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Feynman once selected, as the single most important statement in science, that everything is made of atoms. It follows that the properties of everything depend on how these atoms are joined together, giving rise to the vast field we know of today as chemistry. In this unique book specifically written to bridge the gap between chemistry and the layman, Braterman has put together a series of linked essays on chemistry related themes that are particularly engaging. The book begins with the age of the earth, and concludes with the life cycle of stars. In between, there are atoms old and new, the o
Science --- Stars. --- Stalactites and stalagmites. --- Stalagmites --- Speleothems --- Sidereal system --- Galaxies --- Circumstellar matter --- Science and society --- Sociology of science --- Social aspects.
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Guides de voyages --- Namen (provincie) --- Namur (province) --- Reisgidsen --- Caves --- Stalactites and stalagmites --- Geology --- Geognosy --- Geoscience --- Earth sciences --- Natural history --- Stalagmites --- Speleothems --- Caverns --- Grottoes --- Rock shelters --- Rockshelters --- Landforms --- Speleology --- Han-sur-Lesse (Belgium) --- Han (Namur, Belgium) --- Han'Lesse (Belgium) --- Han-sur-Lesse
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This thesis encompasses a study of past precipitation patterns based on six cave stalagmites from different parts of the Indian Himalaya. This is the first speleothem study in the Indian Himalaya that shows a direct relationship between past precipitation and the collapse of civilization. The stalagmites examined were KL-3 from Jammu and Kashmir; TCS and BR-1 from Himachal Pradesh; and DH-1, SA-1 and CH-1 from Uttarakhand. Based on the high-resolution palaeoclimatic reconstruction (35 U/th dates, 5 AMS dates, 1,500 samples for δ18O and δ13C values) obtained for the duration of the Pleistocene–Holocene transition (16.2–9.5 ka BP) and Mid-Holocene–Present (ca. 4.0 ka BP–Present), three major events were identified, namely the Older Dryas (OD), Bølling–Allerød (BA) period and Younger Dryas (YD) at ca. 14.3–13.9, 13.9–12.7 and 12.7–12.2 ka BP, respectively. The study showed a gradual reduction in the precipitation from 4 ka BP onwards for about a millennium with a peak arid period between 3.2 and 3.1 ka BP. According to the findings, the LIA (Little Ice Age) covers a time span from 1622–1820 AD, during which the climate was wetter than that in the post-LIA period (1820–1950 AD). In addition, this thesis supports the assumption that the WDs (Western Disturbances) contribute significantly to the total rainfall in the Himalaya region.
Speleothems --- Stalactites and stalagmites --- Stalagmites --- Cave formations --- Drip stones --- Dripstones --- Flowstones --- Formations (Speleology) --- Himalaya Mountains. --- Earth sciences. --- Climatology. --- Paleontology. --- Sedimentology. --- Hydrogeology. --- Earth Sciences. --- Caves --- Hydraulic engineering. --- Paleontology . --- Fossilogy --- Fossilology --- Palaeontology --- Paleontology, Zoological --- Paleozoology --- Historical geology --- Zoology --- Fossils --- Prehistoric animals in motion pictures --- Engineering, Hydraulic --- Engineering --- Fluid mechanics --- Hydraulics --- Shore protection --- Petrology --- Climate --- Climate science --- Climate sciences --- Science of climate --- Atmospheric science --- Geohydrology --- Geology --- Hydrology --- Groundwater
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