Concó River
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Concó River
Concó is a river in northern Hungary, a tributary of the Danube. It rises in Fejér County and enters the Danube in Komárom-Esztergom County near the city of Komárom. Geography The Concó rises on the northern slopes of the Bakony range of the Transdanubian Mountains and the western and northwestern slopes of the Vértes Hills. It flows basically north and slightly west. In the mountains there are warm springs due to tectonic uplift. In the lower reaches the Concó is subject to flooding. As of 2009, sewage, wastewater and drainage from community landfills went essentially untreated into the river. Mostly the area of the Concó Basin is wilderness in the south and farmlands in the middle and northern sections. The only significant industrial activity is in Kisbér, in the middle section. The Concó discharges into the Danube at the village of Ács. The bedrock consists of Triassic limestones and sandstones, overlain by a thick layer of more recent alluvial sediments, predom ...
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Hungary
Hungary ( hu, Magyarország ) is a landlocked country in Central Europe. Spanning of the Carpathian Basin, it is bordered by Slovakia to the north, Ukraine to the northeast, Romania to the east and southeast, Serbia to the south, Croatia and Slovenia to the southwest, and Austria to the west. Hungary has a population of nearly 9 million, mostly ethnic Hungarians and a significant Romani minority. Hungarian, the official language, is the world's most widely spoken Uralic language and among the few non-Indo-European languages widely spoken in Europe. Budapest is the country's capital and largest city; other major urban areas include Debrecen, Szeged, Miskolc, Pécs, and Győr. The territory of present-day Hungary has for centuries been a crossroads for various peoples, including Celts, Romans, Germanic tribes, Huns, West Slavs and the Avars. The foundation of the Hungarian state was established in the late 9th century AD with the conquest of the Carpathian Basin by Hungar ...
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Germanic Peoples
The Germanic peoples were historical groups of people that once occupied Central Europe and Scandinavia during antiquity and into the early Middle Ages. Since the 19th century, they have traditionally been defined by the use of ancient and early medieval Germanic languages and are thus equated at least approximately with Germanic-speaking peoples, although different academic disciplines have their own definitions of what makes someone or something "Germanic". The Romans named the area belonging to North-Central Europe in which Germanic peoples lived ''Germania'', stretching East to West between the Vistula and Rhine rivers and north to south from Southern Scandinavia to the upper Danube. In discussions of the Roman period, the Germanic peoples are sometimes referred to as ''Germani'' or ancient Germans, although many scholars consider the second term problematic since it suggests identity with present-day Germans. The very concept of "Germanic peoples" has become the subject of ...
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Battle Of Bolia
The Battle of Bolia, was a battle in 469 between the Ostrogoths ( Amal Goths) and a coalition of Germanic tribes in the Roman province of Pannonia. It was fought on the south side of the Danube near its confluence with the river Bolia, in present-day Hungary. The Ostrogoths won, achieving supremacy in Pannonia, but soon migrated south towards richer lands. Background Following the death of Attila, various Germanic and other tribes sought their independence from his empire. They allied under the command of Ardaric, the Gepid king, and defeated the Huns and supporting forces at the Battle of Nedao in 454 CE. While the role of the Ostrogoths in that battle is unclear, it resulted in their independence as well. After the Battle of Nedao, the newly freed tribes jockeyed for supremacy in Pannonia for the next fifteen years, most eventually becoming federates of the Eastern Roman Empire. Battle The Amal Goths were led by Theodemir, brother-in-law to the Ostrogoths' chief Valamir, wh ...
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Castra
In the Roman Republic and the Roman Empire, the Latin word ''castrum'', plural ''castra'', was a military-related term. In Latin usage, the singular form ''castrum'' meant 'fort', while the plural form ''castra'' meant 'camp'. The singular and plural forms could refer in Latin to either a building or plot of land, used as a fortified military base.. Included is a discussion about the typologies of Roman fortifications. In English usage, ''castrum'' commonly translates to "Roman fort", "Roman camp" and "Roman fortress". However, scholastic convention tends to translate ''castrum'' as "fort", "camp", "marching camp" or "fortress". Romans used the term ''castrum'' for different sizes of camps – including large legionary fortresses, smaller forts for cohorts or for auxiliary forces, temporary encampments, and "marching" forts. The diminutive form ''castellum'' was used for fortlets, typically occupied by a detachment of a cohort or a '' centuria''. For a list of known castr ...
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Roman Empire
The Roman Empire ( la, Imperium Romanum ; grc-gre, Βασιλεία τῶν Ῥωμαίων, Basileía tôn Rhōmaíōn) was the post-Republican period of ancient Rome. As a polity, it included large territorial holdings around the Mediterranean Sea in Europe, North Africa, and Western Asia, and was ruled by emperors. From the accession of Caesar Augustus as the first Roman emperor to the military anarchy of the 3rd century, it was a Principate with Italia as the metropole of its provinces and the city of Rome as its sole capital. The Empire was later ruled by multiple emperors who shared control over the Western Roman Empire and the Eastern Roman Empire. The city of Rome remained the nominal capital of both parts until AD 476 when the imperial insignia were sent to Constantinople following the capture of the Western capital of Ravenna by the Germanic barbarians. The adoption of Christianity as the state church of the Roman Empire in AD 380 and the fall of the Western ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ...
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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: ...
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Komárom
Komárom (Hungarian: ; german: Komorn; la, Brigetio, later ; sk, Komárno) is a city in Hungary on the south bank of the Danube in Komárom-Esztergom County. Komárno, Slovakia, is on the northern bank. Komárom was formerly a separate village called . In 1892 Komárom and Újszőny were connected with an iron bridge and in 1896 the two towns were united under the name city of Komárom. The fortress played an important role in the Hungarian Revolution of 1848 and many contemporary English sources refer to it as the Fortress of Comorn. History Following the Hungarian conquest of the Carpathian Basin at the turn of the 9th and 10th centuries, Prince Árpád gave Komárom and the Komárom county vicinity to tribal chieftain Ketel. Ketel was the first known ancestor of the famous Koppán (genus) clan. At the beginning of the 12th century, this tribe founded the town's Benedictine Monastery in honor of the Blessed Virgin, mentioned in 1222 by the name of Monostorium de Koppán. ...
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