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Changes of the Surface Area of Morskie Oko and Wielki Staw in the Tatra Mountains

Adam Choiński
Adam Choiński
 oraz 
Artur Zieliński
Artur Zieliński
   | 15 paź 2022
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Data publikacji: 15 paź 2022
Zakres stron: 15 - 24
Otrzymano: 18 mar 2022
DOI: https://doi.org/10.14746/quageo-2023-0002
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© 2023 Adam Choiński et al., published by Sciendo
This work is licensed under the Creative Commons Attribution 4.0 International License.

Fig. 1

General view at Morskie Oko and its surroundings from south (Choiński 2021).
General view at Morskie Oko and its surroundings from south (Choiński 2021).

Fig. 2

General view at Wielki Staw and its surroundings (Choiński 1998).
General view at Wielki Staw and its surroundings (Choiński 1998).

Fig. 3

Rockfall from the wall of Mięguszowiecki Szczyt moving towards Morskie Oko on 22 October 2021 (Denega 2021).
Rockfall from the wall of Mięguszowiecki Szczyt moving towards Morskie Oko on 22 October 2021 (Denega 2021).

Fig. 4

General view at the southern shore of Morskie Oko which was reached by the face of rockfalls (Choiński 2016).
General view at the southern shore of Morskie Oko which was reached by the face of rockfalls (Choiński 2016).

Fig. 5

One of the rockfall tongues photographed from a short distance from the water surface. One can clearly see the contact of freshly deposited mantle that penetrated the lake (Choiński 2016).
One of the rockfall tongues photographed from a short distance from the water surface. One can clearly see the contact of freshly deposited mantle that penetrated the lake (Choiński 2016).

Fig. 6

Avalanche field on the surface of Morskie Oko which was formed on 2 February 2022 (Denega 2022).
Avalanche field on the surface of Morskie Oko which was formed on 2 February 2022 (Denega 2022).

Fig. 7

Fragments of dwarf pine deposited by a snow avalanche on 2 February 2022 on the surface of the cover (Zieliński 2022).
Fragments of dwarf pine deposited by a snow avalanche on 2 February 2022 on the surface of the cover (Zieliński 2022).

Fig. 8

Changes in the course of the shoreline in the southern part of Morskie Oko. Source: orthophotomap from the resources of GUGiK.
Changes in the course of the shoreline in the southern part of Morskie Oko. Source: orthophotomap from the resources of GUGiK.

Fig. 9

An example of a northern part of the shore of Morskie Oko that is composed of boulders with relatively vertical walls; thus, water-level fluctuations do not influence the changes in surface area (Choiński 2016).
An example of a northern part of the shore of Morskie Oko that is composed of boulders with relatively vertical walls; thus, water-level fluctuations do not influence the changes in surface area (Choiński 2016).

Fig. 10

An example of a section of shoreline, determination of which is difficult. It results from the fact that it is dispersed by boulders which form very small islands. The water surface between them is so diverse, and it forms an obstacle in finding the ‘solid ground’ (Choiński 2016).
An example of a section of shoreline, determination of which is difficult. It results from the fact that it is dispersed by boulders which form very small islands. The water surface between them is so diverse, and it forms an obstacle in finding the ‘solid ground’ (Choiński 2016).

Surface areas of Morskie Oko and Wielki Staw in the period from 1880 to 2021.

Morskie Oko Wielki Staw
Year1 Author/source Area [ha] Year1 Author/source Area [ha]
1880 E. Dziewulski 30 1880 E. Dziewulski 33
1910 L. Sawicki 33.42 1910 L. Sawicki 35.78
1934 K. Śliwerski 34.54 1934 K. Śliwerski 34.14
1964 Aerial photo 7b_4328 33.07 1964 Aerial photo 7b_4328 34.33
2009 OrthophotomapM-34-101-A-c-4-1 32.95 2009 OrthophotomapM-34-101-A-c-1-4M-34-101-A-c-3-2 34.44
2011 A. ChoińskiA. Strzelczak 33.39 – – –
2012 J. Urbański et al. 32.62 – – –
2021 OrthophotomapM-34-101-A-c-4-1 32.93 2021 OrthophotomapM-34-101-A-c-1-4M-34-101-A-c-3-2 34.44
eISSN:
2081-6383
Język:
Angielski
Częstotliwość wydawania:
4 razy w roku
Dziedziny czasopisma:
Geosciences, Geography
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