The Chelmos-Vouraikos UNESCO Global Geopark is an UNESCO Global Geopark in Greece, containing geosites of special scientific, aesthetic and educational value, as well as of archeological, ecological, historical and cultural interest. [1] It is located in the northern part of Peloponnese, extending to the prefectures of Achaea and Korinthia. In this territory there are rivers, lakes and the entire range of the Chelmos Mountains, as well as the Vouraikos Gorge. [2] With an area of 654 km², 62 municipalities and a total population of 27125 inhabitants are included in the territory. [3]
Within the borders of this UNESCO Global Geopark, five protected areas of the "Natura 2000" Network can be found:
The conservation, protection and management of the Geopark is the responsibility of the Chelmos-Vouraikos Management Body based in Kalavryta. It was established in 2002 and got staffed in 2007. [5] Since October 2009, the Chelmos-Vouraikos Geopark has been a member of the European Geoparks Network, the Global Geoparks Network and the Hellenic Geopark Forum. [6] Based on the successful evaluations in 2013, 2015 and 2019, this Geopark stands out as a UNESCO Global Geopark since 2015. [7]
In 2016 it received the international certification "European Charter for Sustainable Tourism" from the European Federation of National Parks and Protected Areas (EUROPARC FEDERATION). [8]
The management body of Chelmos-Vouraikos is a legal entity under private law supervised by the Greek Ministry of Environment and Energy. The tasks of the management body are varied. Apart from the management of the protected areas and the conservation of the geo and biodiversity, organizing environmental education programs or guided tours are among their responsibilities. Cooperation with various other stakeholders is essential for these assignments.
The staff consists of an environmental scientist, a geologist, a forester, six rangers, a secretary, a deputy accountant, an external staff with the duties of an accountant, a legal advisor, and a scientific advisor on geological issues. [9]
The Chelmos-Vouraikos UNESCO Global Geopark is characterized by its remarkable geological heritage, hosting many unique geological features. The most important geological or geomorphological features in the Geopark are sinkholes, poljes, springs and caves. The Ladon's eye, a sinkhole that forms a deep karst lake (47 m), or the Cave of Lakes in the mountain of Amolinitsa with 13 underground lakes are characteristic examples. Most of the area of the Geopark consists of limestone, which is often strongly karstified. Besides that, the following clearly defined rock types can be found in the Geopark:
cohesive scree and talus cones, conglomerates, sandy marls, sands and sandstones with grit, sand and clay layers, flysch, limestones, radiolarites, dolomites, phyllites, schists, volcanic rocks, quartzites and lignites.
In addition, ten geological periods (Quaternary, Neogene, Paleogene, Cretaceous, Jurassic, Triassic, Permian, Carboniferous, Devonian and Silurian) and three geotectonic zones (Gavrovo-Tripolis zone, Pindos zone, Phyllites-Quartzites suite) are represented in the Geopark.
Geologic formations:
Metamorphic rocks of the Phyllites-Quartzites suite: schists, phyllites, quartzites
Tripoli zone formations: Tyros Formation volcanic rocks, carbonate rocks (limestones-dolomites) and flysch
Pindos zone formations: flysch, limestones, radiolarites
Neogene and Quaternary post alpine sediments and Holocene alluvial sediments: conglomerates, marls, sandstones, lignites, sand and mud sediments
Geological or geomorphological features:
Gorges, alluvial deposits, caves, conglomerates, flysch, lakes, sinkholes, marine terrace, plateaus, tectonic window, poljes, alpine lake, springs, dolines, waterfall, thrusts, faults, landslides, folds, moraines, fossils, mylonites [10]
The different geomorphosites (mountains, caves etc), the abundant water availability and the local climate are the basis for a rich biodiversity in the Geopark. The great geodiversity provides many opportunities for the formation of niches for numerous animal and plant species. Therefore, the ecological value for the flora and fauna of the region is immense.
The Chelmos-Vouraikos Geopark hosts more than 1100 plant species. [12] Among them there are Greek endemics, endemics of Peloponnese or local endemic plant species, many of which either belong to one of the IUCN Red Data Book risk categories, and/or are included in an international conservation regime. The existence of these rare plants is always connected with the soil type. In this context, the limestone mountain Chelmos plays an important role. Due to its considerable habitat diversity, thirty endemic species of the Peloponnese, more than one hundred Greek endemics and five local endemics of Chelmos can be found in this area. One of these plants is Globularia stygia, which got its name from the Styx waters geosite. This species underlines the ecological value of the mount Chelmos, being a priority species of the European Directive 92/43. It grows on rocks in gorges, on ledges, in open scree slopes, on limestone, at an altitude of 1150-2300 meters. Furthermore, a lot of pharmaceutical plants can be found in the region of the Geopark. [13]
The Geopark provides a habitat for the following animals: 76 species of invertebrates, 4 species of fish, including 2 endemics, [13] 9 species of amphibians, 23 species of reptiles, among them there are 9 endemic species, 18 species of mammals. Besides these, 149 bird species find permanent or temporary refuge in the area. A large number of endemic butterflies, including a number of rare species, live in the alpine plains, especially in the alpine grasslands of the Geopark. [14] These species are closely connected to the geological features of the Geopark, as they provide special habitats. For example, one of the most important winter bat colonies in Europe with 18,000 individuals flourishes in the Geosite “Cave of the lakes“. [15]
In the territory of the Geopark there are several sites of cultural, archaeological or aesthetic value, which are of touristic interest:
The special landscape and the climate within the Geopark offer various opportunities for people to cultivate the area. Especially, the primary sector is very distinct.
Areas of the Geopark are used for agriculture with products such as olives, tomatoes or lemons. In addition, the production of honey and livestock farming also play an important role in the cultivation of the park's land. Farms with mainly sheep and goats, but also cattle, contribute greatly to the formation of income in the region. Especially in Planitero and in Krathis, fishing has experienced an increasing expansion due to the inland waters. Trout and salmon farms are found in the area, making aquaculture another important human activity in the Geopark. Furthermore, forestry and thus the supply of wood to the population represents an important factor in the social space of the region.
The secondary sector is represented by small units in the Geopark that process agricultural products or fabricate household items and wood carvings. These products are closely related to the Geopark, as they originate from it.
The tertiary sector is also represented in the Geopark. On the one hand, through the trade of products to meet local needs, but also for the numerous tourists. These products include mainly traditional local items such as honey and aromatic plants. On the other hand, tourism is a very important factor in the area. The geological sites, such as the Cave of the Lakes, the springs of Aroanios River at Planitero or the Vouraikos Gorge etc, attract many visitors every year. Furthermore, a ski resort has developed in the north slopes of the Chelmos mountain. Therefore, this particular area of the Geopark, the Kalayta Ski center, is visited by numerous tourists during the winter months [17]
Pollution, solid waste, land use, destruction and environmental deterioration, construction of new road routes, irrigation works, fertilizers, animal grazing, illegal lumbering, forest fires, inefficient forest management [18]
The Pindus is a mountain range located in Northern Greece and Southern Albania. It is roughly 160 km long, with a maximum elevation of 2,637 metres (8651.5'). Because it runs along the border of Thessaly and Epirus, the Pindus range is known colloquially as the spine of Greece. The mountain range stretches from near the Greek-Albanian border in southern Albania, entering the Epirus and Macedonia regions in northern Greece down to the north of the Peloponnese. Geologically, it is an extension of the Dinaric Alps, which dominate the western region of the Balkan Peninsula.
Kalavryta is a town and a municipality in the mountainous east-central part of the regional unit of Achaea, Greece. The town is located on the right bank of the river Vouraikos, 24 kilometres south of Aigio, 40 km southeast of Patras and 62 km northwest of Tripoli. Notable mountains in the municipality are Mount Erymanthos in the west and Aroania or Chelmos in the southeast. Kalavryta is the southern terminus of the Diakopto-Kalavryta rack railway, built by Italian engineers between 1885 and 1895.
The Vikos–Aoös National Park is a national park in the region of Epirus in northwestern Greece. The park, founded in 1973, is one of ten national parks in mainland Greece and is located 30 kilometres (19 mi) north of the city of Ioannina in the northern part of the Pindus mountain range. It is named after the two major gorges of the area and encompasses 12,600 hectares of mountainous terrain, with numerous rivers, lakes, caves, deep canyons, dense coniferous and deciduous forest. The park is part of the Natura 2000 ecological network and one of UNESCO Geoparks and spans an elevation range from 550 to 2,497 meters. Over 100,000 people visit the park each year and take part in activities including rafting, canoe-kayaking, hiking and mountain biking.
Aroania, also known as Helmos or Chelmos, is a mountain in Achaea, Peloponnese, Greece. At 2,355 m elevation, Aroania is the third highest mountain of the Peloponnese, after Taygetus and Kyllini, and the highest in Achaea. The largest town near the mountain is Kalavryta. The municipal unit Aroania took its name from the mountain.
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Radiolarite is a siliceous, comparatively hard, fine-grained, chert-like, and homogeneous sedimentary rock that is composed predominantly of the microscopic remains of radiolarians. This term is also used for indurated radiolarian oozes and sometimes as a synonym of radiolarian earth. However, radiolarian earth is typically regarded by Earth scientists to be the unconsolidated equivalent of a radiolarite. A radiolarian chert is well-bedded, microcrystalline radiolarite that has a well-developed siliceous cement or groundmass.
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The Danxia landform refers to various landscapes found in southeast, southwest and northwest China that "consist of a red bed characterized by steep cliffs". It is a unique type of petrographic geomorphology found in China. Danxia landform is formed from red-coloured sandstones and conglomerates of largely Cretaceous age. The landforms look very much like karst topography that forms in areas underlain by limestones, but since the rocks that form danxia are sandstones and conglomerates, they have been called "pseudo-karst" landforms. They were formed by endogenous forces and exogenous forces.
The geology of Bosnia & Herzegovina is the study of rocks, minerals, water, landforms and geologic history in the country. The oldest rocks exposed at or near the surface date to the Paleozoic and the Precambrian geologic history of the region remains poorly understood. Complex assemblages of flysch, ophiolite, mélange and igneous plutons together with thick sedimentary units are a defining characteristic of the Dinaric Alps, also known as the Dinaride Mountains, which dominate much of the country's landscape.
The geology of North Macedonia includes the study of rocks dating to the Precambrian and a wide array of volcanic, sedimentary and metamorphic rocks formed in the last 539 million years.
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Mega Spilaio, formally the Monastery of the Dormition of the Theotokos, is a Greek Orthodox monastery in the municipality of Kalavryta, in the Peloponnese peninsula in southern Greece.
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