"Botovskaya Cave is a typical example of a two-dimensional maze with a total length of explored passages exceeding 60 km, which represents the longest limestone cave system in the Russian Federation. The clastic cave sediments filling the cave passages differ in both mineral and mineral magnetic properties and were deposited under different hydrological conditions. The older portion of the clastic cave fills was derived from overlying sandstones, whereas the properties of younger cave sediments show closer affinity to the soils and weathering products originating on the plateau above the cave. The cave sediments underwent repeated periods of deposition and erosion during the Tertiary (?) and Pleistocene. The last catastrophic erosion event occurred in the cave more than 350 ka based on flowstone dating. Water seeping through the overlying sandstone body causes collapses of sandstone slabs from the cave passage ceilings, forming the youngest portion of the clastic cave fills."@en . . "Chadima, Martin" . "Botovskaya Cave is a typical example of a two-dimensional maze with a total length of explored passages exceeding 60 km, which represents the longest limestone cave system in the Russian Federation. The clastic cave sediments filling the cave passages differ in both mineral and mineral magnetic properties and were deposited under different hydrological conditions. The older portion of the clastic cave fills was derived from overlying sandstones, whereas the properties of younger cave sediments show closer affinity to the soils and weathering products originating on the plateau above the cave. The cave sediments underwent repeated periods of deposition and erosion during the Tertiary (?) and Pleistocene. The last catastrophic erosion event occurred in the cave more than 350 ka based on flowstone dating. Water seeping through the overlying sandstone body causes collapses of sandstone slabs from the cave passage ceilings, forming the youngest portion of the clastic cave fills." . "Lis\u00E1, Lenka" . . "Hercman, H." . "Klastick\u00E9 jeskynn\u00ED sedimenty v Botovsk\u00E9 jeskyni (V\u00FDchodn\u00ED Sibi\u0159, Rusko)"@cs . "RIV/67985831:_____/08:00322272" . . . . "3"^^ . "3" . "Kadlec, Jaroslav" . "[EED064FF1DE5]" . . . "Journal of Cave and Karst Studies" . . . . "Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation)"@en . . "Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation)" . "cave sediments; mineral magnetism; Botovskaya Cave"@en . "6"^^ . . . "Klastick\u00E9 sedimenty v Botovsk\u00E9 jeskyni se ukl\u00E1daly ve dvou obdob\u00EDch, jak bylo zji\u0161t\u011Bno pomoc\u00ED magneto-mineralogick\u00FDch a mineralogick\u00FDch metod. Zdrojem star\u0161\u00EDch sediment\u016F jsou p\u00EDskovce, tvo\u0159\u00EDc\u00ED podlo\u017E\u00ED i nadlo\u017E\u00ED zkrasov\u011Bl\u00FDch v\u00E1penc\u016F. Zdrojem mlad\u0161\u00EDch sediment\u016F jsou pedogenez\u00ED posti\u017Een\u00E9 produkty zv\u011Btr\u00E1v\u00E1n\u00ED, p\u0159em\u00EDst\u011Bn\u00E9 do podzem\u00ED z povrchu nad jeskynn\u00EDm syst\u00E9mem."@cs . . "Z(AV0Z30130516)" . . "Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation)"@en . "Oberh\u00E4nsli, H." . "US - Spojen\u00E9 st\u00E1ty americk\u00E9" . "000263275600002" . . "1090-6924" . "Klastick\u00E9 jeskynn\u00ED sedimenty v Botovsk\u00E9 jeskyni (V\u00FDchodn\u00ED Sibi\u0159, Rusko)"@cs . "70" . "14"^^ . . "RIV/67985831:_____/08:00322272!RIV09-AV0-67985831" . "360110" . "Osintsev, A." . "Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation)" .