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Isturitz And Oxocelhaya Caves
The Isturitz and Oxocelhaya caves (French: Grottes d'Isturitz et d'Oxocelhaya) are an important Paleolithic site where a Neanderthal mandible was found, as well as later modern human finds associated with the Aurignacian, Solutrean and Magdalenian. They also include cave paintings and bone flutes. The caves are located in the Gazetelu hill in the Arberoue Valley in the foothills of Pyrenees, in Lower Navarre, a traditional region of the department of Pyrénées-Atlantiques, southwestern France, part of the French Basque Country. The French government has classified the site as a ''Monument historique'' since 1953. Occupation by Neanderthal and Homo sapiens communities extends over a period from 80,000–10,000 years BP, and continued to be use (perhaps only for burials) until Roman times. The site is discussed within the context of Franco-Cantabrian prehistory, as among the easternmost decorated caves that extended along the Pyrenees and Cantabrian Mountains. Topography The ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Navarre
Lower Navarre ( eu, Nafarroa Beherea/Baxenabarre; Gascon/Bearnese: ''Navarra Baisha''; french: Basse-Navarre ; es, Baja Navarra) is a traditional region of the present-day French ''département'' of Pyrénées-Atlantiques. It corresponds to the northernmost ''merindad'' of the Kingdom of Navarre during the Middle Ages. After the Spanish conquest of Iberian Navarre (1512–24), this ''merindad'' was restored to the rule of the native king, Henry II. Its capitals were Saint-Jean-Pied-de-Port and Saint-Palais. In the extreme north there was the little sovereign Principality of Bidache, with an area of and a decreasing population of 44,450 (in 1901), 25,356 (in 1990). Although this denomination is not completely correct from the historical point of view, it is also known as ''Merindad de Ultrapuertos'' ("the regions beyond the mountain passes") by the southerners, and ''Deça-ports'' ("this side of the mountain passes") by the Gascon-speakers. Despite its lost administrative cohe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cantabrian Mountains
, etymology=Named after the Cantabri , photo=Cordillera Cantábrica vista desde el Castro Valnera.jpg , photo_caption=Cantabrian Mountains parallel to the Cantabrian Sea seen from Castro Valnera in an east-west direction. In the background, the Montaña Palentina (left) and the Picos de Europa (right) , country= Spain , subdivision1_type=Communities , subdivision1= , geology= Limestone , age= Carboniferous, Paleozoic, Mesozoic , orogeny= , borders_on= , area_km2= , length_km=300 , length_orientation=WE , width_km= 50 , width_orientation=NS , highest= Torre de Cerredo , elevation_m= 2648 , range_coordinates= , coordinates= , map_image=Cordillera Cantabrica.jpg , map_caption=Location of the Cantabrian Mountains in northern Spain , parent= The Cantabrian Mountains or Cantabrian Range ( es, Cordillera Cantábrica) are one of the main systems of mountain ranges in Spain. They stretch for over 300 km (180 miles) across northern Spain, from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stone Age Sites In France
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing rocks. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Homotherium
''Homotherium'', also known as the scimitar-toothed cat or scimitar cat, is an extinct genus of machairodontine saber-toothed predator, often termed scimitar-toothed cats, that inhabited North America, South America, Eurasia, and Africa during the Pliocene and Pleistocene epochs (4 mya – 12,000 years ago), existing for approximately . It became extinct in Africa some 1.5 million years ago. The most recent Eurasian remains, recovered from what is now the North Sea, have been dated to around 28,000 years BP. In South America it is only known from a few remains in the northern region (Venezuela), from the mid-Pleistocene. Taxonomy and distribution The name ''Homotherium'' (Greek: (, 'same') and (, 'beast')) was proposed by Emilio Fabrini (1890), without further explanation, for a new subgenus of ''Machairodus'', whose main distinguishing feature was the presence of a large diastema between the two inferior premolars. The lineage of ''Homotherium'' is estimated (based on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panthera Spelaea
''Panthera spelaea'', also known as the Eurasian cave lion, European cave lion or steppe lion, is an extinct ''Panthera'' species that most likely evolved in Europe after the third Cromerian interglacial stage, less than 600,000 years ago. Phylogenetic analysis of fossil bone samples revealed that it was highly distinct and genetically isolated from the modern lion (''Panthera leo'') occurring in Africa and Asia. Analysis of morphological differences and mitochondrial data support the taxonomic recognition of ''Panthera spelaea'' as a distinct species that genetically diverged from the lion about . Nuclear genomic evidence shows a more recent split approximately 500,000 years ago, with no subsequent interbreeding with the ancestors of the modern lion. The oldest known bone fragments were excavated in Yakutia and radiocarbon dated at least 62,400 years old. It became extinct about 13,000 years ago. Taxonomy ''Felis spelaea'' was the scientific name used by Georg August Goldfu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assegai
An assegai or assagai (Arabic ''az-zaġāyah'', Berber languages, Berber ''zaġāya'' "spear", French language, Old French ''azagaie'', Spanish ''azagaya'', Italian ''zagaglia'', Middle English ''lancegay'') is a pole weapon used for throwing, usually a light spear or javelin made up of a wooden handle and an iron tip. Area of use The use of various types of the assegai was widespread all over Africa and it was the most common weapon used before the introduction of firearms. The Zulu people, Zulu, Xhosa people, Xhosa and other Nguni people, Nguni tribes of South Africa were renowned for their use of the assegai. ''Iklwa'' Shaka of the Zulu people, Zulu invented a shorter stabbing spear with a two-foot (0.61 m) shaft and a larger, broader blade one foot (0.3 m) long. This weapon is otherwise known as the ''iklwa'' or ''ixwa'', after the sound that was heard as it was withdrawn from the victim's wound. The traditional spear was not abandoned, but was used to ranged we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Projectile Points
In North American archaeological terminology, a projectile point is an object that was hafted to a weapon that was capable of being thrown or projected, such as a javelin, dart, or arrow. They are thus different from weapons presumed to have been kept in the hand, such as knives, spears, axes, hammers, and maces. Stone tools, including projectile points, can survive for long periods, were often lost or discarded, and are relatively plentiful, especially at archaeological sites. They provide useful clues to the human past, including prehistoric trade. A distinctive form of point, identified though lithic analysis of the way it was made, is often a key diagnostic factor in identifying an archaeological industry or culture. Scientific techniques exist to track the specific kinds of rock or minerals that were used to make stone tools in various regions back to their original sources. As well as stone, projectile points were also made of worked wood, bone, antler, horn, or ivory ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Somerset
( en, All The People of Somerset) , locator_map = , coordinates = , region = South West England , established_date = Ancient , established_by = , preceded_by = , origin = , lord_lieutenant_office =Lord Lieutenant of Somerset , lord_lieutenant_name = Mohammed Saddiq , high_sheriff_office =High Sheriff of Somerset , high_sheriff_name = Mrs Mary-Clare Rodwell (2020–21) , area_total_km2 = 4171 , area_total_rank = 7th , ethnicity = 98.5% White , county_council = , unitary_council = , government = , joint_committees = , admin_hq = Taunton , area_council_km2 = 3451 , area_council_rank = 10th , iso_code = GB-SOM , ons_code = 40 , gss_code = , nuts_code = UKK23 , districts_map = , districts_list = County council area: , MPs = * Rebecca Pow (C) * Wera Hobhouse ( LD) * Liam Fox (C) * David Warburton (C) * Marcus Fysh (C) * Ian Liddell-Grainger (C) * James Heappey (C) * Jacob Rees-Mogg (C) * John Penrose (C) , police = Avon and Somerset Police ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gough's Cave
Gough's Cave ( ) is located in Cheddar Gorge on the Mendip Hills, in Cheddar, Somerset, England. The cave is deep and is long, and contains a variety of large chambers and rock formations. It contains the Cheddar Yeo, the largest underground river system in Britain. History The initial sections of the cave, previously known as Sand Hole, were accessible prior to the 19th century. Between 1892 and 1898 a retired sea captain, Richard Cox Gough, who lived in Lion House in Cheddar, found, excavated and opened to the public further areas of the cave, up to Diamond Chamber, which is the end of the show cave today. Electric lighting was installed in the show caves in 1899. – which also contains a detailed description of the cave. The cave is susceptible to flooding often lasting for up to 48 hours, however in the Great Flood of 1968 the flooding lasted for three days. The extensive flooded parts of the cave system were found and explored between 1985 and 1990. Human remains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcite
Calcite is a Carbonate minerals, carbonate mineral and the most stable Polymorphism (materials science), polymorph of calcium carbonate (CaCO3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on the Mohs scale of mineral hardness, based on Scratch hardness, scratch hardness comparison. Large calcite crystals are used in optical equipment, and limestone composed mostly of calcite has numerous uses. Other polymorphs of calcium carbonate are the minerals aragonite and vaterite. Aragonite will change to calcite over timescales of days or less at temperatures exceeding 300 °C, and vaterite is even less stable. Etymology Calcite is derived from the German ''Calcit'', a term from the 19th century that came from the Latin word for Lime (material), lime, ''calx'' (genitive calcis) with the suffix "-ite" used to name minerals. It is thus etymologically related to chalk. When applied by archaeology, archaeologists and stone trade pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bidouze
The Bidouze is a left tributary of the Adour, in the French Basque Country (Pyrénées-Atlantiques), in the Southwest of France. It is long. Geography The Bidouze rises at the base of ''Eltzarreko Ordokia'' in the Arbailles massif. It drains the east of the Lower Navarre, crossing Saint-Palais (the main town). Then it flows into the Adour in Guiche. Bidouze is one of the reference rivers of minor water volume meandering across the Northern Basque territory along with the Nive and Saison. Name The name of the Bidouze can be compared with other Aquitanian placenames as ''Vidouze'' (in the northeast of the Hautes-Pyrénées), ''Bedous'' or ''Bidos'' (both in the Aspe Valley)… Départements and towns * Pyrénées-Atlantiques: Larceveau, Saint-Palais, Came, Bidache, Guiche. Main tributaries * (L) ''Hoztako ur handia'', from Hosta * (L) ''Laminosina'', from Ibarrolle * (L) ''Artikaiteko erreka'', from Utziate * (R) ''Babatzeko erreka'', from Juxue * (R) ''Izpatxur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hasparren
Hasparren (; eu, Hazparne) is a commune in the Pyrénées-Atlantiques department in south-western France. A resident of Hasparren is known as a 'Hazpandar'. Geography Location It's a ''commune fait partie'' of the Basque Province of Labourd. The Côte Basque (''Euskal Kostaldea)'', is 25 km to the west. Access Hasparren is located on the route D 10, between La Bastide-Clairence and Cambo-les-Bains, at the crossroads with D 21, D 22 and D 23. It has got access to autoroute A 64, exit 4 near Briscous. Hydrography The rivers Ardanabia and Suhihandia (a tributary of the Aran), flow through the commune. Locations Eight settlements compose the Commune of Hasparren: * Labiri ; * Elizaberri ; * la Coste (la Côte sur les cartes IGN) ; * Peña (Pegna sur les cartes IGN) ; * Minhotz ; * la Ville ; * Urcuray ; * Bas-Labiri et Zelhaia . Toponymy Ancient attestations It is attestested with various words: ''Hesperenne'' (1247 in Cartulaire de Bayonne) ''Sant ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
BisonsPoursuivisParDesLions.jpg "Click for more on -> Panthera Spelaea")
