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Mayelana nalolu hlelo lokusebenza
Lolu hlelo lokusebenza lweselula luklanyelwe abasebenzisi abathanda ukuhlala benolwazi mayelana nokuzamazama komhlaba kwakamuva emhlabeni jikelele. Uhlelo lokusebenza luqukethe isizindalwazi sokuzamazama komhlaba kwakamuva, esingavezwa ohlwini nasebalazweni. Ukubuka kohlu kuvumela abasebenzisi ukuthi babone indawo, ubukhulu, nesikhathi sokuzamazama komhlaba ngakunye, kuyilapho ukubukwa kwemephu kunikeza ukumelwa okubonakalayo kwezindawo zokuzamazama komhlaba.
Abasebenzisi bangahlunga uhlu lokuzamazama komhlaba ngokusekelwe emandleni, ibanga ukusuka endaweni abakuyo manje, nokujula. Lokhu kwenza kube lula kubasebenzisi ukuthi bathole ukuzamazama komhlaba okuhlobene nabo, futhi babone ukuthi ukuzamazama komhlaba kusondele kangakanani endaweni yakho yamanje.
Uhlelo lokusebenza luhlanganisa nesici sesexwayiso esazisa abasebenzisi mayelana nokuzamazama komhlaba okusha ngesikhathi sangempela. Lesi sici singavulwa noma sicishwe, futhi abasebenzisi bangakhetha ukuthola izexwayiso zokuzamazama komhlaba kwesilinganiso esithile noma phakathi nebanga elithile ukusuka endaweni abakuyo manje.
Kungakhathaliseki ukuthi ungusosayensi, umthandi wokwakheka komhlaba, noma othile nje ofuna ukuhlala azi mayelana nokuzamazama komhlaba, lolu hlelo lokusebenza olwakho.
Ngaphezu kohlu nokubukwa kwemephu, lolu hlelo lokusebenza luhlinzeka ngolwazi oluningiliziwe mayelana nokuzamazama komhlaba ngakunye, okuhlanganisa ukujula, ubukhulu, kanye namandla. Abasebenzisi bangaphinda bafinyelele umlando wokuzamazama komhlaba okwedlule, okubavumela ukuthi balandele imvamisa nokusatshalaliswa kokuzamazama komhlaba ngokuhamba kwesikhathi.
Esinye isici esihle Sesexwayiso Sokuzamazama komhlaba yikhono lakhona lokubonisa ukuzamazama komhlaba kumephu kusetshenziswa isithombe sesathelayithi. Lokhu kunikeza abasebenzisi isithombe esibonakalayo sezindawo zokuzamazama komhlaba, futhi kwenza kube lula ukubona ukusondela kokuzamazama komhlaba ezindaweni ezinabantu abaningi.
Futhi imephu ibonisa imingcele yamapuleti e-tectonic lapho ukuzamazama komhlaba kwenzeka khona, kungenzeka ukuhlola amazwe ayingozi futhi aphephile nezifunda zomhlaba.
Idatha yokuzamazama komhlaba ithathwe ohlelweni olusemthethweni lwe-"USGS", "Uhlelo lwe-European seismic" - "EMSC" kanye "nesevisi yeGeoNet yaseNew Zealand".
Abasebenzisi bangahlunga uhlu lokuzamazama komhlaba ngokusekelwe emandleni, ibanga ukusuka endaweni abakuyo manje, nokujula. Lokhu kwenza kube lula kubasebenzisi ukuthi bathole ukuzamazama komhlaba okuhlobene nabo, futhi babone ukuthi ukuzamazama komhlaba kusondele kangakanani endaweni yakho yamanje.
Uhlelo lokusebenza luhlanganisa nesici sesexwayiso esazisa abasebenzisi mayelana nokuzamazama komhlaba okusha ngesikhathi sangempela. Lesi sici singavulwa noma sicishwe, futhi abasebenzisi bangakhetha ukuthola izexwayiso zokuzamazama komhlaba kwesilinganiso esithile noma phakathi nebanga elithile ukusuka endaweni abakuyo manje.
Kungakhathaliseki ukuthi ungusosayensi, umthandi wokwakheka komhlaba, noma othile nje ofuna ukuhlala azi mayelana nokuzamazama komhlaba, lolu hlelo lokusebenza olwakho.
Ngaphezu kohlu nokubukwa kwemephu, lolu hlelo lokusebenza luhlinzeka ngolwazi oluningiliziwe mayelana nokuzamazama komhlaba ngakunye, okuhlanganisa ukujula, ubukhulu, kanye namandla. Abasebenzisi bangaphinda bafinyelele umlando wokuzamazama komhlaba okwedlule, okubavumela ukuthi balandele imvamisa nokusatshalaliswa kokuzamazama komhlaba ngokuhamba kwesikhathi.
Esinye isici esihle Sesexwayiso Sokuzamazama komhlaba yikhono lakhona lokubonisa ukuzamazama komhlaba kumephu kusetshenziswa isithombe sesathelayithi. Lokhu kunikeza abasebenzisi isithombe esibonakalayo sezindawo zokuzamazama komhlaba, futhi kwenza kube lula ukubona ukusondela kokuzamazama komhlaba ezindaweni ezinabantu abaningi.
Futhi imephu ibonisa imingcele yamapuleti e-tectonic lapho ukuzamazama komhlaba kwenzeka khona, kungenzeka ukuhlola amazwe ayingozi futhi aphephile nezifunda zomhlaba.
Idatha yokuzamazama komhlaba ithathwe ohlelweni olusemthethweni lwe-"USGS", "Uhlelo lwe-European seismic" - "EMSC" kanye "nesevisi yeGeoNet yaseNew Zealand".
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Ukuphepha kuqala ngokuqonda ukuthi onjiniyela baqoqa futhi babelane kanjani ngedatha yakho. Ubumfihlo bedatha nezinqubo zokuphepha zingahluka kuye ngokusebenzisa kwakho, isifunda, nobudala. Unjiniyela unikeze lolu lwazi futhi angalubuyekeza ngokuhamba kwesikhathi.
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Active geological fault lines are now shown on the map — powered by the "The GEM Global Active Faults Database" dataset! Styron, Richard, and Marco Pagani. “The GEM Global Active Faults Database.” Earthquake Spectra, vol. 36, no. 1_suppl, Oct. 2020, pp. 160–180, doi:10.1177/8755293020944182
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