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Aquae calidae salientes

E Vicipaedia
Quomodo scaturigo geyseriana agitatur

Aquae calidae salientes[1] vel scaturigo geyzeriana[2] est fons calidus, interdum aqua ferventi, quae certum post tempus magna сum vi eicitur et iterum quiescit. Calore vulcanico aqua in scaturiginibus geyzerianis calefit et in regionibus montium igniferorum saepius inveniuntur. Regiones tales sunt Islandia, Saeptum nationale Yellowstone. Vallis geyzeriana Kamtschatkae, Nova Zelandia aliaeque. Vocabulum geyzerianus originem Islandicam habet; Geysir scatirigo magna Islandiae nominatur (de geysa, eici, effundi).

Scaturigo Žemčužnyij (Margaritarum) Kamtschatkae

Nexus externi

[recensere | fontem recensere]


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