Reading Volcanic Alert Levels
How a volcanic alert level is constructed, what evidence moves it up or down, and why the number describes the state of the volcano rather than the safety of any particular place.
Audience path
A general reader with no institutional role, arriving without prior context and owed a self-contained explanation.
7 lessons on this path
How a volcanic alert level is constructed, what evidence moves it up or down, and why the number describes the state of the volcano rather than the safety of any particular place.
The reasoning behind the standard earthquake response, what it is protecting against, and the specific situations in which the default advice changes.
What a wind signal and a colour-coded rainfall warning each measure, why the two can disagree, and how to convert an official bulletin into a decision about your own location.
The observable signs that a slope is moving — tilted trees, new springs, cracking ground, changed stream turbidity — and how to act on them before the failure itself.
Why a near-field tsunami arrives before any official warning can, which natural signs constitute the warning themselves, and why the first wave is rarely the largest.
A working procedure for deciding what to act on when reports conflict: establishing provenance, checking timestamps, and distinguishing an absence of information from an all-clear.
How community memory of past events preserves information that instrumental records miss, how to document it without distorting it, and how to hold it alongside official mapping rather than against it.