Departures from Argostoli

Total Page：16

File Type：pdf, Size：1020Kb

24/6 - 10/9/2019 Departures from A r g o s t o l i ROUTES PRICES DAYS DEPARTURE RETURN 8:00 9:30 11:00 12:30 14:00 15:30 8:30 10:00 11:30 13:00 14:30 ARGOSTOLI - AIRPORT 2.0 € Every Day 17:00 18:30 20:00 22:00 16:00 17:30 19:00 20:30 22:30 Monday to Friday 6:45 10:00 13:00 14:45 8:00 9:45 17:00 18:00 ARGOSTOLI - SAMI 4.0 € Saturday 6:45 10:00 13:00 14:45 8:00 17:00 18:00 Sunday 6:45 10:00 14:45 17:00 18:00 Monday to Friday 10:00 13:00 14:45 7:35 9:30 17:55 ARGOSTOLI - MELISSANI 4.0 € Saturday 10:00 13:00 14:45 7:35 17:55 (departure from Sami 18:00) Sunday 10:00 14:45 17:55 (departure from Sami 18:00) Monday to Friday 10:00 11:30 13:00 14:45 6:45 7:25 9:25 17:45 ARGOSTOLI - AG. EFIMIA 4.0 € Saturday 10:00 13:00 14:45 7:25 17:45 Sunday 10:00 14:45 17:45 Monday to Friday 10:40 11:30 13:00 14:45 7:00 7:20 9:15 17:30 ARGOSTOLI - DIVARATA 4.0 € Saturday 10:40 13:00 14:45 7:20 17:30 Sunday 10:40 14:45 17:30 Monday to Friday 10:40 13:00 16:45 ARGOSTOLI - MYRTOS (connect.) 4€ + 1.5€ Saturday & Sunday 10:40 15:45 (Stopover 1 hour at Sami) ARGOSTOLI - ASSOS (connect.) 4€ + 2€ Monday to Friday 11:30 16:10 Monday & Friday 10:40 11:30 14:45 6:00 17:00 ARGOSTOLI - FISKARDO 6.4 € Tuesday to Thursday 10:40 11:30 14:45 6:30 17:00 Saturday & Sunday 10:40 14:45 17:00 Please contact our agencies to get informed for any routes' changes The departures' times in blue may change in case of ferry's departure's time change * The route is not operated on Saturday & Sunday -> Only tourist routes will be operated at 15-16 August 2019 (check the corresponding announcement at www.ktelkefalonias.gr ) 24/6 - 10/9/2019 Departures from A r g o s t o l i ROUTES PRICES DAYS DEPARTURE RETURN Monday to Friday 10:30 14:30 7:00 11:00 15:00 ARGOSTOLI - AG. GERASIMOS 1.8 € Saturday 8:30 13:00 9:00 13:45 Monday to Friday 10:30 14:30 7:30 11:00 14:45 ARGOSTOLI - DILINATA 1.8 € Saturday 8:30 13:00 9:15 13:15 ARGOSTOLI - DIGALETO 4.0 € Monday & Friday 13:00 7:00 ARGOSTOLI - PESSADA 1.8 € Monday to Friday 7:45 10:40 12:30 8:15 11:10 13:00 ARGOSTOLI - SVORONATA 1.8 € Monday to Friday 6:50 10:00 13:40 7:20 10:25** 14:10 Monday to Friday 9:35 10:30 11:30 14:30 16:00 19:00 8:50 15:20 17:30 18:20 ARGOSTOLI - LOURDAS (connect.) 2.0 € Saturday & Sunday 9:35 10:30 14:30 16:00 19:00 8:50 15:20 17:30 18:20 Monday to Friday 10:30 14:30 7:25 9:15 17:15 ARGOSTOLI - KATELIOS 3.1 € Saturday & Sunday 10:30 14:30 9:15 17:15 Monday to Friday 10:30 14:30 7:10 9:00 17:00 ARGOSTOLI - SKALA 4.5 € Saturday & Sunday 10:30 14:30 9:00 17:00 Monday to Friday 7:45 11:30 13:30 7:00 8:30 14:00 16:30 18:45 23:00 ARGOSTOLI - POROS 5.0 € Saturday & Sunday 9:30 13:45 18:00 8:30 14:30 16:30 18:45 23:00 ARGOSTOLI - LASSI 1.8 € Every Day ARGOSTOLI - AMMES 2.0 € Every Day Check Local Buses' Timetable ARGOSTOLI - ΑΙ HELIS 2.0 € Every Day Please contact our agencies to get informed for any routes' changes The departures' times in blue may change in case of ferry's departure's time change * The bus departs from Poros' port Routes with red color start at 15/7 & refer to Pessada port -> Only tourist routes will be operated at 15-16 August 2019 (check the corresponding announcement at www.ktelkefalonias.gr ).

Copy Link

Recommended publications

Bulletin of the Geological Society of Greece
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by National Documentation Centre - EKT journals Bulletin of the Geological Society of Greece Vol. 43, 2010 GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY Gaki - Papanastassiou K. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology Karymbalis E. Harokopio University, Department of Geography Maroukian H. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Tsanakas K. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and http://dx.doi.org/10.12681/bgsg.11193 Copyright © 2017 K. Gaki - Papanastassiou, E. Karymbalis, H. Maroukian, K. Tsanakas To cite this article: Gaki - Papanastassiou, K., Karymbalis, E., Maroukian, H., & Tsanakas, K. (2010). GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY. Bulletin of the Geological Society of Greece, 43(1), 418-427. doi:http://dx.doi.org/10.12681/bgsg.11193 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 10/01/2020 22:39:34 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY Gaki - Papanastassiou K.1, Karymbalis E.2, Maroukian H.1 and Tsanakas K.1 1 University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatologyy, 15771 Athens, Greece Emails: [email protected], [email protected], [email protected] 2 Harokopio University, Department of Geography, 70 El.
[Show full text]
Onshore Drilling Outcomes in Kefalonia Issued 16 September 2015
Onshore Drilling Outcomes in Kefalonia Issued 16 September 2015 Summary The results of the geoscientific campaign unveiled a complex geo-tectonic and geological landscape beneath the Thinia valley, the isthmus separating the western peninsula of Paliki from the rest of Kefalonia. It has superseded the simple side-wall collapse and in-fill hypothesis and has raised another possibility, that of a massive rotational slump, leading to a toe-thrust and the elevation of an ancient marine channel. The critical question then becomes one of timing: could this rotational slump have occurred recently (in the last ~3,200 years) and therefore be responsible for in-filling and displacement of a Mycenaean age marine channel? Other promising findings include the discovery of ancient beach deposits buried under land-slip infill at the northern end of the Thinia valley and evidence of an ancient marine harbour that reached the foot of Kastelli Hill and that contained radiocarbon-datable samples attributable to the Bronze Age. An anomalous late-period lakebed, now dried out, is another intriguing finding. It is also worth reiterating that Mycenaean-era sites have been previously identified on both the western peninsula (called Paliki) and the remaining part of the island of Kefalonia, confirming that this land is of considerable historical and archaeological interest dating to the period in question. The geological research sponsored by Fugro and directed by Professor John Underhill has been completed safely, successfully and with no harm to the environment. Thinia valley panorama looking east from Paliki Project Background The objective of this phase of geoscientific research has been to test the proposition that the island of Ithaca may have been accurately described in Homer’s Odyssey as the furthest west of a group of four islands off the western coast of Greece, facing dusk, the open sea and being of low elevation.
[Show full text]
Applicant UNESCO Global Geopark
Applicant UNESCO Global Geopark Kefalonia-Ithaca, Greece Geographical and geological summary 1. Physical and human geography The Kefalonia – Ithaca applicant UNESCO Global Geopark is located in Western Greece (SE Europe). It is an island complex (Kefalonia-Ithaca-Atokos-Arkoudi) belonging to the Heptanese (Ionian Sea). It is located 340,3 km from Athens, the capital of Greece and 165.37 and 258 km from Albania and Italy respectively. Its surface area reaches 3.006 km2 and includes 913,075 km2 of land and 2.092,9 km2 of marine area. The geopark ‘s area belongs administratively to the Ionian Islands Perfecture. Kefalonia (38°12′44′′ N 20°32′00′′ E) occupies an area of 773 km2. Its capital city is Argostoli. According to the last census, 35.801 inhabitants were recorded living mainly in coastal settlements. Ithaca (38°23′59.28′′ N 20°41′21.11′′E) follows in size with 117 km2 surface area. Vathi is the capital city. In winter 3.084 residents are living on the island but in the summer the population is more than double. The local residents in the geopark ‘s area are mostly occupied with agriculture, fishery and tourism. Especially tourism plays an important role in the economic development of the area. Atokos (4,4 km2) and Arkoudi (4,275 km2) are small desolated islands north of Ithaca. Kefalonia includes four main peninsulas (Paliki, Erisos, Livatho and Atro). The mean altitude of the island is 358,5m. Approximately 37.5% is occupied by mountains, 42,5% is semi-mountainous and 20% is occupied by lowland areas.
[Show full text]
Using Environmental Identity to Promote Environmental Concern and Willingness to Participate in Endangered Species Conservation
USING ENVIRONMENTAL IDENTITY TO PROMOTE ENVIRONMENTAL CONCERN AND WILLINGNESS TO PARTICIPATE IN ENDANGERED SPECIES CONSERVATION A Dissertation Presented to the Faculty of Antioch University New England Keene, New Hampshire In partial fulfillment for the degree of DOCTOR OF PHILOSOPHY by Christina M. Wesolek ORCID Scholar No. 0000-0001-6482-0145 April 2020 USING ENVIRONMENTAL IDENTITY TO PROMOTE ENVIRONMENTAL CONCERN AND WILLINGNESS TO PARTICIPATE IN ENDANGERED SPECIES CONSERVATION This dissertation, by Christina M. Wesolek, has been approved by the committee members signed below who recommend that it be accepted by the faculty of Antioch University New England in partial fulfillment of requirements for the degree of DOCTOR OF PHILOSOPHY Dissertation Committee: Beth A. Kaplin, Ph.D. Chair Jean Kayira, Ph.D. Committee Member Susan Clayton, Ph.D. Committee Member © 2020 by Christina M. Wesolek All rights reserved ABSTRACT USING ENVIRONMENTAL IDENTITY TO PROMOTE ENVIRONMENTAL CONCERN AND WILLINGNESS TO PARTICIPATE IN ENDANGERED SPECIES CONSERVATION Christina M. Wesolek Antioch University New England Keene, New Hampshire Environmental identity (EID), a concept from the social sciences specifically conservation psychology, refers to how we orient ourselves to the natural world, and thereby take action based on our personality, values, and sense of self. The realization that conservation is a human endeavor has prompted the inclusion of the social sciences in conservation research. Research on environmental identity has been conducted in such places as zoos, higher education institutions, and with farmers, and has demonstrated that EID is a good predictor of environmental concern and proenvironmental behaviors. There is a gap in the literature regarding whether environmental identity can be used as a predictor of local environmental concern and willingness to participate in endangered species conservation.
[Show full text]
4 Days of Enjoyment in Kefalonia
4 days of enjoyment in Kefalonia Plan Days 4 4 days swimming at the best beaches and afternoon walks in the picturesque settlements! By: Christina Koraki PLAN SUMMARY Day 1 1. Sami About region/Main cities & villages 2. Drogarati Cave Nature/Caves 3. Cave Lake of Melissani Nature/Lakes 4. Antisamos Nature/Beaches Day 2 1. Fiskardo About region/Main cities & villages 2. Myrtos Beach Nature/Beaches 3. Assos About region/Main cities & villages Day 3 1. Argostoli About region/Main cities & villages 2. Lantern of Agioi Theodori Culture/Monuments & sights 3. Castle of Agios Georgios Culture/Castles 4. Monastery of Agios Gerasimos Culture/Churches & Monasteries 5. Avithos Nature/Beaches Day 4 1. Monastery of Kipouraion Culture/Churches & Monasteries 2. Platia Ammos Nature/Beaches 3. Petani Nature/Beaches WonderGreece.gr - Bon Voyage 1 Day 1 1. Sami Απόσταση: Start - About region / Main cities & villages Χρόνος: - GPS: N38.2514148, W20.64716880000003 2. Drogarati Cave Απόσταση: by car 3.8km Nature / Caves Χρόνος: 09′ GPS: N38.22719751377151, W20.62778308190616 3. Cave Lake of Melissani Απόσταση: by car 6.0km Nature / Lakes Χρόνος: 08′ GPS: N38.25696956372193, W20.62362771807716 4. Antisamos Απόσταση: by car 7.5km Nature / Beaches Χρόνος: 15′ GPS: N38.260570326997204, W20.673716763220227 WonderGreece.gr - Bon Voyage 2 Day 2 1. Fiskardo Απόσταση: Start - About region / Main cities & villages Χρόνος: - GPS: N38.458166, W20.57698019999998 2. Myrtos Beach Απόσταση: by car 24.9km Nature / Beaches Χρόνος: 35′ GPS: N38.3433388495615, W20.536390590856968 3. Assos Απόσταση: by car 11.8km About region / Main cities & villages Χρόνος: 19′ GPS: N38.37865201199259, W20.54058172390137 WonderGreece.gr - Bon Voyage 3 Day 3 1.
[Show full text]
Although Kefalonia Is One of the Largest Ionian Islands, It Is Also One of the Least Populated
WASTE COLLECTION IN EUROPE Yiassou! Collecting waste in Kefalonia Although Kefalonia is one of the largest Ionian Islands, it is also one of the least populated. Tim Byrne explains how the island has a different waste collection system to the rest of its neighbours, looks at its choice of refuse collection vehicles and asks whether the island meets EU legislation on working hours. EFALONIA HAS seven coast of Argostoli and collect the MSW from the dedicated refuse collection holiday resort of Lassi. One is also operational rounds or ‘programmes’ in the Poros, Skala area, one in Sami and Aghi as the Greeks class them. Efthiamia and one in Lixouri. There are no separate There is also an older Mercedes 2024 two municipalities on Kefalonia which collect their axle Faun Variopress unit working on its own Kmunicipal solid waste (MSW) separately like designated collection route around Mineas and their neighbouring islands e.g. Zakynthos, the area close to the Airport. Corfu. Instead a company was set up called the In the summer season, there are an Kefalonia Intermunicipal Enterprise for Waste additional four spare RCVs. These help the Management and Environmental Protection. larger rounds in the summer tourist season. This company is responsible for the entire These vehicles consist of a Steyr 91 two-axle collection and disposal of MSW on Kefalonia complete with Kaoussis Rotopress equipment. and also incorporates the subsequent collection The Steyr 91 two axle Kaoussis Rotopress and disposal of MSW for the neighbouring works near Fiskardo in the summer and three Island of Ithaca. Mercedes Sks two-axle complete with Kuka Rotopress equipment work in Lixouri, Mineas, Vehicle types Poros and Aghi Efthiamia in the summer.
[Show full text]
Ionian Sea, Western Greece) Earthquake Sequence: Damage Pattern on Buildings
16th World Conference on Earthquake, 16WCEE 2017 Santiago Chile, January 9th to 13th 2017 Paper N° 414 THE JANUARY-FEBRUARY 2014 CEPHALONIA (IONIAN SEA, WESTERN GREECE) EARTHQUAKE SEQUENCE: DAMAGE PATTERN ON BUILDINGS S. Mavroulis(1), V. Alexoudi(2), A. Grambas(3), E. Lekkas(4), P. Carydis(5) (1) MSc Geologist, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (2) MSc Engineer, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (3) MSc Geologist, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (4) Professor of Dynamic Tectonic Appleid Geology and Disaster Management, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (5) Professor Emeritus, National Technical University of Athens,Greece, [email protected] Abstract The early 2014 Cephalonia earthquake sequence comprised two main shocks with almost the same magnitude (Mw 6.0) occurred successively in short time (January 26, February 3) and space (western Cephalonia, Paliki peninsula). The first event caused damage mainly in the Paliki peninsula, while the second aggravated damage induced by the first. The dominant buildings types are masonry, reinforced concrete (RC) and monumental buildings. Masonry buildings suffered the most due to their high vulnerability. RC buildings showed good performance due to their good construction quality.
[Show full text]
REVISED Full Paper Cephalonia
6th International Conference on Earthquake Geotechnical Engineering 1-4 November 2015 Christchurch , New Zealand 3-Dimensional Rocking and Sliding Case Histories in the 2014 Cephalonia, Greece Earthquakes E. Garini 1, G. Gazetas 2, I. Anastasopoulos 3 ABSTRACT th A twin event earthquake sequence of an M w6.1 on January 26 and an M w6.0 eight days later on February 3 rd shook the island of Cephalonia, triggering damage in structural and harbor infrastructure. The strongest three recordings of the double event are analyzed in this paper: the Chavriata, Lixouri and Argostoli accelerograms. The Lixouri record bears the effects of near-fault directivity, containing acceleration pulses in its normal to the fault (EW) component. The most extensive damage occurred in the numerous cemeteries of the region, with tombstone topplings and large slippages being the most conspicuous. Some specific “rigid block” failure case histories, from the cemeteries of Lixouri and Chavriata, are explored in the paper. The systems are modeled in 3D, as rigid blocks resting through Coulomb friction on horizontal base. The latter is excited by three component accelerations: two in the horizontal directions and one in the vertical. The rocking, sliding, twisting and overturning of such rigid systems offer a strong indication of the ‘destructiveness potential’ of ground motions, which explain the cemeteries extensive damage. Unilateral and bilateral excitations are studied and the role of vertical acceleration is elucidated. Introduction: Cephalonia's Earthquake History and the 2014 Earthquake Doublet The Greek island of Cephalonia is located in the Ionian Sea, in a high seismicity region of complex tectonics, where the thrust belt along the Ionian and Adriatic sea is connected with the convex part of the Hellenic arc (Papazachos, 1990).
[Show full text]
The Historical Review/La Revue Historique
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by National Documentation Centre - EKT journals The Historical Review/La Revue Historique Vol. 11, 2014 Index Hatzopoulos Marios https://doi.org/10.12681/hr.339 Copyright © 2014 To cite this article: Hatzopoulos, M. (2014). Index. The Historical Review/La Revue Historique, 11, I-XCII. doi:https://doi.org/10.12681/hr.339 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 21/02/2020 08:44:40 | INDEX, VOLUMES I-X Compiled by / Compilé par Marios Hatzopoulos http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 21/02/2020 08:44:40 | http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 21/02/2020 08:44:40 | INDEX Aachen (Congress of) X/161 Académie des Inscriptions et Belles- Abadan IX/215-216 Lettres, Paris II/67, 71, 109; III/178; Abbott (family) VI/130, 132, 138-139, V/79; VI/54, 65, 71, 107; IX/174-176 141, 143, 146-147, 149 Académie des Sciences, Inscriptions et Abbott, Annetta VI/130, 142, 144-145, Belles-Lettres de Toulouse VI/54 147-150 Academy of France I/224; V/69, 79 Abbott, Bartolomew Edward VI/129- Acciajuoli (family) IX/29 132, 136-138, 140-157 Acciajuoli, Lapa IX/29 Abbott, Canella-Maria VI/130, 145, 147- Acciarello VII/271 150 Achaia I/266; X/306 Abbott, Caroline Sarah VI/149-150 Achilles I/64 Abbott, George Frederic (the elder) VI/130 Acropolis II/70; III/69; VIII/87 Abbott, George Frederic (the younger) Acton, John VII/110 VI/130, 136, 138-139, 141-150, 155 Adam (biblical person) IX/26 Abbott, George VI/130 Adams,
[Show full text]
Seismic Performance of Bell Towers in Kefalonia, Greece During the 2014 Earthquake Sequence
Available online at www.eccomasproceedia.org Eccomas Proceedia COMPDYN (2017) 78-100 COMPDYN 2017 6th ECCOMAS Thematic Conference on Computational Methods in Structural Dynamics and Earthquake Engineering M. Papadrakakis, M. Fragiadakis (eds.) Rhodes Island, Greece, 15–17 June 2017 SEISMIC PERFORMANCE OF BELL TOWERS IN KEFALONIA, GREECE DURING THE 2014 EARTHQUAKE SEQUENCE G.C. Manos1 and E. Kozikopoulos2 1 Professor Emeritus and ex-Director of the Lab. of Strength of Materials and Structures, Aristotle Uni- versity, e-mail: [email protected] 2 Postgraduate student, Lab. of Strength of Materials and Structures, Aristotle University e-mail: {[email protected]} Keywords: Bell towers, In-situ Dynamic Measurements, Numerical Simulation, Earthquake Response, Soil-structure Interaction. Abstract. Bell towers are structures that are of particular interest regarding their dynamic and earthquake response, which has been the subject of research in the past. A large number of bell towers with dimensions much larger than the ones examined here are located in nu- merous cities in Italy and around the world. This paper deals with in-situ measurements as means of system identification of two bell-towers located in the island of Kefalonia, Greece which was subjected during the winter of 2014 in an intensive earthquake sequence. The height of both these bell towers is approximately 21.5m; they are made of reinforced concrete with a hollow cross-section. Their dynamic characteristics of these bell towers were meas- ured in-situ through a series of free vibration tests that were performed following the earth- quake sequence. Subsequently their dynamic response was numerically simulated employing a 3-D elastic numerical simulation shell elements.
[Show full text]
War Loss of an Italian Seaplane ‐ Argostoli, Kefalonia ‐ 5 June 1941
War loss of an Italian seaplane ‐ Argostoli, Kefalonia ‐ 5 June 1941 The WWII loss of an Italian seaplane, presumably Cant Z.506B "Airone" In the harbour of Argostoli, Kefalonia Island, on 5 June 1941 A deadly reconnaissance patrol During a reconnaissance patrol in the Ionian Sea on 5 June 1941, a british "Maryland" reconnaissance aircraft (probably of Νο.69 Squadron RAF stationed at Luqa, Malta, operating in the area at the time), sighted attacked and destroyed an Italian seaplane, which was taxiing on the water in Argostoli harbour, Kefalonia. The event is recorded in the “War Cabinet ‐ Weekly Resume May 29th to June 5th 1941” under the section “Αir Situation, Malta.” (paragraph 53): …“Our reconnaissance aircraft have constantly patrolled the coasts of Tunis and Tripoli and the Ionian Sea. During one of these flights a Maryland destroyed an Italian seaplane on the water at Argostoli (Cephalonia).”… Tilemachos Beriatos, 2010‐2014 p. 1/5 War loss of an Italian seaplane ‐ Argostoli, Kefalonia ‐ 5 June 1941 This is also reported in the newspaper “The Courier‐Mail newspaper June 6th, 1941” (National Library of Australia), in the article titled: “ITALIANS’ CONVOY BATTERED”: …“LONDON, June 5. …On a reconnaissance flight off the island of Cephalonia, a British aircraft attacked an Italian seaplane, which was taxiing on the water, and destroyed it.”… The Italian seaplane was probably a Cant Z.506B "Airone" belonging to one of the maritime reconnaissance squadrons (“Squadriglia da Ricognizione Marittima”) of the Italian Royal Air Force (“Regia Aeronautica”) that took part in the assault on the Ionian Islands in April 1941 and operated from bases on the islands during the first period of the Italian‐German occupation.
[Show full text]
Sea Turtles in Kefalonia
sea turtles in kefalonia Kefalonia is home to two of the seven sea turtle species that exist in the world. Loggerhead sea turtles, also known as Caretta caretta, nest and forage on the island's south coast, while Green sea turtles (Chelonia mydas) are rarely seen and only forage on the island's sea grass meadows. Both species migrate across the Mediterranean Sea to find food or warmer waters to spend the winter. After the initial “lost years” of their lives, they become reproductively mature when they reach around 17 to 25 years of age. The loggerheads return to Kefalonia, where they once hatched as baby turtles, every two to three years to reproduce. s They begin mating from late March until early June, while they are still offshore or as soon as they approach the nesting beaches. A female turtle will mate with several different males, and as a result her nests can contain eggs fertilized by up to five different fathers. s[ The nesting season begins in early June and continues until mid-August. One female turtle can lay up to five nests within one season, and each nest has around 90 eggs. To lay their nests, female turtles emerge on the nesting beach during the night. They crawl to the back of the beach looking for soft sand with just the right moisture to lay their eggs. They dig a 50 cm deep eggchamber using only their back flippers and begin laying their eggs. The eggs have the size and shape of a ping-pong ball. The shell is soft, so the eggs don't break as they fall into the eggchamber.
[Show full text]