrange imported from Spain, and 7 of 1,038 plants were infected (0.64%). The virus was successfully graft-transmitted to sweet orange cv. Madame Vinous and sweet lime seedlings, where it was identified by immunoprinting and reverse transcription-polymerase chain reaction (1). Mild vein clearing symptoms appeared on both indicators. Vein clearing on sweet lime was also accompanied by leaf cupping. To our knowledge, this is the first report of CTV in Greece. References: (1) A. Sambade et al. J. Virol. Methods 87:25, 2000. (2) C. Vela et al. J. Gen. Virol. 67:91, 1986.

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20

Tombros, S., and K. St. Seymour. "HERMIONE, EVOLUTION OF ATe-BEARING EPITHERMAL MINERALIZATION, ARGOLIS, HELLAS." Bulletin of the Geological Society of Greece 40, no. 2 (2007): 996. http://dx.doi.org/10.12681/bgsg.16782.

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The Cu-Te-bearing pyrite deposits of Hermione, Argolis are hosted in Miocenic ophiolites. The ophiolites are overlain by a shale-sandstone formation with intercalations of limestones and manganiferous sedimentary rocks. The ore deposits form irregular lenticular or stratiform ore bodies, and veins. These ore bodies are related to volcanic activity in an arc-related rift at the margins of a palaeocontinent. Late N- to NNE-trending, sinistral, milky quartz-pyrite-calcite veins cut the host ophiolites. Alteration haloes of quartz-calcite, albite-sericitechlorite, and chalcedony-epidote-clay minerals are developed in the lavas as concentric shells, or as envelops that parallel the quartz veins. The telluriumbearing mineralization is developed in two successive stages, characterized by the assemblages: pyrite-(pyrrhotite)-magnetite-chalcopyrite-sphalerite (Stage I) and galena-sphalerite-freibergite-marcasite-chalcocite (Stage II), followed by a supergene stage. The cobaltiferous pyrite-chalcopyrite geothermometer defined two ranges of last-equilibration temperatures: 220° to 250°Cfor Stage I, and 120° to 195°Cfor Stage II. The calculated δ18 Ο and SD compositions of the mineralizing fluids, at 200° and 250°C, reflect the dominance of a magmatic component. The calculated δ SH2S fluid values reveal a magmatic source for the sulphur, with minor contribution from submarine sediments, whereas tellurium is proposed to be derived from a mafic-ultramafic source.

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21

Dostal, Jaroslav, Lorenzo Toscani, Adonis Photiades, and Silvio Capedri. "Geochemistry and petrogenesis of Tethyan ophiolites from northern Argolis (Peloponnesus, Greece)." European Journal of Mineralogy 3, no. 1 (1991): 105–22. http://dx.doi.org/10.1127/ejm/3/1/0105.

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22

Zabrana, Lilli. "Vorratshaltung in der mykenischen Argolis als Instmment einer palatialen Zentralgewalt?" Jahreshefte des Österreichischen Archäologischen Institutes in Wien 77 (2010): 375–98. http://dx.doi.org/10.1553/oejh77s375.

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23

Clift, Peter D., and Alastair H. F. Robertson. "A Cretaceous Neo-Tethyan carbonate margin in Argolis, southern Greece." Geological Magazine 127, no. 4 (1990): 299–308. http://dx.doi.org/10.1017/s0016756800014862.

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AbstractThe Argolis Peninsula, southern Greece, is believed to form part of a Pelagonian microcontinent located between two oceanic basins, the Pindos to the west and theVardar to the east, in Triassic to Tertiary time. In eastern Argolis, two important units are exposed: (i) the Ermioni Limestones cropping out in the southwest; (ii) the Poros Formation, observed on an offshore island in the northeast, and on the adjacent mainland. Both these units comprise late Cretaceous (Aptian-Maastrichtian) pelagic limestones, calciturbidites, lenticular matrix- and clast-supported limestone conglomerates and slump sheets. However, the Poros Formation is distinguished from the Ermioni Limestones by the presence of bituminous micritic limestones and an increasing proportion of shale up sequence. These successions are deep-water slope carbonates that once formed the southeast-facing passive margin of the Pelagonian platform (Akros Limestone). Beyond this lay a late Cretaceous ocean basin in the Vardar Zone. This ocean was consumed in an easterly-dipping subduction zone in latest Cretaceous (?) to early Tertiary time, giving rise to an accretionary complex (Ermioni Complex). During early Tertiary (Palaeocene-Eocene) time the passive continental margin (Pelagonian Zone) collided with the trench and accretionary complex to the east. As the suture tightened, former lower-slope carbonates (Ermioni Limestones) were accreted to the base of the over-riding thrust sheets and emplaced onto the platform. Farther west, bituminous upper slope carbonates (Poros Formation) flexurally subsided and passed transitionally upwards into calcareous flysch and olistostromes in a foreland basin. These sediments were then overridden by the emplacing thrust stack and themselves underplated. Late-stage high-angle faulting then disrupted the tectonostratigraphy, in places juxtaposing relatively high and low structural levels of the complex.

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24

Piérart, Marcel. "Le réseau routier d’Argolide et la Périègèse de Pausanias. A propos d'un livre récent (Tausend (K.), Verkehrswege der Argolis . Rekonstruktion und historische Bedeutung. -Stuttgart : Steiner, 2006)." Revue des Études Anciennes 111, no. 1 (2009): 237–56. http://dx.doi.org/10.3406/rea.2009.6626.

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Klaus Tausend's Verkehrswege der Argolis postulates that archaeological evidence should be assessed independently of ancient texts. However concerning the reconstruction of the criss-crossing network of ancient roads in the Peloponese, Pausanias' description of Greece is in a class of its own. In relation to some topographical problems, a re-reading of the Periegesis in the the light of archaeological evidence leads to find alternative solutions to the explanation of the roads and the borders they run across.

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25

Sabatini, Serena. "Textile tools from the East Gate at Mycenaean Midea, Argolis, Greece." Opuscula. Annual of the Swedish Institutes at Athens and Rome 9 (November 2016): 217–47. http://dx.doi.org/10.30549/opathrom-09-08.

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This contribution presents in the first place an analysis and interpretation of all implements and tools possibly related to textile production that were recovered in the East Gate area at Midea during the Greek-Swedish excavation campaigns between 2000 and 2009. Secondly, with the help of comparative evidence from other zones on the citadel of Midea and also from other Mycenaean sites, it is argued that at least one multifunctional unit, where textile manufacture was also carried out, might have existed in the East Gate area. It is also suggested that this textile production comprised fine quality products to a significant extent. Finally, referring to signalling theory it is proposed that the fabrics possibly manufactured in the citadel served as means for the local community or élite to partake in the socio-cultural and political competition which seems to characterize Mycenaean society in general.

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26

CLIFT, PETER D., and ALASTAIR H. F. ROBERTSON. "Deep-water basins within the Mesozoic carbonate platform of Argolis, Greece." Journal of the Geological Society 147, no. 5 (1990): 825–36. http://dx.doi.org/10.1144/gsjgs.147.5.0825.

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27

Rettori, R., L. Angiolini, and G. Muttoni. "Lower and Middle Triassic foraminifera from the Eros Limestone, Hydra Island, Greece." Journal of Micropalaeontology 13, no. 1 (1994): 25–46. http://dx.doi.org/10.1144/jm.13.1.25.

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Abstract. The systematics and stratigraphic ranges (constrained by conodont dating) of abundant and well preserved foraminiferal faunas from six sections in the Lower and Middle Triassic Eros Limestone of central and western Hydra (Argolis Peninsula, Greece) are described. A joint analysis of the conodonts, foraminifera and bivalves has enabled the Scythian and Anisian stages to be recognized with some certainty within the Eros Limestone carbonate platform. The foraminifera have affinities with those of many other Tethyan localities, in particular the Dinarides, Balkans, Carpathians and the Southern Alps.

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28

Photiades, A. "GEOLOGICAL CONTRIBUTION TO THE TECTONO- STRATIGRAPHY OF THE NAFPLION AREA (NW ARGOLIS, GREECE)." Bulletin of the Geological Society of Greece 43, no. 3 (2017): 1495. http://dx.doi.org/10.12681/bgsg.11324.

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The geological mapping in scale 1:5.000 in the greater Nafplion area indicated a Tertiary nappe stack of different Pelagonian-originated tectonic units structurally overlying the Subpelagonian series of Argolis Peninsula. The Subpelagonian series as lower unit is characterized by a shallow-water carbonate platform of Middle Triassic to Early Jurassic age, locally deep-water ammonitico-rosso facies and red cherts and is overlain by a tectono-sedimentary ophiolitic melange of Malm age. After the compressive tectonic phase of late Jurassic, the Nafplion area at that time records a severe extensional intra-Cretaceous syn-rift phase leading to the deposition of diachronous Meso-autochthonous Cretaceous limestone deposits rich in faulted-derived limestone breccias series, topped by deep-water limestone of Campanian-Maastrichtian and then from Lower Tertiary pelagic limestone facies passes upwards into post-Ypresian flysch. The different Pelagonian telescoped tectonic units were contemporaneously overthrusting northwestward, over the Subpelagonian post-Ypresian flysch sequence, during the Late Eocene compressive phase, are successively characterized by: (a) a middle tectonic unit of a flyschoidal melange of Late Cretaceous-Early Tertiary age, like the Adheres Melange surfaces in Southern Argolis, associated with various carbonate and ophiolite tectonosomes trapped and carried within this highly disrupted terrigenous flyschoidal melange and, (b) an upper unit consists of Cretaceous carbonate slivers bearing serpentinite sole (Palamidi, Akronafplia, Profitis Ilias, Aria) and/or of Middle Triassic-Early Jurassic carbonate platform slices. The above nappe stacking may be connected with the Eocene continental collision of the Hellenides.

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29

Catling, R. W. V. "Exports of Attic Protogeometric pottery and their identification by non-analytical means." Annual of the British School at Athens 93 (November 1998): 365–78. http://dx.doi.org/10.1017/s006824540000349x.

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This paper draws attention to the potential for recognizing exported Attic Protogeometric pottery by macroscopic characteristics of its fabric, whose salient features are described. The utility of these criteria are tested on a group of pottery from Asine in the Argolis whose Attic origin was not recognized in the original publication. A brief survey of the distribution of exported Attic Protogeometric pottery shows it to occur mainly in the southern Aegean, with notable concentrations at Lefkandi, Aigina, Asine and Knossos. A list of exports is appended to this survey.

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30

Zervakou, A. D., and P. Tsombos. "GIS IN URBAN GEOLOGY: THE CASE STUDY OF NAFPLIO, ARGOLIS PREFECTURE, GREECE." Bulletin of the Geological Society of Greece 43, no. 3 (2017): 1559. http://dx.doi.org/10.12681/bgsg.11330.

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The aggregation of population in big cities leads to the concentration of human activities, overconsumption of natural resources and urban growth without spatial planning and sustainable management. As a result, urban societies are exposed to various dangers and threats with economic, social, ecological, and environmental impacts on the urban surroundings. Problems associated with urban development are related to the existing geological conditions. Therefore, the provision of appropriate geological information about the urban environment is essential for every sustainable urban planning. The first systematic recording, codification and documentation of “Urban Geology” geothematic information in Greece was implemented by the Institute of Geology and Mineral Exploration (I.G.M.E.) in the framework of the project called “Collection, codification and documentation of geothematic information for urban and suburban areas in Greece - pilot applications”. Through the implementation of this project, geological mapping, geotechnical, geochemical, geophysical research and measurements took place at four pilot cities of Greece. Nafplio, the capital city of Argolis prefecture, was one of them. During the project, all compiled data were stored and processed in specially designed geodatabases in GIS environment in order to produce multifunctional geothematic maps and other digital products (DEMs, 2D - 3D surfaces).

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31

Pomoni-Papaioannou, F. "Facies analysis of Lofer cycles (Upper Triassic), in the Argolis Peninsula (Greece)." Sedimentary Geology 208, no. 3-4 (2008): 79–87. http://dx.doi.org/10.1016/j.sedgeo.2008.04.005.

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32

Vrielynck, Bruno. "Jurassic sedimentary evolution and nappe emplacement in the argolis peninsula(Peloponnesus, Greece)." Geobios 19, no. 5 (1986): 669. http://dx.doi.org/10.1016/s0016-6995(86)80064-x.

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Lisle, Richard J. "Jurassic sedimentary evolution and nappe emplacement in the Argolis Peninsula (Peloponnesus, Greece)." Earth-Science Reviews 24, no. 4 (1987): 292. http://dx.doi.org/10.1016/0012-8252(87)90073-0.

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34

Capedri, S., R. Grandi, A. Photiades, and L. Toscani. "‘Boninitic’ clasts from the Mesozoic olistostromes and turbidites of Angelokastron (Argolis, Greece)." Geological Journal 31, no. 4 (1996): 301–22. http://dx.doi.org/10.1002/(sici)1099-1034(199612)31:4<301::aid-gj707>3.0.co;2-w.

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35

Ahmed, Ahmed A., Husaam E. Hassan, Mohamed F. Hegazy, et al. "Argolic Acid A and Argolic Methyl Ester B, Two New Cyclopentano-monoterpenes Diol from Nepeta Argolica." Natural Product Communications 1, no. 7 (2006): 1934578X0600100. http://dx.doi.org/10.1177/1934578x0600100701.

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Two new cyclopentanomonoterpenes, argolic acid A (1) and argolic methyl ester B (2), in addition to four known compounds, were isolated from the aerial parts of Nepeta argolica subsp. argolica. The structures of the compounds were elucidated by one and two dimensional NMR spectroscopy.

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36

Antonaccio, Carla M., and Birgitta Eder. "Argolis, Lakonien, Messenien: Vom Ende der mykenischen Palastzeit bis zur Einwanderung der Dorier." American Journal of Archaeology 104, no. 3 (2000): 613. http://dx.doi.org/10.2307/507243.

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37

Apostolidis, Em, та An Koutsouveli. "ΕNGINEERING GEOLOGICAL MAPPING IN THE URBAN AND SUBURBAN REGION OF NAFPLION CITY (ARGOLIS, GREECE)". Bulletin of the Geological Society of Greece 43, № 3 (2017): 1418. http://dx.doi.org/10.12681/bgsg.11317.

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In our days the strategy of an integrated planning approach in dealing with urban development matters, is a reality and engineering geology plays a primary role. In the present study an approach of the engineering geological conditions of Nafplion city and the wider area are given. In the region of interest, four (4) sampling boreholes were drilled by IGME, up to the depth of 40m. During the boring procedure in situ SPT and permeability tests were carried out, as well as the lithology of obtained material has been described. Samples, undisturbed and disturbed, have also collected for further laboratory tests. After the completion of each borehole, piezometric tubes were installed, for the monitoring of the underground water table. Laboratory tests for the determination of physical and mechanical characteristics of all drilled formations were executed. The geotechnical distinction and unification of the geological forma tions was made on a 1:5,000 topographical map, in accordance with the up to date in ternational practice. The engineering geological map in the urban and suburban region of Nafplion city is presented and the geotechnical characteristics of the formations struc turing the area are evaluated. The combination of the results of the drilling programme as well as on the engineering geological approach and the geological structure of the studied area, resulted the compilation of the engineering geological map (scale 1:5,000) of Nafplion city wide area, where 18 engineering geological types are distinguished. The boreholes data of other public bodies have been also taken into account for this compilation. As the task of this project was the contribution to the urban development of Nafplion city, this engineering geological map will be a useful tool for engineers, planners, civil authorities, etc.

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Tsombos, P. I., and A. D. Zervakou. "THE “URBAN GEOLOGY” PROJECT OF IGME: THE CASE STUDY OF NAFPLIO, ARGOLIS PREFECTURE, GREECE." Bulletin of the Geological Society of Greece 43, no. 3 (2017): 1528. http://dx.doi.org/10.12681/bgsg.11327.

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The Institute of Geology and Mineral Exploration of Greece (I.G.M.E.), in the framework of CSF 2000 – 2006 (Community Support Framework 2000-2006), implemented the pilot project “Collection, Codification and Documentation of geothematic information for urban and suburban areas in Greece - pilot applications”. Geological, geochemical, geophysical, geotechnical, hydrogeological and other geothematic data concerning the urban and surrounding areas of Drama (North Greece), Nafplio & Sparti (Peloponnese) and Thrakomakedones (Attica) were collected. Drillings, geological and neotectonic mapping and other “in situ” measurements and field work took place. All initial and derived analogical and digital data were compiled and processed in specially designed geo-databases in GIS Environment. The final results are presented in geothematic maps and other digital products (DEMs, 2D – 3D surfaces, geodatabases). Such data constitute the essential knowledge base for land use planning and environmental protection in specific urban areas. Through this pilot project, new scientific approaches, methodologies and standards were developed and improved in order to apply to other future projects concerning the major cities of the whole country.

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Samaropoulou, Sofia, Pepy Bareka, and Georgia Kamari. "Hybridization and karyotype variability of three endemic Fritillaria L. (Liliaceae) in Argolis Peninsula (Greece)." Plant Biosystems - An International Journal Dealing with all Aspects of Plant Biology 154, no. 3 (2019): 348–60. http://dx.doi.org/10.1080/11263504.2019.1612478.

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Ingemark, Dominic. "A Roman bath with broken windows in Asine, Argolis. The result of repeated earthquakes?" Opuscula. Annual of the Swedish Institutes at Athens and Rome 17 (November 2024): 69–93. http://dx.doi.org/10.30549/opathrom-17-05.

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A substantial assemblage of Roman window glass—consisting primarily of “cast”, matt/glossy examples, but also including cylinderblown, double-glossy window glass—was discovered during the 1926 excavations of a Late Roman bath in Asine, Argolis, the Peloponnese, Greece. It is clear that this material emanates from damage done to the building, and the question of whether this had human or natural causes is discussed in this paper: was it the “barbarian” invasion of the Visigoth king Alaric in the late 4th century AD that led to the windows being broken? Or, was the damage caused by the earthquakes known to have hit the Eastern Mediterranean area in Late Antiquity? Traces of destruction typical of earthquakes were found in the bath building, and the destruction occurred in a period known for its high seismic activity: the so-called Early Byzantine Tectonic Paroxysm, which led to the conclusion that the bath was hit by at least one, possibly several, earthquakes, causing the windows to shatter and fall out of their frames. Some of the glass sherds were in all probability hidden under dust and debris and were never recovered despite the fact that glass was extensively recycled at the time.

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Matiatos, Ioannis, and Apostolos Alexopoulos. "Application of stable isotopes and hydrochemical analysis in groundwater aquifers of Argolis Peninsula (Greece)." Isotopes in Environmental and Health Studies 47, no. 4 (2011): 512–29. http://dx.doi.org/10.1080/10256016.2011.617883.

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42

Shipley, Graham. "ARGOS AND THE ARGOLID." Classical Review 50, no. 2 (2000): 550–51. http://dx.doi.org/10.1093/cr/50.2.550.

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Özgünel, Coşkun. "Selçuk Arkeoloji Müzesinde Saklanan Miken Pyxisi ve Düşündürdükleri." Belleten 51, no. 200 (1987): 535–48. http://dx.doi.org/10.37879/belleten.1987.535.

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60'lı yıllarda Batı Anadolu kıyı kesiminde ve içlerinde yapılan yeni kazı ve araştırmalar, Anadolu'nun Geç Bronz Çağ'ında karşılaştığımız kimi sorunlara bizleri tekrar yöneltmektedir. Özellikle II. binin 2. yarısından itibaren Kıta Yunanistan - Argolis kökenli kültür kalıntıları, Batı Anadolu kıyılarında karşımıza çıkar. Kültür ve ticari alış verişle oluşan bu kalıntılar, sorunları daha da güncelleştirmiştir. Konumuzun içeriğini oluşturan Miken-Akha kültür izleri ve kalıntıları Batı Anadolu'da, önceleri Girit-Minos ilişkileriyle başlar. Sonra Miken-Akha ticari egemenliğini yaşar. Ayrıca Ege ile Batı Anadolu-Hitit ilişkileri de günümüz arkeolojisinde göz ardı edilmemiştir. Nitekim bilim adamları yıllardır önemini korumakta olan bu oluşum üzerine ilgilerini yoğunlaştırmışlardır. Daha önceki bir araştırmamızda, Batı Anadolu'daki Miken etkinliklerini irdelemiş, yayınlanmamış kimi özgün buluntuları arkeoloji dünyasına duyurmuştuk. Bu çalışmamızda yine bir yüzey araştırması sırasında Ionia içlerinde ele geçen Miken pyxisini incelemek ve bazı sorunlara değinmek arzusundayız.

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44

Triantafyllidis, Stavros, Stylianos F. Tombros, Degao Zhai, and Sotirios Kokkalas. "The upper Cretaceous Ermioni VMS deposit, Argolis Peninsula, Peloponnese, Greece: Type, genesis, and geotectonic setting." Ore Geology Reviews 138 (November 2021): 104403. http://dx.doi.org/10.1016/j.oregeorev.2021.104403.

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Ekroth, Gunnel. "David Boehringer: Heroenkulte in Griechenland von der geometrischen bis zur klassischen Zeit. Attika, Argolis, Messenien." Gnomon 77, no. 5 (2005): 437–42. http://dx.doi.org/10.17104/0017-1417_2005_5_437.

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46

Papadopoulos, J. K. "Book Review: Argolis, Lakonien, Messenien: vom Ende der Mykenischen Palastzeit bis zur Einwanderung der Dorier." European Journal of Archaeology 4, no. 2 (2001): 287–88. http://dx.doi.org/10.1177/146195710100400215.

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47

Ntageretzis, Konstantin, Andreas Vött, Peter Fischer, et al. "Traces of repeated tsunami landfall in the vicinity of Limnothalassa Moustou (Gulf of Argolis – Peloponnese, Greece)." Zeitschrift für Geomorphologie, Supplementary Issues 59, no. 4 (2015): 301–17. http://dx.doi.org/10.1127/zfg_suppl/2015/s-00206.

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Matiatos, I., A. Alexopoulos, and N. Zouridakis. "USE OF STABLE ISOTOPES IN THE DETERMINATION OF THE MEAN ALTITUDE OF RECHARGE AND THE INVESTIGATION OF FUNCTION MECHANISM OF SPRING WATERS IN ARGOLIS PENINSULA (GREECE)." Bulletin of the Geological Society of Greece 43, no. 4 (2017): 1792. http://dx.doi.org/10.12681/bgsg.11365.

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In the present study, the isotopic composition (δ18Ο) of several spring waters in Argolis peninsula is examined. The use of the specific isotope aimed at the determination of the altitude of recharge areas, while the credibility of the extracted results was verified by in situ geological observations. The applied methodology included the construction of a linear diagram which correlates the stable isotopic values (δ18Ο) in meteoric waters and the altitude. Isotopic data, concerning meteoric waters, came from: a) rain gauge stations of GNIP network (IAEA/WMO), b) rain tanks and selected wells located in Mt. Arachnaio, c) improvised rain collectors which were put in several sites in the peninsula. A decrease of 0.45‰ δ18Ο per 100m altitude was determined. The average isotopic composition of the examined springs, as far as δ18Ο is concerned, resulted from 14 sampling periods between October 2005 and March 2008. This 18O-content of spring waters was used to derive the recharge area and consequently to evaluate the mechanism of water renewal.

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Argyriadis, Ion, and Silvia Forti. "Structure and history of Hellenides." Boletín Geológico y Minero 127, no. 2-3 (2016): 575–92. http://dx.doi.org/10.21701/bolgeomin.127.2-3.019.

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This study is based on some new field observations made on the group of the Eastern Hellenic regions. Our observations have led us to adopt a simplified view of the paleogeography of the Greek mainland before the Alpine orogenesis. The subsequent varied tectonic units originate mainly from the following paleogeographic areas: • A carbonate Arabo-African shelf margin which displays several lateral transitions, ridges and basins. On the Greek mainland this margin is represented by the Preapulian, Ionian, Gavrovo-Tripolis, Parnassos zones, the Olympus platform and probably the Kavala and Thassos marble. • A transition zone from the shelf units to the Tethys ophiolites (Pindos Zone, Styra, Argolis and Hydra, Eretrias new unit). • Tethys ophiolites, which might represent either an “ocean” fault zone or subduction of the lithosphere along a weak area. • A Hercynian continental mass (Serbomacedonian). This group is currently completed by the presence of a large tectonic mélange connected to the ophiolite overthrust.

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Attas, Michael, John M. Fossey, and Leo Yaffe. "An Archaeometric Study of Early Bronze Age Pottery Production and Exchange in Argolis and Korinthia (Corinthia), Greece." Journal of Field Archaeology 14, no. 1 (1987): 77. http://dx.doi.org/10.2307/530208.

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