Literature DB >> 17832349

Paleohydrology of late pleistocene superflooding, altay mountains, siberia.

V R Baker, G Benito, A N Rudoy.   

Abstract

Cataclysmic flooding is a geomorphological process of planetary significance. Landforms of flood origin resulted from late Pleistocene ice-dammed lake failures in the Altay Mountains of south-central Siberia. Peak paleoflows, which exceeded 18 x 10(6) cubic meters per second, are comparable to the largest known terrestrial discharges of freshwater and show a hydrological scaling relation to floods generated by catastrophic dam failures. These seem to have been Earth's greatest floods, based on a variety of reconstructed paleohydraulic parameters.

Year:  1993        PMID: 17832349     DOI: 10.1126/science.259.5093.348

Source DB:  PubMed          Journal:  Science        ISSN: 0036-8075            Impact factor:   47.728


  4 in total

1.  Erosion during extreme flood events dominates Holocene canyon evolution in northeast Iceland.

Authors:  Edwin R C Baynes; Mikaël Attal; Samuel Niedermann; Linda A Kirstein; Andrew J Dugmore; Mark Naylor
Journal:  Proc Natl Acad Sci U S A       Date:  2015-02-09       Impact factor: 11.205

2.  Fluvial geomorphology on Earth-like planetary surfaces: A review.

Authors:  Victor R Baker; Christopher W Hamilton; Devon M Burr; Virginia C Gulick; Goro Komatsu; Wei Luo; James W Rice; J A P Rodriguez
Journal:  Geomorphology (Amst)       Date:  2015-05-16       Impact factor: 4.139

3.  River-margin habitat of Ardipithecus ramidus at Aramis, Ethiopia 4.4 million years ago.

Authors:  M Royhan Gani; Nahid D Gani
Journal:  Nat Commun       Date:  2011-12-20       Impact factor: 14.919

4.  Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community.

Authors:  Vitaly V Kadnikov; Andrey V Mardanov; Denis A Ivasenko; Dmitry V Antsiferov; Alexey V Beletsky; Olga V Karnachuk; Nikolay V Ravin
Journal:  Sci Rep       Date:  2018-04-30       Impact factor: 4.379

  4 in total

北京卡尤迪生物科技股份有限公司 © 2022-2023.