Prodromos PSARROPOULOS Structural & Geotechnical Engineer, Beng, Meng, Msc, Phd
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FREQUENTLY ASKED Questionsi
FREQUENTLY ASKED QUESTIONSi Where is the prefecture of Grevena geographically? ......................................................................................... 2 How can I get to Grevena? .................................................................................................................................. 2 What reasons make Grevena one of the most popular tourist destinations in Greece? ................................... 3 Why is Grevena called "The land of the mushrooms"? ....................................................................................... 3 Which routes can I do in Grevena? ..................................................................................................................... 4 What museums are there? .................................................................................................................................. 6 How many stone bridges exist in the region? ..................................................................................................... 7 Where is the Vasilitsa Ski Center and what does it offer? .................................................................................. 8 What can lovers of religious tourism see in the area? ........................................................................................ 8 How can I go, what can I see in Valia Calda Nature Reserve and National Park of Northern Pindos? ............... 9 Alternative Activities – What sports can I do? ................................................................................................. -
Motorcycle Tour Greece, Trikala and Meteora, Reaching for the Sky , Self
Motorcycle tour Greece, Trikala and Meteora, reaching for the Sky , self guided on a BMW Motorcycle tour Greece, Trikala and Meteora, reaching for the Sky , self guided on a BMW durada dificultat Vehicle de suport 3 días fàcil No Language guia en No Three day guided motorcycle tour that will lead you to the heart of Thessaly and the iconic site of Meteora. We will meet and greet you in our head offices were you will get acquainted with your BMW rental motorbike. We will do a short briefing on the tour, the itinerary and then we will take off for our moto tour. Trikala is one of the most beautiful cities in Greece with excellent urban planning, lovely stone paved roads, monuments of historical importance, big squares excellent for socializing and magnificent local cuisine. It is built where ancient Trikki used to be (mythology states that the nymph Trikki was the daughter of Peneus, the Thessalian river God). The Lithaios River runs through the prefectures capital thus offering another element of relaxation and beauty. Here in also the homeland of the iconic doctor of antiquity, Asclepius. We will park our motorcycles and explore the center on foot. We will visit the famous clock tower, the Koursoum Mosque, one of the best preserved mosques on Greek soil and finally, the “Kliafa” Centre of History and Culture where dazzling display of exhibits always capture the attention of the traveler. A few miles away lies the town of Kalabaka, best known for the location of Meteora (UNESCO World Heritage site since 1988). -
HOTELS | PROGRAMS | ISLAND HOPPING | TOURS | CRUISES | CAR RENTAL | YACHT CHARTER | TURKEY EXTENSIONS Meteora
GREECE 2020 HOTELS | PROGRAMS | ISLAND HOPPING | TOURS | CRUISES | CAR RENTAL | YACHT CHARTER | TURKEY EXTENSIONS Meteora 2 GREECE 2020 • GREECE AND MEDITERRANEAN TRAVEL CENTRE Welcome to Greece As my second home and where Greece and Mediterranean Travel Centre began, Greece holds a special place in my heart. Its hidden gems are still exciting for me to share and I love being able to offer the Halina Kubica traditional Greece, known only to locals, Owner & Managing Director as well as the popular ancient treasures Greece is renowned for. It always surprises travellers when they discover there are 227 idyllic inhabited islands, stunning ruins, and mountainous mainland to explore of unique beauty and rare customs. Sampling freshly cooked local food at the small taverna with the stunning backdrop of the Aegean Sea is the highlight of each of my trips and I hope will be yours too. Let us show you Greece like you’ve never imagined, so you can experience a little piece of our home. GREECE 2020 • GREECE AND MEDITERRANEAN TRAVEL CENTRE 3 Let us take you on the Trip of a Lifetime Greece and Mediterranean Travel Centre is your local boutique Australian owned and operated company. We have been designing holidays with the Australian traveller in mind for over 17 years. With personal, hands-on service, you can rest assured that your holiday will be impeccable from start to finish. Travel with us and experience the difference... Athens Zakynthos 4 GREECE 2020 • GREECE AND MEDITERRANEAN TRAVEL CENTRE Santorini Expert Knowledge Trusted Security We are destination experts of Greece and the Mediterranean. -
03 Pomonis 75
Ofioliti, 2005, 30 (2), 75-84 75 GEOLOGICAL EVOLUTION OF THE KOZIAKAS OPHIOLITIC COMPLEX (WESTERN THESSALY, GREECE) Panagiotis Pomonis*, Basilios Tsikouras and Konstantin Hatzipanagiotou University of Patras, Department of Geology, Section of Earth Materials, Patras, GR-265 00, Greece. * Corresponding author, e-mail: [email protected]. Keywords: ophiolite, mélange, peridotite, serpentinite. Koziakas, Thessaly. ABSTRACT The Koziakas ophiolitic complex is located in Western Thessaly and is interpreted as a dismembered ophiolite sequence, which overthrust the Western Thessaly Unit (WTU). The Koziakas basal Unit consists of sedimentary rocks and occupies the stratigraphically lowermost members of the WTU. The Ophi- olitic Unit overthrust the WTU and consists, from bottom to top, of a well-developed ophiolitic mélange, a sub-ophiolitic metamorphic sole, serpentinites, ser- pentinized peridotites, peridotites (harzburgite, lherzolite, plagioclase lherzolite), massive dolerites, massive basalts and pillow lavas interlayered with Mn- rich radiolarites. The ophiolitic mélange comprises a chaotic multicoloured complex of various rock fragments. A sparse network of gabbroic (locally rodingi- tized), plagiogranitic and doleritic dykes intrudes the mantle tectonites along two main cross-cutting directions: the first strikes NE-SW and dips 50o-70o to the NW, the second strikes N-S to NNW-SSE with a dip of about 65o-80o to the west. The dominant tectonic fabrics such as shear zones, fold axes, foliation planes and mineral streching lineations, imprinted mainly on the Koziakas mantle tectonites trend NW to NE and are consistent with a NE-SW emplacement direction. The similar radiometric ages and the comparable geological characteristics of the Koziakas ophiolitic complex with its adjacent ophiolite suites of Pindos, Vourinos and Othris imply that they probably developed in the same marginal basin represented by the Pindos ocean basin. -
Pinios (Peneus) River (Central Greece): Hydrological - Geomorphological Elements and Changes During the Quaternary
Cent. Eur. J. Geosci. • 3(2) • 2011 • 215-228 DOI: 10.2478/s13533-011-0019-1 Central European Journal of Geosciences PINIOS (PENEUS) RIVER (CENTRAL GREECE): HYDROLOGICAL - GEOMORPHOLOGICAL ELEMENTS AND CHANGES DURING THE QUATERNARY Research article George Migiros 1 ∗, George D. Bathrellos2† , Hariklia D. Skilodimou 2‡ , Theodoros Karamousalis 1 1 Laboratory of Mineralogy – Geology, Department of Science, Agricultural University of Athens, Greece, 2 Department of Geography & Climatology, Faculty of Geology & Geoenvironment, National & Kapodistrian University of Athens, University Campus, Zografou, 15784 Athens, Greece, Received 18 March 2011; accepted 5 June 2011 Abstract: The Pinios River is the third longest river of Greece. It drains the entire drainage basin of Thessaly (eastern part of Central Greece), part of which is the largest plain of the country. In this research the hydrological, geomorpho- logical and geological characteristics of the riverine area of Pinios were studied. Classification and grouping of these characteristics were then carried out, which led to the segmentation of the Pinios River into seven sections, each one with its own set of thematic data. These sets assign separate functions and evolutions of the river system during the Quaternary. Specifically, the basin of the present Pinios River, before its evolution into a river basin, comprised three separate and independent systems. The present Pinios River emerged as a river system from the merging of the lacustrine paleoenvironments along with the major tributaries that drained large parts of the present hydrological basin and as soon as the karstic openings of the central hill valley and the Tempi valley took place during the Quaternary. The followed methodology for the segmentation of the river can be used for the study of heterogeneous river systems. -
Greece - Trikala
GREECE - TRIKALA Meat processing plant in Filyra (municipality of Koziakas) The case study described here can be characterised as a typical example of an activity which can potentially affect in a positive way the existence of higher linkages between primary agricultural production and the wider rural economy in the study area of Trikala (Greece). More specifically, the utilization of this particular investment project can potentially result into the more effective use of agricultural resources, the increase of local value-added, the diversification of the local economic-base and the generation of rural jobs. 1. Project details: Nature of the project Purpose : The establishment of a modern processing and packaging plant for sausages made of local pork meat as the area is the centre of Trikala’s pork production. Content : Factory buildings of 205m 2 and electrical and mechanical equipment for processing and packaging sausages. Installation of a HACCP quality control system. Inspiration : The owner had a long working experience in the sales department of a soft drinks company and acquired a fairly good knowledge of the techniques promoting food and drinks all over Greece. Due to parental background, the owner had a good knowledge of the hog farming sector at Trikala and of the local production techniques for sausages. Policy coherence : The project is in accordance with the major strategic aims of regional (Region of Thessaly) and local (Trikala) rural development policy. Especially with the aim concerning the utilization of local agricultural production, and the aim to increase links between primary production and processing. Finally, these strategic aims are also compatible with the Leader+ programme of the local Local Action Group (KENAKAP). -
FOR INDEPENDENT TRAVELLERS Hotels Programs Island Hopping Tours Cruises Car Rental Yacht Charter Turkey Extensions
GREECEFOR INDEPENDENT TRAVELLERS Hotels Programs Island Hopping Tours Cruises Car Rental Yacht Charter Turkey Extensions 2019 www.greecemedtravel.com.au Welcome to Greece From cosmopolitan nightlife to blue water lapping at serene beaches, Greece is a dreamy destination with something for everyone. Whether you are interested in seeing famous UNESCO World Heritage listed sites like the Acropolis, the monasteries in Meteora, and Ancient Delphi or you want to hop across the unspoilt islands scattered like jewels across the Aegean Sea, it’s all up to you. As one of the most visited destinations on the planet, you can experience the classical Greece you’ve always imagined to the hidden Greece known only to locals. Greece is comprised of a mountainous mainland and 227 idyllic inhabited islands. With its friendly locals, stunning ruins, delicious cuisine, and natural beauty, Greece offers a huge variety of options, a temperate year round climate, and world-class culture. 2 GREECE 2019 • GREECE AND MEDITERRANEAN TRAVEL CENTRE Soak in the unhurried day-to-day life of a small Grecian village. Drink handcrafted cocktails on a sophisticated island resort. Explore the art and history of Athens on exclusive tours. Watch the sunset paint the buildings in Santorini with splashes of colour. Snorkel or dive in crystal clear waters off the coast of Crete. Let us show you Greece like you’ve never imagined. Halina Kubica Owner & Managing Director GREECE 2019 • GREECE AND MEDITERRANEAN TRAVEL CENTRE 3 Let Us Take You on the Trip of a Lifetime Greece and Mediterranean Travel Centre is your local boutique Australian owned and operated company. -
Geomorphological Study of Kleinovitikos Stream Drainage Network (Trikala Prefecture - Western Thessaly)
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. ΧΧΧΧ, Bulletin of the Geological Society of Greece vol. XXXX, 2007 2007 Proceedings of the 11th International Congress, Athens, Πρακτικά 11ου Διεθνούς Συνεδρίου, Αθήνα, Μάιος 2007 May, 2007 GEOMORPHOLOGICAL STUDY OF KLEINOVITIKOS STREAM DRAINAGE NETWORK (TRIKALA PREFECTURE - WESTERN THESSALY) Bathrellos G. D.1, Skilodimou H. D.1, Livaditis G. , and Verikiou- Papaspiridakou E.1 1 National andKapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography - Climatology, [email protected], [email protected] Abstract The Kleinovitikos stream is a tributary ofPineios River in the Western Thessaly. Its basin drainages parts of mountain range of Southern Pindos as well as the mountain of Koziaka. In this study a quantitative analysis of drainage network was accom plished and the relation of tectonics features with the watershed and the channels of drainage network were investigated. The main channel of the drainage network is of 6th order, while the dominated type of the network is the trellis drainage pattern. The morphological slopes of the basin show various fluctuations. The gentle slopes express erosional landforms while the steep ones represent geological and tectonic structures. It was noted by the quantitative analysis of the drainage network that the geological and tectonic structure of the area affects in its evolution. Moreover, the outcrop of heterogeneous lithological formations in the basin affects the values of drainage density and frequency. The lithology and the secondary cracks involve in the prevailing direction of the watershed. The streams of 1st -3r order are controlled by the younger cracks; the younger cracks as well as the older Alpine cracks have an influence on the streams of 4' and 5' order, and the Alpine tectonic activity affects the stream of 6' order. -
Geomorphological Study of Kleinovitikos Stream Drainage Network (Trikala Prefecture Western Thessaly)
6E.>.Tlo T~~ EM~VIK~~ reW,>,aYIK~~ ETalpia~ TO~. XXXX. Bulletin of the Geological Society of Greece vol. XXXX. 2007 2007 Proceedings ofthe 11 It> International Congress, Athens, npaKTIKO 11°U 6leevou~ Luve<5piou, Ae~va, Mcilo~ 2007 May, 2007 GEOMORPHOLOGICAL STUDY OF KLEINOVITIKOS STREAM DRAINAGE NETWORK (TRIKALA PREFECTURE WESTERN THESSALY) Bathrellos G. D.1, Skilodimou H. D.t, Livaditis G. I, and Verikiou Papaspiridakou E.! 1 National and Kapodistrian University ofAthens, Faculty o.fGeology and Geoenvironment, Department o.fGeography - Climatology, [email protected], [email protected] Abstract The Kleinovitikos stream is a tributary ofPineios River in the Western Thessa~y. Its basin drainages parts ofmountain range o.fSouthern Pindos as well as the mountain of Kozlaka. In this study a quantitative analysis o.f drainage network was accom plished and the relation oftectonicsfeatures with the watershed and the channels o.f drainage network were investigated The main channel o.fthe drainage network is o.f (jlt order, while the dominated type ofthe network is the trellis drainage pattern. The morphological slopes ofthe basin show various fluctuations. The gentle slopes express erosional landforms while the steep ones represent geological and tectonic structures. It was noted by the quantitative analysis o.fthe drainage network that the geological and tectonic structure of the area affects in its evolution. Moreover, the outcrop of heterogeneous lithological formations in the basin affects the values of drainage density andfrequency. The lithology and the secondmy cracks involve in the prevailing direction of the watershed The streams o.f 1"'1 _3,d order are controlled ~y the younger cracks; the younger cracks as well as the older Alpine cracks have an influence on the streams of4'1t and Silt order, and the Alpine tectonic activity affects the stream of6'1t order. -
Landslides, a Recurrent Phenomenon
Landslides, a recurrent phenomenon by George D. BATHRELLOS & Hariklia D. SKILODIMOU What is a Landslide? Landslide is a general term used to describe the down-slope movement of soil, rock, and organic materials under the effects of gravity and also the landform that results from such a movement (Highland & Bobrowsky, 2008). Gravity affects all objects on Earth. From the largest mountains to the smallest grains of sand, gravity pulls everything in a direction toward the center of the planet (Nagel, 2004). Mass movements are the result of shear stresses on slopes (caused by gravity, the weight of material and soil water) overcoming the inherent resistance of the materials (made up of the cohesive properties of slope particles and their internal friction) (Hart, 1986). In general, the scientists use many terms worldwide for this phenomenon, such as "landslide", "landslide events", "mass movements", "gravity movements" and "slope movements" (Terzaghi, 1950; Coates, 1977; Varnes, 1978). What does Landslides cause? Gravity The main force which is responsible for mass movement is the gravity. Gravity is the force that acts everywhere on the Earth's surface, pulling everything toward the center of the Earth. On a flat surface the force of gravity acts downward. So long as the material remains on the flat surface (Fig. 1) it will not move under the force of gravity (Nelson, 2013). Fig. 1: Influence of gravity on an object to a horizontal surface (modified from Nelson, 2013). On a slope, the force of gravity can be decomposed into two components (Fig. 2): a component acting parallel to the slope and a component acting tangential to the slope (Nelson, 2013). -
Project LIFE09 NAT/ES/000533 “INNOVATION AGAINST POISON”
Project LIFE09 NAT/ES/000533 “INNOVATION AGAINST POISON” “Innovative actions against illegal poisoning in EU Mediterranean pilot areas” Actions in GR 1 pilot area: Antihasia – Meteora - Koziakas Implemented by ARCTUROS Lazaros Georgiadis Biologist, Director of Programmes Cordoba 15-17 November 2012 Poison, Wildlife and Society International Scientific and Technical Congress ARCTUROS is an Environmental NGO founded in 1992 in Thessaloniki with the aim of the “Protection and Management of the Natural Environment and Wildlife” and specialization on Conservation of large carnivores and their habitats using Brown Bear (Ursus arctos) as flag species • Basic first action was the solution of the Dancing Bear Problem in Greece • And the hospitality of confiscated captive bears and wolves in special facilities of the ARCTUROS Environmental Centre Bear sanctuary Veterinary Station Wolf sanctuary Hellenic Livestock Guarding Dog Breeding Centre Public awareness Environmental Education Volunteerism Bear Information Center Wildlife Emergency Team Scientific studies and conservation activities on national and international level for the wildlife Bear distribution in Greece LIFE09 NAT/ES/000533 “Innovation Against Poison” Duration: 1/10/2010 – 30/09/2015 (5 years) ARCTUROS budget: 593.883 € ARCTUROS Contribution: 317.149 € (51,76%) Ε.C. Contribution : 284.548 € (48,24%) LIFE09 NAT/ES/000533 “Innovation Against Poison” GR1 Pilot Area: Antichasia – Meteora - Koziakas The best habitat for monks, ….……………birds of prey…and…. LIFE09 NAT/ES/000533 “Innovation -
A Small Valley in Greece and Its Bridges Throughout the Centuries
Transactions on the Built Environment vol 66, © 2003 WIT Press, www.witpress.com, ISSN 1743-3509 A small valley in Greece and its bridges throughout the centuries M. ~araveziro~lou',E. ~arayianni*,E. ~tavrakakis' & A. vaggelakosl I Department of Civil Engineering, Aristotle University, Greece. 2 Technical Services, Prefecture of Trikala, Greece. Abstract This paper refers to the bridges of the Pyli valley. The most important bridge is the stone one of St. Bessario. The single-arched bridge of St. Bessario, with an arch span of 28.73m and total length of 68m, was built in the 16' century and until 1936 it was the only link between the Thessaly fields and the mountainous villages of Pindos. In the 2ofh century (up to 1997), at a distance of approximately 1500m around the stone bridge, four concrete bridges which differ in size, architectural style, structural technique and use (vehicular or pedestrian crossing) have been constructed over the Portaikos river in order to serve increased modem transportation needs in the region; the oldest of them, finished in 1936 lies at the west of the stone bridge at a distance of 1000m and has a length of 45m, while the following structures at the east of the ancient bridge, where the Portaikos river is broader, reach a length up to 170m; among these reinforced or prestressed concrete bridges, a suspension one, with a length of 120~was constructed in 1981 very close to the Byzantine church of Porta Panagia (13& century) and it is used only for pedestrian crossing. A brief description of the bridges, their present state, the necessary works for their repair, historical data as well as photographic documentation are included in the paper.