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Antiathonas
Antiathonas ( el, Αντιάθωνας or ) is a peak in the Athos peninsula. Its summit is 1042 metres above sea level. The peak can be reached via footpaths from Dionysiou Monastery. It is located a few kilometers northwest of the summit of Mount Athos. Lakkoskiti Lakkoskiti (, ro, Schitul Lacu) is the short form name of a small "monastic village" of not more than 15 "huts" (houses) consisting the idiorrhythmic "skete of Agiou Dimitriou tou Lakkou". It is situated in the north foothills of Mount Athos, in ..., a Romanian skete, is located on its eastern slopes. Gallery Mount Athos with way in foreground.png, Antianthonas is in the foreground, with the summit of Mount Athos slightly visible in the background. Mount Athos 2.jpg, View of Antiathonas from the sea Athos Peninsula (1).JPG, Aerial view of Antiathonas (lower center) References Mount Athos Landforms of Chalkidiki Mountains of Central Macedonia Mountains associated with Byzantine monasticism Mountains a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Footpaths Of Mount Athos
Mount Athos has an extensive network of footpaths, many of which date back to the Byzantine period. These paths are typically trails designed for human foot traffic and mules, and are not wide enough for motor vehicles. They connect the various monasteries, sketes, cells, kathismas, and hermitages on the peninsula to each other. History Many of the footpaths of Mount Athos date back to the Byzantine period. Some are cobblestone paths (''kalderimi''), while most are dirt trails (''monopatia''). Starting in the 1960s, many of the footpaths began to fall into disrepair. However, in the 21st century, the Friends of Mount Athos and other volunteers have been restoring and maintaining the footpaths for pilgrims and monks to use. Today, most of the footpaths are signed, well maintained, and in good condition. The Friends of Mount Athos footpath group also maps out GPX files for the footpaths and monitors their conditions. Eastern coast From north to south in order, the footpath networ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lakkoskiti
Lakkoskiti (, ro, Schitul Lacu) is the short form name of a small "monastic village" of not more than 15 "huts" (houses) consisting the idiorrhythmic "skete of Agiou Dimitriou tou Lakkou". It is situated in the north foothills of Mount Athos, in Greece, in the Morfonou River valley and surrounded by a forest of chestnut trees. The summit of Antiathonas (1042 m) is located just to the southwest of the skete. Lakkoskiti is inhabited by Romanian monks. Lakkoskiti belongs to Agiou Pavlou (Greek: Αγίου Παύλου, English: Saint Paul) Monastery. Spiritually, through its mother monastery, and like all the Athos peninsula, it is under the jurisdiction of the Ecumenical Patriarchate of Constantinople. History Very little is known about the history of Romanian Lakkoskiti. Monks were living there since the 10th century, belonging to the old Amalfinon Monastery which was soon abandoned and ruined, after the Schism between Eastern Orthodox and Western Roman Catholic Church in 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalkidiki
Chalkidiki (; el, Χαλκιδική , also spelled Halkidiki, is a peninsula and regional unit of Greece, part of the region of Central Macedonia, in the geographic region of Macedonia in Northern Greece. The autonomous Mount Athos region constitutes the easternmost part of the peninsula, but not of the regional unit. The capital of Chalkidiki is the town of Polygyros, located in the centre of the peninsula, while the largest town is Nea Moudania. Chalkidiki is a popular summer tourist destination. Name ''Chalkidiki'' also spelled ''Halkidiki'' () or ''Chalcidice'' () was the name given to this peninsula after Chalkida. In ancient times, the area was a colony () of the ancient Ionian Greek city-state of Chalcis. Geography The Cholomontas mountains lie in the north-central part of Chalkidiki. Chalkidiki consists of a large peninsula in the northwestern Aegean Sea, resembling a hand with three 'fingers' (though in Greek these peninsulas are often referred to as 'legs'). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Athos Peninsula
Mount Athos (; el, Ἄθως, ) is a mountain in the distal part of the eponymous Athos peninsula and site of an important centre of Eastern Orthodox monasticism in northeastern Greece. The mountain along with the respective part of the peninsula have been governed as the monastic community of Mount Athos, an autonomous region within the Hellenic Republic, ecclesiastically under the direct jurisdiction of the Ecumenical Patriarch of Constantinople, while the remainder of the peninsula forms part of the Aristotelis municipality. Mount Athos has been inhabited since ancient times and is known for its long Christian presence and historical monastic traditions, which date back to at least AD 800 and the Byzantine era. Because of its long history of religious importance, the well-preserved agrarian architecture within the monasteries, and the preservation of the flora and fauna around the mountain, Mount Athos was inscribed on the UNESCO World Heritage List in 1988. In modern Greek, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Athos
Mount Athos (; el, Ἄθως, ) is a mountain in the distal part of the eponymous Athos peninsula and site of an important centre of Eastern Orthodox monasticism in northeastern Greece. The mountain along with the respective part of the peninsula have been governed as the monastic community of Mount Athos, an autonomous region within the Hellenic Republic, ecclesiastically under the direct jurisdiction of the Ecumenical Patriarch of Constantinople, while the remainder of the peninsula forms part of the Aristotelis municipality. Mount Athos has been inhabited since ancient times and is known for its long Christian presence and historical monastic traditions, which date back to at least AD 800 and the Byzantine era. Because of its long history of religious importance, the well-preserved agrarian architecture within the monasteries, and the preservation of the flora and fauna around the mountain, Mount Athos was inscribed on the UNESCO World Heritage List in 1988. In modern Greek, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Chalkidiki
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Central Macedonia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Associated With Byzantine Monasticism
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Associated With Christian Monasticism
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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