Ukunyakaza kwe-Seismic kuyinto engavamile kakhulu yemvelo, njengama-tsunami noma ukuqhuma kwentaba-mlilo. Kodwa-ke, isenzakalo esenzeka kaningi kunalezi zenzakalo ezimbili, ikakhulukazi ezindaweni lapho ama-plate tectonics azinzile kancane. Ukubona noma ukuhlaziya lesi simo kusenesikhathi, sinokuthile izinhlelo zokusebenza zokuxwayisa ngokuzamazama komhlaba Kusuka ocingweni.
Izilinganiso zokulinganisa ukunyakaza kokuzamazama komhlaba
Kuze kube muva nje, ososayensi balinganise ukuzamazama komhlaba besebenzisa isikali se Richter, eyasungulwa izazi zokuzamazama komhlaba zaseMelika UCharles F. Richter y Beno Guatenberg ngo-1093 nango-1940.
Esikalini sakho se-logarithmic sobukhulu bokuzamazama komhlaba, inombolo ngayinye imelela amandla amakhulu ngokuphindwe kashumi kunangaphambili. Akukho ukuzamazama komhlaba okudlule ku-9,5 degrees eChile ngoMeyi 22, 1960.
Isikali sikaRichter sikala ubukhulu kuphela. Ezinye izikali zinesibopho sokuhlukanisa ukuzamazama komhlaba kusetshenziswa ezinye izindlela. I Isilinganiso se-seismological sobukhulu besikhathi Ikala indawo yedwala elisusiwe, ukuqina kwetshe kanye nebanga eliphakathi lokufuduka.
La Isilinganiso se-Mercalli seismological sebenzisa izinombolo zesiRoman ukuze ulinganise ukuzamazama komhlaba ngemiphumela yako endaweni ezungezile. Ngesikhathi sokuzamazama komhlaba okukalwe ngokuthi I, abantu abazizwa noma yikuphi ukunyakaza komhlaba. Durina one V, cishe wonke umuntu uye wakuzwa ukunyakaza. Ekuzamazameni komhlaba okungu-X, izakhiwo ziyawa, amadamu ayaphuka, bese kuba nemifantu emhlabathini.
Imithombo lezi zinhlelo zokusebenza zisekelwe kuyo
Kubalulekile ukwazi ukuthi lezi zinhlelo zokusebenza ziqoqa kuphi idatha ukuze zibonise ukunyakaza kokuzamazama komhlaba. Kunenqwaba yemithombo eqopha ukuzamazama komhlaba noma, kunalokho, ukuziphatha kwezindawo ezingaphezulu namapuleti e-tectonic. Lezi zikhungo zikhona kokubili ezingeni lesifunda, likazwelonke kanye namazwe ngamazwe.
Okudume kakhulu eSpain yiNational Seismic Network, engaphansi koMnyango Wezangaphakathi. Esinye isici esivelele yi-Euro-Mediterranean Seismological Center, inhlangano yesayensi engenzi nzuzo ezinikele ocwaningweni lokuzamazama komhlaba. Ezinye kungase kube i-National Institute of Geophysics and Volcanology, ezinze e-Italy, noma i-Geonet, okuyinkampani ephethwe umphakathi ngokucatshangelwa kwenhlangano ezimele i-Suma Gestión Tributaria ephethwe nguMkhandlu WesiFundazwe wase-Alicante.
Zonke izinhlelo zokusebenza ezikuxwayisa ngokuzamazama komhlaba
Sihamba nazo zonke izinketho i-Android esinika zona ukuze sibe nazo kumathuluzi ethu eselula ukuthola nokuqapha umsebenzi wokuzamazama komhlaba womhlaba.
I-IGN Seismology PRO
Kuyinto isicelo esisemthethweni seNational Seismic Network, eyakhiwe uMnyango Wezangaphakathi. Ngokufanayo, ivumela ukwamukela nokuboniswa kwazo zonke izehlakalo zokuzamazama komhlaba eSpain nasezindaweni ezizungezile kudivayisi yethu ye-Android. Ngaphezu kwalokho, uma kwenzeka uzwe ukuzamazama komhlaba, kunikeza ithuba lokuthumela ifomu le-macroseismic ngokusebenzisa izithonjana ezilula ezipopayi.
Ukuqwashisa Ngokuzamazama komhlaba
Lolu hlelo lokusebenza, olutholakala kuphela ku-Android, lunemephu ene ulwazi ngakho konke ukuzamazama komhlaba okwenzeka emhlabeni jikelele, ukwazi ukwenza izihlungi zendawo ethile, usuku noma ubukhulu.
Uma ufuna ukuthola izaziso zalokho okwenzekayo uzodinga futhi ukufaka i-Earthquake Alerter Free, kusukela kunjiniyela ofanayo. Zombili zilinganiselwe kakhulu ku-Google Play Isitolo kuze kube manje.
I-SkyAlert
Uma usedolobheni noma kwelinye lamazwe asanda kuhlaselwa ukuzamazama komhlaba, lolu hlelo lokusebenza luzokuthumela izaziso kumakhalekhukhwini wakho sibonga ohlelweni lwayo lwesexwayiso oluhambisana nezitholi zokuzamazama komhlaba. Ngohlelo lwabo lokubhala phansi, kancane kancane bandisa inani lezifundazwe ezisezindaweni eziyingozi kakhulu.
Izaziso Zami Zomhlaba
Iwuhlelo lokusebenza olunolwazi lokuzamazama komhlaba okubalulekile olukunikeza yonke idatha oyidingayo futhi lufaka phakathi izaziso zohlelo lokusebenza, konke lokhu mahhala. Kuphinde kuhlanganise nedizayini enhle elula, elungiselelwe izinguqulo zakamuva ze-Android. Ngaphezu kwalokho, inenjini yokusesha yokuthola amafayela kweminye imicimbi efanayo, enezinsuku ezifika onyakeni we-1970.
Izaziso Zokuzamazama Komhlaba
Lolu hlelo lokusebenza lukubonisa ulwazi mayelana lapho ukuzamazama komhlaba kwenzeka noma kuphi emhlabeni. Ungabona ukuzamazama komhlaba kwakamuva kakhulu futhi uthole izaziso uma kwenzeka ngokususelwa kubuningi nobukhulu obukhethile.
I-interface isinika izinketho eziningi zokwenza ngokwezifiso, njengamaphrofayili emisindo ahlukahlukene wezexwayiso, ithuba lokukhetha imvamisa oyifunayo nobukhulu bokutholwa kokuzamazama komhlaba, izindikimba zokuklama ongakhetha kuzo kusixhumi esibonakalayo, njll.
I-Earthquake Tracker - Izaziso nemephu
Leli thuluzi libonisa konke ukuzamazama komhlaba kwakamuva okuvela emhlabeni jikelele. Ngakho-ke, kuwuhlelo olubalulekile lokubona ukuzamazama komhlaba. Okuthile okufisa ukwazi ukuthi esigabeni "Izici" sohlelo lokusebenza ungabona iqiniso elithokozisayo njengenani lokuzamazama komhlaba emahoreni angama-24 edlule, ukuzamazama komhlaba okukhulu kwakamuva kanye nokuzamazama komhlaba okuningi eduze kwethu.
Tremors
Uhlelo lokusebenza lubonisa ukuzamazama komhlaba kwakamuva okuvela emhlabeni wonke ohlwini nakumephu. Ungakwazi ukuhlunga idatha ngezindlela ezihlukahlukene, njengamandla okuzamazama komhlaba, ibanga ukusuka endaweni, ukujula. Inemephu yokuzamazama komhlaba ngesikhathi sangempela kanye nethuba lokukhetha isikhawu sesikhathi ofuna ukubona imininingwane yaso.
Isithasiselo kumephu sibonisa imikhawulo yamapuleti e-tectonic lapho ukuzamazama komhlaba kwenzeka khona, kungenzeka ukuhlola amazwe ayingozi noma aphephile nezifunda zomhlaba. Njengakwezinye izinhlelo zokusebenza, ikuvumela ukuthi ulungiselele izexwayiso zokuzamazama komhlaba kuselula yakho ngokukhetha ubukhulu nebanga ukusuka endaweni yakho.
Ukuzamazama komhlaba
Olunye uhlelo lokusebenza olusibonisa ukunyakaza kokuzamazama komhlaba ngesikhathi sangempela, okuvela emhlabeni wonke. Ukunikeza lonke lelo nani lolwazi, linemithombo eminingana njenge EMSC, USGS, INGV, I-IRIS, CSUSP o I-GEONET. Yonke idatha ebonisiwe ingaboniswa ngefomethi yohlu noma ngokuqondile kumephu. Njengazo zonke ezinye izindlela, ikuvumela ukuthi ulungiselele izaziso zohlelo lokusebenza ukuze uqaphele mayelana nezindaba zokuzamazama komhlaba.
Imitha yokudlidliza
Uhlelo lokusebenza olubizwa nge-seismograph noma i-seismometer, ekala amandla okudlidliza, ukundindizela, ukuzamazama komhlaba, ukudlidliza komzimba womuntu nanoma iyiphi enye into ewuzungezile. Uhlelo lwethu lokusebenza luvumela ukutholwa nokubhaliswa kwamagagasi e-seismic akhiqizwa ukuzamazama komhlaba, ukuqhuma kwentaba-mlilo, ama-avalanche neminye imithombo yokudlidliza nokushaqeka.
I-accelerometer yeselula isetshenziselwa ukuthola ukudlidliza nokuhlaziya ukulinganisa. Futhi igrafu iveza irekhodi lokuhamba komhlaba endaweni yokulinganisa, njengoba nje ukunyakaza komhlaba noma into kuvezwa njengomsebenzi wesikhathi ezimbazweni ezintathu zeCartesian.
Umtshina wokuzamazama komhlaba we-Adv
Ngezinye izikhathi ukuzamazama komhlaba kwandulelwa ukuzamazama komhlaba okuncane futhi uma lokhu kwenzeka ngenkathi silele, lolu hlelo lokusebenza lungasixwayisa ngesikhathi ukuze sifune indawo ephephile, ngaphandle kwalokho imizuzwana eyigugu izolahleka ngaphambi kokuqaphela okwenzekayo. Kusivumela ukuthi sibone izikali zokuzamazama komhlaba futhi sibeke imisindo ehlukene ukuze uthole izexwayiso.
