loves.day
The oldest deposit. Filial love is the bedrock on which everything else accretes -- not because it was chosen but because it was given before the recipient could refuse or accept. It is the first compression: the weight of being held, the heat transfer of proximity, the chemical signature of recognition before language.
This stratum is dense with unexamined material. Core samples show a high concentration of obligation minerals, layered with genuine tenderness, shot through with veins of resentment that formed under pressure. The fossil record here is incomplete -- memory compresses early experience into thin bands that yield surprisingly little when drilled.
A cooler deposit. Platonic love has the grain of slate -- it splits cleanly along the bedding plane, revealing surfaces that are flat, reliable, load-bearing. It does not fracture unpredictably. It is the love that shows up, not because it must, but because the showing up is the substance of it.
The mineral composition here is unusual: low in possessiveness, high in patience, with trace elements of shared silence that function as the binding agent. Geologists note that platonic strata are among the most structurally sound in the column. They rarely fault. When they do, the displacement is lateral, not vertical -- the relationship shifts sideways, not downward.
The thickest deposit in the column. Romantic love has laid down more cultural sediment than any other form -- centuries of poetry, legislation, architecture, warfare, and pop music compressed into a stratum so dense it warps the layers above and below it. The unconformity at its upper boundary suggests a gap in the record: a period when this love was not named, then a sudden explosive deposit when it was.
Core analysis reveals a complex mineralogy: obsession crystallized into devotion, desire metamorphosed by time into something harder and less brilliant but more useful. The terracotta coloring comes from oxidized iron -- romantic love rusts beautifully. Its warmth is not decorative but chemical: an exothermic reaction that happened long ago, still radiating.
This stratum contains the most fossils. Nearly every impression found here is of two organisms in proximity -- not necessarily touching, but oriented toward each other, preserved in the act of attention.
An intrusion -- devotional love did not settle gradually but pushed upward from deep heat, cooling into crystalline structures as it met the surface. The boundary below is sharp: a clean line where amethyst meets terracotta with no transitional zone. Devotion arrives; it does not accumulate.
The mineral here is harder than anything above it. It holds an edge. Under magnification the crystal lattice reveals a recursive pattern: each unit of devotion contains within it a smaller unit of devotion, and within that another, and so on until the structure resolves into something that can no longer be distinguished from obsession -- or from prayer.
A thin stratum -- recent, still consolidating. Self-love is a shallow deposit in geological terms, laid down within living memory. Its amber translucence suggests incomplete compression: you can still see through it, still see the strata beneath. It is the only layer in the column that is aware of itself as a layer.
The deep bedrock. Communal love is so compressed it no longer resembles the organisms that deposited it. It is infrastructure: the geological basement on which neighborhoods, congregations, mutual-aid networks, and potluck dinners rest. Its color is dark forest -- not the canopy but the root system, unseen, load-bearing, vast.
Core samples from this depth show almost no individual fossils. The organic material has been so thoroughly compressed that individual contributions are indistinguishable from the collective mass. This is the point: communal love erases the signature of the giver. What remains is structure.
The deepest stratum. Grief is love with nowhere to go -- the final mineral layer before the drill hits metamorphic rock. It is warm-black, nearly void, but not quite. Hold it to the light and you can see the ghost of what it was before compression changed its structure entirely.
There are no fossils here. Only heat.
Total depth: 80 meters.