Дѣло:Fryxellsee Opt.jpg

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Wikipedia Commons Сь видъ Викикладѣ (Wikimedia Commons) съхранѥнъ ѥстъ ⁙ Cѥ ѥгожє опьсаниѥ ѥстъ
опьсаниѥ
English: Antarctica: The blue ice covering Lake Fryxell, in the Transantarctic Mountains, comes from glacial meltwater from the Canada Glacier and other smaller glaciers. The freshwater stays on top of the lake and freezes, sealing in briny water below.
Français : Antarctique: La glace bleue couvrant le Lac Fryxell, dans la Chaîne Transantarctique, vient des eaux de fonte du Glacier Canada et d'autres glaciers plus petits. L'eau douce se trouve en surface du lac et gèle, scellant une eau saumâtre située en-dessous.
Українська: Льодовикове озеро Фрікселл, що наповнюється водами з льодовика Канада. Трансантарктичні гори, Антарктида.
врѣмѧ сътворѥниꙗ
кладѧꙃь From Antarctic Photo Library: LAKEFRYXELL.JPG
творьць Joe Mastroianni, National Science Foundation
Permission
(Reusing this file)
Public domain This image is a work of a National Science Foundation employee, taken or made as part of that person's official duties. As a work of the U.S. federal government, the image is in the public domain.
Other versions Image:Fryxellsee.jpg


This is a retouched picture, which means that it has been digitally altered from its original version. Modifications: Artificial sky (colour gradient). Modifications made by Thomas G. Graf.

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10 дєкємврїи 2002

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дьнь / врѣмѧмалъ обраꙁъмѣрапольꙃєватєл҄ьопьсаниѥ
нꙑнѣщьн҄ь обраꙁъ11:22, ноємврїꙗ 28 числа, 2004Thumbnail for version as of 11:22, ноємврїꙗ 28 числа, 20041.560 × 1.083 (671 Х҃Б)Thomas G. Graf~commonswiki
18:49, ноємврїꙗ 27 числа, 2004Thumbnail for version as of 18:49, ноємврїꙗ 27 числа, 20041.950 × 1.354 (426 Х҃Б)Thomas G. Graf~commonswiki

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