Mountain slope dynamics due to debris-flows activity in the high tatra mountains, Poland (Dynamique des versants montagnards due a l'activité des « debris flows » dans les Tatras polonaises)

1992 ◽  
Vol 69 (3) ◽  
pp. 257-259 ◽  
Author(s):  
Adam Kotarba
Keyword(s):  
Debris Flows ◽  
Tatra Mountains ◽  
Mountain Slope ◽  
High Tatra Mountains

A New Bolide Station at the High Tatra Mountains

2007 ◽  
Vol 102 (1-4) ◽  
pp. 253-256 ◽  
Author(s):  
Jan Svoren ◽  
Pavel Spurny ◽  
Vladimir Porubcan ◽  
Zuzana Kanuchova
Keyword(s):  
Tatra Mountains ◽  
High Tatra Mountains

Cosmic ray measurements in High Tatra mountains: 1957–2007

2009 ◽  
Vol 44 (10) ◽  
pp. 1166-1172 ◽  
Author(s):  
Karel Kudela ◽  
Ronald Langer
Keyword(s):  
Cosmic Ray ◽  
Tatra Mountains ◽  
High Tatra Mountains

Acidification of lakes in Šumava (Bohemia) and in the High Tatra Mountains (Slovakia)

Hydrobiologia ◽  
1994 ◽  
Vol 274 (1-3) ◽  
pp. 37-47 ◽  
Author(s):  
Jan Fott ◽  
Miroslava Pražáková ◽  
Evžen Stuchlík ◽  
Zuzana Stuchliková
Keyword(s):  
Tatra Mountains ◽  
High Tatra Mountains

scholarly journals Variability of Pinus mugo Turra clones from Ostry Wierch peat bog

2014 ◽  
Vol 66 (1) ◽  
pp. 79-82
Author(s):  
Alina Bączkiewicz ◽  
Wiesław Prus-Głowacki
Keyword(s):  
Statistical Analysis ◽  
Genetic Structure ◽  
Morphological Traits ◽  
Peat Bog ◽  
Pinus Mugo ◽  
Tatra Mountains ◽  
High Tatra Mountains

Present study aimed at determining genetic structure of the <em>Pinus mugo</em> Turra population, growing at a peat bog, on Ostry Wierch slopes in the High Tatra mountains, in respect to the number of genotypes present in the population, and at defining variabilities of morphological and anatomical traits. In the examined plants, isoenzymatic analysis demonstrated existence of only two genotypes (A and B), which formed relatively vast clones. Mathematical-statistical analysis of 13 anatomical - morphological traits of the needles proved that the examined clump consisted of two clearly distinguishable groups, corresponding to the two earlier electrophoretically identified clones A and B. The obtained data allowed to conclude that the method based on anatomical-morphological measurements may, at least in some cases, permit identification of <em>Pinus mugo</em> clones

The Influence of Debris Flow on Lake Depositon: An Case from Guanba River in Qionghai Lake Basin

2014 ◽  
Vol 1010-1012 ◽  
pp. 1129-1139
Author(s):  
Jian Guo Yue ◽  
Yun Long Qi ◽  
Xue Li Wei ◽  
Ning Sheng Chen
Keyword(s):  
Debris Flow ◽  
Debris Flows ◽  
Environmental Problem ◽  
River Estuary ◽  
Sediment Deposition ◽  
Lake Basin ◽  
Lake Area ◽  
Important Process ◽  
Mountain Slope ◽  
Control Factors

Sediment deposition caused by debris flows is an important process controlling the evolution and regression of lake, and even a pervasive environmental problem. The frequent debris flows construct a vital links between mountain slope and Qiong Lake transporting lots of sediment into lake, and further making the lake depth and lake area shallower and smaller constantly. In the paper, we select the Guanba River in the northeast of Qiong Lake as a case studying the effect of debris flows on Lake depositon and the characteristics of typical debris flow, and document the sediment deposition in the Guanba River estuary. The control factors contributing to debris flow initiation indicate that the debris flows are drove by rainfall, earthquake and human activities together, and the occurrence frequency of debris flows in the study area will continue to increase.

Study on the Effect of Debris Flows from Guanba River on Qiong Lake, Sichuan, China

2012 ◽  
Vol 599 ◽  
pp. 709-715 ◽  
Author(s):  
Xue Li Wei ◽  
Yun Long Qi ◽  
Qian Gong Cheng ◽  
Ning Sheng Chen
Keyword(s):  
Debris Flow ◽  
Debris Flows ◽  
Environmental Problem ◽  
Water Area ◽  
Sediment Deposition ◽  
Disaster Mitigation ◽  
Mountain Slope ◽  
Change Pattern ◽  
Push Forward ◽  
Deep Water Area

Sediment deposition caused by debris flows and floods is an important process controlling the evolution and regression of lake, and even a pervasive environmental problem. Qiong Lake is regards as a “bright phearl of the altiplano” in the Yunnan Plateau, and because debris flows construct a vital links between mountain slope and Qiong Lake, so the debris flows drove by rainfall will control the evolution rule of rift lakes. Based on the data of lake shorelines of Qiong Lake, it was found that the shoreline was push forward by 665 m since 1998. In addition, in the recent 30 years, turbidity current deposits have generated underwater levee and other landscapes in the deep water area of Qiong River. This paper has analyzed the matter migration process induced by debris flows, and presented the regime change pattern of debris flow along river channel and corresponding mechanical mechanism, mainly revealed the submarine transportation and deposition pattern of debris flow. The above studies provide a helpful way of comprehending the formation mechanism of turbidity flow induced by debris flow, and the transportation pattern. Based on severe sediment deposition catastrophes in this kind of rift lakes from debris flows and floods, disaster mitigation must be planned and appropriate engineering countermeasures put in place as soon as possible.

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