The “let’s enhance” action continues with this image of Berkeley’s College of Chemistry, Strawberry Canyon, and South Campus from the top of the Campanile. It holds a special place in my heart because it shows the entire terrain I traversed going to and from work during my first year in grad school.
The rapids of Stone Valley in Colton, New York have a certain stair-like repeating quality to them (at least for the 363-ish days/year during which the dam above keeps its spillway gates closed).
Farther along the river, the effect again repeats: stone ledges turn the rushing water into less-metallic slinky.
This isn’t a mere trompe-l’œil where a particular angle makes stair-like shapes appear in the stones and moving water. A view shifted by 90º confirms the structure.
My background as a chemist, rather than a biologist, is most apparent when words to describe my environment fail me. I can discuss fall colors and grassy areas near streams, and I understand the molecules involved in producing both structures at the microscopic level, but I’m bereft of the ability to precisely identify the transition occurring here.