Datoteka:Sublimation Of Ice In Martian Spring.jpg
Veličina ovog prikaza: 800 × 600 piksela. Ostale razlučivosti: 320 × 240 piksela | 640 × 480 piksela | 1.024 × 768 piksela | 1.280 × 960 piksela | 2.560 × 1.920 piksela.
Vidi sliku u punoj veličini (2.560 × 1.920 piksela, veličina datoteke: 839 KB, MIME tip: image/jpeg)
|
Ova je datoteka sa Zajedničkog poslužitelja i mogu je rabiti drugi projekti. Opis s njezine stranice s opisom datoteke prikazan je ispod. |
Sažetak
| Opis |
English: In spring, the sublimation of the ice (going directly from ice to gas) causes a host of uniquely Martian phenomena. In this image streaks of dark basaltic sand have been carried from below the ice layer to form fan-shaped deposits on top of the seasonal ice. The similarity in the directions of the fans suggests that they formed at the same time, when the wind direction and speed was the same. They often form along the boundary between the dune and the surface below. |
| Datum | |
| Izvor | HiRISE |
| Autor | NASA/JPL/University of Arizona |
Local Mars time: 1:50 PM. Latitude (centred): 80.0 °. Longitude (East): 122.5 °. Range to target site: 319.0 km. Original image scale range: 31.9 cm/pixel (with 1 x 1 binning) so objects ~96 cm across are resolved. Map projected scale: 25 cm/pixel. Map projection: POLAR STEREOGRAPHIC. Emission angle: 2.6 °. Phase angle: 67.3 °. Solar incidence angle: 69 °, with the Sun about 21 ° above the horizon. Solar longitude: 29.7 °. Northern Spring.
Licencija
|
This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.) |  |
 |
Warnings:
|
Povijest datoteke
Kliknite na datum/vrijeme kako biste vidjeli datoteku kakva je tada bila.
| Datum/Vrijeme | Minijatura | Dimenzije | Suradnik | Komentar | |
|---|---|---|---|---|---|
| sadašnja | 17:21, 23. ožujka 2010. | | 2.560 × 1.920 (839 KB) | Originalwana | {{Information |Description={{en|1=In spring, the sublimation of the ice (going directly from ice to gas) causes a host of uniquely Martian phenomena. In this image streaks of dark basaltic sand have been carried |
Uporaba datoteke
Na ovu sliku vode poveznice sa sljedećih stranica:
Globalna uporaba datoteke
Sljedeći wikiji rabe ovu datoteku:
- Uporaba na ar.wikipedia.org
- Uporaba na ca.wikipedia.org
- Uporaba na de.wikipedia.org
- Uporaba na en.wikipedia.org
- Uporaba na it.wikipedia.org
- Uporaba na lb.wikipedia.org
- Uporaba na pnb.wikipedia.org
- Uporaba na sr.wikipedia.org
- Uporaba na ur.wikipedia.org
- Uporaba na zh.wikipedia.org
