Łysica
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Łysica
Łysica is the highest mountain in the Świętokrzyskie Mountains of Poland. Its height is . It is located in the Świętokrzyski National Park and there is an abbey below it, on a site that might have been a pagan temple in the times before Christianization of Poland. Łysica, which is also called Góra Świętej Katarzyny (St. Catherine's Mountain) lies in western part of the Łysogóry range, near the village of Święta Katarzyna. It belongs to the so-called Crown of Polish Mountains (“Korona Gór Polskich”), as it is the highest mountain of Holy Cross Mountains. Łysica has two peaks - western (613 m) and eastern Skała Agaty (eng. Agatha's Rock) or Zamczysko (614 m). The mountain is made of quartzite and slate, its northern and southern slopes are marked by the stone run. Furthermore, on the southern slope, at the height of 590 meters, there is a small bog. Most of Łysica is covered by a forest, near the peak there are fir trees, below which are beeches. Łysica ...
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Łysa Góra
Łysa Góra , translated as Bald Mountain, is a well-known hill in Świętokrzyskie Mountains, Poland. With a height of 595 metres (1,952 ft), it is the second highest point in that range (after Łysica at 612 meters or 2,008 ft). On its slopes and atop its summit are several hiking trails, the ruins of a pagan wall from 9th century, the Benedictine monastery from the 11th century, and the Święty Krzyż TV Tower. The mountain also features prominently in a Lysa Hora (folklore), local legend about witches' sabbath (witchcraft), sabbaths. Names Former or corresponding names of the site include Łysica and Święty Krzyż. Location Łysa Góra, composed primarily of quartzite and Cambrian slates, lies in the eastern part of the Łysogóry range, and is the second largest peak of the larger Świętokrzyskie Mountains (after Łysica). A notable summit within the Świętokrzyski National Park, it is a vital point in many sightseeing trails of the region. The blue path to P ...
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Świętokrzyskie Mountains
The Świętokrzyskie Mountains (, ), often anglicized to Holy Cross Mountains, are a mountain range in central Poland, near the city of Kielce. The mountain range comprises several lesser ranges, the highest of which is Łysogóry (literally "Bald Mountains"). The two highest peaks are Łysica, 614 m (2014.44 ft), and Łysa Góra, 594 m (1948.81 ft). Together with the Jura Krakowsko-Częstochowska and some other regions, the mountains form a region called the Lesser-Poland Upland (''Wyżyna Małopolska''). Geologically speaking, the Holy Cross Mountains possess also a margin which extends further than the mountains themselves; the Owadów–Brzezinki palaeontological site is situated in the margin of the Holy Cross Mountains, but not in the mountains themselves. They cover an area of 1684 km2 (650 mi2). The approximate location is . Prehistory The Świętokrzyskie Mountains are one of the oldest mountain ranges in Europe. They were forme ...
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Crown Of Polish Mountains
Crown of Polish Mountains (Polish: ''Korona Gór Polski'') – a list of 28 peaks one per each of the mountain ranges of Poland. It was suggested by geographer, traveller and writer and Dr. Wojciech Lewandowski in the tourism and local lore magazine '. The list was on December 12, 1997 at a meeting convened by the editors of ''Know Your Country'' and at the same time the Club of the Conquerors of the Crown of Polish Mountains was inaugurated. The original idea was to be a list containing the highest peak of each range. However it was decided to consider only most prominent peaks which had a marked hiking trail at the time of the compiling of the list. In addition, the authors made several significant mistakes in the selection of peaks, e.g. by omitting some mountain ranges in the rank of a mesoregion, and placing others in the rank of a microregion. According to the new physical and geographical regionalization of Poland published in 2018, there are more peaks in the Crown ...
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Świętokrzyski National Park
Świętokrzyski National Park () is a National Park in Świętokrzyskie Voivodeship in central Poland. It covers the highest ridge of the Świętokrzyskie (Holy Cross) Mountains – the Łysogory – with its two highest peaks: Łysica at and Łysa Góra ("Bald Mountain") at . It also covers the eastern part of the Klonowski Ridge and part of the Pokrzywianski Ridge. The park has its headquarters in Bodzentyn. History The history of efforts to protect this part of Poland dates back to the times before World War I. In 1921 a first forest reserve in the Swiętokrzyskie mountains was created – this was Józef Kostyrko's reserve on Chełmowa Góra (1.63 km2). The following year, two parts of the Łysogory with a total area of 3.11 km2 also became protected. In 1932 the area of the reserve was officially expanded to 13.47 km2, but the National Park was not created until 1950. Its initial area was 60.54 km2, but it has since been expanded to , of which 72.12&nbs ...
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Slate
Slate is a fine-grained, foliated, homogeneous, metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade, regional metamorphism. It is the finest-grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate, called " slaty cleavage", is caused by strong compression in which fine-grained clay forms flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation with a specialized tool in the quarry, many slates display a property called fissility, forming smooth, flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen ''en masse'' covering roofs. However, slate occurs in a variety of colors even from a single locality; for ...
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Eurasian Hobby
The Eurasian hobby (''Falco subbuteo'') or just hobby, is a small, slim falcon. It belongs to a group of similar falcons often considered a subgenus '' Hypotriorchis''. Taxonomy and systematics The first formal description of the Eurasian hobby was by the Swedish naturalist Carl Linnaeus in 1758 in the tenth edition of his ''Systema Naturae'' under the present binomial name ''Falco subbuteo''. The genus name ''falco'' derives from Late Latin ''falx'', ''falcis'', a sickle, referring to the wing profile of the bird. The species name ''subbuteo'' is from Latin ''sub'', "below, less than, under" and ''buteo'', "buzzard". The species' English name comes from Old French ''hobé'' or ''hobet''. It became the trademark for the Subbuteo games company after its creator, who was an ornithologist, was refused permission to register "Hobby". Two subspecies are recognized: * ''F. s. subbuteo'': the nominate race is resident in Africa, Europe and Central and East Asia, winters in Central an ...
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Eurasian Sparrowhawk
The Eurasian sparrowhawk (''Accipiter nisus''), also known as the northern sparrowhawk or simply the sparrowhawk, is a small bird of prey in the family Accipitridae. Adult male Eurasian sparrowhawks have bluish grey upperparts and orange-barred underparts; females and juveniles are brown above with brown barring below. The female is up to 25% larger than the male – one of the greatest size differences between the sexes in any bird species. Though it is a predator which specialises in catching woodland birds, the Eurasian sparrowhawk can be found in any habitat and often hunts garden birds in towns and cities. Males tend to take smaller birds, including Tit (bird), tits, finches and Old World sparrow, sparrows; females catch primarily Thrush (bird), thrushes and starlings but are capable of killing birds weighing or more. The Eurasian sparrowhawk is found throughout the temperate and subtropical parts of the Old World; whilst birds from the northern parts of the range Bird mig ...
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Lesser Spotted Eagle
The lesser spotted eagle (''Clanga pomarina'') is a large Eastern European bird of prey. Like all typical eagles, it belongs to the family Accipitridae. The typical eagles are often united with the buteos, sea eagles, and other more heavy-set Accipitridae, but more recently it appears as if they are less distinct from the more slender accipitrine hawks than believed. Description This is a medium-sized eagle, about in length and with a wingspan of . Its head and wing coverts are pale brown and contrast with the generally dark plumage. The head and bill are small for an eagle. Usually, a white patch occurs on the upper wings, and even adults retain a clearly marked white "V" on the rump; the wing markings are absent and the white "V" is not well-defined in the greater spotted eagle. The juvenile has less contrast in the wings, but the remiges bear prominent white spots. It differs from greater spotted eagle juveniles by a lack of wing covert spotting and the presence of a cre ...
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Beech
Beech (genus ''Fagus'') is a genus of deciduous trees in the family Fagaceae, native to subtropical (accessory forest element) and temperate (as dominant element of Mesophyte, mesophytic forests) Eurasia and North America. There are 14 accepted species in two distinct subgenera, ''Englerianae'' and ''Fagus''. The subgenus ''Englerianae'' is found only in East Asia, distinctive for its low branches, often made up of several major trunks with yellowish bark. The better known species of subgenus ''Fagus'' are native to Europe, western and eastern Asia and eastern North America. They are high-branching trees with tall, stout trunks and smooth silver-grey bark. The European beech ''Fagus sylvatica'' is the most commonly cultivated species, yielding a utility timber used for furniture construction, flooring and engineering purposes, in plywood, and household items. The timber can be used to build homes. Beechwood makes excellent firewood. Slats of washed beech wood are spread around ...
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Stone Run
A stone run (called also ''stone river'', ''stone stream'' or ''stone sea''Vitosha Nature Park: Basic Information. Landscape.
Vitosha Nature Park website.
) is a rock landform resulting from the erosion of particular rock varieties caused by freezing-thawing cycles in periglacial conditions during the last glacial period, last Ice Age. The actual formation of stone runs involved five processes: weathering, solifluction, frost heaving, frost sorting, and washing.Stone, Phillip.
Periglacial Princes Street - 52° South.
''The Edinburgh Geologist''. Issue No 35, 2000.
The stone runs are essentially different from ...
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List Of Mountains In Poland
:''This is a sub-article to Geography of Poland'' Two major mountain ranges populate Poland's south-east and south-west borders, respectively: the Sudetes and Carpathian Mountains mountain ranges. Those ranges are located both within and outside of Poland. Within Poland, neither of them is forbidding enough to prevent substantial habitation; the Carpathians are especially densely populated. The rugged form of the Sudeten range derives from the geological shifts that formed the later Carpathian uplift. The Carpathians in Poland, formed as a discrete topographical unit in the relatively recent Tertiary Era, are the highest mountains in the country. They are the northernmost edge of a much larger range that extends into the Czech Republic, Slovakia, Ukraine, Hungary, and Romania. The Świętokrzyskie Mountains, one of the oldest mountain ranges in Europe, are located in central Poland, in the vicinity of the city of Kielce. The mountain range consists of a number of separate ran ...
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Quartzite
Quartzite is a hard, non- foliated metamorphic rock that was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts, and hence quartzite is a metasandstone. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resist ...
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