(Cross posted from this at Facebook)
In Snow on the Water I wrote about the ‘low threshold of death” for what media folks call “content” — which always seemed to me like another word for packing material. But its common parlance now.
For example, a couple days ago I heard a guy on WEEI, my fave sports station in Boston, yell “Coming up! Twenty-five straight minutes of content!”
Still, it’s all gone like snow on the water, melting at the speed of short term memory decay. Unless it’s in a podcast. And then, even if it’s saved, it’ll still get flushed or 404’d in the fullness of time.
So I think about content death a lot.
Back around the turn of the millennium, John Perry Barlow said “I didn’t start hearing the word ‘content’ until the container business felt threatened.” Same here. But the container business now looks more like plumbing than freight forwarding. Everything flows. But to where?
My Facebook timeline, standing in the vertical, looks like a core sample of glacier ice, drilled back to 1947, the year I showed up. Memory, while it lasts, is of old stuff which in the physical world would rot, dry, disintegrate, vanish or lithify from the bottom up.
But here we are on the Web, which was designed as a way to share documents, not to save them. It presumed a directory structure, inherited from Unix (e.g. domain.something/folder/folder/file.html). Amazingly, it’s still there. Whatever longevity “content” enjoys on the Web is largely owed to that structure, I believe.
But in practice most of what we pile onto the top of the Web is packed into silos such as Facebook. What happens to everything we put there if Facebook goes away? Bear in mind that Facebook isn’t even yet a decade old. It may be huge, but it’s no more permanent than a sand dune. Nothing on the Web is.
Everything on the Web, silo’d or not, flows outward from its sources like icebergs from glaciers, melting at rates of their own.
Anyway, just wanted to share some thoughts on digital mortality this morning.
As you were. Or weren’t. Or will be. Or not.
Bonus link: Locking the Web open.