We tend to talk about time as though there’s one clean scale running underneath everything, with seconds and years acting like neutral containers that every process simply fills at its own pace. That works fine for ordinary life, where a clock gives us a shared reference and there’s no real need to ask what a second means to the thing being measured, but once you start comparing systems that change on radically different timescales, that shared reference begins to look more useful than fundamental. A nervous system can go through an enormous amount of activity in a fraction of a second, while a geological process may barely register any visible change over the course of a human lifetime. The same amount of clock time can contain very different amounts of meaningful change depending on the system, which suggests that our everyday sense of “fast” and “slow” is tied much more closely to the kinds of processes we’re used to experiencing than we usually admit. That got me wondering whether ...