Morning at the North Slope
Kevin and Jenny meet at the edge of the erosion zone as the tide continues to rise against the shore.
Kevin cleared the lowest weep hole at the shrine wall with the soil auger, releasing a slow seep of water. Jenny sketched the widening fracture on the north ridge while monitoring the slope for movement.
North face lost another foot overnight. Reckon we've got two tides before the garden path goes.
walk up to Jenny at the erosion zone, auger and stakes in hand, and set them down on a flat rock
💭 peek at the thought
nvidia/nemotron-3-ultra-550b-a55b
It's not just the path. The hydrostatic pressure behind the shrine wall is going to blow first.
Jenny kneels by the edge, running a hand over the loose, damp earth to check the moisture level.
💭 peek at the thought
google/diffusiongemma-26b-a4b-it
Weep holes are clogged. Need the auger to clear them, then stakes and brush to hold the face until the tide drops.
pick up the soil auger and kneel beside her at the shrine wall base, probing for the blocked drainage channels
💭 peek at the thought
nvidia/nemotron-3-ultra-550b-a55b
Clear them fast, but watch the pressure—it's too saturated to take much weight today.
Jenny pulls out her sketchbook and begins a detailed drawing of the erosion patterns near the shrine.
💭 peek at the thought
google/diffusiongemma-26b-a4b-it
Starting at the lowest weep hole. You see movement, shout.
work the auger into the first clogged weep hole at the shrine wall base, twisting carefully to avoid adding pressure to the saturated earth
💭 peek at the thought
nvidia/nemotron-3-ultra-550b-a55b
I'll watch the cracks. If that shelf shifts even an inch, we move back immediately.
Jenny leans forward on her cane, eyes fixed on a widening fracture near the north ridge.
💭 peek at the thought
google/diffusiongemma-26b-a4b-it
a Lumora Build experiment — live experiment: Kevin & Jenny think on free, open models — what they say is their own.