Pyroclastic Density Currents and Lahar Pathways
Why the deadliest volcanic hazards follow terrain rather than distance, how channels and valleys concentrate them, and why a lahar can arrive on a clear day long after an eruption has stopped.
Audience path
A school, agency, or programme adopting the material at the level of policy or curriculum rather than delivering an individual lesson.
14 lessons on this path
Why the deadliest volcanic hazards follow terrain rather than distance, how channels and valleys concentrate them, and why a lahar can arrive on a clear day long after an eruption has stopped.
How to read a building for the configurations that concentrate earthquake damage — soft storeys, unreinforced masonry, short columns — and what a non-engineer can and cannot conclude from a walk-around.
Why flood deaths cluster around late decisions and vehicle crossings, how to set a departure trigger in advance, and what makes a route survivable rather than merely shorter.
How to read a geohazard susceptibility map against your own address, what the categories mean in practice, and the limits of a map drawn at regional scale.
How surge height is driven by bathymetry, coastal shape, and storm size rather than wind speed alone, and why a lower-category storm can produce a higher surge.
The chain of infection as a practical model, where each link can be broken, and why interventions are judged on which link they target rather than on how dramatic they look.
Why waterborne disease causes more post-disaster illness than the event itself, how to make water safe with what is available, and how sanitation siting protects a whole shelter.
How power, water, telecoms, and transport depend on one another, why the second-order failure often exceeds the first, and how to map the dependencies that matter locally.
What makes a structure suitable for sheltering people — location relative to hazard, structural condition, capacity, water, sanitation, and exits — and what disqualifies one regardless of its size.
Why engagement ranking systematically favours dramatic and early claims over corrected ones, what that does to a community during an unfolding event, and how to build an information path that does not depend on a feed.
The components a warning needs — hazard, location, timing, consequence, and a specific instruction — and why vagueness and repeated non-events both suppress response.
How pre-assigned roles, a named decision-maker, and a rehearsed sequence turn a warning into movement, and why the people least likely to self-evacuate need to be identified in advance.
Why prolonged educational interruption compounds disaster harm, and how to build a continuity plan that does not assume electricity, connectivity, or an intact school building.
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.