{"schema": "too.foo.history.image-prompt.v1", "slug": "1964-march-27-good-friday-the-great-alaskan-earthquake-the-second-most-powerful", "release": "4b157fe58dc3a255", "image_key": "1964-march-27-good-friday-the-great-alaskan-earthquake-the-second-most-powerful-", "image_sha256": "decf2ca589caf545ef8601dee197dee4aaf3246139b516ceaf8659b390219821", "job": "20260827-004333-tier2", "model": "Ideogram 4 (fp8)", "preset": "V4_DEFAULT_20", "steps": 20, "seed": 20260823, "width": 1216, "height": 832, "caption_mode": "json", "caption": {"high_level_description": "At Chenega, the churning leading edge of a local tsunami reaches a racked timber building while quake-opened ground splits beneath its shoreward piers, documenting the wave's arrival before the four-and-a-half-minute shaking has ended. Chenega's Prince William Sound shoreline in late afternoon on 27 March 1964, tightly framed around one timber building, gravel bank, cold seawater, patchy late-winter snow, and a steep spruce-covered slope across the sound. The surge contacts every shoreward pier and curls around them; turbulent water carries diffuse grey sky tones and fragments of the dark wall colour. Four inland piers remain embedded in the gravel while two shoreward piers stay attached to the building and move with the subsiding bank. The ground fissure passes beneath the building between the inland and shoreward piers. The building's sill rests on all six piers, and its wall racks in the same seaward direction as the displaced pair. Three porch boards remain attached at one end while rotating downward; their free ends travel toward the surge and gravel. A 2.0-metre doorway anchors the building's roughly 9-metre width; the surge reaches its 0.8-metre-high floor beams. It is 27 March 1964: People remain beyond the tight shoreline crop.; Spruce framing, painted wood shiplap, rough timber piers, steel fasteners, gravel, seawater, and late-winter snow.; 1964 coastal timber construction on driven piers; utility hardware remains beyond the crop. Ordinary dark turbulent seawater advances across shore gravel while active shaking registers through a widening fissure, displaced piers, and the racked wall.", "style_description": {"aesthetics": "immediate physical peril. Documentary photographic realism: subtle film grain, believable wear on every material, candid imperfect framing.", "lighting": "One broad overcast source from upper left gives soft lower-right contact shadows; wet boards, water foam, and fresh gravel faces share the same highlights.", "photo": "50mm, f/2.8, approximately 20 metres, Candid medium-wide shoreline reconstruction, building crowded against the right edge and incoming water dominating the left foreground", "medium": "photograph, A 1/250-second documentary frame preserves the surge edge and falling boards, with subtle 1960s colour grain and a softly focused distant slope.", "color_palette": ["#1E1913", "#4A3B28", "#8A7350", "#C9B892", "#2B2B2A"]}, "compositional_deconstruction": {"background": "Chenega's Prince William Sound shoreline in late afternoon on 27 March 1964, tightly framed around one timber building, gravel bank, cold seawater, patchy late-winter snow, and a steep spruce-covered slope across the sound. One broad overcast source from upper left gives soft lower-right contact shadows; wet boards, water foam, and fresh gravel faces share the same highlights.", "elements": [{"type": "obj", "bbox": [440, 0, 870, 785], "desc": "One sediment-clouded seawater surge reaches the building's floor beams; its irregular foaming edge wraps around shoreward piers and pushes inland."}, {"type": "obj", "bbox": [165, 555, 715, 955], "desc": "One single-storey wood-frame building, roughly 9 metres wide, with shiplap wall racked off-square and porch boards tearing loose at the shoreward corner."}, {"type": "obj", "bbox": [535, 585, 835, 915], "desc": "Six irregular timber piers support the building; two shoreward piers are pulled seaward while four inland piers remain embedded in gravel."}, {"type": "obj", "bbox": [685, 345, 1000, 1000], "desc": "One fresh 20-centimetre fissure splits gravel beneath the building, its shoreward lip subsiding and dragging two piers toward the water."}, {"type": "obj", "bbox": [570, 485, 850, 725], "desc": "Exactly three torn boards rotate downward from the porch corner, travelling toward the surge and fractured gravel beneath them."}, {"type": "obj", "bbox": [70, 0, 465, 710], "desc": "A steep spruce-covered slope with irregular snow patches crosses the background, softened by cold mist and shallow focus."}, {"type": "obj", "bbox": [845, 620, 1000, 1000], "desc": "Wet angular gravel at the lower-right edge falls out of focus; darker fresh fracture faces expose the fissure's recent movement."}]}}, "rendered_input": "{\"high_level_description\": \"At Chenega, the churning leading edge of a local tsunami reaches a racked timber building while quake-opened ground splits beneath its shoreward piers, documenting the wave's arrival before the four-and-a-half-minute shaking has ended. Chenega's Prince William Sound shoreline in late afternoon on 27 March 1964, tightly framed around one timber building, gravel bank, cold seawater, patchy late-winter snow, and a steep spruce-covered slope across the sound. The surge contacts every shoreward pier and curls around them; turbulent water carries diffuse grey sky tones and fragments of the dark wall colour. Four inland piers remain embedded in the gravel while two shoreward piers stay attached to the building and move with the subsiding bank. The ground fissure passes beneath the building between the inland and shoreward piers. The building's sill rests on all six piers, and its wall racks in the same seaward direction as the displaced pair. Three porch boards remain attached at one end while rotating downward; their free ends travel toward the surge and gravel. A 2.0-metre doorway anchors the building's roughly 9-metre width; the surge reaches its 0.8-metre-high floor beams. It is 27 March 1964: People remain beyond the tight shoreline crop.; Spruce framing, painted wood shiplap, rough timber piers, steel fasteners, gravel, seawater, and late-winter snow.; 1964 coastal timber construction on driven piers; utility hardware remains beyond the crop. Ordinary dark turbulent seawater advances across shore gravel while active shaking registers through a widening fissure, displaced piers, and the racked wall.\", \"style_description\": {\"aesthetics\": \"immediate physical peril. Documentary photographic realism: subtle film grain, believable wear on every material, candid imperfect framing.\", \"lighting\": \"One broad overcast source from upper left gives soft lower-right contact shadows; wet boards, water foam, and fresh gravel faces share the same highlights.\", \"photo\": \"50mm, f/2.8, approximately 20 metres, Candid medium-wide shoreline reconstruction, building crowded against the right edge and incoming water dominating the left foreground\", \"medium\": \"photograph, A 1/250-second documentary frame preserves the surge edge and falling boards, with subtle 1960s colour grain and a softly focused distant slope.\", \"color_palette\": [\"#1E1913\", \"#4A3B28\", \"#8A7350\", \"#C9B892\", \"#2B2B2A\"]}, \"compositional_deconstruction\": {\"background\": \"Chenega's Prince William Sound shoreline in late afternoon on 27 March 1964, tightly framed around one timber building, gravel bank, cold seawater, patchy late-winter snow, and a steep spruce-covered slope across the sound. One broad overcast source from upper left gives soft lower-right contact shadows; wet boards, water foam, and fresh gravel faces share the same highlights.\", \"elements\": [{\"type\": \"obj\", \"bbox\": [440, 0, 870, 785], \"desc\": \"One sediment-clouded seawater surge reaches the building's floor beams; its irregular foaming edge wraps around shoreward piers and pushes inland.\"}, {\"type\": \"obj\", \"bbox\": [165, 555, 715, 955], \"desc\": \"One single-storey wood-frame building, roughly 9 metres wide, with shiplap wall racked off-square and porch boards tearing loose at the shoreward corner.\"}, {\"type\": \"obj\", \"bbox\": [535, 585, 835, 915], \"desc\": \"Six irregular timber piers support the building; two shoreward piers are pulled seaward while four inland piers remain embedded in gravel.\"}, {\"type\": \"obj\", \"bbox\": [685, 345, 1000, 1000], \"desc\": \"One fresh 20-centimetre fissure splits gravel beneath the building, its shoreward lip subsiding and dragging two piers toward the water.\"}, {\"type\": \"obj\", \"bbox\": [570, 485, 850, 725], \"desc\": \"Exactly three torn boards rotate downward from the porch corner, travelling toward the surge and fractured gravel beneath them.\"}, {\"type\": \"obj\", \"bbox\": [70, 0, 465, 710], \"desc\": \"A steep spruce-covered slope with irregular snow patches crosses the background, softened by cold mist and shallow focus.\"}, {\"type\": \"obj\", \"bbox\": [845, 620, 1000, 1000], \"desc\": \"Wet angular gravel at the lower-right edge falls out of focus; darker fresh fracture faces expose the fissure's recent movement.\"}]}}", "prompt_sha256": "5ff79a0cd916489295aae0ed9ed75a516be6f4cdc8bc91fcdc0497952641b279"}