Fasciculus:Fryxellsee Opt.jpg

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Sua resolutio ‎(1 560 × 1 083 elementa imaginalia, magnitudo fasciculi: 671 chiliocteti, typus MIME: image/jpeg)

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Descriptio
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.
Datum
Fons From Antarctic Photo Library: LAKEFRYXELL.JPG
Auctor Joe Mastroianni, National Science Foundation
Permissio
(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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depicts Anglica

blue sky Anglica

inceptio

10 Decembris 2002

MIME type Anglica

image/jpeg

image/jpeg

Historia fasciculi

Presso die vel tempore fasciculum videbis, sicut tunc temporis apparuit.

Dies/TempusMinutioDimensionesUsorSententia
recentissima11:22, 28 Novembris 2004Minutum speculum redactionis 11:22, 28 Novembris 2004 factae1 560 × 1 083 (671 chiliocteti)Thomas G. Graf~commonswiki
18:49, 27 Novembris 2004Minutum speculum redactionis 18:49, 27 Novembris 2004 factae1 950 × 1 354 (426 chiliocteti)Thomas G. Graf~commonswiki

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Hic fasciculus alias res continet, saepius a machina originatore additas, et (si fasciculus postea recensus sit) fortasse corrigendas.

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