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Plačkovica
Plačkovica () is a mountain located in the eastern part of North Macedonia, it extends between the cities of Radoviš, and Vinica, North Macedonia, Vinica. The highest Summit (topography), peak is Lisec () at 1,754 m, the length of main valley slopes of the peak Lisec is 34 km. The valley of Zrnovska river splits the mountain in two, eastern and western parts. The peak of the western part is Turtel at 1,689 m. Lisec is a popular climbing route for the local climbers, being one of the harder peaks to scale in this part of Macedonia. It is not unusual to have snow on the peak during the month of June. The peak is served by two mountain lodges: Vrteška from Štip's side and, Dzumaja from Radoviš's side. Geological components of Plačkovica are mainly granite and marble. Name The ancient name of Mount Plačkovica is believed to have been Pangaium (or Pangaeum). This name is thought to be of Thracian origin, and the mountain was referenced in historical sources from the classical ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Radoviš
Radoviš ( ) is a city in the Southeastern statistical region, southeastern part of North Macedonia. It is the second largest city in the southeastern region. The city is the seat of Radoviš Municipality, which is spread on the bottom of Plačkovica Mountain and the northern part of the Radoviš-Strumica valley. The main road M6 Štip–Radoviš-Strumica is tangentially placed on the township of Radoviš. This road is a main communication route with other parts of the country. History The town of Radoviš was mentioned for the first time in 1019 during the reign of the Byzantine King Basil II (which was the name of the town during the Middle Ages). At this time in history, Radoviš is an important center for regional trade, craftsmanship and mining. At that time, the town was located in the North-West of the town's present location, on the banks of the Old river, where we can find traces of several churches, for example ''St. Archangel church''. In the 14th century, after the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vinica, North Macedonia
Vinica ( ) is a town in North Macedonia, in the Eastern Statistical Region of the country. The town of Vinica is the seat of Vinica Municipality. The town is located under the mountain of Plačkovica, in the southeastern part of the Kočani Valley. It covers the northern part of the river Bregalnica sinks. There are also several other rivers that flow through Vinica, like the Vinička, Gradečka and Osojnica. The town is known for its historic Roman fortress, Viničko Kale, situated on a hill overlooking the modern town. Etymology The name Vinica is derived from word vine, since the city was formerly noted for its vineyards. On terracotta icons found in Viničko Kale, the name of town is noted as Vinea or Vince. History Neolithic times The territory of Vinica was inhabited in Neolithic times. More recent evidence of habitation comes from findings on Viničko Kale from the 6th to the 12th century AD. Byzantine Empire The original settlement was a fort from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Štip
Štip ( ) is the largest urban agglomeration in the eastern part of North Macedonia, serving as the economic, industrial, entertainment and educational focal point for the surrounding municipalities. As of the 2021 census, the city of Štip had a population of about 44,866.Macedonian Census (2021) ''Book 5 - Total population according to the Ethnic Affiliation, Mother Tongue and Religion'' The State Statistical Office, Skopje, 2002, p. 196. Štip is the largest textile production center in the country. It is the center of the fashion industry in North Macedonia, as well as the site of the sole public university in eastern North Macedonia, Goce Delčev University of Štip. The city of Štip is the seat of Štip Municipality. Name The name Astibos is mentioned first by the ancient historian Polyaenus in 2nd century BC, who notes that Paeonian kings did ritualistic bathing in the Astibo / Brigantium (today: Bregalnica) river, as a coronation ritual. Astibo is also marked in the Ta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Macedonia
North Macedonia, officially the Republic of North Macedonia, is a landlocked country in Southeast Europe. It shares land borders with Greece to the south, Albania to the west, Bulgaria to the east, Kosovo to the northwest and Serbia to the north. 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 population of over 1.83 million. 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, Roma, Serbs in North Macedonia, Serbs, Bosniaks in North Macedonia, Bosniaks, Aromanians in North Macedonia, Aromanians and a few other minorities. The region's history begins with the Paeonia (kingdom), kingdom of Paeonia. In the la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Summit (topography)
A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topography, topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for a mountain peak that is located at some distance from the nearest point of higher elevation. For example, a big, massive rock next to the main summit of a mountain is not considered a summit. Summits near a higher peak, with some Topographic prominence, prominence or Topographic isolation, isolation, but not reaching a certain cutoff value for the quantities, are often considered ''subsummits'' (or ''subpeaks'') of the higher peak, and are considered part of the same mountain. A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top. For summits that are permanently covered in significant layers of ice, the height may be measured by the highest point of rock (rock height) or the highest point of permanent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
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 above the surrounding land. A few mountains are inselberg, isolated summits, but most occur in mountain ranges. mountain formation, Mountains are formed through tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations hav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow
Snow consists of individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide, or Sublimation (phase transition), sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes Nucleation, nucleate around particles in the atmosphere by attracting supercooling, supercooled water droplets, which Freezing, freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns, and Hard rime, rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marble
Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO3) or Dolomite (mineral), dolomite (CaMg(CO3)2) that have recrystallized under the influence of heat and pressure. It has a crystalline texture, and is typically not Foliation (geology), foliated (Layered intrusion, layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. The extraction of marble is performed by quarrying. Marble production is dominated by four countries: China, Italy, India and Spain, which account for almost half of world production of marble and decorative stone. Because of its high hardness and strong wear resistance, and because it will not be deformed by temperature, marble is often used in Marble sculpture, sculpture and construction. Etymology The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
