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Stone Town Of Kuklica
The stone town is an area consisting of over 120 naturally formed stone pillars, located in the village of Kuklica, near Kratovo in North Macedonia. Location Kuklica is located 8 km northwest of Kratovo. The stone formations are situated on the right bank of the Kriva River valley. The area has an altitude of 415-420 m and extends over an area of 0.3 square km. Legends There are two main legends surrounding the formation of the strange stone pillars in Kuklica. The most famous legend is that of a man who could not decide which of two women he should marry. So, the man planned to marry each woman on the same day at different times. When the first wedding was in progress, the woman to marry the man second went to see who was getting married on the same day as she. When she saw her future husband marrying another woman, she cursed all in attendance at the wedding and turned them into stone. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kuklica
Kuklica ( mk, Куклица) is a small village in the municipality of Kratovo, North Macedonia North Macedonia, ; sq, Maqedonia e Veriut, (Macedonia before February 2019), officially the Republic of North Macedonia,, is a country in Southeast Europe. It gained independence in 1991 as one of the successor states of Yugoslavia. It .... It is known for the hundreds of naturally formed stone pillars that resemble humans. The village has about 100 inhabitants. Geographic location Kuklica is located northwest from Kratovo. It is known by natural phenomena of characteristic erosive landforms called ''earth pyramids'', ''earth pillars'' or ''stone dolls''. These landforms are found on the right side of Kriva River valley, at the above sea level, and extend over an area of . Demographics According to the 2002 census, the village had a total of 97 inhabitants. Ethnic groups in the village include:Macedonian Census (2002) ''Book 5 - Total population according to the Eth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kratovo, North Macedonia
Kratovo ( mk, Кратово ) is a small town in North Macedonia. It is the seat of Kratovo Municipality. It lies on the western slopes of Mount Osogovo at an altitude of above sea level. Having a mild and pleasant climate, it is located in the crater of an extinct volcano. It is known for its bridges and towers. History Early Middle Ages In the Roman period there was a settlement called ''Tranatura'' located within the modern city municipality. There was a mine nearby and the town was the seat of local authorities. No remains of the settlement has been found, however, remnants of Roman fortification were found on Zdravče kamen hill above the town. Byzantine and Bulgarian Empires ruled the area subsequently. Late Middle Ages In 1282 Kratovo became part of the Kingdom of Serbia. In all probability the wealth of the town came from its mines. Saxon miners and Croatian merchants from Dubrovnik who already had worked in other parts of Macedonia settled here. The town was first ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Macedonia
North Macedonia, ; sq, Maqedonia e Veriut, (Macedonia before February 2019), officially the Republic of North Macedonia,, is a country in Southeast Europe. It gained independence in 1991 as one of the successor states of Socialist Federal Republic of Yugoslavia, Yugoslavia. It is a landlocked country bordering Kosovo to the northwest, Serbia to the north, Bulgaria to the east, Greece to the south, and Albania to the west. It constitutes approximately the northern third of the larger geographical Macedonia (region), region of Macedonia. Skopje, the capital and largest city, is home to a quarter of the country's 1.83 million people. The majority of the residents are ethnic Macedonians (ethnic group), Macedonians, a South Slavs, South Slavic people. Albanians in North Macedonia, Albanians form a significant minority at around 25%, followed by Turks in North Macedonia, Turks, Romani people in North Macedonia, Romani, Serbs in North Macedonia, Serbs, Bosniaks in North Mac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kriva River (Pčinja)
The Kriva River ( mk, Крива Река, ''Kriva Reka'') is a 75 km long river in northeastern North Macedonia, and the biggest left tributary of the Pčinja River. The name ''Kriva Reka'' means "Curved River" in Macedonian. Geography and tributaries The river rises at the northeastern slopes of Osogovo Mountain below the peak Carev Vrv , at an altitude of . On the mouth close to village Klečevce river flows at an altitude of . From the spring to the first tributary of the ''Kiselička reka'' ( from the source), the river flows northwest, then turns sharply to the southwest. The major tributaries of the Kriva Reka are: Kiselicka reka, Gaberska reka, Raska reka, Rankovecka reka, Vetunicka reka, Drzava (or Rudjinska drzava), Zivusa, Duracka reka, Kratovska reka, Povisnica and Vrlej. It belongs to the Aegean sea drainage basin. Kriva reka drains an area of around . Bibliography * ''Kvalitet na površinskite vodi vo slivot na Kriva reka'', O. Dimitrovska, I.Milevski, B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kuklica Pillars
Kuklica ( mk, Куклица) is a small village in the municipality of Kratovo, North Macedonia. It is known for the hundreds of naturally formed stone pillars that resemble humans. The village has about 100 inhabitants. Geographic location Kuklica is located northwest from Kratovo. It is known by natural phenomena of characteristic erosive landforms called ''earth pyramids'', ''earth pillars'' or ''stone dolls''. These landforms are found on the right side of Kriva River valley, at the above sea level, and extend over an area of . Demographics According to the 2002 census, the village had a total of 97 inhabitants. Ethnic groups in the village include:Macedonian Census (2002) ''Book 5 - Total population according to the Ethnic Affiliation, Mother Tongue and Religion'' The State Statistical Office, Skopje, 2002, p. 314. * Macedonians 97 See also *Stone town of Kuklica The stone town is an area consisting of over 120 naturally formed stone pillars, located in the villa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of North Macedonia
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. Stratigraphy, tectonics and geological history Geologists have partitioned the country up into four distinct zones (ZMZ - Western Macedonian Zone, PM - Pelagonian Massif, VZ - Vardar Zone, SMM - Serbo-Macedonian Massif) with three major fault lines and pock-marked by two volcanic areas (CKZ - Cukali-Krasta Zone, KZ - Kraistide Zone). Generally, the fault lines strike NNW to S. Precambrian formations include highly metamorphosed crystalline rocks and are distinguished as Pelagonian Horst Anticlinorium (also known as the Pelagon, or the Pelagonian Massifhttp://eprints.ugd.edu.mk/4181/1/geologica_balcanica_v.mircovski.pdf ) together with some blocks in the Vardar Zone. They are widely distributed in the Serbian-Macedonian Massif. The lower part of the segment includes gneiss, biotite, muscovi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoodoo (geology)
A hoodoo (also called a tent rock, fairy chimney, or earth pyramid) is a tall, thin spire of rock formed by erosion. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the elements. They generally form within sedimentary rock and volcanic rock formations. Hoodoos range in size from the height of an average human to heights exceeding a 10-story building. Hoodoo shapes are affected by the erosional patterns of alternating hard and softer rock layers. Minerals deposited within different rock types can cause hoodoos to have different colors throughout their height. Etymology In certain regions of western North America these rocky structures are called hoodoos. The name is derived from Hoodoo spirituality, in which certain natural forms are said to possess certain powers, but by the late 19th century, this spirituality became associated with bad luck. Prior to the English name for these geographic formations ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
