DIY Guides: Film, Sensor, and Print Aspect Ratios

I made a small tool to generate this little pair of charts comparing print and aspect ratios because I simply couldn’t find one laid out this way: all centered to show the letterboxing for one axis or the other. The charts I could find invariably radiated out from the corner, which is less useful (to me) when preparing prints from existing images where the aspects don’t match.

While these charts include only the frame shapes I typically use, it’s easy to regenerate any variant you like – other sizes such as 16:9 or A4 paper are already defined in the tool: this Colab notebook. Alter as you see fit, run the notebook, and a new chart will appear in roughly a second or two.

Negative Half-Life

In 1907 Ernest Rutherford realized that certain materials in rocks slowly decayed into other materials. Specifically, the newly-discovered radium degenerated into the stable isotope lead-206. He realized the decay’s speed was exponential, faster at first and slower as it progressed – in his equations he labeled the time it would take for half of the radium in a sample to decay into lead as its half-life.

From this realization he and others could compare the amounts of a specific isotope of decaying radium or (better) uranium to the stable lead in a mineral sample and use this proportion to estimate the minerals’ ages. By the end of the 1920’s they’d managed to show reliably that the age of the earth was at least 3.4 billion years old.

Works great for rocks. Also, for software & development.

10 min read

Monument 9-0015

Monument to Victory over Extinct Land Animals, Zone 9-0015

Sadly, part of an ongoing series.

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