Serak (geografia)
Olbrzymi serak na zboczu Rakaposhi
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Serak (od fr. sérac - rodzaj kruchego białego sera) – element lodowca, wielotonowa bryła lodu tworząca się w wyniku pękania lodowca, spowodowanego przez ruch progu lodowcowego ponad wybrzuszeniami i progami podłoża[1].
Przypisy
- ↑ Wojciech Lewandowski, Marek Zgorzelski: Góry wysokie. Leksykon. Warszawa: Wiedza Powszechna, 2002. ISBN 83-214-1278-5.
Media użyte na tej stronie
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Argentina - Mt Tronador Ascent - 43 - seracs & crevasses (6962480275).jpg
Autor: McKay Savage from London, UK, Licencja: CC BY 2.0
The gorgeous lines of seracs and crevasses were a never-ending source of wonder and a 3-d puzzle to navigate.
Autor: McKay Savage from London, UK, Licencja: CC BY 2.0
The gorgeous lines of seracs and crevasses were a never-ending source of wonder and a 3-d puzzle to navigate.
Serac of Rakaposhi.JPG
Autor: FarazRafaqat, Licencja: CC BY-SA 4.0
The closest view of serac of Rakaposhi
Autor: FarazRafaqat, Licencja: CC BY-SA 4.0
The closest view of serac of Rakaposhi
Sérac sur le glacier des Bans.jpg
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Sérac sur le glacier des Bans, massif des Écrins, France.
This file is not in the public domain. Therefore you are requested to use the following next to the image if you reuse this file: © Yann Forget / Wikimedia Commons, CC BY-SA 4.0
Sérac sur le glacier des Bans, massif des Écrins, France.