Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains

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Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains. / Deline, Philip; Ravanel, Ludovic; Delannoy, Jean Jacques et al.

In: Journal of Maps, Vol. 16, No. 2, 09.12.2020, p. 595-604.

Research output: Contribution to journal › Article › peer-review

Harvard

Deline, P, Ravanel, L, Delannoy, JJ, Le Roy, M, Molodin, VI, Cheremisim, DV, Zotkina, LV, Cretin, C, Geneste, JM & Plisson, H 2020, 'Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains', Journal of Maps, vol. 16, no. 2, pp. 595-604. https://doi.org/10.1080/17445647.2020.1800529

APA

Deline, P., Ravanel, L., Delannoy, J. J., Le Roy, M., Molodin, V. I., Cheremisim, D. V., Zotkina, L. V., Cretin, C., Geneste, J. M., & Plisson, H. (2020). Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains. Journal of Maps, 16(2), 595-604. https://doi.org/10.1080/17445647.2020.1800529

Vancouver

Deline P, Ravanel L, Delannoy JJ, Le Roy M, Molodin VI, Cheremisim DV et al. Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains. Journal of Maps. 2020 Dec 9;16(2):595-604. doi: 10.1080/17445647.2020.1800529

Author

Deline, Philip ; Ravanel, Ludovic ; Delannoy, Jean Jacques et al. / Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains. In: Journal of Maps. 2020 ; Vol. 16, No. 2. pp. 595-604.

BibTeX

@article{7c470bcddb7445c7b1af0f1723b3f0bd,

title = "Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains",

abstract = "As part of an archaeological research project, we investigate the geomorphology of the cold and arid study area by combining field mapping with use of orthoimages and DEM. To the north of a broad trunk valley floor, gentle slopes continuously vegetated culminate around 3000 m, while to the south steep slopes reaching to 3500 m are deeply incised and covered mainly by regolith. The basin has been intensively glaciated as evidenced by the till covering the gentler slopes, several morainic complexes, kame terraces and roches moutonn{\'e}es. The present morphodynamics of this permafrost-affected basin is mainly periglacial, with blockfields, solifluction lobes, patterned ground and rock glaciers on gentle slopes to high-elevated flat terrain, and block slopes and rockfall talus on steeper slopes. Large alluvial fans at the outlet of the steep lateral valleys constrain the anastomosing channel of the Kalguty river. Active braided channels in those valleys evidence seasonal high peak discharge.",

keywords = "Altai mountains, geomorphological mapping, Glacial and periglacial geomorphology, Ukok Plateau, PERMAFROST, TALUS SLOPES, ICE, YUKON-TERRITORY, ROCK GLACIERS, FEATURES",

author = "Philip Deline and Ludovic Ravanel and Delannoy, {Jean Jacques} and {Le Roy}, Melaine and Molodin, {Vyacheslav I.} and Cheremisim, {Dimitri V.} and Zotkina, {Lydia V.} and Catherine Cretin and Geneste, {Jean Michel} and Hugues Plisson",

note = "Publisher Copyright: {\textcopyright} 2020 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps.",

year = "2020",

month = dec,

day = "9",

doi = "10.1080/17445647.2020.1800529",

language = "English",

volume = "16",

pages = "595--604",

journal = "Journal of Maps",

issn = "1744-5647",

publisher = "Taylor and Francis Ltd.",

number = "2",

}

RIS

TY - JOUR

T1 - Geomorphology of the upper Kalguty Basin, Ukok Plateau, Russian Altai mountains

AU - Deline, Philip

AU - Ravanel, Ludovic

AU - Delannoy, Jean Jacques

AU - Le Roy, Melaine

AU - Molodin, Vyacheslav I.

AU - Cheremisim, Dimitri V.

AU - Zotkina, Lydia V.

AU - Cretin, Catherine

AU - Geneste, Jean Michel

AU - Plisson, Hugues

PY - 2020/12/9

Y1 - 2020/12/9

N2 - As part of an archaeological research project, we investigate the geomorphology of the cold and arid study area by combining field mapping with use of orthoimages and DEM. To the north of a broad trunk valley floor, gentle slopes continuously vegetated culminate around 3000 m, while to the south steep slopes reaching to 3500 m are deeply incised and covered mainly by regolith. The basin has been intensively glaciated as evidenced by the till covering the gentler slopes, several morainic complexes, kame terraces and roches moutonnées. The present morphodynamics of this permafrost-affected basin is mainly periglacial, with blockfields, solifluction lobes, patterned ground and rock glaciers on gentle slopes to high-elevated flat terrain, and block slopes and rockfall talus on steeper slopes. Large alluvial fans at the outlet of the steep lateral valleys constrain the anastomosing channel of the Kalguty river. Active braided channels in those valleys evidence seasonal high peak discharge.

AB - As part of an archaeological research project, we investigate the geomorphology of the cold and arid study area by combining field mapping with use of orthoimages and DEM. To the north of a broad trunk valley floor, gentle slopes continuously vegetated culminate around 3000 m, while to the south steep slopes reaching to 3500 m are deeply incised and covered mainly by regolith. The basin has been intensively glaciated as evidenced by the till covering the gentler slopes, several morainic complexes, kame terraces and roches moutonnées. The present morphodynamics of this permafrost-affected basin is mainly periglacial, with blockfields, solifluction lobes, patterned ground and rock glaciers on gentle slopes to high-elevated flat terrain, and block slopes and rockfall talus on steeper slopes. Large alluvial fans at the outlet of the steep lateral valleys constrain the anastomosing channel of the Kalguty river. Active braided channels in those valleys evidence seasonal high peak discharge.

KW - Altai mountains

KW - geomorphological mapping

KW - Glacial and periglacial geomorphology

KW - Ukok Plateau

KW - PERMAFROST

KW - TALUS SLOPES

KW - ICE

KW - YUKON-TERRITORY

KW - ROCK GLACIERS

KW - FEATURES

UR - http://www.scopus.com/inward/record.url?scp=85089499511&partnerID=8YFLogxK

U2 - 10.1080/17445647.2020.1800529

DO - 10.1080/17445647.2020.1800529

M3 - Article

AN - SCOPUS:85089499511

VL - 16

SP - 595

EP - 604

JO - Journal of Maps

JF - Journal of Maps

SN - 1744-5647

IS - 2

ER -

ID: 24984681