Technology accidents

a. Nostradamus on the dangers of weaponry mixed with natural disaster
b. Weather modulation devices go awry, cause ice and hail
c. Nuclear reactor meltdown near city with underground chambers
d. Space shuttle accident releases microorganisms into atmosphere
e. Devastating accidental weaponry explosions from earth tumult
f. Ruptured earth energy fields cause meteorite storm
g. Research into warping time leads to disaster

f. Ruptured earth energy fields cause meteorite storm
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I p 243 (cI-46)

Research scientists will be investigating the powers associated with
the various energy fields of the earth. They'll try to harness the
powers for different purposes, including warfare. When they begin
experiments, in an area near the North Sea they will accidentally
rupture one of the earth's fields so that a beam of energy will shoot
out into space and draw a steady stream of meteorites to earth. They
will continue to rain down until the scientists can repair the
damage. Doing so will cause an earthquake from built up stress. The
research will be a secret government project. To the world at large
this will appear to be a natural phenomenon and will be recorded as
such in future history books, because the government will keep the
project concealed even after the accident.

Seismic hazard estimates, currently primarily based on a sparse catalog of sturdy floor motion records from stations near huge earthquakes, will more and more be based totally upon sensible simulations of hypothetical ruptures. Those fashions account for the transport of warmth and fluids inside the fault zone, dramatic weakening of fault friction at some point of speedy slip, and inelastic deformation of heavily fractured rocks surrounding the fault core. One modern awareness of the group is exploring how geometric complexity of faults, within the form of fractal floor roughness as well as branches and bends, affects earthquake dynamics. Those functions result in abnormal rupture propagation and the generation of incoherent high frequency seismic waves which can be ubiquitous in seismograms. The picture indicates effects from a hard fault model. The colored regions surrounding the nonplanar fault (purple line) are areas that skilled inelastic deformation throughout the rupture process, and the blue hint is a pace seismogram recording the history of shaking on the station (pink triangle). Any other consciousness of the research institution is the development of numerical methods for computing the boom of ruptures from nucleation areas at the scale of some meters to absolutely developed earthquakes that propagate tens or hundred of kilometers — all with out making compromises in parameter values limited through laboratory studies.