Fayl:GebelEdmonstone ISS009-E-12441.jpg
Bu prevyuning hajmi: 800 × 528 piksel. Boshqa oʻlchamlari: 320 × 211 piksel | 640 × 422 piksel | 1 000 × 660 piksel.
Asl fayl (1 000 × 660 piksel, fayl hajmi: 555 KB, MIME tipi: image/jpeg)
Qisqa izoh
| Taʼrif | Astronaut photo of w:Gebel Edmonstone, Egypt. Image has been processed to enhance color variations in the various rock and soil units. The color variations reflect differences in composition (or weathering) of the various rock units. The limestone unit capping Gebel Edmonstone and the adjacent scarp ranges from white to gray in color, while the underlaying fine-grained sedimentary layers are blue-gray. Hillslope pathways for sediment movement downslope are clearly visible as brown to tan streamers originating from Gebel Edmonstone. Barchan dune fields are also visible in this color-enhanced image (lower left), and are distinct due to their mineralogical composition. Evaporite deposits are bright white (center top), while vegetated portions of the Oasis—mostly agricultural fields—are dark blue-black. |
| Sanasi | |
| Manba | http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=16714 |
| Muallif | ISS Crew Earth Observations experiment and the Image Science & Analysis Group, Johnson Space Center. |
| Ruxsat (Bu faylning takror foydalanilishi) |
NASA, public domain |
Litsenziyalash
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This file is in the public domain in the United States because it was created by the Image Science & Analysis Laboratory, of the NASA Johnson Space Center. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (NASA media use guidelines or Conditions of Use of Astronaut Photographs).
Photo source: ISS009-E-12441.
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Faylning biror paytdagi holatini koʻrish uchun tegishli sana/vaqtga bosingiz.
| Sana/Vaqt | Miniatura | Oʻlchamlari | Foydalanuvchi | Izoh | |
|---|---|---|---|---|---|
| joriy | 18:23, 19-May 2006 | | 1 000 × 660 (555 KB) | Holly Cheng | ==Summary== {{Information | Description=Astronaut photo of w:Gebel Edmonstone, Egypt. Image has been processed to enhance color variations in the various rock and soil units. The color variations reflect differences in composition (or weathering) of t |
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