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Kůlna Cave
Kůlna Cave
Photo: Doronenko
Permission: Creative Commons Attribution-Share Alike 3.0 Unported license
Kůlna Cave forms a massive tunnel on the eastern slope of the Sloupské Valley. The first archaeological excavation was carried out in 1880 by J. Wankel and a year later M. Kříž began extensive excavations, which lasted until 1886. The discovery layer of the Middle Paleolithic was first identified by his successor Jan Knies. In 1943-45 the Nazis converted the entire cave into an aircraft factory. When K. Valoch prepared the terrain for systematic research here in 1959, he had the concrete floor blasted off the entire cave.Text above: Anthropos Pavilion/Moravian Museum, Brno, Czech Republic and Wikipedia
It turned out that the lower Middle Palaeolithic layers are almost untouched by older works, albeit interspersed with natural processes. Under the cave there is a system of deep cross chasms, into which the Sloupský river flowed sometimes.
The researches of the Anthropos Institute in the years 1961-1976 brought not only extensive collections of Middle Palaeolithic tools and at the same time the oldest evidence of the settlement of the Moravian Karst, but also the most numerous remains of Neanderthal man in the Czech Republic. The collaboration of many natural scientists has brought a lot of ecological data.
The oldest settlements fall at the end of the penultimate (Risian) ice age, followed by a culture called Taubachien ( Neanderthal, 130 000 to 80 000 BP) with small-scale tools using mostly pebbles as cores, in the warm interglacial. The remnants of the Neanderthals (skull fragment, upper jaw, and 3 milk teeth) come from layer 7a, which belongs to the Micoquian.
Location: 49° 24′ 30.81″ N, 16° 44′ 19.79″ E
Kůlna Cave (near Sloup, Blansko DIstrict):
1. Maxila fragment.
2. Right parietal bone.
3. Milk teeth.
Švédův stůl Cave :
4. Lower jaw.
Photo: Zde
Permission: Creative Commons Attribution-Share Alike 4.0 International license.
Source: From a Temporary exhibition 'Welcome to the Neandertals' in the Anthropos Pavilon, Brno.
Kůlna Cave
a, b – locality of the cave
c – entrance into the cave, the so-called southern entrance
d – schematic profile of the Middle & Upper Palaeolithic layers and the cave area with designated sectors.
Digitised and compiled by P. Neruda.
Valoch (1988)
Proximal source and text: Nerudová et al. (2014)
Kůlna Cave is located 45 km from Brno, on the northern margin of the Moravian Karst. It belongs to the nearby Sloup-Sosuvka cave system, in which Sloupský potok Brook that drains the area currently vanishes.Kůlna is a tunnel-shaped cavern with two entrances, a smaller northern and a large SSW-oriented portal entrance. The cavern is 91 m long, the maximum width is 25 m, and the height is 8 m.Text above: Neruda (2013)
Stratigraphy in the entrance part of the cave, sector C.
6a to 9: Micoquian
10 to 12a: Taubachian
Photo and text: Valoch (1988)
Proximal source: Neruda (2013)
Stratigraphy in the central part of the cave, sector G1 .
6: Gravettian/Magdalenian
6a to 7e: Micoquian
Photo and text: Valoch (1988)
Proximal source: Neruda (2013)
Ideal stratigraphic sequence of Kůlna Cave.
Photo: Valoch (1989)
Proximal source: Neruda et al. (2015)
Points and cuspidate (terminating in a point) sidescrapers.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Points and cuspidate (terminating in a point) sidescrapers.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Large transverse sidescrapers.
( Transverse in this sense means at right angles to the general shape of the tool, where a single retouched edge lies opposite the butt - Don )
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Additional text: Klein (2009)
On numerous broken bones we can see grooves caused by stone tools, probably during quartering and carving of the downed animal or scraping of bones.
In other objects where grooves cannot be explained by some practical activity, we can consider motifs resulting from random or symbolic thought processes.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Additional text: https://www.ginellames.fr/us/tailler_le_silex/bases_de_la_taille/02_matieres.php
Reindeer antler modified for use, perhaps as a hammer.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Retouchers from mammoth tusk.
Left: a thin, convex-concave layer of ivory glued together from four parts. The maximum preserved length and width are 125.3 mm and 44.2 mm, respectively. The thickness of the layer varies from 1.71 to 3.35 mm. Layer 7a1, G2. Micoquian.
Right: a layer of mammoth ivory, with a maximum length of 157 mm and 52.8 mm width. The thickness of the layer varies between 4.1 mm and 4.7 mm. Layer 7a1, sector G3, Micoquian.
Photo: K. Jursa
Source and text: Neruda et al. (2015)
Handaxe.
Photo: Don Hitchcock 2018
Source and text: Facsimile, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Discoid and prismatic cores.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Cores and a handaxe.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Tools made of rock crystal, or crystalline quartz.
Rock crystal is not a good material for tools, but it is beautiful. It is very difficult to work with, rock crystal produces chips that cannot be controlled easily and often make step fractures. The Neanderthals of l'Abri des Merveilles at Castel-Merle - Vallon des Roches also made tools of rock crystal.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Additional text: https://www.ginellames.fr/us/tailler_le_silex/bases_de_la_taille/02_matieres.php
Taubachien tools (and cores below) are typically small in size and utilise a diverse range of raw materials.
From layer 11 of the Riss-Würm interglacial, 126 000 BP - 100 000 BP.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Additional text: Wikipedia
Taubachien tools (and cores right hand image) are typically small in size and utilise a diverse range of raw materials.
From layer 11 of the Riss-Würm interglacial, 126 000 BP - 100 000 BP.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Additional text: Wikipedia
Chipped pebble.
( this may have been used as a knapping tool - Don )
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Fractured, healed, penile bones of cave bears.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
The oldest traces of settlement in the Moravian Karst are Levallois flakes, a few retouched tools and cores from layer 14, dated to the end of Riss glaciation, about 130 000 BP.
Photo: Don Hitchcock 2018
Source and text: Originals, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Model of Kůlna Cave in the Moravian Karst. Below, the profile of archaeological layers revealed in the cave in 1961 - 1976.
Photo: Don Hitchcock 2018
Model and graphics design: Unknown
Source and text: Diorama, Anthropos Pavilion/Moravian Museum, Brno, Czech Republic
Kůlna Cave | ||||||
---|---|---|---|---|---|---|
Layer | Age | |||||
1,2 | Neolithic 6 000 BP | |||||
3,4 | Epi-Magdalenian (Azilian) 11 000 BP | |||||
5,6 | Magdalenian 12 000 BP - 13 000 BP | |||||
6b | Gravettian 22 000 BP | |||||
6c | Micoquian 40 000 BP - 45 000 BP | |||||
7a | Micoquian 50 000 BP | |||||
7b | Micoquian 50 000 BP | |||||
7c,d, 8a | Micoquian 50 000 BP | |||||
8b,9a | Micoquian 60 000 BP | |||||
9b | Micoquian 70 000 BP | |||||
10, 11a-d | Taubachian 100 000 BP | |||||
12, 13 Taubachian | 110 000 BP | |||||
14 | Old Middle Palaeolithic 120 000 BP |
Layers and ages at Kůlna Cave.
Extra data on ages from Neruda, Nerudová (2013)
( note that there are minor inconsistencies with layer contents and ages between this table from the Brno Museum and the data from Neruda, Nerudová (2013) - Don )
Upper Palaeolithic of Kůlna Cave
Kůlna Cave, Magdalenian, circa 14 000 BP.
( Double bevel spear points such as these had a very long life in the tool kit of hunter gatherers, and are known since at least the Gravettian.
A double bevel attachment takes more time and skill to make than a single bevel, but it is less likely to fail at the moment of impact than the single bevel - Don )
Photo: Don Hitchcock 2008
Source: Museum of Natural History, Vienna
Near Kůlna Cave is Žitný Cave, another Magdalenian site. Shown here are some needles and a carved rod.
Circa 14 000 BP.
Photo: Don Hitchcock 2008
Source: Museum of Natural History, Vienna, Naturhistorisches Museum Wien
References
- Klein R., 2009: The Human Career: Human Biological and Cultural Origins, Third Edition, University of Chicago Press, 22 Apr 2009 - Social Science - 1024 pages
- Kozlowski S. et al., 2012: New information from Maszycka Cave and the Late Glacial recolonisation of Central Europe, Quaternary International, 272-273 (2012) 288e296
- Kozlowski S., Lozek V., Vlcek E., 2013: Hunters between East and West: The Paleolithic of Moravia, Springer Science & Business Media, 29 Jun 2013 - Social Science - 311 pages
- Kříž, M., 1909: Die Schwedentischgrotte bei Ochos in Mähren und Rzehaks Bericht über homo primigenius Wilseri. Verhandlungen der k. k., Geologischen Reichsanstalt, Nr. 10, 217–233.
- Neruda P., Nerudová Z., 2013: New data from Micoquian layers of the Kůlna Cave (Czech Republic),Quaternary International (2013), http://dx.doi.org/10.1016/j.quaint.2013.10.015
- Neruda P., Lázničková-Galetová M., 2015: Retouchers from mammoth tusks in the Middle Palaeolithic. a case study from Kůlna Cave layer 7a1 (Czech Republic),Retouching the Palaeolithic: Becoming Human and the Origins of Bone Tool Technology, The Origins of Bone Tool Technologies, Retouching the Palaeolithic International Workshop was held from 21-23 October 2015 at Hannover.
- Nerudová Z., Nývltová Fišáková M., Míková J., 2014: Palaeoenvironmental analyses of animal remains from the Kůlna Cave (Moravian Karst, Czech Republic), Quartär 61 (2014) : 147-157, doi: 10.7485/QU61_08
- Oliva M., 2017: Švédův stůl v Moravském krasu Geschichte des Neandertalerkiefers aus der Švédův stůl-höhle (Schwedentischgrotte) im Mährischen Karst, Anthropos, ISSN 0323-0570 Acta Mus. Moraviae, Sci. soc. CII: 1, 3–16, 2017
- Svoboda J., Sachse-Kozlowska E., 1995: Magdalenian family from the Maszycka Cave. In: Kozlowski, et al. (Eds.), pp. 115-205.
- Valoch K., 1988: Die Erforschung der Kulna-Höhle 1961-1976. In: Anthropos, vol. 24 (N.S. 16). Moravské zemské muzeum, Brno.