By I. Peter Martini, V. R. Baker, Guillermina Garzón
The purpose of this book is the knowledge of huge floods and their influence at the Earth's floor. the main targets are: 1) to take a re-examination at what constitutes a megaflood that the main of uniformitarianism is at a few loss to give an explanation for and a couple of) to attempt to figure out what may well take place in such huge floods by means of studying those who ensue in entrance of glaciers, in alluvial-fans and in alluvial valleys. the goods of those floods are awarded when it comes to sedimentary deposits, erosional beneficial properties and harm to human actions. the quantity bears out the concept sedimentological research could be a strong device, not just for reconstructing strategies that experience acted on old landscapes, but in addition as a method for probability evaluation of convinced afflicted parts. for that reason, this quantity is of curiosity not just to sedimentologists/gemorphlogists, but in addition to engineers, landuse planners and someone drawn to the interrelation among people and the surroundings. when you are a member of the foreign organization of Sedimentologists, for buying info, please see: http://www.iasnet.org/publications/details.asp?code=SP32
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Extra resources for Flood and Megaflood Processes and Deposits: Recent and Ancient Examples (IAS Special Publication 32)
Sample text
Taken IFAC02 9/12/08 4:25 PM Page 25 Late Quaternary catastrophic flooding, Altai Mountains, Siberia together this evidence is interpreted to represent unsteady downstream migration of two-dimensional dunes, about 2 m in height in an aggradational setting. As well as the dunefields described by Carling (1996a), additional dunefields were located in 1999 and 2000. 51″) within minor sidevalleys close to the Chuja gorge. At an altitude of 1710 m, these bedforms indicate strong currents moving towards the lake outlet into the Chuja valley.
A. (1977) Dimensions and characteristics of Late Pleistocene glaciation of the Altay Mountains. Trans. Glaciol. Stud. Chron. 29, 203–210. A. (1997) Some questions of the genesis problem of the high Altai terraces. Questions Geogr. Siberia 22, 9–18. Plink-Björklund, P. & Ronnert, L. (1999) Depositional processes and internal architecture of Late Weichselian ice-margin submarine fan and delta settings, Swedish west coast. Sedimentology 46, 215–234. A. (1942) Middle Katun valley terrace. In: Investigation and Exploration of the Productive Force of Siberia, pp.
In each example the contact is distinct and unconformable. Consequently, the bar sediments must pre-date the terrace sequences. 7 ka). This layer is overlain by a 3-m to 10-m thickness of cobbles with a distinctive cream-coloured (Munsell 10 YR 8/2) silt matrix. Above is the rest of the terrace succession. This has not been mapped in detail but consists of trough cross-bedded braided river deposits, conformably and unconformably interspersed with several decametres of very poorly sorted, coarse gravel beds, which include numerous boulders up to 2 m in diameter.
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