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Visegrád Mountains
The Visegrád Mountains (Hu: ''Visegrádi hegység'') is a mountain range in Hungary, not far from Budapest. Geography The Visegrád Mountains are the direct northern neighbour of the Pilis Mountains. Although the two ranges form a geographical unit as both of them officially belong to the Transdanubian Mountains, the Visegrád Mountains connect to Börzsöny and the North Hungarian Mountains. The mountain range is the southernmost part of the Inner Western Carpathians. The basic rock of these mountains is volcanic, mainly andesite, while the Transdanubian Mountains are based on sedimentary rocks. Geology Visegrád Mountains were shaped by volcanic events. History of the region The whole range served as the hunting area for the medieval kings. Notable locations The highest peak of the range is at Dobogókő (699 m above sea level), a hiking and ski resort area with a panoramic view on the Danube Bend The Danube Bend ( hu, Dunakanyar) is a curve of the Danube in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Budapest
Budapest (, ; ) is the capital and most populous city of Hungary. It is the ninth-largest city in the European Union by population within city limits and the second-largest city on the Danube river; the city has an estimated population of 1,752,286 over a land area of about . Budapest, which is both a city and county, forms the centre of the Budapest metropolitan area, which has an area of and a population of 3,303,786; it is a primate city, constituting 33% of the population of Hungary. The history of Budapest began when an early Celtic settlement transformed into the Roman town of Aquincum, the capital of Lower Pannonia. The Hungarians arrived in the territory in the late 9th century, but the area was pillaged by the Mongols in 1241–42. Re-established Buda became one of the centres of Renaissance humanist culture by the 15th century. The Battle of Mohács, in 1526, was followed by nearly 150 years of Ottoman rule. After the reconquest of Buda in 1686, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pilis Mountains
Pilis Mountains is a mountainous region in the Transdanubian Mountains. Its highest peak is ''Pilis-tető'' at . It is a popular hiking destination in Hungary. It is the direct southern neighbour of the Visegrád Mountains which are based on volcanic rocks while Pilis is sedimentary. History of the region The region used to be a hunting area for the mediaeval kings. Numerous hunting lodges have survived. One of the most frequented areas was around the village Pilisszentkereszt. Mountains of the range * , the second highest point of Transdanubia Transdanubia ( hu, Dunántúl; german: Transdanubien, hr, Prekodunavlje or ', sk, Zadunajsko :sk:Zadunajsko) is a traditional region of Hungary. It is also referred to as Hungarian Pannonia, or Pannonian Hungary. Administrative divisions Trad .... * * Csikóváralja References Transdanubian Mountains Biosphere reserves of Hungary {{Hungary-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Transdanubian Mountains
__NOTOC__ The Transdanubian Mountains (sometimes also referred to as ''Bakony Forest, Dunántúl Highlands, Highlands of Dunántúl, Highlands of Transdanubia, Mountains of Dunántúl, Mountains of Transdanubia, Transdanubian Central Range, Transdanubian Hills, Transdanubian Midmountains'' or ''Transdanubian Mid-Mountains'', ) are a mountain range in Hungary covering about 7000 km2. Its highest peak is the ''Pilis'', with a height of . Parts of the mountains *Bakony ** ''Southern Bakony'' ** ''Northern Bakony'' *** Keszthely Plateau *** Tapolca Basin *** Balaton Uplands **** Bakonyalja **** Sokoró Hills *Vértes Mountains ** Vértesalja (Bársonyos) *Velence Hills * Dunazug Mountains **Gerecse Mountains **Buda Hills ** Pilis Mountains Visegrád Mountains are often considered a part of it for geopolitical reasons, but geographically they are part of the North Hungarian Mountains. Gallery File:Gulács01.jpg File:Pliocene Volcanoes near Lake Balaton in Hungary.jpg File: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Börzsöny
Börzsöny (; sk, Novohradské hory, New City Mountains) is a mountain range in Northern Hungary. Its tallest peak is the Csóványos with . It is the westernmost member of the North Hungarian Mountains, which belongs to the Inner Western Carpathians. The varied landscape offers good hiking opportunities. A large part of the Börzsöny is national park. From the top of Csóványos we can see one of the country's most beautiful panorama on the Danube Bend (''Dunakanyar''). Geography The mountain is structurally divided into four parts: High Börzsöny, Northern Börzsöny, Western Börzsöny and Southern Börzsöny. High Börzsöny Here are the highest peaks of Börzsöny: the Csóványos (938 m), Magos-fa (916 m), Nagy-hideg Hill (864 m) and Nagy-Inóc (826 m). Northern Börzsöny Western Börzsöny Southern Börzsöny Hydrography There are about 470 creeks in Börzsöny. The major parts of the creeks are clean water. The mountain's longest and largest river is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Hungarian Mountains
The North Hungarian Mountains ( hu, Északi-középhegység), sometimes also referred to as the Northeast Hungarian Mountains, Northeast Mountains, North Hungarian Highlands, North Hungarian Mid-Mountains or North Hungarian Range, is the northern, mountainous part of Hungary. It forms a geographical unity with the Mátra-Slanec Area, the adjacent parts of Slovakia. It is a separate geomorphological area within the Western Carpathians. The mountains run along the northeastern border of Hungary as well as eastern parts of the Hungarian–Slovak border in broadband from the Danube Bend to the town of Prešov. Subdivisions The area consists of the following geomorphological units: * Börzsöny Regional Map Series of Hungary ( hu, Börzsöny + [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inner Western Carpathians
Divisions of the Carpathians are a categorization of the Carpathian mountains system. Below is a detailed overview of the major subdivisions and ranges of the Carpathian Mountains. The Carpathians are a "subsystem" of a bigger Alps-Himalaya System that stretches from western Europe all the way to southern Asia, and are further divided into "provinces" and "subprovinces". The last level of the division, i.e. the actual mountain ranges and basins, is usually classified as "units". The main divisions are shown in the map on the right. To generalize, there are three major provinces (regions): Western Carpathians, Eastern Carpathians, and the Southern Carpathians. Naming conventions The division is largely (with many exceptions) undisputed at the lowest level (except for the Ukrainian part), but various divisions are given for the higher levels, especially for the penultimate level. A geomorphological division has been used as much as the data was available; other new physio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Rock
Volcanic rock (often shortened to volcanics in scientific contexts) is a rock formed from lava erupted from a volcano. In other words, it differs from other igneous rock by being of volcanic origin. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into hypabyssal and metamorphic rocks and constitute an important element of some sediments and sedimentary rocks. For these reasons, in geology, volcanics and shallow hypabyssal rocks are not always treated as distinct. In the context of Precambrian shield geology, the term "volcanic" is often applied to what are strictly metavolcanic rocks. Volcanic rocks and sediment that form from magma erupted into the air are called "volcaniclastics," and these are technically sedimentary rocks. Volcanic rocks are among the most common rock types on Earth's surface, particularly in the oceans. On land, they are very common at plate boundaries and in flood basalt provinces. It has been estimated t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kingdom Of Hungary
The Kingdom of Hungary was a monarchy in Central Europe that existed for nearly a millennium, from the Middle Ages into the 20th century. The Principality of Hungary emerged as a Christian kingdom upon the coronation of the first king Stephen I at Esztergom around the year 1000;Kristó Gyula – Barta János – Gergely Jenő: Magyarország története előidőktől 2000-ig (History of Hungary from the prehistory to 2000), Pannonica Kiadó, Budapest, 2002, , p. 687, pp. 37, pp. 113 ("Magyarország a 12. század második felére jelentős európai tényezővé, középhatalommá vált."/"By the 12th century Hungary became an important European factor, became a middle power.", "A Nyugat részévé vált Magyarország.../Hungary became part of the West"), pp. 616–644 his family (the Árpád dynasty) led the monarchy for 300 years. By the 12th century, the kingdom became a European middle power within the Western world. Due to the Ottoman occupation of the central and south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dobogókő
Dobogókő is a popular tourist area near Pilisszentkereszt in Hungary, and the site of the highest point in the Visegrád Hills at 699 meters. 133 people live here. Up in the hills lies the Ödön Téry Memorial, a stone pyramid built in memory of one of great pioneers of Hungarian tourism. In Dobogókő there is a tourist museum and accommodation. There are hiking possibilities to , , and . Nearby larger settlements are Dömös and Szentendre. Dobogókő is also a pilgrimage site for Hungarian neopagans (followers of the revived Táltos faith, that is similar to shamanism Shamanism is a religious practice that involves a practitioner (shaman) interacting with what they believe to be a Spirit world (Spiritualism), spirit world through Altered state of consciousness, altered states of consciousness, such as tranc ...) who believe that the place is the " heart chakra" of the earth. References External links Dobogókői kirándulások képekkel - Dobogókő Hiking page ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Danube Bend
The Danube Bend ( hu, Dunakanyar) is a curve of the Danube in Hungary, close to the town of Visegrád. Geology The present-day U-shaped loop is probably the result of an eruption of the volcano stretching over the whole area some 15 million years ago. The caldera of Keserűs Hill-volcano, with the associated lava dome formed a later eroded central in the north. The river follows the southern edge of this caldera. The region This region is touristically very significant. The landscape and the river attracts a lot of visitors both from the homeland and abroad. The most important towns are Visegrád, Szentendre and Budapest, while on the other (left) bank of the river can be found Vác, Nagymaros and some smaller towns, villages. The islands of the region are also interesting, mainly the large Szentendrei-sziget and Margaret Island (Margitsziget) within the capital city. Gallery Catedral of Vác.jpg, The Cathedral of Vác Visegrad danube.jpg, Szentendrei-sziget RedBio T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
