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Sources of Basaltic Sand (extra-detail mgnf n. 2; MULTISPECTRUM - credits: Lunexit)
This rocky layer may originally have been a lava flow; Martian lava flows are predominantly composed of basalt, which would account for the dark color of the sand. 
The polygonal pattern of the bright upper layer may be due to repeated freezing and thawing of the soil that buries the lava flow. The tracks of Dust-Devils are clearly visible on the smooth, sandy surface but largely vanish when they cross into the polygonally fractured terrain.
Parole chiave: Mars from orbit - Southern Highlands - Mitchell Crater

Sources of Basaltic Sand (extra-detail mgnf n. 2; MULTISPECTRUM - credits: Lunexit)

This rocky layer may originally have been a lava flow; Martian lava flows are predominantly composed of basalt, which would account for the dark color of the sand.
The polygonal pattern of the bright upper layer may be due to repeated freezing and thawing of the soil that buries the lava flow. The tracks of Dust-Devils are clearly visible on the smooth, sandy surface but largely vanish when they cross into the polygonally fractured terrain.

PSP_006528_1120_RED_abrowse-00~0.jpg PSP_006528_1120_RED_abrowse-01.jpg PSP_006528_1120_RED_abrowse-02.jpg PSP_006538_1035_RED_abrowse-01.jpg PSP_006538_1035_RED_abrowse-02.jpg
Informazioni sul file
Nome del file:PSP_006528_1120_RED_abrowse-02.jpg
Nome album:MareKromium / Mars Reconnaissance Orbiter (MRO)
Valutazione (7 voti):55555(Mostra dettagli)
Parole chiave:Mars / from / orbit / - / Southern / Highlands / - / Mitchell / Crater
Copyright:NASA/JPL/University of Arizona e Lunar Explorer Italia per l'ingrandimento, l'elaborazione addizionale e la colorizzazione del frame
Dimensione del file:673 KiB
Data di inserimento:Feb 02, 2008
Dimensioni:2242 x 1800 pixels
Visualizzato:53 volte
URL:https://www.lunexit.it/gallery/displayimage.php?pid=19447
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