Advanced Search

Journal Navigation

Journal Home

Subscriptions

Archive

Contact Us

Table of Contents

Environmental Sciences: A Students Companion

Sign In to gain access to subscriptions and/or personal tools.
The Holocene
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to Saved Citations
Right arrow Download to citation manager
Right arrowRequest Permissions
Right arrow Request Reprints
Right arrow Add to My Marked Citations
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Right arrow Citing Articles via Scopus
Google Scholar
Right arrow Articles by Solomina, O.N.
Right arrow Articles by Cherkinsky, A.E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Social Bookmarking
 Add to CiteULike   Add to Complore   Add to Connotea   Add to Del.icio.us   Add to Digg   Add to Reddit   Add to Technorati   Add to Twitter  
What's this?

Glacier variations, mudflow activity and landscape development in the Aksay Valley (Tian Shan) during the late Holocene

O.N. Solomina

(Institute of Geography, Russian Academy of Science, Staromonetny pereulok 29, Moscow 109017, Russia)

O.S. Savoskul

(Institute of Geography, Russian Academy of Science, Staromonetny pereulok 29, Moscow 109017, Russia)

A.E. Cherkinsky

(Institute of Geography, Russian Academy of Science, Staromonetny pereulok 29, Moscow 109017, Russia)

The object of this paper is to reconstruct the history of glaciation and the dynamics of mudflow activity as part of the development of landscapes in the Aksay Valley, Kirgizsky Ridge, over the last 2000 years. Glacial, mudflow and slope deposits were dated by lichenometry and the radiocarbon method. The results of 14C dating of buried soils shows that at about 1700 BP a period of activization of slope processes took place in the valley. The zone of alpine meadow was situated at that time at an elevation of about 2750 m and glacier termini were situated at about 3100-3200 m. The oldest mudflow surface, which was investigated by lichenometry, dates from the same time.

New equations for the rate of growth of the lichens Aspicilia tianshanica and Rhizocarpon geographicum use the oldest mudflow surface as a control point. Two periods of reduced mudflow activity are identified by lichenometry, i.e., 350-450 and 130-240 BP, and the latter is confirmed by 14C dating of peat-soil interlayers in a mudflow stratum with the specific activity of samples exceeding NBS standard. Thus, a new modification of the 14C-dating method is demonstrated. Lichenometry on moraines of the Aksay Glacier shows that advances of the glacier took place in the fourteenth and late- nineteenth centuries as well as at the beginning of this century. The depression of equilibrium-line altitude (ELA) for the fourteenth and nineteenth centuries was 150-170 m and 100-120 m, respectively.

Key Words: Glacier variations • mudflows • landscape development • lichenometric dating • radiocarbon dating • soil dating • late Holocene • Tian Shan.

The Holocene, Vol. 4, No. 1, 25-31 (1994)
DOI: 10.1177/095968369400400104


Add to CiteULike CiteULike   Add to Complore Complore   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg   Add to Reddit Reddit   Add to Technorati Technorati   Add to Twitter Twitter    What's this?


This article has been cited by other articles:


Home page
The HoloceneHome page
S. Harrison, S. Harrison, and V. Winchester
Age and nature of paraglacial debris cones along the margins of the San Rafael Glacier, Chilean Patagonia
The Holocene, January 1, 1997; 7(4): 481 - 487.
[Abstract] [PDF]


Home page
The HoloceneHome page
O. S. Savoskul, O.S. Savoskul, and O.N. Solomina
Late-Holocene glacier variations in the frontal and inner ranges of the Tian Shan, central Asia
The Holocene, January 1, 1996; 6(1): 25 - 35.
[Abstract] [PDF]