Life precarious on crustal cracks

Life precarious on crustal cracks

Nevado del Ruiz in 2013 • Photo by Adrian Jacobo Restrepo Granada (CC BY-SA 4.0)

Originally published 25 November 1985

For a year the moun­tain had been unqui­et. Smoke, rum­blings, and tremors sig­naled that pres­sure was build­ing inside the peak. Then, on the evening of Wednes­day, Novem­ber 13, 1985, Neva­do del Ruiz blew its top. The heat of eject­ed ash, steam, and lava melt­ed part of the moun­tain’s cap of snow and ice. In the ensu­ing rivers of mud that poured down the moun­tain’s flanks more than 20,000 peo­ple lost their lives.

The erup­tion of the Colom­bian vol­cano, like the Mex­i­can earth­quake sev­er­al weeks ear­li­er, was a human calami­ty. But both events were pre­dictable. Both were inevitable. And both will occur again.

A thin-skinned planet

We live on a dynam­ic plan­et. The cool, rigid crust of the Earth is as thin com­pared to the plan­et as the skin of a grape. Peel off the Earth­’s rocky skin and you would find a sphere of hot, plas­tic, almost molten rock. The Earth under its skin is as hot as the bar of iron in a black­smith’s forge. Peel off the Earth­’s thin skin and the plan­et would glow in the night like a small red star.

And the mate­r­i­al of the Earth­’s inte­ri­or is in motion. The almost molten rock moves in great con­vec­tive loops — hot­ter rock ris­ing, cool­er rock sink­ing — churn­ing like pud­ding in a pan. Per­haps “churn­ing” is too strong a word. The red-hot rock under the crust moves at a snail’s pace of a few cen­time­ters per year. On a human time scale it creeps, as iron slow­ly deforms under the pres­sure of the black­smith’s ham­mer. But in the Earth­’s own time — in geo­log­i­cal time — it churns.

As the inte­ri­or of the Earth churns, the crust moves and breaks. It is along the breaks that most geo­log­i­cal activ­i­ty occurs. One of the liveli­est breaks in the Earth­’s crust runs along the west­ern coast of Cen­tral and South Amer­i­ca. Along that coast the floor of the Pacif­ic Ocean is being pushed down under the con­ti­nents, back into the red-hot forge of the Earth. As the crust goes down, it bends and breaks and gen­er­ates heat. All along the crack there will be earth­quakes and vol­canic erup­tions. In human time, these will occur here and there, and now and then. But in the Earth­’s own time the west­ern coast of the Amer­i­c­as is a con­tin­u­ous­ly shiv­er­ing chain of fire.

Life on the cracks in the Earth­’s crust (called “plate bound­aries” by geol­o­gists) is inevitably risky. In any one place or in any sin­gle life­time the chance may be small that a major dis­as­ter will occur. For exam­ple, the Ruiz vol­cano last erupt­ed with cat­a­stroph­ic con­se­quences in 1595, as Span­ish con­quis­ta­dors explored the area. Along the 4000-mile-long line of the Andes Moun­tains there are present­ly only a dozen or so active vol­ca­noes. But soon­er or lat­er every place on a plate bound­ary will expe­ri­ence tragedy.

It is unlike­ly that humans will refrain from liv­ing on plate bound­aries. Many of the world’s great cities lie on or near cracks in the Earth­’s crust. Mex­i­co City is removed from the active coast by more than 100 miles, but still it felt the shake of the descend­ing crust. If humans will not avoid the cracks, then geol­o­gists must do what­ev­er they can to pre­dict immi­nent cat­a­stro­phes. But most geol­o­gists would say that reli­able pre­dic­tion of earth­quakes and vol­canic erup­tions is still decades away.

In Colom­bia, the moun­tain sig­naled the com­ing erup­tion. Earth tremors were felt as long ago as Novem­ber of 1984, almost a full year before the erup­tion. In the fol­low­ing months, swarms of earth­quakes of mag­ni­tude 3 or 4 on the Richter Scale shook the region. In Sep­tem­ber of 1985 there were heavy ash emis­sions and a small erup­tion that sent mud slid­ing 27 kilo­me­ters down a moun­tain val­ley. Smoke plumes were vis­i­ble daily.

Geologists called in

The Colom­bian gov­ern­ment did take notice. An inter­na­tion­al team of geol­o­gists began to close­ly mon­i­tor the moun­tain. Dis­as­ter plans were for­mu­lat­ed. But no deci­sive action was taken.

There are those who say that the moun­tain gave fair warn­ing, and that the huge loss of life was due to a human fail­ure to act deci­sive­ly on avail­able infor­ma­tion. But vol­ca­noes are not that sim­ple. The Are­nal vol­cano that erupt­ed with vio­lence in Cos­ta Rica in 1968 pro­duced earth tremors for only a day before the erup­tion. The Mount St. Helens erup­tion was pre­ced­ed by sev­en and a half weeks of quakes. Ruiz broad­cast its inten­tions for almost a year. Clear­ly, it is imprac­ti­cal to evac­u­ate entire com­mu­ni­ties in antic­i­pa­tion of a dis­as­ter that may be weeks or months in coming.

Geol­o­gists are work­ing hard to refine their abil­i­ty to give reli­able warn­ings of immi­nent earth­quakes and vol­canic erup­tions. But the dynam­ic Earth will not wait for their suc­cess. Those who live by choice or neces­si­ty on the cracks in the Earth­’s crust must be pre­pared for the kinds of human tragedies we have wit­nessed in these past few weeks.


There have been sev­er­al minor erup­tions of Nava­do del Ruiz in the decades since this essay was first writ­ten, but thank­ful­ly none of the sever­i­ty of the 1985 tragedy. ‑Ed.

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