A couple additional images. The same area as above at #20, with less contrast. Still high in contrast for a scenic image, but better ice small feature detail is seen here, and the actual contrast and tonal values of the items referenced is better seen in this view.A hard to find item.
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As these objects are not all the same, but are in a range of altered similar appearances in various other spots around the same large JP2 image area, I believe the basic question as to whether this is a geological or mineral formation can still be seen as open and unanswered. I would accept a single example as more likely to be an unexplained artifact of intelligent manufacture if I saw just this one item. As the others are varied states of wear, varied size, and differing context/physical content, I would estimate a process of an item type which is manipulated and alterable in effective display contextual to the scene as a integrated item type. The statement would be,' this is a type of object which is present throughout the scene in varied physical terms. It is therefore a proper element in the scene, and may be a common natural item type despite the manufactured appearance, and despite the in-congruence of the placement and complex symmetric assembly.' As this is a very shallow view as yet, we can wonder about the validation of the image content basically, and question the similarity to the MER spheroids in the complex 'stems' and chirality type displays along the stems issuing from some of the axial stems in both this large type spheroidal shape and the MER rover 'blueberry' spheroids.
This item matches the layered mounds generally, and they appear to be a ice suspended structure of concentric rings or hemispheric stacked spheroidal growths often covered by ices, or even made within the ices, in this JP2. Finding an item this ordered to be a natural process of inorganic mineral assembly will be a challenge to most all, I believe.
The second image is a cropped display of the HiRISE browse image from PSP_009943_2650.
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The ice cap scarp face shows a history of weathering and activity. I have marked a series of very old, even ghosted, or worn, craters which appear at differing layers within the Lower Unit of the Northern Polar Cap. The tremendous age of the craters, and the continuous regular circular edges show a pattern of ancient exposure(no ice of depth), at 2+ levels in the Lower Unit upon crater formation, and a stable subsequent stacking of the upper unit, with probable burial of the now exposed craters saving a clean edge for our current viewing. No real cratering of recent origin is seen at the collection of scarp face layers, and any produced might well be hidden by the ice cover, or healed rapidly by current processes. These are a history of dry and exposed surface at the high latitudes of the current ice cap. As the dunes are close in latitude to these formerly exposed craters making dry land events, can we assume that the climate of the dunes would be also a drier or less polar rotational oriented position? As the dunes are near gypsum deposits seen in some of the local dunes, can the items seen here be considered as massive crystalline structures from a warmer climate possibly? Can the large structures of bright material be fairly recent instead, with such large deposits forming in recent times?
Can crystalline structures form this way in deep ices as appears to be underway?
Are these a product immersion in a shallow sea of brines not frozen, but of possibly either ancient or recent liquid water?
Was this a hot environment when these large structures were formed?
I can see what appears to be wind or current influence in some of the other areas of the bright material in this JP2. Can the bitterly cold wind and ice build these structures, as in rime ice plaguing in permafrost layering?
The bright concentric stacked or encased semi-spheroids appear to be very well organized as growths across the main image. Can the less well regulated items be related to this 'stem/geared collar/spheroid' shaped item?
Can we imagine a class of scaled growths with such a routine widely varied size range as these related to the small MER 'berry' spheroids?
Are these geological and inorganic in appearances?