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Inizio > MARS > Mars Reconnaissance Orbiter (MRO)

Piú viste - Mars Reconnaissance Orbiter (MRO)
PSP_007492_2265_RED_abrowse-PCF-LXTT.jpg
PSP_007492_2265_RED_abrowse-PCF-LXTT.jpgPolygons in Deuteronilus Mensae (Enhanced Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)316 visiteThis image reveals hexagonal and polygonal patterns formed by networks of soil troughs on the floor of a valley in the Deuteronilus Mensae Region, located on the Northern edge of Arabia Terra and borders the Martian Southern Highlands and Northern Lowlands.
The polygonal patterns indicate that the surface has undergone stress, potentially caused by subsidence (sinking), desiccation (drying out), or thermal contraction. These polygon features are similar to permafrost thermal-contraction polygons that form in Polar and High Alpine Regions on Earth by seasonal-to-annual contraction of the subsoil. On Earth, such polygon features are indicative of the presence of ground ice and are commonly referred to as “patterned ground”. The patterns are the result of thermal contraction in ice-cemented soil or permafrost that forms a honeycomb network of small fractures below the surface.

The network of fractures is eventually manifested as shallow troughs at the surface, forming the hexagonal and polygonal patterns visible in this image.

The polygons in this scene average approx. 100 meters (110 yards) in size and appear to be higher in elevation in the center than in the surrounding troughs. Boulders are accumulated in the center of the polygons and dunes are visible in several of the troughs.

The landforms we observe here most likely indicate that ice-rich permafrost is present or has been present in the past.
MareKromium
ESP_021757_1975_RED_abrowse-PCF-LXTT.jpg
ESP_021757_1975_RED_abrowse-PCF-LXTT.jpgScarp in Syrtis Major (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)316 visitenessun commentoMareKromium
ESP_020926_1815_RED_abrowse-PCF-LXTT.jpg
ESP_020926_1815_RED_abrowse-PCF-LXTT.jpgLibya Montes (Absolute Natural Colors; credits: Dr Paolo C. Fienga - Lunexit Team)315 visitenessun commentoMareKromium
ESP_015900_1465_RED_abrowse-00-PCF-LXTT.jpg
ESP_015900_1465_RED_abrowse-00-PCF-LXTT.jpgUnnamed Southern Crater with Gullies, Rolling Boulders and Dunes (CTX Frame - Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)315 visiteCaption NASA:"Although this image was primarily taken to study the Gullies in the Inner Walls of the Crater, it also reveals a few other interesting things.
Near the Gullies in the Northern Wall of the Crater, for instance, some Boulders have bounced down the Slope, leaving trails of Hollows along their paths (see EDM n. 1).
MareKromium
PSP_002193_1670_red-PCF-LXTT.jpg
PSP_002193_1670_red-PCF-LXTT.jpgFeatures of Margaritifer Terra (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)315 visitenessun commentoMareKromium
PSP_002345_1095_red-PCF-LXTT.jpg
PSP_002345_1095_red-PCF-LXTT.jpgSouthern Dunes (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)314 visitenessun commento11 commentiMareKromium
ESP_022999_1335_RED_abrowse-PCF-LXTT-00.jpg
ESP_022999_1335_RED_abrowse-PCF-LXTT-00.jpgUnnamed Crater with Gullies (CTX Frame - Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C . Fienga - Lunar Explorer Italia)311 visitenessun commentoMareKromium
ESP_020892_1275_RED_abrowse-PCF-LXTT.jpg
ESP_020892_1275_RED_abrowse-PCF-LXTT.jpgLike a "Dry Waterfall" (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)309 visitenessun commentoMareKromium
ESP_021569_1650-PCF-LXTT.jpg
ESP_021569_1650-PCF-LXTT.jpgOver the Columbia Hills (Absolute Natural Colors; credits: Dr Paolo C. Fienga - Lunexit Team)309 visiteAcquisition date: 04 March 2011
Mars Local Time (M.L.T.): 15:11 (Early Afternoon)
Latitude (centered): 14,6° South
Longitude (East): 175,6°
Spacecraft Altitude: approx. 264 Km (163,944 miles)
Original Image Scale Range: 26,4 cm/pixel (with 1 x 1 binning) so objects ~79 cm across are resolved
Map Projected Scale: 25 cm/pixel and North is up
Map Projection: EQUIRECTANGULAR
Emission Angle: 2,9°
Sun-Surface-Spacecraft Angle (i.e.: Phase Angle): 48,7°
Solar Incidence Angle (S.I.A.): 46°, with the Sun about 44° above the Local Horizon
Solar Longitude: 247,7° - Northern Autumn
MareKromium
ESP_020959_0985_RED_abrowse.jpg
ESP_020959_0985_RED_abrowse.jpgEarly Spring in Inca City (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)308 visitenessun commento3 commentiMareKromium
Psp_001700_2505_red-00~0.jpg
Psp_001700_2505_red-00~0.jpgLauth Crater and the Frozen "Pseudo-Lake" of Vastitas Borealis (CTX Frame - Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)308 visiteThe right side of PSP_001700_2505 shows a portion of a Frost Patch on a Mound inside a Northern Hemisphere Crater (unofficially known as "Lauth Crater").
The Frost Patch has remained largely stable at least since the Viking era (late 1970s). The bright Frost Region is bounded by a Dunefield on the North-East. Several sizes of Dunes are visible. The size classes probably represent generations of Dunes that formed under a variety of dominant wind conditions.
MareKromium
ESP_021577_1375_RED_abrowse-PCF-LXTT.jpg
ESP_021577_1375_RED_abrowse-PCF-LXTT.jpgKnob in Argyre Planitia (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)308 visitenessun commentoMareKromium
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