Tunel Wielki
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Tunel Wielki
Tunel Wielki (literally "Big Tunnel") is a cave in Ojców National Park, Poland. It is an archaeological site, located in the karst area of Kraków-Częstochowa Upland, about 20 km north of Kraków.Michelle StarrHalf-a-Million Year Old Signs of Extinct Human Species Found in Poland Cave ''ScienceAlert'', October 18, 2022Szymon Zdzieblowski/ref> The 1967–1968 excavations identified 15 layers in sediments in five distinct series coming from early Würm stage and early prehistorical cultures—Lengyel culture, Corded Ware culture, Funnelbeaker culture, Lusatian culture—as well as from the Middle Ages to 19th century.T. Madyska. Osady jaskiń i schronisk Doliny Sąspowskiej, w: Jaskinie Doliny Sąspowskiej. Tło przyrodnicze osdnictwa pradziejowego. Prace Instytutu Archeologii Uniwersytetu Warszawskiego, Warszawa: 1988, s. 77–173.Michał Wojenka et al., Sprawozdanie z badań wykopaliskowych przeprowadzonych w Jaskini Tunel Wielki w wąwozie Koziarnia w 2016 roku, „Prądn ...
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Ojców National Park
Ojców National Park ( pl, Ojcowski Park Narodowy) is a national park in Kraków County, Lesser Poland Voivodeship in southern Poland, established in 1956. It takes its name from the village of Ojców, where it also has its headquarters. Chopin visited Ojców in 1829. It is Poland's smallest national park, with an original area of , since expanded to . Of this area, is forested and is strictly protected. The park is approximately north of Kraków, in the Jurassic Kraków-Częstochowa Upland. Geography Karst topography of soluble bedrock characterizes the park, which in addition to two river (the Prądnik and Saspówka) valleys contains numerous limestone cliffs, ravines, and over 400 caves. The largest of these, Łokietek's Cave (said to have sheltered King Władysław I Łokietek, for whom it was named), is deep. The area is also noted for its rock formations, the most famous being Hercules' Club, a -high limestone column. Ojcowski Park is very biodiverse; over 550 ...
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Corded Ware Culture
The Corded Ware culture comprises a broad archaeological horizon of Europe between ca. 3000 BC – 2350 BC, thus from the late Neolithic, through the Copper Age, and ending in the early Bronze Age. Corded Ware culture encompassed a vast area, from the contact zone between the Yamnaya culture and the Corded Ware culture in south Central Europe, to the Rhine on the west and the Volga in the east, occupying parts of Northern Europe, Central Europe and Eastern Europe. The Corded Ware culture is thought to have originated from the westward migration of Yamnaya-related people from the steppe-forest zone into the territory of late Neolithic European cultures such as the Globular Amphora and Funnelbeaker cultures, and is considered to be a likely vector for the spread of many of the Indo-European languages in Europe and Asia. Nomenclature The term ''Corded Ware culture'' (german: Schnurkeramik-Kultur) was first introduced by the German archaeologist Friedrich Klopfleisch in ...
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Caves Of Poland
This article is about the caves of Poland. Geographic distribution Tatra Mountains , there are 843 caves known in the Polish Tatra Mountains with the total length exceeding 134 km. They are within Tatra National Park. All the prominent ones are limestone karst caves of the Western Tatras, but there are also some tectonic caves. The largest and deepest caves of the Tatras (and of Poland) are located in the Czerwone Wierchy and Kominiarski Wierch massifs. Another highly promising region, the massif of Giewont, is largely unexplored due to its strict nature conservation status. * Bańdzioch Kominiarski * Bliźniacza Studnia * Dudnica * Dudowa Studnia * Dziura * Dziura Wyżnia – Jaskinia Lisia * Dziurka w Trawce * Górne Kominy * Jasiowa Dziura * Jaskinia Bystrej * Jaskinia Czarna * Jaskinia Goryczkowa * Jaskinia Kalacka * Jaskinia Kamienne Mleko * Jaskinia Kasprowa Niżnia * Jaskinia Kasprowa Średnia * Jaskinia Kasprowa Wyżnia * Jaskinia Kozia * Jaskinia Lejbusi ...
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Homo Heidelbergensis
''Homo heidelbergensis'' (also ''H. sapiens heidelbergensis''), sometimes called Heidelbergs, is an extinct species or subspecies of archaic human which existed during the Middle Pleistocene. It was subsumed as a subspecies of ''H. erectus'' in 1950 as ''H. e. heidelbergensis'', but towards the end of the century, it was more widely classified as its own species. It is debated whether or not to constrain ''H. heidelbergensis'' to only Europe or to also include African and Asian specimens, and this is further confounded by the type specimen (Mauer 1) being a jawbone, because jawbones feature few diagnostic traits and are generally missing among Middle Pleistocene specimens. Thus, it is debated if some of these specimens could be split off into their own species or a subspecies of ''H. erectus''. Because the classification is so disputed, the Middle Pleistocene is often called the "muddle in the middle." ''H. heidelbergensis'' is regarded as a chronospecies, evolving from an Africa ...
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Before Present
Before Present (BP) years, or "years before present", is a time scale used mainly in archaeology, geology and other scientific disciplines to specify when events occurred relative to the origin of practical radiocarbon dating in the 1950s. Because the "present" time changes, standard practice is to use 1 January 1950 as the commencement date (epoch) of the age scale. The abbreviation "BP" has been interpreted retrospectively as "Before Physics", which refers to the time before nuclear weapons testing artificially altered the proportion of the carbon isotopes in the atmosphere, which scientists must now account for. In a convention that is not always observed, many sources restrict the use of BP dates to those produced with radiocarbon dating; the alternative notation RCYBP stands for the explicit "radio carbon years before present". Usage The BP scale is sometimes used for dates established by means other than radiocarbon dating, such as stratigraphy. This usage differs from t ...
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Middle Ages
In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the post-classical period of global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern period. The medieval period is itself subdivided into the Early, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralized authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the 7th century, North Africa and the Middle East—most recently part of the Eastern Ro ...
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Lusatian Culture
The Lusatian culture existed in the later Bronze Age and early Iron Age (1700 BC – 500 BC) in most of what is now Poland and parts of the Czech Republic, Slovakia, eastern Germany and western Ukraine. It covers the Periods Montelius III (early Lusatian culture) to V of the Northern European chronological scheme. There were close contacts with the Nordic Bronze Age. Hallstatt and La Tène influences can also be seen particularly in ornaments (fibulae, pins) and weapons. Origins The Lusatian culture developed as the preceding Trzciniec culture experienced influences from the Tumulus culture of the Middle Bronze Age, essentially incorporating the local communities into the socio-political network of Iron Age Europe. It formed part of the Urnfield systems found from eastern France, southern Germany and Austria to Hungary and the Nordic Bronze Age in northwestern Germany and Scandinavia. It was followed by the Billendorf culture of the Early Iron Age in the West. In Poland, th ...
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Funnelbeaker Culture
The Funnel(-neck-)beaker culture, in short TRB or TBK (german: Trichter(-rand-)becherkultur, nl, Trechterbekercultuur; da, Tragtbægerkultur; ) was an archaeological culture in north-central Europe. It developed as a technological merger of local neolithic and mesolithic techno-complexes between the lower Elbe and middle Vistula rivers. These predecessors were the Lengyel-influenced Stroke-ornamented ware culture (STK) groups/Late Lengyel and Baden-Boleráz in the southeast, Rössen groups in the southwest and the Ertebølle-Ellerbek groups in the north. The TRB introduced farming and husbandry as a major source of food to the pottery-using hunter-gatherers north of this line. The TRB techno-complex is divided into a northern group including modern northern Germany and southern Scandinavia (TRB-N, roughly the area that previously belonged to the Ertebølle-Ellerbek complex), a western group in the Netherlands between the Zuiderzee and lower Elbe that originated in the Swifte ...
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Lengyel Culture
__NOTOC__ The Lengyel culture is an archaeological culture of the European Neolithic, centered on the Middle Danube in Central Europe. It flourished from 5000 to 4000 BC, ending with phase IV, e.g., in Bohemia represented by the ' Jordanow/Jordansmühler culture'. It is followed by the Funnelbeaker/TrB culture and the Baden culture. The eponymous type site is at Lengyel in Tolna county, Hungary. It was preceded by the Linear Pottery culture and succeeded by the Corded Ware culture. In its northern extent, overlapped the somewhat later but otherwise approximately contemporaneous Funnelbeaker culture. Also closely related are the Stroke-ornamented ware and Rössen cultures, adjacent to the north and west, respectively. Subgroups of the Lengyel horizon include the Austrian/Moravian Painted Ware I and II, Aichbühl, Jordanów/Jordanov/Jordansmühl, Schussenried, Gatersleben, etc. It is a wide interaction sphere or cultural horizon rather than an archaeological culture in the n ...
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Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It is divided into 16 administrative provinces called voivodeships, covering an area of . Poland has a population of over 38 million and is the fifth-most populous member state of the European Union. Warsaw is the nation's capital and largest metropolis. Other major cities include Kraków, Wrocław, Łódź, Poznań, Gdańsk, and Szczecin. Poland has a temperate transitional climate and its territory traverses the Central European Plain, extending from Baltic Sea in the north to Sudeten and Carpathian Mountains in the south. The longest Polish river is the Vistula, and Poland's highest point is Mount Rysy, situated in the Tatra mountain range of the Carpathians. The country is bordered by Lithuania and Russia to the northeast, Belarus and Ukraine to the east, Slovakia and the Czech Republic to the south, and Germany to the west. It also shares maritime boundaries with Denmark and Sweden. ...
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Würm Stage
The Würm is a river in Bavaria, Germany, right tributary of the Amper. The length of the river is , or including the ''Steinbach'', the main feed of Lake Starnberg. It drains the overflow from Lake Starnberg and flows swiftly through the villages of Gauting, Krailling, Planegg, Gräfelfing and Lochham as well as part of Munich (in the borough of Pasing) before joining, near Dachau, the Amper, which soon afterwards flows into the Isar and eventually flowing into the Danube. Although the Würm is not a very large river, it is well known as it gave its name to the Würm glaciation. A small man-made channel extracts water from the river at Pasing to feed the water features at Nymphenburg Palace, before flowing on to join the Isar at the public park Englischer Garten in Munich. See also *List of rivers of Bavaria A list of rivers of Bavaria, Germany: A * Aalbach *Abens * Ach * Afferbach * Affinger Bach * Ailsbach *Aisch * Aiterach *Alpbach *Alster * Altmühl *Alz * Amper * Anlau ...
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Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain shape, and c ...
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