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Ľadový štít
Ľadový štít (translated into English as ''Ice Peak''; , literally, Ice Valley Peak) is the third highest of the Tatra Mountains, in Slovakia, and in the whole long Carpathian Mountains, Carpathian mountain chain, as well as in northern and eastern Central Europe. History The first confirmed ascent was made by 1843 John Ball (naturalist), John Ball, Wilhelm Richter, Carl Ritter, a Polish philologist, a Hungarian landscape painter and three Polish mountain guides.Wilhelm Richter, ''Wanderungen in Ungarn und unter seinen Bewohnern'', 1844pp.419-420/ref> In 1843, the first ascent was recorded, via Suchý žlab (Dry Couloir). Mounteineering The most popular climbing routes: Normal route. As first men on the top. Scale UIAA I. Ľadový koň (Ice ridge). North ridge from Tery hut to Ľadová priehyba (Ice pass) and on the top. Scale UIAA II. Grósz route. The left side of southeast wall. Scale UIAA III. Brnčal pillar. The central southeast wall. Scale UIAA IV. Referenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovakia
Slovakia, officially the Slovak Republic, is a landlocked country in Central Europe. It is bordered by Poland to the north, Ukraine to the east, Hungary to the south, Austria to the west, and the Czech Republic to the northwest. Slovakia's mostly mountainous territory spans about , hosting a population exceeding 5.4 million. The capital and largest city is Bratislava, while the second largest city is Košice. The Slavs arrived in the territory of the present-day Slovakia in the 5th and 6th centuries. From the late 6th century, parts of modern Slovakia were incorporated into the Pannonian Avars, Avar Khaghanate. In the 7th century, the Slavs played a significant role in the creation of Samo's Empire. When the Avar Khaghanate dissolved in the 9th century, the Slavs established the Principality of Nitra before it was annexed by the Great Moravia, Principality of Moravia, which later became Great Moravia. When Great Moravia fell in the 10th century, the territory was integrated i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpathian Mountains
The Carpathian Mountains or Carpathians () are a range of mountains forming an arc across Central Europe and Southeast Europe. Roughly long, it is the third-longest European mountain range after the Ural Mountains, Urals at and the Scandinavian Mountains at . The highest peaks in the Carpathians are in the Tatra Mountains, exceeding , closely followed by those in the Southern Carpathians in Romania, exceeding . The range stretches from the Western Carpathians in Austria, the Czech Republic, Slovakia and Poland, clockwise through the Eastern Carpathians in Ukraine and Romania, to the Southern Carpathians in Romania and Serbia.About the Carpathians – Carpathian Heritage Society [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Ball (naturalist)
John Ball (20 August 1818 – 21 October 1889) was an Irish politician, naturalist and Alpine traveller. Background and education Ball was born in Dublin, the eldest son of Nicholas Ball, judge of the Court of Common Pleas (Ireland) and his wife Jane Sherlock. He was educated at Oscott College near Birmingham, and at Christ's College, Cambridge, where he was 41st Wrangler but as a Roman Catholic could not be admitted to a BA degree. He showed in his early years a taste for natural science, particularly botany; and after leaving Cambridge he travelled in Switzerland and elsewhere in Europe and North Africa, studying his favourite pursuits, and contributing papers on botany and the Swiss glaciers to scientific periodicals. Political career In 1846 Ball was made an assistant poor-law commissioner, but resigned in 1847, and in 1848 stood unsuccessfully as a parliamentary candidate for Sligo. In 1849 he was appointed second poor-law commissioner, but resigned in 1852 and succ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carl Ritter
Carl Ritter (August 7, 1779September 28, 1859) was a German geographer. Along with Alexander von Humboldt, he is considered one of the founders of modern geography, as they established it as an independent scientific discipline. From 1825 until his death, he occupied the first chair in geography at the University of Berlin. Biography Carl Ritter was born in Quedlinburg, one of the six children of a doctor, F. W. Ritter. Ritter's father died when he was two. At the age of five, he was enrolled in the Schnepfenthal Salzmann School, a school focused on the study of nature (apparently influenced by Jean-Jacques Rousseau's writings on children's education). This experience would influence Ritter throughout his life, as he retained an interest in new educational modes, including those of Johann Heinrich Pestalozzi. Indeed, much of Ritter's writing was based on Pestalozzi's three stages in teaching: the acquisition of the material, the general comparison of material, and the estab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Slovakia
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 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 climate, mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Two-thousanders Of Slovakia
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spiš
Spiš ( ; or ; ) is a region in north-eastern Slovakia, with a very small area in south-eastern Poland (more specifically encompassing 14 former Slovak villages). Spiš is an informal designation of the territory, but it is also the name of one of the 21 official tourism regions of Slovakia. The region is not an administrative division in its own right, but between the late 11th century and 1918 it was an administrative county of the Kingdom of Hungary (see separate article Szepes County in this regard). Etymology The name is probably related to the appellative ''spiška'', ''špiška'' known from Slovak (Eastern Slovakia and Orava) and Moravian dialects ( Haná) - a (cut) stick, a piece of wood or sugar, etc. Old Slavic ''pьchjati'', ''pichjati'' - to stab, to cut → prefixed form sъ-pich-jь → after palatalization and extinction of yers ''spiš''. Spiš probably means "a cut forest". The theory is supported also by the fact that almost all early Latin documents ment ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirques Of Europe
A (; from the Latin word ) is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from , meaning a pot or cauldron) and ; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the downstream limit of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
