incubo
Početnik
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- 47
I da ima dokaza zašto bi iko to saopštio javnosti...tek ćemo da postanemo Marsovci...
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MARS - Dokaz postojanja civilizacije na Marsu; Jesmo li mi zapravo Marsovci?!
- Začetnik teme dominguez
- Datum pokretanja
dominguez
Zainteresovan član
- Poruka
- 106
Slažem se, zato mislim da je na nama (proletarijatu) da dođemo sami do istine!!! Pa nek Zlobama i elita pričaju i veruju u šta god žele....
A da ćemo postati Marsovci, to je neizbežno, da.... Samo se nadam da će naše magnetno polje biti u funkciji još par vekova da proživimo malo
...
dominguez
Zainteresovan član
- Poruka
- 106
Нађена глина богата минералним материјама...
''The discovery of Martian clays rich in minerals formed by water activity suggest the planet could have supported life relatively recently in its history.
Identified from data collected by NASA’s Mars Reconnaissance Orbiter (MRO), the minerals were found inside two small depressions in a region of the planet known as Noctis Labyrinthus, or the ‘labyrinth of the night’.
The findings, published earlier this month in the journal Geology, suggest the region may have previously been habitable when drier conditions existed on the planet’s surface.
“We discovered locations at Noctis Labyrinthus that show many kinds of minerals that formed by water activity,” said Catherine Weitz, lead author and senior scientist at the Planetary Science Institute in Arizona.
“The clays we found, called iron/magnesium (Fe/Mg)-smectites, are much younger at Noctis Labyrinthus relative to those found in the ancient rocks on Mars, which indicates a different water environment in these depressions relative to what was happening elsewhere on Mars.”
Mapping hydrated minerals
Smectites are a specific type of clay mineral that expand and contract when immersed in water. They are common on Earth where they form by chemical reactions between circulating water and primary silicate rocks.
Weitz and her co-authors studied approximately 300 meters of vertically exposed layered rocks within two 30 to 40-kilometre-wide depressions, called troughs, near the western end of the Valles Marineris canyon system.
The team used high-resolution images and hyperspectral data from instruments aboard the MRO spacecraft. They combined this with digital terrain models to determine elevations and view geometric relationships between units.
The team was then able to map hydrated minerals and understand how the water chemistry had varied with time within each trough, said Weitz.
Retracing water activity and volcanism
Each trough probably experienced multiple episodes where water partially filled in low-lying regions and deposited minerals.
As each trough continued to enlarge and experience collapse over time, older minerals became buried and separated, followed by deposition of younger minerals, then finally erosion to re-expose buried units.
Volcanism from the Tharsis volcanoes to the west may have created subsurface water that was subsequently transported through the ground and into the troughs.
Localised volcanism that produced ash and gases, hydrothermal activity, and melting snow or ice within the troughs could have also produced some of the minerals.
The observed minerals indicate water varied in pH levels over time, in one trough from acidic to neutral, and in the other trough from neutral to acidic and back to neutral.
Potential oasis for life
“These types of minerals had already been discovered in some of the older terranes on Mars when the climate there may have been warmer and wetter,” explained geologist Marc Norman from the Australian National University, who was not involved in the study.
“But life may not have had a chance to get started or at least would have been very simple and perhaps difficult to recognise or distinguish from abiogenic chemicals.”
The significance of this discovery, said Norman, “is that they found these hydrated alteration products in a much younger geological terrane of Mars, which looks like it has an age of perhaps only 2 billion years old”.
This is less than half the age of the solar system – both Earth and Mars are about 4.5 billion years old. At the same time life on Earth was robust and complex, making it easier to identify as uniquely biological, commented Norman.
“This terrane may have provided an oasis for life on Mars to survive and evolve, and would certainly be an interesting place to explore further with landers and possibly sample return missions to bring real material back to labs on Earth for detailed study,” he added.
However, such a mission may prove too risky given the landscape. “These troughs would be fantastic places to send a rover, but unfortunately the rugged terrain makes it unsafe both for landing and for driving,” said Weitz.''
http://www.cosmosmagazine.com/news/martian-clay-hints-life/
''The discovery of Martian clays rich in minerals formed by water activity suggest the planet could have supported life relatively recently in its history.
Identified from data collected by NASA’s Mars Reconnaissance Orbiter (MRO), the minerals were found inside two small depressions in a region of the planet known as Noctis Labyrinthus, or the ‘labyrinth of the night’.
The findings, published earlier this month in the journal Geology, suggest the region may have previously been habitable when drier conditions existed on the planet’s surface.
“We discovered locations at Noctis Labyrinthus that show many kinds of minerals that formed by water activity,” said Catherine Weitz, lead author and senior scientist at the Planetary Science Institute in Arizona.
“The clays we found, called iron/magnesium (Fe/Mg)-smectites, are much younger at Noctis Labyrinthus relative to those found in the ancient rocks on Mars, which indicates a different water environment in these depressions relative to what was happening elsewhere on Mars.”
Mapping hydrated minerals
Smectites are a specific type of clay mineral that expand and contract when immersed in water. They are common on Earth where they form by chemical reactions between circulating water and primary silicate rocks.
Weitz and her co-authors studied approximately 300 meters of vertically exposed layered rocks within two 30 to 40-kilometre-wide depressions, called troughs, near the western end of the Valles Marineris canyon system.
The team used high-resolution images and hyperspectral data from instruments aboard the MRO spacecraft. They combined this with digital terrain models to determine elevations and view geometric relationships between units.
The team was then able to map hydrated minerals and understand how the water chemistry had varied with time within each trough, said Weitz.
Retracing water activity and volcanism
Each trough probably experienced multiple episodes where water partially filled in low-lying regions and deposited minerals.
As each trough continued to enlarge and experience collapse over time, older minerals became buried and separated, followed by deposition of younger minerals, then finally erosion to re-expose buried units.
Volcanism from the Tharsis volcanoes to the west may have created subsurface water that was subsequently transported through the ground and into the troughs.
Localised volcanism that produced ash and gases, hydrothermal activity, and melting snow or ice within the troughs could have also produced some of the minerals.
The observed minerals indicate water varied in pH levels over time, in one trough from acidic to neutral, and in the other trough from neutral to acidic and back to neutral.
Potential oasis for life
“These types of minerals had already been discovered in some of the older terranes on Mars when the climate there may have been warmer and wetter,” explained geologist Marc Norman from the Australian National University, who was not involved in the study.
“But life may not have had a chance to get started or at least would have been very simple and perhaps difficult to recognise or distinguish from abiogenic chemicals.”
The significance of this discovery, said Norman, “is that they found these hydrated alteration products in a much younger geological terrane of Mars, which looks like it has an age of perhaps only 2 billion years old”.
This is less than half the age of the solar system – both Earth and Mars are about 4.5 billion years old. At the same time life on Earth was robust and complex, making it easier to identify as uniquely biological, commented Norman.
“This terrane may have provided an oasis for life on Mars to survive and evolve, and would certainly be an interesting place to explore further with landers and possibly sample return missions to bring real material back to labs on Earth for detailed study,” he added.
However, such a mission may prove too risky given the landscape. “These troughs would be fantastic places to send a rover, but unfortunately the rugged terrain makes it unsafe both for landing and for driving,” said Weitz.''
http://www.cosmosmagazine.com/news/martian-clay-hints-life/
- Poruka
- 2.667
Zivot ne moze da stigne sa Marsa.
Sa Marsa (ili neke druge planete) mogu da stignu samo odredjene vrste zivih bica, a ne zivot kao takav.
Tj. - sem ukoliko ne verujete u gluposti o evoluciji zivota iz neorganske materije.
Sa Marsa (ili neke druge planete) mogu da stignu samo odredjene vrste zivih bica, a ne zivot kao takav.
Tj. - sem ukoliko ne verujete u gluposti o evoluciji zivota iz neorganske materije.
Brzi Bravari Srbije
Veoma poznat
- Poruka
- 12.987
Mada...neki na forumu deluju kao da su sa Marsa pali....
Mada...neki na forumu deluju kao da su sa Marsa pali....
Ne bih se začudio tome
gost 326638
Primećen član
- Poruka
- 726
Mi smo Merkurci , a ne Marsovci .
sremski vuk
Elita
- Poruka
- 16.113
nerazumem sta se vidi
Poznavalac stvari
Legenda
- Poruka
- 60.338
Наравно да може као неки од примитивних облика на нивоу вируса, бактерија...
Приликом удара великих метеорита о тло Марса, а због много слабије гравитације и ређе атмосфер хиљаде тона ,,марсетине(
)" бива избачено у простор сунчевог система, нешто од тог камења привуче земаљска гравитација, а већи комади преживе пад кроз атмосферу као она два фрагмента марсетине нађених на Антарктику за које се сматра да имају неки види биолошке активности неземаљског порекла.https://sr.wikipedia.org/sr/Метеор
http://static.astronomija.org.rs/suncsist/planete/Mars/meteoriti.htm
http://www.rts.rs/page/magazine/sr/...9508/zivot-na-zemlji-poreklom-iz-svemira.html
Бтв Цвето еволуција је чињеница као и велики прасак, гравитација и многе друге ствари које ниси способан да појмиш па их мрзиш из незнања!
Poslednja izmena:
jos_1_5ak
Poznat
- Poruka
- 9.462
Ne ni evolucija a ni Veliki prasak nisu cinjenice jer da su cinjenice ne se zvale samo TEORIJE.
Inace sto je interesantno za Mars , tamo su nasli jednu odredjenu vrstu izotopa koja nastaje samo posle nuklearne eksplozije , sto je ovako veoma intrigantno otkrice , inace cak mozda i nije bilo nekog velikog rata globalnih razmera na Marsu koji je unistio civilizaciju, moguce da je cak i neka civilizacija Mars koristila kao poligon za testiranje oruzja ili neke druge vrste tehnologije.
Inace sto je interesantno za Mars , tamo su nasli jednu odredjenu vrstu izotopa koja nastaje samo posle nuklearne eksplozije , sto je ovako veoma intrigantno otkrice , inace cak mozda i nije bilo nekog velikog rata globalnih razmera na Marsu koji je unistio civilizaciju, moguce da je cak i neka civilizacija Mars koristila kao poligon za testiranje oruzja ili neke druge vrste tehnologije.
Poznavalac stvari
Legenda
- Poruka
- 60.338
Њутнова теорија гравитације, Специјална теорија релативитета, Општа теорија релативитета, Теорија рада топлотних машина, Квантна теорија...
Хипотеза која се у пракси докаже осматрањима, мерењима и експериментима сматра се научном истином и зове се теорија.
http://cudaprirode.com/portal/inosk...odnevnom-govoru-se-esto-teorija-krivo-koristi
Moze neki link gde postoji ta inormacija vezana za nuklearne eksplozije i izotope?
Što se tiče Marsa, moje lično mišljenje je da je na njemu prvo nastao život, mnogo pre nego na Zemlji.
Nalazi se u odgovarajućem pojasu gde je moguća tekuća voda, a obzirom da je manji od Zemlje zasigurno se površina planete mnogo pre formirala..
Zagrejenao jezgro je gledajući brzinu rotacije Marsa zasigurno formiralo dovoljno jako magnetno polje, koje je omogućavalo gustu atmosferu na bazi vodonika, sasvim sličnu praatmosferi Zemlje.
Kako je to Miler još davno dokazao u takvoj atmosferi se veoma lako stvaraju organski molekuli.
Uostalom, ako je život nastao na Zemlji nema nikakvog razloga da ne nastane i na Marsu, i to PRE nego na Zemlji jer je prosto manji i brže se ohladio.
Šta je nastalo na tom Marsu, to je nešto sasvim drugo.............
Hladjenjem jezgra Marsa nestalo je magnetnog polja koje je "čuvalo" atmosferu, a samim tim i život.
Inače Teorija evolucije se zove teorijom samo zbog pritiska i velikog uticaja religije.Ona je ubedljivo dokazana na mnogo primera, kroz fosilne ostatke ali i danasnje posmatranje evolucionih ciklusa ogledanih u borbi za opstanak i prirodnoj selekciji.
Za Veliki prasak se to opet ne može reći, jer postoje velike nedoumice u vezi istog, a neki modeli svemira(teorija mehura) skoro isto teko dobro objasnjavaju svemir oko nas, te to i dalje ostaje samo teorija.
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