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 | 39th EGN Coordination 
			Committee Meeting 
 Burren and Cliffs 
			of Moher 
			(Ireland), 23rd - 25th March 2017
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		Thursday 23.03.2017
 The 39th European Geoparks Network Meeting is hosted by the Burren and 
		Cliffs of Moher UNESCO Global Geopark at the Falls Hotel in Ennistymon 
		(County Clare).
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		Thursday 23.03.2017
 The representatives of the European UNESCO Global Geoparks are ready for 
		the 39th European Geoparks Network Coordination Committee In the third 
		row from the bottom most of the Italian delegates, from the left to the 
		right: Luigi Bloise and Egidio Calabrese (Pollino UGG), Alessia Amorfini 
		and Giuseppe Ottria (Apuan Alps UGG), Violet Masè (Adamello Brenta UGG), 
		Marco Firpo and Maurizio Burlando (Beigua UGG) and Aniello Aloia (Cilento 
		and Vallo di Diano UGG).
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		Thursday 23.03.2017
 The chairman's table (from the left): Patrick Mc Keever (UNESCO Head of 
		the Earth Sciences and Risk reduction), Nikolas Zouros (EGN and GGN 
		Coordinator), Kristin Rangnes (EGN Vice Coordinator) and Carol Gleeson (Burren 
		and Cliffs of Moher UGG Manager).
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		Thursday 23.03.2017
 Here is the most awaited moment for the Italian representatives and 
		particularly for the Apuan Alps Geopark. Alessia Amorfini from the Apuan 
		Alps UNESCO Global Geopark is submitting to the Coordination Committee 
		her application as new member of the EGN Advisory Committee. Her program 
		has been fully convincing and her candidacy has obtained the unanimous 
		vote.
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		Thursday 23.03.2017
 Along with Alessia, Artur Sa and Sophie Justice have also joined the 
		Advisory Committee as voted members. For Artur from the Arouca Geopark 
		(Portugal) this is a confirmation that attests the good work done in the 
		past years.
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		Thursday 23.03.2017
 Sophie Justice from the Chablais UNESCO Global Geopark (France) while 
		presenting her possible contribution into the activities of the EGN 
		Advisory Committee.
 
		
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		Thursday 23.03.2017
 In the afternoon meeting of the Geohazard Working Group. This is a new 
		working group born from the need to address one of the most important 
		issues within the UNESCO. It is no coincidence that the attending 
		delegates are from geoparks from tectonically active areas such as 
		Iceland (Katla Geopark), Greece (Lesvos and Psiloritis geoparks) and 
		Italy (Apuan Alps, Beigua and Pollino geoparks
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		Thursday 23.03.2017
 Again in the afternoon, the agenda includes time for separate meetings 
		of the EGN National Committees. The Italian delegates are sharing and 
		coordinating the activities at the national level mostly for the next 
		main appointment: the 8th International Conference on UNESCO 
		Global Geoparks to be held in the Adamello Brenta UGG in September 2018.
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		Friday 24.03.2017
 Today is a sunny day. The landscape from the accommodation hosting the 
		EGN Meeting includes the falls that give the name to the Falls Hotel. 
		Actually, they are not naturals falls; they were formed by deviating the 
		river across an abandoned quarry. In the background, on the hill top, 
		the old Church
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		Friday 24.03.2017
 The work of the meeting starts with an open session regarding 
		sustainable tourism. Short presentations show examples of sustainable 
		tourism in Irish and European Geoparks. Here, Aniello Aloia, Coordinator 
		of the Italian National Geopark Committee, is speaking about the 
		European Charter of Sustainable Tourism.
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		Friday 24.03.2017
 The open session continues in the foyer of the Falls Hotel where the 
		public can mingle and meet the attending Geoparks that display (pull up 
		and leaflets) their work in sustainable tourism. In the photo the 
		representatives from the Azores UGG in front of their pull up 
		advertising the next 14th European Geoparks Conference 
		(September 2017) that will be hosted in their Geopark.
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		Friday 24.03.2017
 Hereinafter, the hall gets crowded. In the foreground Violet Masè and 
		Joseph Masè from the Adamello Brenta UGG.
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		Friday 24.03.2017
 You know these smiling personalities! Nickolas Zouros (EGN and GGN 
		Coordinator) asked Alessia Amorfini (Apuan Alps UGG) to have a picture 
		together as new member of the EGN Advisory Committee.
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		Friday 24.03.2017
 In the afternoon, Joseph Masè, president of Adamello Brenta UNESCO 
		Global Geopark, presents the organization of the 8th 
		International Conference on UNESCO Global Geoparks that will be hosted 
		by his geopark in September 2018.
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		Saturday 25.03.2017
 Today is the field trip day. At the start, Eamon Doyle, Geopark 
		Geologist of the Burren and Cliffs of Moher UGG, explains the geology we 
		will observe by showing us the map “Geology of Ireland” by the 
		Geological Survey of Ireland.
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		Saturday 25.03.2017
 We arrive at the Cliffs of Moher Visitor Experience, the most visited 
		natural attraction in Ireland. It shows a low visual impact being built 
		inside the hills. The weather is extraordinarily nice.
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		Saturday 25.03.2017
 Divided into groups of few people, the guided tour of the Cliffs of 
		Moher begins. The guide explains the geological features of the Cliffs 
		and illustrates the rules of behavior and security.
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		Saturday 25.03.2017
 The explanations by the guide are summarized in this and other panels 
		along the path to the Cliffs of Moher. Note that the panels are written 
		in English and Gaelic languages.
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		Saturday 25.03.2017
 The Cliffs of Moher stand more than 200 meters above the sea level of 
		the Atlantic Ocean. The rocks that form the cliffs are layers of 
		sandstones, siltstones and mudstones that on the whole represent 
		sediments belonging to a river delta formed about 320 million years ago 
		during the Carboniferous period. The Cliffs of Moher formed as a result 
		of coastal erosion by the Atlantic’s waves and wind.
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		Saturday 25.03.2017
 The good weather and the lack of wind allow a short cruise from the 
		marina of Doolin village. At the start, the sub-horizontal 
		stratification of limestones is clearly visible, testifying to the 
		almost total absence of deformation. The limestones are the oldest rocks 
		outcropping in the Burren region. They formed in a warm, shallow, 
		tropical sea during the Carboniferous period, about 345 million years 
		ago.
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		Saturday 25.03.2017
 From the boat the Cliffs of Moher are against the light. It is not 
		possible to distinguish the geological details but they give very 
		suggestive pictures anyway!
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		Saturday 25.03.2017
 At the Lisdoonvarna Pavilion, meeting with representatives of Community 
		and Schools. Students from the Lisdoonvarna secondary school present 
		their project about the local river. All the European UNESCO Global 
		Geoparks delegates have recognized the high quality of this 
		multidisciplinary project, the result of collaboration between School, 
		Galway University and Burren and Cliffs of Moher UGG, which has dealt 
		with knowledge and protection of this community’s heritage.
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		Saturday 25.03.2017
 Lisdoonvarna’s primary schools have done a research on the European 
		UNESCO Global Geoparks. Pupils have then chosen a geopark for each 
		country for a more detailed study. For Italy, the Pollino UGG was 
		chosen. The smiling Egidio Calabrese (left) and Luigi Bloise (right) are 
		proud in front of the poster of their geopark.
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		Saturday 25.03.2017
 Outside the Lisdoonvarna Pavilion, a striated boulder is an example of a 
		glacial erratic, a reminder of how the Burren region was formed by 
		melting glaciers at the end of the Ice Age 12,000 years ago. Erratics 
		are rocks that have been transported from their original location by 
		moving glaciers that eroded soil and bedrock.
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		Saturday 25.03.2017
 Scenic drive along the portion of the Wild Atlantic Way voted one of the 
		top 10 scenic drives in Europe. We can appreciate the peculiarity of the 
		Burren region: the karst landscape. The word Burren comes from the Irish 
		word “boireann” which means “a stony place”. It is one of the largest 
		karst region in the world. Here the limestone pavement “dives” into the 
		sea by the side of a small lighthouse.
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		Saturday 25.03.2017
 A short stop to look closely the limestone pavement along the Atlantic 
		coast. A limestone pavement is a bare limestone surface from which the 
		soil has been removed by glaciers and then the exposed rock is dissolved 
		by rain water. In foreground deep vertical fissures (grikes) in the 
		limestones.
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		Saturday 25.03.2017
 A close-up photo showing the nature of the Carboniferous limestones 
		derived from marine organisms with fossils of crinoids and corals.
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		Saturday 25.03.2017
 The field trip continues at the Poulnabrone geosite, a megalithic tomb 
		that is one of Ireland’s most iconic archaeological monuments. It is the 
		oldest dated megalithic monument in Ireland as Poulnabrone revealed the 
		remains of 36 individuals in the main tomb chamber and radiocarbon 
		dating of their bones provided a date range of between 5,800 and 5,200 
		years ago.
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		Saturday 25.03.2017
 Poulnabrone portal tomb is located on the high Burren limestone plateau, 
		about 150 m above sea level. A panel deals with the geology, ecology and 
		farming of the Poulnabrone area.
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		Saturday 25.03.2017
 Around the Poulnabrone geosite a dry-stone wall shows a characteristic 
		arrangement of the blocks from the bedrock, i.e. the Carboniferous 
		limestones.
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		Saturday 25.03.2017
 A period of prolonged rainfall allows us to enjoy the Carran Turlough 
		filled with water which, otherwise, it is normally drained and empty.
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		Saturday 25.03.2017
 The field trip ends at Kilfenora which gives us an unforgettable sunset!
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