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. 3