{"id":787256,"date":"2024-08-13T20:35:52","date_gmt":"2024-08-14T01:35:52","guid":{"rendered":"http:\/\/spaceweekly.com\/?p=787256"},"modified":"2024-08-13T20:35:52","modified_gmt":"2024-08-14T01:35:52","slug":"we-keep-finding-water-on-mars-here-are-all-the-places-it-might-be","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=787256","title":{"rendered":"We keep finding water on Mars \u2013 here are all the places it might be"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div id=\"\">\n<figure class=\"ArticleImage\">\n<div class=\"Image__Wrapper\"><\/div><figcaption class=\"ArticleImageCaption\">\n<div class=\"ArticleImageCaption__CaptionWrapper\">\n<p class=\"ArticleImageCaption__Title\">Martian water may be lurking beneath \u2013 or even above \u2013 the planet\u2019s surface<\/p>\n<p class=\"ArticleImageCaption__Credit\">NASA\/JPL\/USGS<\/p>\n<\/div>\n<\/figcaption><\/figure>\n<\/p>\n<p>Mars is not as arid as it may seem. Billions of years ago, the surface of the Red Planet rippled with oceans and rivers of liquid water, but now it seems that all of that fluid has disappeared, leaving behind a dusty wasteland. However, as we have explored the planet with orbiters, landers, rovers and even telescope images from afar, traces of water keep popping up.<\/p>\n<p>Each hint tantalises researchers because of how crucial water is for living organisms and how helpful it could be for future exploration. Water has now been discovered all over Mars, in many different forms \u2013 here are five places it has been spotted.<\/p>\n<h2>1. Buried underground<\/h2>\n<figure class=\"ArticleImage\">\n<div class=\"Image__Wrapper\"><img decoding=\"async\" class=\"Image lazyload\" width=\"1350\" height=\"900\" alt=\"The InSight Lander NASA ID: PIA22227 This artist's concept shows the InSight lander, its sensors, cameras and instruments. InSight is will take the first-ever-in-depth look at Mars' &quot;inner space.&quot; InSight stands for Interior Exploration using Seismic Investigations, Geodesy and Heat Transport. Its three instruments are a seismometer, a heat flow probe, and a radio science experiment. These instruments will shed light on how warm and geologically active Mars still is, study its reflexes as it whips about in its orbit around the sun, and provide essential clues on the evolution of the rocky planets of our solar system. So while InSight is a Mars mission, it's also more than a Mars mission. InSight will launch between May 5 through June 8, 2018 from Vandenberg Air Force Base in California. https:\/\/photojournal.jpl.nasa.gov\/catalog\/PIA22227\" sizes=\"auto, (min-width: 1288px) 837px, (min-width: 1024px) calc(57.5vw + 55px), (min-width: 415px) calc(100vw - 40px), calc(70vw + 74px)\" srcset=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=300 300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=400 400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=500 500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=600 600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=700 700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=800 800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=837 837w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=900 900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1003 1003w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1100 1100w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1200 1200w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1300 1300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1400 1400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1500 1500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1600 1600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1674 1674w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1700 1700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1800 1800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=1900 1900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg?width=2006 2006w\" src=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200312\/SEI_217275619.jpg\" loading=\"lazy\" data-image-context=\"Article\" data-image-id=\"2443771\" data-caption=\"The InSight lander, visualised here, recently found another potential water reservoir on Mars\" data-credit=\"NASA\/JPL-Caltech\"\/><\/div><figcaption class=\"ArticleImageCaption\">\n<div class=\"ArticleImageCaption__CaptionWrapper\">\n<p class=\"ArticleImageCaption__Title\">The InSight lander, visualised here, recently found another potential water reservoir on Mars<\/p>\n<p class=\"ArticleImageCaption__Credit\">NASA\/JPL-Caltech<\/p>\n<\/div>\n<\/figcaption><\/figure>\n<\/p>\n<p>Just beneath Mars\u2019s parched surface lies a wonderland of water ice. These deposits are kept insulated by the layers of dust on top of them, but erosion and meteorite impacts can expose them to the prying eyes of our orbiters. A single ice deposit recently identified using data from the Mars Express orbiter seems to contain enough water to cover the entire surface of Mars in an ocean 1.5 to 2.7 metres deep.<\/p>\n<p><span class=\"js-content-prompt-opportunity\"\/><\/p>\n<p>It\u2019s not just ice buried under the shifting orange sands. Hints of a huge lake beneath the planet\u2019s south pole have been controversial \u2013 it may simply be wet silt or volcanic rock. But a new study using data from the InSight lander has revealed another possible reservoir of water near the planet\u2019s equator. InSight found this water buried 11.5\u00a0to 20 kilometres underground by feeling for marsquakes and measuring how fast those seismic waves travelled, which revealed that the rocks those quakes were propagating through seemed to be saturated with water.<\/p>\n<h2>2. Frosting over the poles<\/h2>\n<figure class=\"ArticleImage\">\n<div class=\"Image__Wrapper\"><img decoding=\"async\" class=\"Image lazyload\" width=\"1350\" height=\"900\" alt=\"Most surface ice on Mars is temporary. The polar layered deposits are thick stacks of permanent water ice at each pole, and the South Polar residual cap may be a permanent (although dynamic) layer of carbon dioxide ice as seen by NASA's Mars Reconnaissanc\" sizes=\"auto, (min-width: 1288px) 837px, (min-width: 1024px) calc(57.5vw + 55px), (min-width: 415px) calc(100vw - 40px), calc(70vw + 74px)\" srcset=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=300 300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=400 400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=500 500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=600 600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=700 700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=800 800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=837 837w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=900 900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1003 1003w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1100 1100w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1200 1200w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1300 1300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1400 1400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1500 1500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1600 1600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1674 1674w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1700 1700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1800 1800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=1900 1900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg?width=2006 2006w\" src=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200307\/SEI_217276142.jpg\" loading=\"lazy\" data-image-context=\"Article\" data-image-id=\"2443770\" data-caption=\"Frost in a crater on Mars's Northern Plains\" data-credit=\"NASA\/JPL-Caltech\/Univ. of Arizona\"\/><\/div><figcaption class=\"ArticleImageCaption\">\n<div class=\"ArticleImageCaption__CaptionWrapper\">\n<p class=\"ArticleImageCaption__Title\">Frost in a crater on Mars\u2019s Northern Plains<\/p>\n<p class=\"ArticleImageCaption__Credit\">NASA\/JPL-Caltech\/Univ. of Arizona<\/p>\n<\/div>\n<\/figcaption><\/figure>\n<\/p>\n<p>Getting at the buried water\u00a0on Mars would be difficult, so perhaps a more promising reservoir for future explorers is bared right on the surface. The poles on Mars have ice caps just like on Earth, and we have known about them for decades. Many craters on Mars also have smaller ice sheets inside them. These are the only places on Mars\u2019s\u00a0surface that stay cold enough for ice to stick around.<\/p>\n<p>However, there is also some transient frost that forms at high latitudes on Mars, where the air tends to be colder and more humid. On some frigid Martian mornings, volcanic peaks frost over as well, which is probably due to water vapour freezing out of the atmosphere.<\/p>\n<h2>3. Floating in the atmosphere<\/h2>\n<figure class=\"ArticleImage\">\n<div class=\"Image__Wrapper\"><img decoding=\"async\" class=\"Image lazyload\" width=\"1350\" height=\"901\" alt=\"Mars Daily Global Image from April 1999 Twelve orbits a day provide NASA Mars Global Surveyor MOC wide angle cameras a global napshot of weather patterns across the planet. Here, bluish-white water ice clouds hang above the Tharsis volcanoes.\" sizes=\"auto, (min-width: 1288px) 837px, (min-width: 1024px) calc(57.5vw + 55px), (min-width: 415px) calc(100vw - 40px), calc(70vw + 74px)\" srcset=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=300 300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=400 400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=500 500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=600 600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=700 700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=800 800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=837 837w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=900 900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1003 1003w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1100 1100w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1200 1200w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1300 1300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1400 1400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1500 1500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1600 1600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1674 1674w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1700 1700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1800 1800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=1900 1900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg?width=2006 2006w\" src=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13205951\/SEI_217292749.jpg\" loading=\"lazy\" data-image-context=\"Article\" data-image-id=\"2443792\" data-caption=\"Mars's atmosphere may hold hints of travelling water\" data-credit=\"NASA\/JPL\/MSSS\"\/><\/div><figcaption class=\"ArticleImageCaption\">\n<div class=\"ArticleImageCaption__CaptionWrapper\">\n<p class=\"ArticleImageCaption__Title\">Mars\u2019s atmosphere may hold hints of travelling water<\/p>\n<p class=\"ArticleImageCaption__Credit\">NASA\/JPL\/MSSS<\/p>\n<\/div>\n<\/figcaption><\/figure>\n<\/p>\n<p>Because of the bitter cold and tenuous\u00a0atmosphere on Mars, any liquid water on the surface would sublimate away, turning directly into gas and floating up into the air. Water vapour in the atmosphere is a sign of water and ice migrating across the planet\u2019s surface to form frost, but it is only present in minuscule amounts. Occasionally, there is enough water vapour in one area to generate a few wispy clouds, but for the most part it is nearly negligible.<\/p>\n<h2>4. Running downhill<\/h2>\n<figure class=\"ArticleImage\">\n<div class=\"Image__Wrapper\"><img decoding=\"async\" class=\"Image lazyload\" width=\"1350\" height=\"900\" alt=\"Recurring Lineae on Slopes at Hale Crater, Mars NASA ID: PIA19916 Dark, narrow streaks on Martian slopes such as these at Hale Crater are inferred to be formed by seasonal flow of water on contemporary Mars. The streaks are roughly the length of a football field. The imaging and topographical information in this processed, false-color view come from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. These dark features on the slopes are called &quot;recurring slope lineae&quot; or RSL. Planetary scientists using observations with the Compact Reconnaissance Imaging Spectrometer on the same orbiter detected hydrated salts on these slopes at Hale Crater, corroborating the hypothesis that the streaks are formed by briny liquid water. The image was produced by first creating a 3-D computer model (a digital terrain map) of the area based on stereo information from two HiRISE observations, and then draping a ...more Date Created:2015-09-28\" sizes=\"auto, (min-width: 1288px) 837px, (min-width: 1024px) calc(57.5vw + 55px), (min-width: 415px) calc(100vw - 40px), calc(70vw + 74px)\" srcset=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=300 300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=400 400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=500 500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=600 600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=700 700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=800 800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=837 837w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=900 900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1003 1003w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1100 1100w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1200 1200w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1300 1300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1400 1400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1500 1500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1600 1600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1674 1674w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1700 1700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1800 1800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=1900 1900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg?width=2006 2006w\" src=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13200313\/SEI_217275789.jpg\" loading=\"lazy\" data-image-context=\"Article\" data-image-id=\"2443772\" data-caption=\"Dark, narrow streaks on Martian slopes like these at Hale Crater may be formed by seasonal water flow\" data-credit=\"NASA\/JPL-Caltech\/Univ. of Arizona\"\/><\/div><figcaption class=\"ArticleImageCaption\">\n<div class=\"ArticleImageCaption__CaptionWrapper\">\n<p class=\"ArticleImageCaption__Title\">Dark, narrow streaks on Martian slopes like these at Hale Crater may be formed by seasonal water flow<\/p>\n<p class=\"ArticleImageCaption__Credit\">NASA\/JPL-Caltech\/Univ. of Arizona<\/p>\n<\/div>\n<\/figcaption><\/figure>\n<\/p>\n<p>Perhaps the most controversial of the possible signs of water on Mars are recurring slope lineae, which are dark streaks that sporadically appear running down the sloped edges of craters. They were first discovered in 2011, and since then there has been lively debate among researchers about what causes them. They occur primarily in the warmest parts of the year, so they could be caused by ice melting and then running downhill before evaporating away \u2013 which would make them the only liquid water ever spotted on the surface of Mars. Or, they could be simple sand flows. Over time, the latter hypothesis has gained support, but some researchers hold out hope that there could be a trickle of liquid water on the Red Planet.<\/p>\n<h2>5. Trapped in rocks<\/h2>\n<figure class=\"ArticleImage\">\n<div class=\"Image__Wrapper\"><img decoding=\"async\" class=\"Image lazyload\" width=\"1350\" height=\"900\" alt=\"This image from NASA's Mars Reconnaissance Orbiter shows one of millions of small (10s of meters in diameter) craters and their ejecta material that dot the Elysium Planitia region of Mars. The small craters were likely formed when high-speed blocks of rock were thrown out by a much larger impact (about 10-kilometers in diameter) and fell back to the ground.\" sizes=\"auto, (min-width: 1288px) 837px, (min-width: 1024px) calc(57.5vw + 55px), (min-width: 415px) calc(100vw - 40px), calc(70vw + 74px)\" srcset=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=300 300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=400 400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=500 500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=600 600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=700 700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=800 800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=837 837w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=900 900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1003 1003w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1100 1100w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1200 1200w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1300 1300w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1400 1400w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1500 1500w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1600 1600w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1674 1674w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1700 1700w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1800 1800w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=1900 1900w, https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg?width=2006 2006w\" src=\"https:\/\/images.newscientist.com\/wp-content\/uploads\/2024\/08\/13204308\/SEI_217291903.jpg\" loading=\"lazy\" data-image-context=\"Article\" data-image-id=\"2443788\" data-caption=\"The Red Planet's rocks may have sucked up its water\" data-credit=\"NASA\/JPL-Caltech\/Univ. of Arizona\"\/><\/div><figcaption class=\"ArticleImageCaption\">\n<div class=\"ArticleImageCaption__CaptionWrapper\">\n<p class=\"ArticleImageCaption__Title\">The Red Planet\u2019s rocks may have sucked up its water<\/p>\n<p class=\"ArticleImageCaption__Credit\">NASA\/JPL-Caltech\/Univ. of Arizona<\/p>\n<\/div>\n<\/figcaption><\/figure>\n<\/p>\n<p>If Mars used to be covered in water, and now all that\u2019s left is a bit of ice and a whole lot of dust and stone, where did all that water go? One possible solution is that it got slurped up into the rocks themselves. Mars rovers have found no shortage of minerals with water molecules incorporated into their chemical structures all over the planet.<\/p>\n<p>This process is irreversible, so there is no way for us to get all that water back \u2013 but accounting for where all the water went is crucial to understanding what Mars was like before it dried out. That may be our best chance for understanding if Mars ever really was hospitable to life.<\/p>\n<section class=\"ArticleTopics\">\n<p class=\"ArticleTopics__Heading\">Topics:<\/p>\n<\/section><\/div>\n<p><br \/>\n<br \/><a href=\"https:\/\/www.newscientist.com\/article\/2443738-we-keep-finding-water-on-mars-here-are-all-the-places-it-might-be\/?utm_campaign=RSS%7CNSNS&#038;utm_source=NSNS&#038;utm_medium=RSS&#038;utm_content=space&#038;rand=772163\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Martian water may be lurking beneath \u2013 or even above \u2013 the planet\u2019s surface NASA\/JPL\/USGS Mars is not as arid as it may seem. Billions of years ago, the surface&hellip; <\/p>\n","protected":false},"author":1,"featured_media":787257,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[39],"tags":[],"class_list":["post-787256","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-new-scientist"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/787256","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=787256"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/787256\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/787257"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=787256"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=787256"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=787256"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}