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Grottes de roumanie
Year: 1961 Publisher: Bucarest : Meridiens,

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From stars to stalagmites : how everything connects
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ISBN: 1280669314 9786613646248 9814324981 9789814324984 9789814324977 9814324973 9781280669316 6613646245 Year: 2012 Publisher: Singapore : World Scientific Pub. Co.,

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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


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Han-sur-Lesse en zijn grotten : De 100 mooiste foto's van de geheime Lesse
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ISBN: 2870886438 9782870886434 Year: 1989 Publisher: Brussel Didier Hatier


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High Resolution Palaeoclimatic Changes in Selected Sectors of the Indian Himalaya by Using Speleothems : Past Climatic Changes Using Cave Structures
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ISBN: 3319735977 3319735969 Year: 2018 Publisher: Cham : Springer International Publishing : Imprint: Springer,

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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.

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