More Tremors Shake Belizeposted (May 29, 2009)
Did you feel a tremor around 8:45 last night? Or maybe those in the south felt one at 6:45 this morning. If you felt either of them, it wasn’t your imagination, nor was it post-traumatic stress; those were real, both aftershocks of Thursday morning’s powerful 7.1 magnitude earthquake. The epicenter of the major quake was about 140 miles east of the Stann Creek Coast and caused major structural damage in the villages of Monkey River, Independence and Placencia. As we showed you last night, that structural damage was quite remarkable in Monkey River where
many wooden houses on stilts simply sunk into the ground – some sunk as much as eight to ten feet. As we told you last night,
that’s called earthquake liquefaction and today geologist Andre Cho explained what causes the strange phenomenon.
Andre Cho, Geologist: “What happens in an earthquake whenever the seismic waves pass through sediment, loose sediments, it is a natural phenomenon for the sediment to become like a liquid just for a short period of time, just a couple seconds, and that is what is known as liquefaction and that is what causes buildings to sink like what happened in Monkey River. It is on coastal alluvium or sediments which is unconsolidated. So places like Monkey River and Belize City as well, because it is on the coast and it lies on top of unconsolidated sediments or coastal sediments, those places are very vulnerable to liquefaction.”
http://www.7newsbelize.com/sstory.php?nid=14097mom explained alluvial soils and liquefaction to us kids thusly:
"It's like Santa Claus's belly, shakes when he laughs, like a bowlful of jelly!"that's what happened in the Marina District in SF, during the Loma Prieta Quake of '89.
http://en.wikipedia.org/wiki/1989_Loma_ ... earthquake