tangan:Sulfur Fumarole (23998018863).jpg
pataayaway miazih hacica ku tabaki: 800 × 533 syangsu. u zuma katingalaw: 320 × 213 syangsu | 640 × 427 syangsu | 1,024 × 683 syangsu | 1,280 × 853 syangsu | 2,560 × 1,707 syangsu | 5,184 × 3,456 syangsu.
saayaway a tangan （5,184 × 3,456 syangsu, hacica ku tabaki nu tangan: 13.67 MB, MIME kakuniza: image/jpeg）
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pecu’ nu lacul
| sapuelac |
In this recent photo taken at Puʻu ʻŌʻō Crater in Hawaii, we can see that elemental sulfur vapor escaping from the fumarole has cooled to form yellow-colored crystals around the margins of the crack. Fumaroles are vents from which volcanic gas escapes into the atmosphere. Fumaroles may occur along tiny cracks or long fissures, in chaotic clusters or fields, and on the surfaces of lava flows and thick deposits of pyroclastic flows. They may persist for decades or centuries if they are above a persistent heat source or disappear within weeks to months if they occur atop a fresh volcanic deposit that quickly cools. |
| demiad | |
| saangangan | Sulfur Fumarole |
| masacudaday | U.S. Geological Survey from Reston, VA, USA |
sapabeli tu kinli a cedang
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tangan nu nazipa’an
sapecec ku demiad/tuki sapiciwsace ku tuki nina demiad a tangan baziyong
| demiad/tuki | sukep tu zunga | ditek | misaungayay | pacunus sakacaay kapawan | |
|---|---|---|---|---|---|
| ayza | 2018年1月20日 (sakaenem a demied nu lipay) 05:26 | | 5,184 × 3,456（13.67 MB） | Artix Kreiger 2 | Transferred from Flickr via Flickr2Commons |
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