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A Closer Look at Water-Related Geoloqic Activity on Mars

机译:仔细研究火星上与水有关的地球活动

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Water has supposedly marked the surface of Mars and produced characteristic tandforms. To understand the history of water on Mars, we take a close look at key locations with the High-Resolution imaging Science Experiment on board the Mars Reconnaissance Orbiter, reaching fine spatial scales of 25 to 32 centimeters per pixel. Boulders ranging up to ~2 meters in diameter are ubiquitous in the middle to high latitudes, which include deposits previously interpreted as finegrained ocean sediments or dusty snow. Bright gully deposits identify six locations with very recent activity, but these lie on steep (20° to 35°) slopes where dry mass wasting could occur. Thus, we cannot confirm the reality of ancient oceans or water in active gullies but do see evidence of fluvial modification of geologically recent mid-latitude gullies and equatorial impact craters.
机译:据说水已经在火星表面留下了痕迹,并形成了特征性的形状。为了了解火星上水的历史,我们通过火星侦察轨道飞行器上的高分辨率成像科学实验,仔细观察了关键位置,达到了每像素25到32厘米的精细空间尺度。直径约2米的巨石在中高纬度地区普遍存在,其中包括以前被解释为细粒海洋沉积物或多尘雪的沉积物。明亮的沟壑沉积物确定了最近活动的六个位置,但这些位置位于可能发生干物质浪费的陡峭(20°至35°)斜坡上。因此,我们无法确定活跃沟渠中古代海洋或水的真实存在,但确实可以看到最近发生的中纬度沟壑和赤道撞击坑的河流改造。

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