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• W2512459160 abstract "Abstract The growing inventory of post‐Noachian fluvial valleys may represent a late, widespread episode of aqueous activity on Mars, contrary to the paradigm that fluvial activity largely ceased around the Noachian‐Hesperian boundary. Fresh shallow valleys (FSVs) are widespread from ~30 to 45° in both hemispheres with a high concentration in northern Arabia Terra. Valleys in northern Arabia Terra characteristically start abruptly on steeper slopes and terminate in topographic depressions at elevations corresponding to model‐predicted lake levels. Longer valley systems flowed into and out of chains of paleolakes. Minimum discharges based on the dimensions of the incised channel assuming medium to coarse sand‐size grains ranges from tens to hundreds of m 3 s −1 , respectively, consistent with formation via snowmelt from surface or sub‐ice flows. Hydrologic calculations indicate the valleys likely formed in hundreds of years or less, and crater statistics constrain the timing of fluvial activity to between the Hesperian and middle Amazonian. Several craters with channels extending radially outward supports evidence for overflow of interior crater lakes possibly fed by groundwater. Most FSVs occur away from young impact craters which make an association with impact processes improbable. The widespread occurrence of FSVs along with their similar morphology and shared modest state of degradation is consistent with most forming during a global interval of favorable climate, perhaps contemporaneous with alluvial fan formation in equatorial and midlatitudes. Evidence for a snowmelt‐based hydrology and considerable depths of water on the landscape in Arabia supports a cold, wet, and possibly habitable environment late in Martian history." @default.
• W2512459160 created "2016-09-16" @default.
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• W2512459160 date "2016-09-01" @default.
• W2512459160 modified "2023-10-12" @default.
• W2512459160 title "A cold‐wet middle‐latitude environment on Mars during the Hesperian‐Amazonian transition: Evidence from northern Arabia valleys and paleolakes" @default.
• W2512459160 cites W1484710375 @default.
• W2512459160 cites W1501439318 @default.
• W2512459160 cites W1537887980 @default.
• W2512459160 cites W1570573117 @default.
• W2512459160 cites W1600910017 @default.
• W2512459160 cites W1839376471 @default.
• W2512459160 cites W1933067697 @default.
• W2512459160 cites W1963985271 @default.
• W2512459160 cites W1964272745 @default.
• W2512459160 cites W1970851121 @default.
• W2512459160 cites W1981061458 @default.
• W2512459160 cites W1981401653 @default.
• W2512459160 cites W1981559436 @default.
• W2512459160 cites W1983550241 @default.
• W2512459160 cites W1984031617 @default.
• W2512459160 cites W1984174198 @default.
• W2512459160 cites W1987184953 @default.
• W2512459160 cites W1992642150 @default.
• W2512459160 cites W1996620243 @default.
• W2512459160 cites W2000231115 @default.
• W2512459160 cites W2001825236 @default.
• W2512459160 cites W2003774542 @default.
• W2512459160 cites W2004688163 @default.
• W2512459160 cites W2009550312 @default.
• W2512459160 cites W2010299337 @default.
• W2512459160 cites W2011010849 @default.
• W2512459160 cites W2017532608 @default.
• W2512459160 cites W2018059259 @default.
• W2512459160 cites W2018463199 @default.
• W2512459160 cites W2020756894 @default.
• W2512459160 cites W2023934786 @default.
• W2512459160 cites W2024639732 @default.
• W2512459160 cites W2028483491 @default.
• W2512459160 cites W2028545091 @default.
• W2512459160 cites W2030356981 @default.
• W2512459160 cites W2032433525 @default.
• W2512459160 cites W2037372977 @default.
• W2512459160 cites W2039319719 @default.
• W2512459160 cites W2044927815 @default.
• W2512459160 cites W2050465882 @default.
• W2512459160 cites W2050653203 @default.
• W2512459160 cites W2053497149 @default.
• W2512459160 cites W2054945157 @default.
• W2512459160 cites W2058179762 @default.
• W2512459160 cites W2059008736 @default.
• W2512459160 cites W2062029016 @default.
• W2512459160 cites W2064534798 @default.
• W2512459160 cites W2065782610 @default.
• W2512459160 cites W2067292283 @default.
• W2512459160 cites W2074649556 @default.
• W2512459160 cites W2076509405 @default.
• W2512459160 cites W2077081790 @default.
• W2512459160 cites W2079799239 @default.
• W2512459160 cites W2081130960 @default.
• W2512459160 cites W2093624600 @default.
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• W2512459160 cites W2095004082 @default.
• W2512459160 cites W2098622281 @default.
• W2512459160 cites W2102748867 @default.
• W2512459160 cites W2109184821 @default.
• W2512459160 cites W2118613375 @default.
• W2512459160 cites W2122075744 @default.
• W2512459160 cites W2124049260 @default.
• W2512459160 cites W2126791288 @default.
• W2512459160 cites W2129518001 @default.
• W2512459160 cites W2134922972 @default.
• W2512459160 cites W2138401170 @default.
• W2512459160 cites W2144111452 @default.
• W2512459160 cites W2147284262 @default.
• W2512459160 cites W2148026027 @default.
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• W2512459160 cites W2168142301 @default.
• W2512459160 cites W2171672780 @default.
• W2512459160 cites W2226813615 @default.
• W2512459160 cites W2408497954 @default.
• W2512459160 cites W2588612296 @default.
• W2512459160 cites W3102438208 @default.
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• W2512459160 doi "https://doi.org/10.1002/2016je005052" @default.
• W2512459160 hasPublicationYear "2016" @default.
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