2.2 - 1
	Class: ecr Source: 02003 Comment: Evaporite near crater rim

2.2 - 2
	Class: ecr Source: 2003 Comment: Evaporites at crater rim only remains of crater

2.2 - 3
	Class: ecr er X Source: 2104 Comment: Crater (vulcanic?) covered by rim pyramid and ridge extending outside

2.2 - 4
	Class: ecr Source: 4303 Comment: Evaporite ridge from rim

2.2 - 5
	Class: ecr X Source: 9403 Comment: Evaporite extending von rim (of vulcanic crater?) far outside

2.2 - 5a

Class: u X Source: fha01434 Comment: All flow features prefer the same general direction. It could be related to the unknown local topography. But the wide angle of direction, up to 180°  and upslope a crater rim, points to wind as the main modulator. The classical interpretation is that 'muddy' craters are an impact phenomenon. But this gets challanged by the large amount of material involved in the presence of evaporites at craters elsewhere.

2.2 - 6
	Class: ecr Source: fha00525 Comment: Irregular rim pyramid

2.2 - 7
	Class: ecr X Source: fha00742 Comment: Two craters covered by rim-evaporites in area of intense evaporite ridges

2.2 - 8
	Class: ecr Source: fha00761 Comment: Evaporite extending from the rim of the impact crater to the outside and even down a cliff

2.2 - 9
	Class: ecr er X Source: sp120805 Comment: Evaporites at ridges and crater rims all modulated by same direction of prevailing local wind

2.2 - 10
	Class: ecr Source: SP121803 Comment: Irregular rim pyramid covers most of crater

2.2 - 11
	Class: ecr Source: SP122105 Comment: same

2.2 - 12
	Class: ecr X Source: SP122504 Comment: Ridge from rim inside and outside crater

2.2 - 13
	Class: ecr er Source: SP123703 Comment: Ouside ridges cross craters and generate large evaporites inside. More in left then in right part of crater. Indication of source flow deep below what created ridge?

2.2 - 14
	Class: ecr Source: SP124504 Comment: Evaporite flow from rim to inside and outside crater

2.2 - 14a
	Class: u Source: sp244003 Comment: Black area streak and possible evaporite at crater rim

2.2 - 15
	Class: ecr Source: sp234804 Comment: Rim pyramid and ridges perhaps only remains of crater

2.2 - 16
	Class: ecr Source: sp234905 Comment: Crater with two large rim pyramids

2.2 - 17
	Class: ecr a Source: sp235106_gr Comment: Evaporite structures at rim and (airborne transported?) diffuse black streak from rim too

2.2 - 18
	Class: ecr Source: sp236403 Comment: Rim pyramids cover crater

2.2 - 19
	Class: ecr Source: sp236403 Comment: Large evaporite slap grown from rim

2.2 - 20
	Class: ecr Source: sp240003 Comment: Rim pyramids of evaporite

2.2 - 21
	Class: ecr Source: sp242104 Comment: same

2.2 - 22
	Class: ecr Source: sp242704 Comment: same

2.2 - 23
	Class: ecr Source: sp244003 Comment: same

2.2 - 23a
	Class: ecr er Source: sp244003 Comment: Evaporite ridges L1-3 grown from the rim of a depression. The depression is probably not the remains of an impact crater row  but  of vulcanic related origine.

2.2 - 23b

Class: vul Source: fha01048 Comment: Like the above structure but less eroded. To the left two domes, probably hollow and three collapsed domes to the right. These domes were created by an upward movement of steam or water supported by subsurface volcanism, a process similar to but less violent than the creation of pseudocraters. In the craters or inside the domes could be an entrance to the subsurface world of Mars.

2.2 - 24
	Class: ecr er Source: sp247105 Comment: Evaporite ridge crosses crater

2.2 - 25
	Class: ecr Source: sp249003 Comment: Evaporites from crater rim

2.2 - 26
	Class: ecr er Source: sp252003 Comment: Long evaporite ridge crosses crater and there most intense grow

2.2 - 27
	Class: ecr Source: sp252903 Comment: Rim pyramid, ridges and possible black streaks

2.2 - 28
	Class: ecr er Source: sp252903 Comment: same

2.2 - 29
	Class: ecr Source: sp252903 Comment: Evaporites at rim and some flow inside

2.2 - 30
	Class: ecr Source: sp252903 Comment: same, but here dunes not ruled out

2.2 - 31
	Class: ecr Source: sp253404 Comment: Two parts of evaporite covered rim are the only remains of a crater. Recent evaporite smooth, most area rough. No wind features. Perhaps area quite old and main errosion of evaporites by ice cracks during night cooling down to dust size.