File:J25 231 »tubo volcánico«.jpg
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editDescriptionJ25 231 »tubo volcánico«.jpg |
Deutsch: Vom Höhleneingang talwärts, noch mit Tageslicht. Lavahöhlen entstehen aus Lavaströmen bei Vulkanausbrüchen, wenn die Lava noch während des Fließens von außen und oben durch den Wärmeverlust erstarrt. Im Gegensatz zur Vulkanhöhle von Todoque auf La Palma gibt es hier neben dem Einstieg keine weiteren Tagesöffnungen. Die raue Sohle entstand nach dem Ablaufen der flüssigen Lava beim Abkühlen. Zwar dringen Moose am weitesten in die Höhle vor, doch die Flächen links und rechts sind ein typischer Fall von Lampenflora. |
Date | |
Source | Own work |
Author | Falk2 |
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editTransferred from de.wikipedia to Commons by Wdwdbot using script bot_filetrans.pl (r119M).
- 2021-04-02 03:59:05 Falk2 (6761342 Bytes)
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current | 14:32, 3 April 2021 | ![]() | 5,934 × 3,956 (6.45 MB) | Wdwdbot (talk | contribs) | Bot Move: Original uploader of this revision (#1) was Falk2 at de.wikipedia |
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Camera manufacturer | Canon |
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Camera model | Canon EOS 5D Mark III |
Author | Falk Arnhold |
Copyright holder | Falk Arnhold |
Width | 5,934 px |
Height | 3,956 px |
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Compression scheme | Uncompressed |
Pixel composition | RGB |
Image data location | 26,980 |
Orientation | Normal |
Number of components | 3 |
Number of rows per strip | 3,956 |
Bytes per compressed strip | 70,424,712 |
Horizontal resolution | 350 dpi |
Vertical resolution | 350 dpi |
Data arrangement | chunky format |
Software used | Adobe Photoshop CS2 Windows |
File change date and time | 20:43, 9 March 2016 |