Carpathians in the context of "Polish–Soviet border agreement of August 1945"

In archaeogenetics, western hunter-gatherer (WHG, also known as west European hunter-gatherer, western European hunter-gatherer or Oberkassel cluster) (c. 15,000~5,000 BP) is a distinct ancestral component of modern Europeans, representing descent from a population of Mesolithic hunter-gatherers who scattered over western, southern and central Europe, from the British Isles in the west to the Carpathians in the east, following the retreat of the ice sheet of the Last Glacial Maximum. It is closely associated and sometimes considered synonymous with the concept of the Villabruna cluster, named after the Ripari Villabruna cave specimen in Italy, known from the terminal Pleistocene of Europe, which is largely ancestral to later WHG populations.

WHGs share a closer genetic relationship to ancient and modern peoples in the Middle East and the Caucasus than earlier European hunter-gatherers. Their precise relationships to other groups are somewhat obscure, with the origin of the Villabruna cluster likely somewhere in the vicinity of the Balkans. The Villabruna cluster (which is associated with the Epigravettian and other related archaeological cultures) had expanded into the Italian and Iberian Peninsulas by approximately 19,000 years ago, with the WHG cluster subsequently expanding across Western Europe at the end of the Pleistocene around 14-12,000 years ago, largely replacing the Magdalenian peoples who previously dominated the region. These Magdalenian peoples largely descended from earlier Western European Cro-Magnon groups that had arrived in the region over 30,000 years ago, prior to the Last Glacial Maximum.

Flysch (/flɪʃ/) is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians.

The Tatra Mountains (pronounced), Tatras (Tatry either in Slovak (pronounced [ˈtatri] ) or in Polish (pronounced [ˈtatrɨ]) - plurale tantum), are a series of mountains within the Western Carpathians that form a natural border between Slovakia and Poland. They are the highest mountains in the Carpathians. The Tatras are distinct from the Low Tatras (Slovak: Nízke Tatry), a separate Slovak mountain range further south.

The Tatra Mountains occupy an area of 785 square kilometres (303 sq mi), of which about 610 square kilometres (236 sq mi) (77.7%) lie within Slovakia and about 175 square kilometres (68 sq mi) (22.3%) within Poland. The highest peak, called Gerlachovský štít, at 2,655 metres (8,711 feet), is located north of Poprad, entirely in Slovakia. The highest point in Poland, Rysy, at 2,500 metres (8,200 ft), is located southeast of Zakopane, on the border with Slovakia.

The Paratethys Sea, Paratethys Ocean, Paratethys realm or just Paratethys (meaning "beside Tethys"), was a large shallow inland sea that covered much of mainland Europe and parts of western Asia during the middle to late Cenozoic, from the late Paleogene to the late Neogene, and is regarded as the largest inland sea in history. At its greatest extent, it stretched from the region north of the Alps over Central Europe to the Aral Sea in Central Asia.

Paratethys formed about 34 Mya (million years ago) at the beginning of the Oligocene epoch, when the northern region of the Tethys Ocean (Peri-Tethys) was separated from the Mediterranean region of the Tethys realm due to the formation of the Alps, Carpathians, Dinarides, Taurus and Elburz mountains. Paratethys was at times reconnected with the Tethys or its successors (the Mediterranean Sea or the Indian Ocean) during the Oligocene and the early and middle Miocene times, but at the onset of the late Miocene epoch, the tectonically trapped sea turned into a megalake from the eastern Alps to what is now Kazakhstan. From the Pliocene epoch onward (after 5 million years ago), Paratethys became progressively shallower. Today's Black Sea, Caspian Sea, and Aral Sea are remnants of the Paratethys Sea.

The Przeworsk culture (Polish pronunciation: [ˈpʂɛvɔrsk]) was an Iron Age material culture in the region of what is now Poland, that dates from the 3rd century BC to the 5th century AD. It takes its name from the town Przeworsk, near the village where the first artifacts were identified.

In its earliest form it was located in what is now central and southern Poland, in the upper Oder and Vistula basins. It later spread southwards, beyond the Carpathians, towards the headwaters of the Tisza river, and eastwards, past the Vistula, and towards the headwaters of the Dniester.

The Vienna Basin (German: Wiener Becken, Czech: Vídeňská pánev, Slovak: Viedenská kotlina, Hungarian: Bécsi-medence) is a geologically young tectonic burial basin and sedimentary basin in the seam area between the Alps, the Carpathians and the Pannonian Plain. Although it topographically separates the Alps from the Western Carpathians, it connects them geologically via corresponding rocks underground.