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I S Bushueva

Biographic Data

ID6571395
NAMEI S Bushueva
GIVEN NAMESI S
FAMILY NAMEBushueva
SIGNATUREBUSHUEVA I S
AFFILIATIONSRussian Academy of Sciences
ORCID0000-0002-8324-4822
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS0
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2022
LATEST PUBLICATION YEAR2025
H-INDEX0
  • Late Holocene glacier fluctuations in the Northern Greater Caucasus (Russia) inferred from 10 Be cosmic ray exposure moraine dating

    Open Access•Vincent Jomelli, Olga Solomina et al.•ARTICLE•The Holocene•2025•References: 16

    Our understanding of mountain glacier changes located in the Greater Caucasus during the Holocene is only loosely constrained. So far moraines were tentatively dated from sporadic cosmic ray exposure (CRE) ages, tree rings and radiocarbon ages. Here, we present 78 10 Be CRE ages that were obtained from samples collected on moraine boulders and roches moutonnees from one debris-free Terskol glacier and two debris-covered Bashkara and Donguz-Orun g…

  • Late-Holocene advances of the Greater Azau Glacier (Elbrus area, Northern Caucasus) revealed by 14 C dating of paleosols

    Open Access•Olga N Solomina, A L Alexandrovskiy et al.•ARTICLE•The Holocene•2022

    Three paleosols buried in the left lateral moraines of the Greater Azau Glacier (Northern Caucasus) were identified in an excavated outcrop (43.2658 N, 42.4766 E, 2370 m a.s.l.). When the glacier was overlying the surface of the lateral moraines at this site, the thickness of the ice was 50 m and more above the valley floor. Fragments of charcoal from the uppermost soil (S1) buried 0.6 m below the surface yielded the radiocarbon date 130 ± 20 yr …

No prominent works on this page.

  • Late-Holocene advances of the Greater Azau Glacier (Elbrus area, Northern Caucasus) revealed by 14 C dating of paleosols

    Open Access•Olga N Solomina, A L Alexandrovskiy et al.•ARTICLE•The Holocene•2022

    Three paleosols buried in the left lateral moraines of the Greater Azau Glacier (Northern Caucasus) were identified in an excavated outcrop (43.2658 N, 42.4766 E, 2370 m a.s.l.). When the glacier was overlying the surface of the lateral moraines at this site, the thickness of the ice was 50 m and more above the valley floor. Fragments of charcoal from the uppermost soil (S1) buried 0.6 m below the surface yielded the radiocarbon date 130 ± 20 yr …

  • Late Holocene glacier fluctuations in the Northern Greater Caucasus (Russia) inferred from 10 Be cosmic ray exposure moraine dating

    Open Access•Vincent Jomelli, Olga Solomina et al.•ARTICLE•The Holocene•2025•References: 16

    Our understanding of mountain glacier changes located in the Greater Caucasus during the Holocene is only loosely constrained. So far moraines were tentatively dated from sporadic cosmic ray exposure (CRE) ages, tree rings and radiocarbon ages. Here, we present 78 10 Be CRE ages that were obtained from samples collected on moraine boulders and roches moutonnees from one debris-free Terskol glacier and two debris-covered Bashkara and Donguz-Orun g…

Climate change and permafrost (2 works) · Geology and Paleoclimatology Research (2 works) · Glacier (2 works) · Holocene (2 works) · Moraine (2 works) · Radiocarbon dating (2 works) · Charcoal (1 work) · Cirque glacier (1 work) · Geography (1 work) · Geology (1 work)

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