File:Структура пакового льда.png

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Русский: Паковые льдины могут быть такими большими, что на их поверхности могут быть свои особенности рельефа (если так можно сказать) — снежные дюны, талые озёра, ледяные ущелья и впадины.
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Source https://t.me/imhograf/29
Author Имхограф, Amanda Grobe, Hannes Grobe, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
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This file, which was originally posted to https://t.me/imhograf/29, was reviewed on 12 April 2022 by reviewer Magog the Ogre, who confirmed that it was available there under the stated license on that date.
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Date/TimeThumbnailDimensionsUserComment
current19:47, 4 September 2024Thumbnail for version as of 19:47, 4 September 20242,800 × 1,576 (134 KB)ReneeWrites (talk | contribs)Removed watermark
21:10, 11 April 2022Thumbnail for version as of 21:10, 11 April 20222,800 × 1,576 (137 KB)RASPBERRY VIBE (talk | contribs)Uploaded a work by Имхограф, Amanda Grobe & Hannes Grobe from https://t.me/imhograf/29 with UploadWizard

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