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Groups > sci.physics > #525357 > unrolled thread
| Started by | Sam Wormley <swormley1@gmail.com> |
|---|---|
| First post | 2015-10-08 20:07 -0500 |
| Last post | 2015-10-14 16:44 -0700 |
| Articles | 13 — 7 participants |
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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
| From | Sam Wormley <swormley1@gmail.com> |
|---|---|
| Date | 2015-10-08 20:07 -0500 |
| Subject | Parts of Mars used to be Earth-like |
| Message-ID | <peCdnShrJMzxjorLnZ2dnUU7-bkAAAAA@giganews.com> |
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.
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| From | The Starmaker <starmaker@ix.netcom.com> |
|---|---|
| Date | 2015-10-09 00:41 -0700 |
| Message-ID | <56176FBB.431E@ix.netcom.com> |
| In reply to | #525357 |
Sam Wormley wrote: > > Parts of Mars used to be Earth-like have you been to earth lately? there is no planet...Like Earth.
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| From | "reber g=emc^2" <herbertglazier0@gmail.com> |
|---|---|
| Date | 2015-10-09 10:33 -0700 |
| Message-ID | <ec9a61fb-baaf-4fa2-bced-fcb921657b14@googlegroups.com> |
| In reply to | #525357 |
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. Reality is Calif.is getting to look like Mars.No water.Lots of sand and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get the picture TreBert
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| From | Double-A <double-a3@hush.com> |
|---|---|
| Date | 2015-10-09 15:11 -0700 |
| Message-ID | <10f5d8da-93c3-426b-91ce-548a555f3edd@googlegroups.com> |
| In reply to | #525453 |
On Friday, October 9, 2015 at 10:33:04 AM UTC-7, reber g=emc^2 wrote: > 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. > > Reality is Calif.is getting to look like Mars.No water.Lots of sand and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get the picture TreBert That is how it started on Mars, Bert! Double-A
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| From | "reber g=emc^2" <herbertglazier0@gmail.com> |
|---|---|
| Date | 2015-10-11 11:16 -0700 |
| Message-ID | <f2993845-e738-4ed2-a5d6-977e7d801255@googlegroups.com> |
| In reply to | #525510 |
On Friday, October 9, 2015 at 3:11:21 PM UTC-7, Double-A wrote: > On Friday, October 9, 2015 at 10:33:04 AM UTC-7, reber g=emc^2 wrote: > > 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. > > > > Reality is Calif.is getting to look like Mars.No water.Lots of sand and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get the picture TreBert > > > That is how it started on Mars, Bert! > > Double-A AA Its Oct.10 and this weekend is over 100f.Not a cloud.Dry as a comet that swings in close to the Sun.People are fighting over shady parking spots.To hot to even go to a pool.Eating a raw MSP Tuna out of the can.Lots of liquids.This heat kills people over 75,and Iḿ tying to live as long as my granpa Good thing the Van runs cool,and has great air.TreBert
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| From | Double-A <double-a3@hush.com> |
|---|---|
| Date | 2015-10-11 14:21 -0700 |
| Message-ID | <0d59da3d-b66a-4163-a4b3-a62831772b63@googlegroups.com> |
| In reply to | #525724 |
On Sunday, October 11, 2015 at 11:16:19 AM UTC-7, reber g=emc^2 wrote: > On Friday, October 9, 2015 at 3:11:21 PM UTC-7, Double-A wrote: > > On Friday, October 9, 2015 at 10:33:04 AM UTC-7, reber g=emc^2 wrote: > > > 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. > > > > > > Reality is Calif.is getting to look like Mars.No water.Lots of sand and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get the picture TreBert > > > > > > That is how it started on Mars, Bert! > > > > Double-A > > AA Its Oct.10 and this weekend is over 100f.Not a cloud.Dry as a comet that swings in close to the Sun.People are fighting over shady parking spots.To hot to even go to a pool.Eating a raw MSP Tuna out of the can.Lots of liquids.This heat kills people over 75,and Iḿ tying to live as long as my granpa Good thing the Van runs cool,and has great air.TreBert How can you afford all the gas that van must consume? Double-A
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| From | "reber g=emc^2" <herbertglazier0@gmail.com> |
|---|---|
| Date | 2015-10-12 09:28 -0700 |
| Message-ID | <40be2690-ca7e-4952-99da-f31848f7ed63@googlegroups.com> |
| In reply to | #525747 |
On Sunday, October 11, 2015 at 2:21:32 PM UTC-7, Double-A wrote: > On Sunday, October 11, 2015 at 11:16:19 AM UTC-7, reber g=emc^2 wrote: > > On Friday, October 9, 2015 at 3:11:21 PM UTC-7, Double-A wrote: > > > On Friday, October 9, 2015 at 10:33:04 AM UTC-7, reber g=emc^2 wrote: > > > > 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. > > > > > > > > Reality is Calif.is getting to look like Mars.No water.Lots of sand and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get the picture TreBert > > > > > > > > > That is how it started on Mars, Bert! > > > > > > Double-A > > > > AA Its Oct.10 and this weekend is over 100f.Not a cloud.Dry as a comet that swings in close to the Sun.People are fighting over shady parking spots.To hot to even go to a pool.Eating a raw MSP Tuna out of the can.Lots of liquids.This heat kills people over 75,and Iḿ tying to live as long as my granpa Good thing the Van runs cool,and has great air.TreBert > > > How can you afford all the gas that van must consume? > > Double-A AA True van only gets 12 mpg but it saves me 120 bucks on motel bill.It runs like new.It has refrig,and I like can tuna,Lox,and Ocean Spray Cranberry.It has 5 speaker sterio and lots of storage.I love my van + I have a few bucks coming in on M&M. When nyou collect SS and have extra $$$$ coming in gas is not a big expense.Plus I shoot great pool when shooting for a Bud or 5 bucks. TreBert
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| From | "hanson" <hanson@quick.net> |
|---|---|
| Date | 2015-10-11 08:45 -0700 |
| Message-ID | <mve095$ufj$1@dont-email.me> |
| In reply to | #525453 |
<herbertglazier0@gmail.com> Glazier, the Swine "reber g=emc^2" wrote: > Sam Wormley wrote: >> Parts of Mars used to be Earth-like >> > http://arstechnica.com/science/2015/10/curiosity-is-climbing-a-martian-mountain-that-used-to-be-a-lake-bottom/ >> to which > Filthy Swine Glazier wrote > Reality is Calif.is getting to look like Mars.No water.Lots of sand and > dust. > Rocks everywhere.This is now,and not Once Upon a Time. Get the picture > TreBert > hanson wrote: As usual, Glazier you Swine, everybody but you did get the picture. "Reality is your Van look like Mars.No water.Lots of sand and dust. **Stolen** Rocks everywhere.This is now,and not Once Upon a Time. Get the picture, Glazier" > So, Glazier you filthy Swine, clean up your Van. > But the underlying question is that you, who bragged to have a Jewish Superiority complex, and an IQ of 122, and claims to know how everything works, ... ended up shitting into a bucket in a 25 year old van that you use as your residence on Wal-Mart's Parking Lot? > What went wrong, Glazier? ,
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| From | gilber34 <fafa@invalid.com> |
|---|---|
| Date | 2015-10-11 11:09 -0500 |
| Message-ID | <mve1it$g1a$1@speranza.aioe.org> |
| In reply to | #525453 |
On 10/9/2015 12:33 PM, reber g=emc^2 wrote: > On Thursday, October 8, 2015 at 6:07:59 PM UTC-7, Sam Wormley wrote: >> Parts of Mars used to be Earth-like > > Reality is Calif.is getting to look like Mars.No water.Lots of sand > and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get > the picture TreBert > California is already full of Aliens and spaced out entities, and Wallmarts California's hollywood continually broadcasts out fake history, and propaganda to support paid politicians. now, God is *getting* California, and thanks to its democrats cailfornia will never solve its water, or its tax problems. California needs to be walled off, and its beaches and surf relocated to Texas.
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| From | "reber g=emc^2" <herbertglazier0@gmail.com> |
|---|---|
| Date | 2015-10-12 13:34 -0700 |
| Message-ID | <a7edc1fd-5300-42f1-93ae-24a00e850b74@googlegroups.com> |
| In reply to | #525453 |
On Friday, October 9, 2015 at 10:33:04 AM UTC-7, reber g=emc^2 wrote: > 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. > > Reality is Calif.is getting to look like Mars.No water.Lots of sand and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get the picture TreBert As I type many parts on Earth look like Mars.S.Calif.looks more and more like Mars. It has dust and no water. TreBert
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| From | "reber g=emc^2" <herbertglazier0@gmail.com> |
|---|---|
| Date | 2015-10-13 15:41 -0700 |
| Message-ID | <4a98bbaa-8a07-40dc-b87f-024abef756b4@googlegroups.com> |
| In reply to | #525897 |
On Monday, October 12, 2015 at 1:34:29 PM UTC-7, reber g=emc^2 wrote: > On Friday, October 9, 2015 at 10:33:04 AM UTC-7, reber g=emc^2 wrote: > > 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. > > > > Reality is Calif.is getting to look like Mars.No water.Lots of sand and dust.Rocks everywhere.This is now,and not Once Upon a Time. Get the picture TreBert > > As I type many parts on Earth look like Mars.S.Calif.looks more and more like Mars. It has dust and no water. TreBert Once upon a time when Mars had great oceans just like Earth,and it was closer to the sun the Martians eat lobsters clams and cod.They washed it down with beer.I'm telling you all this for I'm looking to work with NASA. TreBert
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| From | Wally W. <ww84wa@aim.com> |
|---|---|
| Date | 2015-10-11 12:40 -0400 |
| Message-ID | <754l1b53mqpvjo1f0giu4m2tko504ds9a5@4ax.com> |
| In reply to | #525357 |
On Thu, 8 Oct 2015 20:07:56 -0500, 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/ ... and now, they are not. We had to go to Mars to find an example of something that changed?
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| From | "reber g=emc^2" <herbertglazier0@gmail.com> |
|---|---|
| Date | 2015-10-14 16:44 -0700 |
| Message-ID | <fc17db18-4ff9-41cc-ae71-e7e2ea6294dd@googlegroups.com> |
| In reply to | #525357 |
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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