The Rapid Earthquake Viewer (3)
The Rapid Earthquake Viewer (REV) gives you access to information from seismograph stations around the globe. REV displays the earth and posts details about current earthquakes so you’ll be able to see where they happened and examine the seismograms from world seismograph stations for each notable earthquake REV even enables you to inspect seismograph stations in your area, so if you assume you felt the bottom shake, check REV!
As with many megaquakes, the exact casualties are unknown, but estimates are as a lot as 70,000. The nice quake leveled towns and villages, then tsunamis scoured the coasts, fully obliterating the port of Arica. Heavy freighters and warships had been flung onto the shore. Tsunamis prompted flooding and harm in Hawaii, and New Zealand took a hard hit from this one, damaging properties and harbors. Amazingly, the tsunami waves seem to have continued disturbing New Zealand for a number of … Read the rest
Sadly, we have just witnessed one. It’s arduous to wrap our minds across the scale of the devastation we’re seeing. It is even more durable to realize that nearly anyplace else would have had a lot worse devastation: Japan’s architects and engineers ought to be justly happy with their quake-proofing. Yet it wasn’t enough. Tsunamis, spilling over even the world record seawalls built for them, have proved an even stronger foe than earthquakes.
The graphic beneath could be very cool, integrating a number of information about the geography and historical motion on this fault. Edward Tufte could be happy.
If the bottom does not transfer, the rod does not swing, and the pen stays in place, so the ink line is easy and straight. If the ground shakes, however, the row swings and so the pen attracts a zigzag line because the paper turns. The stronger the shaking, the sharper the zigzags. This zigzag image made on the paper roll is known as a seismogram.
I’ve been studying to use the software program and database World Earthquake Explorer for my geophysics course this semester. It appears very useful, although I’m nonetheless making an attempt to figure out how I can get well ground movement amplitudes so as to have my students calculate magnitudes.





