Morphometrical analysis of glacial landforms in the Northern part of

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Morphometrical analysis of glacial landforms in the Northern part of
the High Tatra Mountains, Slovakia (Title - Calibri Font size 14, Bold,
Justified)
Veronika KUPKOVÁ1* and Pavel MENTLÍK1 (Names of authors - Calibri Font size 10.5, Bold,
Justified)
1 University of West Bohemia, Plzeň (Authors‘ affiliation addresses - Calibri font size 10.5,
Justified)
* Correspondence to: Veronika Kupková, University of West Bohemia, Plzeň, Czech Republic. E-mail: kupkovav@students.zcu.cz
(Contact data for corresponding author - Calibri Font size 8, Justified)
ABSTRACT: (Abstract will be written in Calibri Font size 10, Justified,
within the table frame)
KEY WORDS: (A maximum of 6 key words - Calibri Font size 6, Justified)
1. Introduction (Section titles, numbered according to Guide – Calibri Font size 12,
Bold, Justified)
The High Tatra Mts. is 26,5km long mountain range consisting mainly of granite. It is located on
the Polish-Slovakian borders in the Central Europe and belongs to the Carpathian mountain range
formed in Tertiary during the Alpine orogenesis. The highest peak reaches 2655m a.s.l. (Gerlach,
Slovakia) and it is situated almost in the middle of the High Tatras. (Text will be in Calibri Font size
10.5, Justified)
1.1. (Subsection title – Calibri Font size 11, Justified)
A remarkable symmetry of valleys (called dolina in Slovakia), which are separated by side-ranges
lowering to the piedmont area, is typical for the High Tatras. From the geological point of view
the High Tatras are defined as a horst with the southern slope uplifted (Lukniš, 1973). This results
in a fact that southern valleys are characterized with higher average altitudes (in comparison to
northern slope valleys) and also slope aspects (Midriak, 1983).
Figure 1. The High Tatra Mts - region of interest (yellow demarcation). This figure is available in colour
online at www.georeview.ro (Figure caption – Calibri Font size 10, Justified; figure number in Bold)
2. Methods
3. Results
Table 2. Cirques characteristics for both slopes of the High Tatra Mts (Table caption – Calibri Font size
10, Justified; table number in Bold)
Emin [m a.s.l.]
Emax [m a.s.l.]
Eaver [m a.s.l.]
H [m]
N
S
N
S
N
S
N
S
minimum
1 300
1 751
1 600
2 000
1 450
1 900
80
80
maximum
2 150
2 200
2 500
2 523
2 275
2 288
590
772
average value
1 775
2 023
2 051
2 232
1 913
2 127
276
209
4. Conclusions
References
Batko P. 2009. Morfometrická analýza vybraných glaciálních forem ve Vysokých Tatrách [Bachelor
thesis]. 55 s.: il. + 1 CD-ROM.
Evans I. S., Cox N. J. 2005. Global variations of local asymmetry in glacier altitude: separation of
north-south and east-west components. Journal of glaciology 51 (174): 469-482.
García-Ruiz M. J., Gómez-Villar A., Ortigosa L., Martí-Bono C. 2000. Morphometry of Glacial
Cirques in the Central Spanish Pyrenees. Geografiska Annaler 82 A, 4: 433-442.
Lindner L., Dzierżek J., Marciniak B., Nitychoruk J. 2003. Outline of Quaternary glaciations in the
Tatra Mts.: their development, age and limits. Geological Quarterly 47 (3): 269–280.
Warszawa.
Lukniš M. 1973. Reliéf Vysokých Tatier a ich predpolia. Bratislava: Slovenská akadémia vied. Vyd.
1. 375 s.: il.
Mentlík P., Minár J., Břízová E., Lisá L., Tábořík P., Stacke V. 2009. Glaciation in the surroundings
of Prášilské Lake (Bohemian Forest, Czech Republic). Geomorphology, doi:
10.1016/j.geomorph.2009.12.001.
Midriak R. 1983. Morfogenéza povrchu vysokých pohorí. Bratislava: Veda, nakladatelství SAV.
Vyd. 1. 516 s.: il.
Steffanová P., Mentlík P. 2007. Comparison of morphometric characteristics of cirques in the
Bohemian Forest. In Silva Gabreta. Vimperk: Správa Národního parku Šumava, vol. 13 (3):
191–204.
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