跳转到内容

File:PIA19805-SeasonalFlows-CopratesChasma-VallesMarineris-20150721.jpg

页面内容不支持其他语言。
这个文件来自维基共享资源
维基百科,自由的百科全书

原始文件 (975 × 1,023像素,文件大小:107 KB,MIME类型:image/jpeg


摘要

描述
English: PIA19805: For Anniversary of Orbiter's Launch: Seasonal Flows in Mars' Valles Marineris

http://photojournal.jpl.nasa.gov/catalog/PIA19805

Among the many discoveries by NASA's Mars Reconnaissance Orbiter since the mission was launched on Aug. 12, 2005, are seasonal flows on some steep slopes. These flows have a set of characteristics consistent with shallow seeps of salty water.

This July 21, 2015, image from the orbiter's High Resolution Imaging Science Experiment (HiRISE) camera shows examples of these flows on a slope within Coprates Chasma, which is part of the grandest canyon system on Mars, Valles Marineris. The image covers an area of ground one-third of a mile (536 meters) wide.

These flows are called recurring slope lineae because they fade and disappear during cold seasons and reappear in warm seasons, repeating this pattern every Martian year. The flows seen in this image are on a north-facing slope, so they are active in northern-hemisphere spring. The flows emanate from the relatively bright bedrock and flow onto sandy fans, where they are remarkably straight, following linear channels. Valles Marineris contains more of these flows than everywhere else on Mars combined. At any season, some are active, though on different slope aspects at different seasons.

Future human explorers (and settlers?) will need water to drink, grow food, produce oxygen to breath, and make rocket fuel. Bringing all of that water from Earth would be extremely expensive, so using water on Mars is essential. Although there is plenty of water ice at high latitudes, surviving the cold winters would be difficult. An equatorial source of water would be preferable, so Valles Marineris may be the best destination. However, the chemistry of this water must be understood before betting any lives on it.

For more information about recurring slope lineae, see http://www.jpl.nasa.gov/news/news.php?feature=3981 and http://www.uahirise.org/sim/2013-12-10/.

The location of the site in this image is 12.9 degrees south latitude, 295.4 degrees east latitude. The image is an excerpt from HiRISE observation ESP_042228_1670. Other image products from this observation are available at http://hirise.lpl.arizona.edu/ESP_042228_1670.

HiRISE is one of six instruments on the Mars Reconnaissance Orbiter. The University of Arizona, Tucson, operates HiRISE, which was built by Ball Aerospace & Technologies Corp., Boulder, Colorado. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter Project for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems, Denver, built the orbiter and collaborates with JPL to operate it.
日期
来源 http://photojournal.jpl.nasa.gov/jpeg/PIA19805.jpg
作者 NASA/JPL-Caltech/Univ. of Arizona

许可协议

Public domain 本文件完全由NASA创作,在美国属于公有领域。根据NASA的版权方针,NASA的材料除非另有声明否则不受版权保护。(参见Template:PD-USGov/zhNASA版权方针页面JPL图片使用方针。)
警告:

说明

添加一行文字以描述该文件所表现的内容

此文件中描述的项目

描绘内容

文件历史

点击某个日期/时间查看对应时刻的文件。

日期/时间缩⁠略⁠图大小用户备注
当前2015年8月11日 (二) 12:152015年8月11日 (二) 12:15版本的缩略图975 × 1,023(107 KB)DrbogdanUser created page with UploadWizard

以下页面使用本文件:

全域文件用途

以下其他wiki使用此文件: