Middle and Late Pleistocene glaciations in the southwestern Pamir and their effects on topography [Topography of the SW Pamir shaped by middle-late Pleistocene glaciation]

Stübner, Konstanze; Grin, Elena; Hidy, Alan J.; Schaller, Mirjam; Gold, Ryan D.; Ratschbacher, Lothar; Ehlers, Todd

doi:10.1016/j.epsl.2017.03.012

Title: Middle and Late Pleistocene glaciations in the southwestern Pamir and their effects on topography [Topography of the SW Pamir shaped by middle-late Pleistocene glaciation]

Journal Article · Mon Mar 27 00:00:00 EDT 2017 · Earth and Planetary Science Letters

DOI:https://doi.org/10.1016/j.epsl.2017.03.012· OSTI ID:1351141

^[1]; Grin, Elena ^[1]; Hidy, Alan J. ^[2]; Schaller, Mirjam ^[1]; Gold, Ryan D. ^[3]; Ratschbacher, Lothar ^[4]; Ehlers, Todd ^[1]

Eberhard Karls Univ. Tubingen, Tubingen (Germany)
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
U.S. Geological Survey, Golden, CO (United States)
Technische Univ. Bergakademie Freiberg, Freiberg (Germany)

Glacial chronologies provide insight into the evolution of paleo-landscapes, paleoclimate, topography, and the erosion processes that shape mountain ranges. In the Pamir of Central Asia, glacial morphologies and deposits indicate extensive past glaciations, whose timing and extent remain poorly constrained. Geomorphic data and 15 new ¹⁰Be exposure ages from moraine boulders and roches moutonnées in the southwestern Pamir document multiple Pleistocene glacial stages. The oldest exposure ages, View the MathML source113 ± 10ka, underestimate the age of the earliest preserved glacial advance and imply that the modern relief of the southwestern Pamir (peaks at ~5000–6000 m a.s.l.; valleys at ~2000–3000 m a.s.l.) already existed in the late Middle Pleistocene. Younger exposure ages (~40–80 ka, ~30 ka) complement the existing Central Asian glacial chronology and reflect successively less extensive Late Pleistocene glaciations. The topography of the Pamir and the glacial chronologies suggest that, in the Middle Pleistocene, an ice cap or ice field occupied the eastern Pamir high-altitude plateau, whereas westward flowing valley glaciers incised the southwestern Pamir. Since the Late Pleistocene deglaciation, the rivers of the southwestern Pamir adjusted to the glacially shaped landscape. As a result, localized rapid fluvial incision and drainage network reorganization reflect the transient nature of the deglaciated landscape.

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Research Organization:: Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)

Sponsoring Organization:: USDOE

Grant/Contract Number:: AC52-07NA27344

OSTI ID:: 1351141

Alternate ID(s):: OSTI ID: 1396588

Report Number(s):: LLNL-JRNL-700769; TRN: US1700577

Journal Information:: Earth and Planetary Science Letters, Vol. 466, Issue C; ISSN 0012-821X

Publisher:: ElsevierCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 9 works

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58 GEOSCIENCES
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Title: Middle and Late Pleistocene glaciations in the southwestern Pamir and their effects on topography [Topography of the SW Pamir shaped by middle-late Pleistocene glaciation]

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