Plate 38 of 52
Kenny Lienhard, Plates, 2026
Owner: kenny83.eth
How it is made
The Plate in detail
Plate 38 of 52 · one of one
The past. At the ice age peak the sea here was about 4 to 6 degrees Celsius colder than today, and a little later the Cordilleran ice sheet reached the continental shelf off Vancouver Island, about 40 kilometres from the plate. The plate itself is deep ocean floor, so it never held ice or dry land. Between about 20,000 and 14,000 years ago, dozens of floods from glacial Lake Missoula burst down the Columbia River and ran on as underwater currents along Cascadia Channel, across the plate, leaving sand beds up to 57 metres thick in Escanaba Trough on its southern edge.
Sources: Paul et al. 2021, Climate of the Past 17:805; Prahl et al. 1995, Paleoceanography 10:763; Gowan et al. 2021, Nature Communications 12:1199; Dalton et al. 2020, Quaternary Science Reviews 234:106223; O’Connor et al. 2020, Earth-Science Reviews 208:103181; Normark and Reid 2003, Journal of Geology 111:617; Reid and Normark 2003, USGS Bulletin 2216; Zuffa et al. 2000, Journal of Geology 108:253 · Rosa and Molnar 1988, Journal of Geophysical Research 93:2997 · Seton et al. 2020, age grid v2020.1 processed here, Geochemistry Geophysics Geosystems
Onchain
One HTML file, to be etched to Ethereum in full: the code that draws the work (151,144 bytes before compression), this plate’s settings and its record. Nothing is fetched from anywhere else. It reads your clock and slides the view to where the plate is today.
engine sha256 a7fbc03acc0fc9ba343881bb88ddaf2b7564564d8bc9cbed16e75e47e01fb3f2
The work
One HTML file that drifts with your clock, a few centimetres a year.