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Keprník is a mountain in the Hrubý Jeseník mountain range in the
Czech Republic The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europe. The country is bordered by Austria to the south, Germany to the west, Poland to the northeast, and Slovakia to the south ...
. It has an elevation of
above sea level Height above mean sea level is a measure of a location's vertical distance (height, elevation or altitude) in reference to a vertical datum based on a historic mean sea level. In geodesy, it is formalized as orthometric height. The zero level ...
. It is located in the municipality of Ostružná, on the historical border between
Silesia Silesia (see names #Etymology, below) is a historical region of Central Europe that lies mostly within Poland, with small parts in the Czech Silesia, Czech Republic and Germany. Its area is approximately , and the population is estimated at 8, ...
and
Moravia Moravia ( ; ) is a historical region in the eastern Czech Republic, roughly encompassing its territory within the Danube River's drainage basin. It is one of three historical Czech lands, with Bohemia and Czech Silesia. The medieval and early ...
.


Characteristics


Location

Keprník is located in the northwestern region of the entire Hrubý Jeseník range, lying almost centrally in the Hrubý Jeseník area, in a sub-region called the (). It sits on the main ridge that runs from pass to pass. The peak is easily recognizable due to its characteristic summit rock formation, situated on a deforested summit area among high-altitude vegetation. It appears to be the highest peak in this part of the Hrubý Jeseník range at first glance and is the main central peak of the Keprník Massif. It is very visible and recognizable from the road surrounding the summit area of Praděd mountain (visible to the right of the peak). Another notable viewpoint is from the road around the Dlouhé stráně peak, from where it is also very visible and recognizable, located to the right of the Vozka peak. Keprník is the fifth-highest peak in the Hrubý Jeseník range (following the peaks: Praděd, Vysoká hole, Vysoká hole–JZ, and Petrovy kameny). The mountain is bounded by: * to the north, the pass towards the
Šerák Šerák () is a mountain in the Hrubý Jeseník mountain range in the Czech Republic. It has an elevation of above sea level. It is located in the municipality of Ostružná, on the historic border of Moravia and Silesia. Characteristics Loc ...
mountain; * to the northeast, the valleys of the Keprnický potok and Bystrý potok streams; * to the east, a minor pass (the highest in the Keprník Massif) at an elevation of 1,344 m above sea level towards the peak * to the southeast, the valley of the Rudohorský potok stream and the Sedlo pod Vřesovkou pass towards the Červená hora–S peak; * to the south, the valley of the Hučivá Desná stream; * to the southwest, the Sedlo Trojmezí pass towards the Vozka peak and the valley of the Jelení potok stream; * to the northwest, the valley of the Klepáčský potok stream. Surrounding peaks include: * to the northeast, , Spálená stráň, Nad Výrovkou, and Domašovský kopec (located in the
Opawskie Mountains The Opawskie Mountains (, ) or Zlatohorská Highlands / Zlaté Hory Highlands (, ) are a mountain range of the Eastern Sudetes in the Czech Republic and Poland. Location The Opawskie Mountains stretch from northern Czech Silesia into Polish Uppe ...
range ()); * to the east, Žalostná; * to the southeast, Bršť (also in the Opawskie Mountains range), , Červená hora–S,
Červená hora Červená Hora () is a municipality and village in Náchod District in the Hradec Králové Region of the Czech Republic The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europ ...
, and ; * to the south, Spálený vrch–SV; * to the southwest, Vozka, , and Jelení stráň; * to the west, Černava–JZ; * to the northwest,
Černava Černava () is a municipality and village in Karlovy Vary District in the Karlovy Vary Region of the Czech Republic The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europe. The ...
, , Šerák–JZ, and Šerák.


Slopes

Within Keprník, 7 main slopes can be distinguished: * northern; * northeastern, known as ''V Žalostné''; * eastern, known as ''Vlčinec''; * southern; * southwestern, known as ''Trojmezí'' * western, known as ''Jelení stráň'' The slopes, roughly from an elevation of 1,260 to 1,390 m above sea level and downward, are predominantly forested with spruce. Above this range, in accordance with the
altitudinal zonation Altitudinal zonation (or elevational zonation) in mountainous regions describes the natural layering of ecosystems that occurs at distinct elevations due to varying environmental conditions. Temperature, humidity, soil composition, and solar radi ...
,
alpine tundra Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets ...
dominates, covered with grass and planted dwarf mountain pine. The slopes feature all types of forests: spruce forest,
mixed forest Temperate broadleaf and mixed forest is a temperate climate terrestrial habitat type defined by the World Wide Fund for Nature, with broadleaf tree ecoregions, and with conifer and broadleaf tree mixed coniferous forest ecoregions. These ...
, and
deciduous forest In the fields of horticulture and botany, the term deciduous () means "falling off at maturity" and "tending to fall off", in reference to trees and shrubs that seasonally shed leaves, usually in the autumn; to the shedding of petals, after flo ...
. On the northeastern, eastern, and western slopes, besides the spruce forests, there are small areas of mixed forest as the elevation decreases, and even small patches of deciduous forest on the eastern slope. Almost all slopes are characterized by significant variability in forest cover, with substantial clearings and thinning, and even bare areas. On the northern slope, close to the summit area, there is a single larger rock formation, while on the northeastern, eastern, and western slopes there are numerous groups of rocks. Approximately 1.6 km southwest of the summit (on the western slope), at an elevation of around 1,060 m above sea level, near the flowing stream named Jelení potok, there is a rock group called ''Jelení stráň''. Additionally, on the western slope near the pass, there is an area covered with rock debris. The slopes have relatively uneven and varied gradients. The average slope inclination ranges from 6° (eastern slope) to 17° (southeastern slope). The average inclination of all the mountain's slopes (weighted average of the slopes' gradients) is about 12°. The maximum average inclination of the eastern slope, at elevations around 1,150 m above sea level, does not exceed 40° over a 50-meter section. The slopes are covered with a network of roads and generally unmarked paths and tracks. Approximately 995 m north of the summit, close to the red tourist trail (about 30 m away), at an elevation of 1,309 m above sea level, there is a monument with a stone commemorative plaque, erected on 26 September 1935. It features the image of the Silesian writer and mountain enthusiast
Hermann Löns Hermann Löns (29 August 1866 – 26 September 1914) was a German journalist and writer. He is most famous as "The Poet of the Heath" for his novels and poems celebrating the people and landscape of the North German moors, particularly the L ...
, along with the following inscription:


Main summit

There are no marked tourist trails leading directly to the main summit. The main ridge path crosses the summit area, along with a red tourist trail and a green educational path, which leads to the secondary peak Keprník–JV. Near this path is a tourist intersection named ''Keprník (vrchol)'' with an informational sign indicating an elevation of 1,423 m. The summit of the mountain is on an exposed rocky outcrop about 20 m in length, which serves as a
scenic viewpoint A scenic viewpoint—also called an observation point, viewpoint, viewing point, vista point, scenic overlook,These terms are more commonly used in North America. etc.—is an elevated location where people can view scenery (often with binocu ...
. From there, expansive views can be seen, including the peaks of
Černava Černava () is a municipality and village in Karlovy Vary District in the Karlovy Vary Region of the Czech Republic The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europe. The ...
,
Šerák Šerák () is a mountain in the Hrubý Jeseník mountain range in the Czech Republic. It has an elevation of above sea level. It is located in the municipality of Ostružná, on the historic border of Moravia and Silesia. Characteristics Loc ...
, ,
Červená hora Červená Hora () is a municipality and village in Náchod District in the Hradec Králové Region of the Czech Republic The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europ ...
, and , as well as distant mountain ranges such as the
Giant Mountains The Giant Mountains, Krkonoše, or Karkonosze (Czech: , , ), are a mountain range located in the north of the Czech Republic and the south-west of Poland, part of the Sudetes mountain system (part of the Bohemian Massif). The Czech–Polish bor ...
with
Sněžka Sněžka () or Śnieżka (, ) is a mountain on the border between the Czech Republic and Poland, the most prominent point of the Silesian Ridge in the Giant Mountains. At , its summit is the highest point in the Czech Republic, in the Lower Siles ...
, the
Králický Sněžník Mountains The Králický Sněžník Mountains or Śnieżnik Mountains (, , ) is a massif and mountain range in the Eastern Sudetes on the border of the Czech Republic and Poland. Geomorphology The Králický Sněžník Mountains is a mesoregion of the ...
, the
Beskids The Beskids or Beskid Mountains (, , , (), ()) are a series of mountain ranges in the Carpathians, stretching from the Czech Republic in the west along the border of Poland with Slovakia up to Ukraine in the east. The highest mountain in the Be ...
, the
Malá Fatra Malá Fatra (; also Little Fatra or Lesser Fatra, , ) is a mountain range in the Western Carpathians in the north-west of Central Slovakia. In the geomorphological system, it is a part of the Fatra-Tatra Area.Craig Stephen Cravens ''Culture And Cu ...
, and even the Slovak Tatras. Additionally, a small conical monument called ''Kámen'' with a worn commemorative inscription is located on this rocky outcrop: On top of this monument, lines with the names of visible peaks are marked. The summit area also features a
triangulation station A triangulation station, also known as a trigonometrical point, and sometimes informally as a trig, is a fixed surveying station, used in geodetic surveying and other surveying projects in its vicinity. The station is usually set up by a map ...
, marked on geodetic maps as number 22, with an elevation of 1,422.80 m above sea level and geographical coordinates , located about 10 m north of the summit. The State Geodetic and Cadastral Office lists the highest point of the mountain – the summit – at an elevation of 1,423.3 m above sea level and geographical coordinates . Access to the summit is via the main path and the ''Keprník (vrchol)'' tourist intersection, from which a path about 30 m long with wooden railings on either side leads to the summit.


Secondary summits

Keprník is a mountain with three summits. Apart from the main summit, the mountain massif includes two lower secondary summits.


Geology

Geologically, the Keprník massif belongs to the unit known as the Keprník Dome and is composed of
metamorphic rock Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, caus ...
s, mainly
gneiss Gneiss (pronounced ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. This rock is formed under p ...
es (
biotite Biotite is a common group of phyllosilicate minerals within the mica group, with the approximate chemical formula . It is primarily a solid-solution series between the iron- endmember annite, and the magnesium-endmember phlogopite; more al ...
),
orthogneiss Gneiss (pronounced ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. This rock is formed under p ...
es, ,
mylonite Mylonite is a fine-grained, compact metamorphic rock produced by dynamic recrystallization of the constituent minerals resulting in a reduction of the grain size of the rock. Mylonites can have many different mineralogical compositions; it is a ...
s, blasto-mylonites,
migmatite Migmatite is a composite rock (geology), rock found in medium and high-grade metamorphic environments, commonly within Precambrian craton, cratonic blocks. It consists of two or more constituents often layered repetitively: one layer is an old ...
s,
schist Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced ''schistosity'' (named for the rock). This means that the rock is composed of mineral grains easily seen with a l ...
s, and
igneous rock Igneous rock ( ), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rocks are formed through the cooling and solidification of magma or lava. The magma can be derived from partial ...
s, primarily meta-
granites Granite ( ) is a coarse-grained ( phaneritic) 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 under ...
. The geological structure also contains admixtures of
gemstone A gemstone (also called a fine gem, jewel, precious stone, semiprecious stone, or simply gem) is a piece of mineral crystal which, when cut or polished, is used to make jewellery, jewelry or other adornments. Certain Rock (geology), rocks (such ...
s such as
staurolite Staurolite is a reddish brown to black, mostly opaque, nesosilicate mineral with a white streak. It crystallizes in the monoclinic crystal system, has a Mohs hardness of 7 to 7.5 and the chemical formula: Fe2+2Al9O6(SiO4)4(O,OH)2. Magnesium, zinc ...
,
andalusite Andalusite is an aluminium nesosilicate mineral with the chemical formula Al2SiO5. This mineral was called andalousite by Delamétherie, who thought it came from Andalusia, Spain. It soon became clear that it was a locality error, and that the sp ...
,
garnet Garnets () are a group of silicate minerals that have been used since the Bronze Age as gemstones and abrasives. Garnet minerals, while sharing similar physical and crystallographic properties, exhibit a wide range of chemical compositions, de ...
, and
sillimanite Sillimanite or fibrolite is an aluminosilicate mineral with the chemical formula Al2SiO5. Sillimanite is named after the American chemist Benjamin Silliman (1779–1864). It was first described in 1824 for an occurrence in Chester, Connecticut ...
. The summit features
cryoplanation In geomorphology, cryoplanation or is a term used to both describe and explain the formation of plains, terraces and pediments in periglacial environments. Uncertainty surrounds the term, and the effectiveness of the cryoplanation process is held ...
terraces and frost cliffs formed during the
Pleistocene The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fin ...
in a
periglacial Periglaciation (adjective: "periglacial", referring to places at the edges of glacial areas) describes geomorphic processes that result from seasonal thawing and freezing, very often in areas of permafrost. The meltwater may refreeze in ice wedg ...
climate. It is likely that a small mountain glacier existed on the southeastern slope during this period, leaving behind the so-called ''Keprnický kar''.


Waters

Keprník lies on the European watershed boundary, with its northeastern, eastern, and southeastern slopes draining into the
Baltic Sea The Baltic Sea is an arm of the Atlantic Ocean that is enclosed by the countries of Denmark, Estonia, Finland, Germany, Latvia, Lithuania, Poland, Russia, Sweden, and the North European Plain, North and Central European Plain regions. It is the ...
basin (
Oder The Oder ( ; Czech and ) is a river in Central Europe. It is Poland's second-longest river and third-longest within its borders after the Vistula and its largest tributary the Warta. The Oder rises in the Czech Republic and flows through wes ...
river basin), and its southwestern and western slopes draining into the
Black Sea The Black Sea is a marginal sea, marginal Mediterranean sea (oceanography), mediterranean sea lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia. It is bound ...
basin (
Danube The Danube ( ; see also #Names and etymology, other names) is the List of rivers of Europe#Longest rivers, second-longest river in Europe, after the Volga in Russia. It flows through Central and Southeastern Europe, from the Black Forest sou ...
river basin). Several streams originate from its slopes: Jelení potok from the southwestern slope, Klepáčský potok from the western slope, Keprnický potok from the northeastern slope, and Rudohorský potok from the southeastern slope. Small swampy areas can be found on the southwestern and southern slopes at elevations around 1,320 and 1,300 m above sea level.


Waterfalls

For landscape enthusiasts, the waterfalls scattered across the slopes of the mountain on nearly all streams are a major attraction. Reaching them is challenging and requires the use of detailed maps.


Climate

At the summit, harsh climatic conditions prevail (the average annual temperature is about 2.2°C, the average annual precipitation is about 1,200 mm, and the snow cover on the mountain remains for about 180 days a year).


Nature protection

The summit area and parts of all slopes are within the (), which is part of the designated protected area known as the (). This reserve was established to protect rock, soil, and plant formations as well as rare animal species. No nature monuments have been established on the slopes. Along the red tourist trail, an educational path named ''With Koprníček on an excursion to the Keprník Mountains'' () has been created, with 13 observation points, running from Červenohorské sedlo to .


Šerák-Keprník National Nature Reserve

The Šerák-Keprník National Nature Reserve is located at elevations ranging from 1,300 to 1,423 m above sea level, covering an area of (with a protective buffer zone of up to 1,169.83 ha). Established on 31 December 1933, the reserve protects a series of preserved rock and soil formations formed during the harsh climate of the
Ice age An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages, and g ...
, such as cryoplanation terraces, frost ribs, and
hummocks In geology, a hummock is a small knoll or mound above ground.Bates, Robert L. and Julia A. Jackson, ed. (1984). "hummock." Dictionary of Geological Terms, 3rd Ed. New York: Anchor Books. p. 241. They are typically less than in height and ten ...
s, along with the flora and fauna found within these areas. The reserve is open to tourists, with both hiking and cycling trails as well as an educational path running through it.


Tourism


Tourist trails

The Czech Tourist Club has marked four tourist trails: Červenohorské sedlo –
Červená hora Červená Hora () is a municipality and village in Náchod District in the Hradec Králové Region of the Czech Republic The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europ ...
– spring – Sedlo pod Vřesovkou pass – Keprník-JV – ''Trojmezí'' – Keprník summit – Sedlo pod Keprníkem pass – Šerák mountain – –
Černava Černava () is a municipality and village in Karlovy Vary District in the Karlovy Vary Region of the Czech Republic The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europe. The ...
mountain – Ramzová Branná – Tři kameny – mountain – Volská louka pass – mountain – ''Trojmezí'' Branná – Pekelec mountain – Pekelec-SV summit – Alojzovské louky pass – Troják-JZ mountain – Hučava stream valley – Troják mountain – Vozka summit – Sedlo pod Vřesovkou pass
Lipová-lázně Lipová-lázně (until 1960 Dolní Lipová; ) is a spa municipality and village in Jeseník District in the Olomouc Region of the Czech Republic. It has about 2,000 inhabitants. Administrative division Lipová-lázně consists of three municipal p ...
– Sněhulák mountain – Strmý mountain – – Šerák Mountain – Sedlo pod Keprníkem pass – mountain – mountain – Filipovice


Cycling and skiing trails

A small section at the foot of the northeastern slope features the only designated cycling trail: ''Spojená cesta'' – mountain – mountain – Šumná-JV – Šumná mountain – Nad Borovým mountain – Borový potok valley – Bělá pod Pradědem – mountain – Šumný mountain – Sedlo pod Keprníkem pass – Šerák mountain – Mračná hora – Černava mountain – Ostružná – Petříkov During snowy periods, cross-country ski trails are marked along the hiking and cycling trails (except the green tourist trail), including a trail named ''Jesenická magistrála''. No downhill skiing trails are marked within the mountain area.


Notes


References

{{reflist One-thousanders of the Czech Republic Mountains and hills of the Czech Republic