爱社交
发表于 2025-3-28 17:58:18
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stress-test
发表于 2025-3-28 18:55:49
Outline of Geology and Cenozoic Evolution of Slovakiazoic Basin system in the central and southern parts. The Western Carpathians are an integral part of the northern branch of the Carpathian arc and the whole European Alpine orogenic system, which was formed by the closure of the Tethys and Alpine Atlantic oceans during the Mesozoic and Cenozoic time
animated
发表于 2025-3-29 02:16:54
Climate in the Past and Present in the Slovak Landscapes—The Central European Contextom the Mesozoic Era to the present. The climate for the earliest period can only be reconstructed in the broadest terms. The level of detail possible increases as we approach to the period of the instrumental observations. The regular systematic meteorological measurements began in Slovakia in the m
innovation
发表于 2025-3-29 03:29:55
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Ligneous
发表于 2025-3-29 09:28:42
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确定方向
发表于 2025-3-29 12:13:07
The Longest and the Most Symmetrical Mountain Ridge of Slovakia—Low Tatra Mts.mately 1,240 km. and culminates in Mt. Ďumbier (2,043 m a.s.l.). As a geomorphological unit of the Inner Western Carpathians, the Low Tatra belong to the Fatra–Tatra region. In terms of the geological structure, it belongs to two different units, the structure of which also conditioned their geomorp
vertebrate
发表于 2025-3-29 18:24:34
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