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Your Guide to Kyrgyzstan s Alpine Ala Kul Lake Hiking Trail

Your Guide to Kyrgyzstan s Alpine Ala Kul Lake Hiking Trail
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Your Guide to Kyrgyzstan s Alpine Ala Kul Lake Hiking Trail

Your Guide to Kyrgyzstan s Alpine Ala Kul Lake Hiking Trail
theroanokestar.com - get the latest breaking news, showbiz & celebrity photos, sport news & rumours, viral videos and top stories from theroanokestar.com Daily Mail and Mail on Sunday newspapers.

Impact of Quaternary Glaciations on Denudation Rates in North Pamir—Ti by Anna Kudriavtseva, Alexandru T Codilean et al

We explore the spatial and temporal variations in denudation rates in the northern Pamir Tian Shan region using 10Be-derived denudation rates from modern (n = 110) and buried sediment (2.0–2.7 Ma; n = 3), and long-term exhumation rates from published apatite fission track (AFT; n = 705) and apatite (U-Th-Sm)/He (AHe; n = 211) thermochronology. We found moderate correlations between denudation rates and topographic metrics and weak correlations between denudation rates and annual rainfall, highlighting complex linkages among tectonics, climate, and surface processes that vary locally. The 10Be data show a spatial trend of decreasing modern denudation rates from west to east, suggesting that deformation and precipitation control denudation in the northern Pamir and western Tian Shan. Farther east, the denudational response of the landscape to Quaternary glaciations is more pronounced and reflected in our data. Modern 10Be denudation rates are generally higher than the long-term AFT and

Interactions between tectonics, climate, and surface processes in the by Anna Kudriavtseva

During the Cenozoic, global cooling and uplift of the Tian Shan, Pamir, and Tibetan plateau modified atmospheric circulation and reduced moisture supply to Central Asia. These changes led to aridification in the region during the Neogene. Afterwards, Quaternary glaciations led to modification of the landscape and runoff. In the Issyk-Kul basin of the Kyrgyz Tian Shan, the sedimentary sequences reflect the development of the adjacent ranges and local climatic conditions. In this work, I reconstruct the late Miocene – early Pleistocene depositional environment, climate, and lake development in the Issyk-Kul basin using facies analyses and stable δ18O and δ13C isotopic records from sedimentary sections dated by magnetostratigraphy and 26Al/10Be isochron burial dating. Also, I present 10Be-derived millennial-scale modern and paleo-denudation rates from across the Kyrgyz Tian Shan and long-term exhumation rates calculated from published thermochronology data. This allows me to examine s

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