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Originally posted by crackerjack
I'm sure Zorgon and Mike would be licking their chops over this thread,
Originally posted by rocksarerocks
Question, in which mission did the shuttle go to Mars?
Originally posted by rocksarerocks
The first thing you should learn is to never ever use marsanomoly research. The guy thinks NASA has an "automatic software removal" system that checks every picture and removes all artifacts.
Originally posted by habu71
1> As I recall (and I am sure I will be corrected if my recollection is wrong), original Rover imaging is black and white......if so, the colorization may affect what we see.
Originally posted by SuperSlovak
but offcoarse, the ats skeptic wont believe anything untill they themself are standing on mars looking up at the ruins.
Originally posted by puzzled2
Why wrong camera I see 3 metalic objects and a fence and its the wrong Camera??
Originally posted by zorgon
2) Phage showed water errosion... are you saying water eroded the rocks on Mar? But not in that area... those are not water errosion marks...
Phage also showed the basalt colums that fracture into hexagonal posts... that requires a huge lava flow under special conditions... there is no lava flow present so that is an erroneous comparson
If your going to use geology in your case, at least have an understanding of geology, or you just look silly, or desparate
Wiki
Gusev Crater is a crater on the planet Mars and is located at 175.4°E 14.6°S. The crater is about 170 kilometers in diameter and formed approximately three to four billion years ago. It was named after Russian astronomer Matvei Gusev (1826–1866) in 1876.
A channel system named Ma'adim Vallis drains into it that probably carried liquid water, or water and ice, at some point in Mars' past. The crater appears to be an old crater lake bed, filled with sediments up to 3000 feet thick. Some exposed outcrops appear to show faint layering, and some researchers also believe that landforms visible in images of the mouth of Ma'adim Vallis where it enters Gusev Crater resemble landforms seen in some terrestrial river deltas.
Wiki
Ma'adim Vallis is one of the largest canyons on Mars, about 700 km long and significantly larger than Earth's Grand Canyon. It is over 20 km wide and 2 km deep in some places. It runs from a region of southern lowlands thought to have once contained a large group of lakes (see Eridania Lake) north to Gusev crater near the equator.
Ma'adim Vallis is thought to have been carved by flowing water early in Mars' history. Some of the short narrow channels along the walls of Ma'adim are probably sapping channels. Sapping occurs when groundwater partially dissolves and undermines the rock, which collapses into debris deposits and is carried away by other erosion processes.
Wiki
Apollinaris Patera is the former name of Apollinaris Mons, a shield volcano on Mars's surface. It is situated near the equator in the south hemisphere, southeast of the shield volcano Elysium Mons on the Elysium Planitia, and north of Gusev crater.
Apollinaris Mons is about 5 kilometres high with a base about 296 kilometres in diameter.[1] On the top of this volcano is a small crater with an irregular border (the "patera"), which was probably made by an explosive, or pyroclastic, eruption.
Scientists Say Volcanic Activity Formed Home Plate (In Gusev) on Mars
Scientists have found evidence that Home Plate at Gusev crater on Mars is composed of debris deposited from a hydrovolcanic explosion. The finding suggests that water may have been involved in driving an eruption that formed the deposits found on Home Plate.
In a paper published in the May 4, 2007, issue of the journal Science, the team of scientists reports that Home Plate is composed of debris deposited from a hydrovolcanic explosion that occurred when molten volcanic basalt came into contact with subsurface fluid, perhaps brine.
...
A particularly notable feature in the lower unit is a clast with deformed layers beneath it, interpreted to be a bomb sag. Bomb sags are found in volcanic deposits on Earth, where large clasts, or fragments of rock, ejected from an explosive event are emplaced ballistically into deformable materials, causing depression of layering. Bomb sags on Earth typically indicate that the deformed materials were wet at the time of emplacement, but the scientists cannot rule out the possibility of sag formation resulting from compaction and gas-supported flow of dry materials.
Pyroclastic Activity at Home Plate in Gusev Crater, Mars
Home Plate is a layered plateau in Gusev crater on Mars. It is composed of clastic rocks of moderately altered alkali basalt composition, enriched in some highly volatile elements. A coarsegrained lower unit lies under a finer-grained upper unit. Textural observations indicate that the lower strata were emplaced in an explosive event, and geochemical considerations favor an explosive volcanic origin over an impact origin. The lower unit likely represents accumulation of pyroclastic materials, whereas the upper unit may represent eolian reworking of the same pyroclastic materials.
Originally posted by Phage
Here is the raw image
marsrovers.jpl.nasa.gov...
Notice a similar porous rock in the right foreground
Originally posted by rocksarerocks
reply to post by SuperSlovak
We won't believe it because it's a damn rock. Nothing more. How about you provide some proof of your belief before you go throwing the word skeptic around every time someone questions the day after day RIDICULOUS posts that are made here.