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Groups > sci.physics > #526198
| Newsgroups | sci.physics |
|---|---|
| Date | 2015-10-14 16:44 -0700 |
| References | <peCdnShrJMzxjorLnZ2dnUU7-bkAAAAA@giganews.com> |
| Message-ID | <fc17db18-4ff9-41cc-ae71-e7e2ea6294dd@googlegroups.com> (permalink) |
| Subject | Re: Parts of Mars used to be Earth-like |
| From | "reber g=emc^2" <herbertglazier0@gmail.com> |
On Thursday, October 8, 2015 at 6:07:59 PM UTC-7, Sam Wormley wrote: > Parts of Mars used to be Earth-like > > http://arstechnica.com/science/2015/10/curiosity-is-climbing-a-martian-mountain-that-used-to-be-a-lake-bottom/ > > > > One of the joys of geology is painting a picture of a different > > world--a long-ago world otherwise completely lost to us. If you're a > > planetary geologist, you have the chance to pull off that trick with > > a properly different world, one not currently named Earth. Courtesy > > of Curiosity, the robotic geologist currently exploring Mars, we have > > a new picture of the history of the crater the rover is roving in. > > > > Gale Crater was excavated by an impact event roughly 3.7 billion > > years ago. Rising over five kilometers from the floor of the crater > > is Mount Sharp (officially Aeolis Mons). How'd it get there? That > > question is, in a way, interesting enough that we went there to find > > out. > > > > After landing safely on the plain surrounding Mount Sharp, Curiosity > > has made its way to the base of the mountain, stopping to smell the > > rocks along the way. Climbing Mount Sharp takes the rover on a trip > > through martian history, as the mountain is basically a layer cake of > > sedimentary rock. A new study published this week by 47 researchers > > back on Earth focuses on what we've seen so far in the two layers at > > the base of the cake. > > > > In the lower part of the basal layer, there are sandstones as well as > > some gravelly layers. The sandstones show a pattern called > > "cross-bedding"--repeated diagonal lines between the top and bottom of > > a layer. These are the remains of crawling ripples or dunes. In this > > case they are short ripples deposited by something flowing toward the > > center of the crater. Together with the presence of the gravels, this > > points to the action of streams. > > > > -- > > sci.physics is an unmoderated newsgroup dedicated > to the discussion of physics, news from the physics > community, and physics-related social issues. Mars never could have had an atmosphere like Earth.It never rained on Mars not even once apon a time.It has the tallest volcano good reason why.43 years ago a lander came down on a huge dust storm,and I was hit by a dust storm driving out of Vegas. Today I was in a swimming pool that has more water in it than all that NASA will ever find on Mars TreBert
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Parts of Mars used to be Earth-like Sam Wormley <swormley1@gmail.com> - 2015-10-08 20:07 -0500
Re: Parts of Mars used to be Earth-like The Starmaker <starmaker@ix.netcom.com> - 2015-10-09 00:41 -0700
Re: Parts of Mars used to be Earth-like "reber g=emc^2" <herbertglazier0@gmail.com> - 2015-10-09 10:33 -0700
Re: Parts of Mars used to be Earth-like Double-A <double-a3@hush.com> - 2015-10-09 15:11 -0700
Re: Parts of Mars used to be Earth-like "reber g=emc^2" <herbertglazier0@gmail.com> - 2015-10-11 11:16 -0700
Re: Parts of Mars used to be Earth-like Double-A <double-a3@hush.com> - 2015-10-11 14:21 -0700
Re: Parts of Mars used to be Earth-like "reber g=emc^2" <herbertglazier0@gmail.com> - 2015-10-12 09:28 -0700
Re: Parts of Mars used to be Earth-like "hanson" <hanson@quick.net> - 2015-10-11 08:45 -0700
Re: Parts of Mars used to be Earth-like gilber34 <fafa@invalid.com> - 2015-10-11 11:09 -0500
Re: Parts of Mars used to be Earth-like "reber g=emc^2" <herbertglazier0@gmail.com> - 2015-10-12 13:34 -0700
Re: Parts of Mars used to be Earth-like "reber g=emc^2" <herbertglazier0@gmail.com> - 2015-10-13 15:41 -0700
Re: Parts of Mars used to be Earth-like Wally W. <ww84wa@aim.com> - 2015-10-11 12:40 -0400
Re: Parts of Mars used to be Earth-like "reber g=emc^2" <herbertglazier0@gmail.com> - 2015-10-14 16:44 -0700
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