dc.contributorUniversidade Estadual Paulista (UNESP)
dc.creatorU.S. Geological Survey
dc.date2016-10-26T18:12:39Z
dc.date2016-10-26T18:12:39Z
dc.date.accessioned2017-04-06T13:22:06Z
dc.date.available2017-04-06T13:22:06Z
dc.identifierhttp://acervodigital.unesp.br/handle/unesp/372903
dc.identifierhttp://objetoseducacionais2.mec.gov.br/handle/mec/16946
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/969185
dc.descriptionEnsino Médio::Geografia
dc.descriptionThe animation shows the directivity of an earthquake, caused due to the focus of seismic waves energy along the fault, in the direction of rupture. Observing the seismic stations (known as Seismic Station #1 and Seismic Station #2) it is possible to understand why the damages of an earthquake are not necessarily near the epicenter, but depend on the direction of waves
dc.publisherU.S. Geological Survey
dc.relationdirectivity.swf
dc.rightsUSGS-authored or produced data and information are considered to be in the U.S. public domain. When using information from USGS information products, publications, or Web sites, we ask that proper credit be given
dc.subjectEducação Básica::Ensino Médio::Geografia::Produção e organização do espaço geográfico
dc.subjectDirectivity
dc.titleDirectivity
dc.typeOtro


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