Noma kunjalo Akukho nokukodwa kwalokhu kuzamazama komhlaba okubangele umonakalo Akukho monakalo womuntu siqu noma wezinto ezibonakalayo olahlekile, kodwa kusisize sakhumbula ukuthi iMalaga itholakala kwenye yezindawo ezinomsebenzi omkhulu wokuzamazama komhlaba eNhlonhlweni yase-Iberia, ithonywe kakhulu amandla oLwandle i-Alboran kanye nokusebenzisana phakathi kwamapuleti e-tectonic ase-Afrika nase-Eurasia.
Impelasonto enomhlaba omncane wokuzamazama komhlaba okuhlanu eMalaga
Ngempelasonto, i- I-National Geographic Institute (IGN) Iqophe ukuzamazama komhlaba okuhlanu okuphansi kakhulu ezingxenyeni ezahlukene zesifundazwe saseMalaga, konke kungaphansi kwama-degree angu-2,5 esikalini sikaRichter futhi ngaphandle kwemiphumela ephawulekayo ngaphandle kokuzamazama okuncane okungabonakali kubantu.
Ukuzamazama komhlaba kokuqala kwenzeke ekuseni kakhulu NgoMgqibelo, cishe ngo-3:19 ekuseni, eduze kwase AbdalajÃs Valleyngobukhulu obungu-1,8. Kwakuwukunyakaza okuhlukile, okujwayelekile emsebenzini ojwayelekile we-micro-seismic ngaphakathi kwesifundazwe futhi, empeleni, okungabonwa iningi lezakhamuzi.
Ngemva nje kwalokho, cishe ngo-4:31 ekuseni, kwaqoshwa okunye ukuzamazama komhlaba kumasipala wase UJimera de LÃbar, eSerranÃa de Ronda, enobukhulu obungu-1,7. Lokhu kuzamazama komhlaba kwesibiliNjengeyangaphambilini, ayizange ibe nomthelela omkhulu ebusweni ngenxa yokuqina kwayo okuphansi kanye nokujula kwayo.
Ekuseni ngoMgqibelo ntambama, ngo-14:37 ntambama, izinzwa ze-IGN zithole ukunyakaza komhlaba okusha eduze kwase- I-AlpandeireUkuzamazama nakho kwaba nobukhulu obuphansi, cishe ama-degrees angu-1,5. Kulesi senzakalo, ukuzamazama kwaphinde kwahlukaniswa ngokwemisebenzi evamile yokuzamazama komhlaba, okuyinto, nakuba ingavamile, engavamile ukubonwa umphakathi.
Kamuva ntambama, cishe ngo-18:10 ntambama, kuzokwenzekani ukuzamazama komhlaba okukhulu kakhulu kwempelasonto esifundazweni saseMalaga, lapho inhloko yaso iqale khona I-Villanueva de la Concepción kanye nobukhulu obungu-2,2 esikalini sikaRichter. Nakuba kungokubaluleke kakhulu kulolu chungechunge oluthile, kwahlala kumazinga abhekwa njengamancane, kungekho monakalo wesakhiwo noma izehlakalo ezinkulu ezibikiwe.
Isinyathelo sesihlanu nesokugcina kulolu chungechunge senzeke ekuseni kakhulu ilanga, ngo-3:06 ekuseni, lapho inhloko yayo iseduze nedolobha uqobo inhlokodolobha ye-malaga kanye nobukhulu obungu-1,6. Futhi, kwakuwukuzamazama okuncane, okuhambisana no ukuzamazama komhlaba okuncane okuphindaphindiwe lokho kuphawula lesi sifundazwe sase-Andalusia.
Uma kubhekwa konke, uhlu lwalokhu kuzamazama komhlaba okuhlanu lubonisa ukusatshalaliswa okubanzi kwezindawo kuso sonke isifundazwe, kanye namarekhodi asenhloko-dolobha, iSerranÃa de Ronda, indawo yase-Antequera kanye neGuadalhorce Valley, okubonisa ukuthi umsebenzi wokuzamazama komhlaba awugxili endaweni eyodwa kodwa uthinta izifunda ezahlukene, ezinye zezindawo Izindawo ezisengozini enkulu yokuzamazama komhlaba eSpain.
Ubukhulu 3,1 eduze kwaseMarbella: ukuzamazama okukhulu kwakamuva
Ngaphandle kochungechunge lokuzamazama komhlaba okuncane ngempelasonto, i-IGN ibike futhi ukuzamazama komhlaba okuyisilinganiso esingu-3,1 ibhaliswe eduze kwase Marbella Ngo-10:35:44 ngoLwesibili lwamuva nje, ngaphakathi komongo ofanayo wokuzamazama komhlaba esifundazweni. Indawo eyayiyinkaba yayitholakala cishe ngekhilomitha elilodwa ukusuka UJimera de LÃbar, futhi eSerranÃa de Ronda, ekujuleni okulingene okuye kwasiza ekunciphiseni imiphumela yayo ebusweni.
Nakuba lokhu kuzamazama kuhlukaniswa njengokuqina okuphansi kuya kokuphakathi, ukuzamazama kungaba kubonakala komasipala abaningana Amadolobha aseduze, njenge-Atajate, i-Benadalid, ne-Alpandeire, athintekile, ngokusho kwedatha yokuqala. Naphezu kwalokhu, ukulinganisa kusikisela ukuthi akufanele kubangele noma yimuphi umonakalo noma ukulimala kwezinto ezibonakalayo, ngaphezu kokukhathazeka okuqondakalayo kulabo abazwe ukuzamazama.
Lesi sigameko sokuzamazama komhlaba esingu-3,1 magnitude siyingxenye ye- umugqa osebenzayo ikakhulukazi Kule ndawo, kuye kwaqoshwa ukuzamazama komhlaba okungaphezu kwekhulu phakathi nesonto futhi cishe okungu-470 kuyo yonke inyanga. Leli yinani eliphakeme, nokho, elihlanganisa kakhulu ama-microseism angabonakali kubantu.
Kulolu chungechunge lwezinyathelo, ukuzamazama komhlaba kweMarbella-Jimera de LÃbar kuvelele kakhulu enye yezibaluleke kakhulu ezinyangeni zakamuva Kulesi sifundazwe, nakuba zisalokhu zingaphakathi kwebanga elinobungozi obuphansi futhi zingaphansi kwemingcele evamile yesifunda, iningi lalokhu kuzamazama komhlaba kubhekwa njengengxenye yesixuku sokuzamazama komhlaba noma isigaba somsebenzi ophakeme, okuyinto evamile kakhulu endaweni yoLwandle i-Alboran.
Umongo we-geology: kungani umhlaba unyakaza kangaka eMalaga?
Incazelo yalolu chungechunge lokuzamazama komhlaba itholakala ku- indawo eyingqayizivele ye-geological yaseMalaga futhi, ngokuvamile, eningizimu ye-peninsula. Lesi sifundazwe sitholakala endaweni yokuguquka phakathi kwamapuleti e-tectonic ase-Afrika nase-Eurasia, okusebenzisana kwawo okudala ukuguquka okuqhubekayo koqweqwe loMhlaba, futhi ngenxa yalokho, kwaqhubeka nomsebenzi wokuzamazama komhlaba ngokuhamba kwesikhathi.
Empeleni, lokhu kusho ukuthi isifunda sijwayele uhlobo oluthile ukuphindaphinda kokuthuthumelaIningi lalokhu kuzamazama komhlaba alidluli ama-degree angu-3-4 futhi akuvamile ukubangela umonakalo omkhulu. Kodwa-ke, iziphathimandla kanye nezinhlangano zesayensi zisikhumbuza ukuthi asinakuyeka ukuqapha kwethu nokuthi kubalulekile ukuba [nokuthile/into ethile]. izinqubo zokuvimbela kanye nokuphendula phambi kwezehlakalo ezingaba khona ezinkulu kakhulu.
I-IGN igcina i- inethiwekhi ebanzi ye-seismographs E-Andalusia nakwezinye izindawo zaseSpain, la mathuluzi asetshenziswa ukuqapha ukunyakaza kokuzamazama komhlaba ngesikhathi sangempela. Ngenxa yala mathuluzi, ubukhulu, indawo, kanye nokujula kokuzamazama komhlaba ngakunye kunganqunywa ngokunemba okukhulu, kanye nomthelela ongaba khona ohlolwa ngokushesha.
Lokhu kuqapha okuqhubekayo kuvumela nokutadisha ukuvela kwezixuku zokuzamazama komhlaba futhi bahlole ukuthi ngabe kungenxa yokuziphatha okuvamile kwendawo noma ukuthi, ngokuphambene nalokho, kungenzeka ukuthi balindele isenzakalo esikhulu, yize ukubikezela okunembile kokuzamazama komhlaba kuseyinto engenakwenzeka kuze kube namuhla.
Umthelela kubantu kanye nendima yemibuzo ye-macroseismic
Nakuba iningi lokuzamazama komhlaba kwakamuva eMalaga bekuncane kakhulu, okunye kwakho kube omakhelwane baqaphela kancane komasipala abahlukahlukene, ikakhulukazi ezindaweni ezithule noma ngezikhathi zokuthula, njengasekuseni kakhulu. Lo muzwa wokudlidliza noma ukungqongqoza okuncane, okubukhali esakhiweni kuvame ukudala ukungabaza, futhi ngezinye izikhathi, ukukhathazeka.
Ukuze kuhambisane nolwazi oluqoqwe ngamadivayisi okulinganisa, I-National Geographic Institute kwenza umphakathi utholakale imibuzo ye-macroseismic kuwebhusayithi yabo. Ngaleli fomu, noma ubani oke wezwa ukuzamazama komhlaba angachaza lokho abekwenza, kungakhathaliseki ukuthi ubelele noma uvukile, kungakhathaliseki ukuthi izinto zinyakazile noma zawa, noma ngabe wezwa imisindo engavamile.
Lobu bufakazi okuyisisekelo sokwakha kabusha isimo sangempela kokuzamazama komhlaba, njengoba kusenza sikwazi ukulinganisa ubukhali obuzwakalayo ezindaweni ezahlukene bese siqhathanisa leyo datha nezilinganiso zezinsimbi. Ngale ndlela, kutholakala imephu ephelele kakhulu yokuthi ukuzamazama kusakazeke kanjani nokuthi yiliphi izinga lemiphumela okube nayo empilweni yansuku zonke.
Ulwazi olunikezwa yizakhamuzi, oluhlanganiswe namarekhodi e-seismograph, lubhekwa ngochwepheshe njengolufanele. kubalulekile ekuhlolweni komonakalo kanye nokuthuthukisa amathuluzi okuxwayisa kusenesikhathi kanye nokuxhumana asebenza kahle kakhulu. Ngaphezu kwalokho, kukhuthaza isiko lokubamba iqhaza nolwazi mayelana nezimo zokuzamazama komhlaba, okungaba yinto ebalulekile ezimweni eziphuthumayo.
Izincomo eziyisisekelo ezivela ku-IGN uma kwenzeka ukuzamazama komhlaba
Izinhlangano ezisemthethweni zigcizelela ukuthi, ngisho noma kukhulunywa ukuzamazama komhlaba okunamandla aphansi Njengoba kunjalo ngokuzamazama komhlaba okulotshwe eMálaga, kubalulekile ukuba neziqondiso eziyisisekelo zesenzo. I-National Geographic Institute (IGN) isikhumbuza ukuthi, ngesikhathi sokuzamazama komhlaba, into yokuqala okufanele uyenze ukuzama ukuhlala uzolile nokugwema ukusabela okungazelelwe okungandisa ingozi.
Uma ukuzamazama kwenzeka ngaphakathi kwendlu noma kwesinye isakhiwo, kuyalulekwa ukuthi Gwema amafasitela, ingilazi, ifenisha ende, kanye nezibani okungaphuka noma kuwa. Kungcono ukufuna indawo yokukhosela ngaphansi kwamatafula aqinile noma ezindongeni zangaphakathi, uvikele ikhanda nentamo yakho ngezingalo zakho noma yiziphi izinto ezifakwe uboya ezitholakalayo.
Ngaphandle, isincomo sithi Gcina kude nezindonga, ama-cornices, izindonga, izinsika zikagesi kanye nezihlahlanjengoba izinto zingase ziphume noma ziwe. Indawo ephephile kakhulu ongaya kuyo kusezindaweni ezivulekile, kude nezakhiwo nezakhiwo ezingazinzile, kuze kube yilapho ukuzamazama okukhulu sekudlulile futhi sekuqinisekisiwe ukuthi azikho ezinye izingozi.
Uma kwenzeka ukuzamazama komhlaba ngenkathi ushayela, ochwepheshe batusa misa imoto kancane kancane endaweni ephephile, ugweme amabhuloho, imigudu, kanye nezindawo zokudlula, futhi ugcine izibani zakho zengozi zivuliwe. Kungcono ukuhlala emotweni kuze kube yilapho imoto iyeka ukuhamba, ngaphandle uma kukhona ingozi esheshayo endaweni ezungezile.
Ezindaweni ezinabantu abaningi njengezindawo zokuthenga, ama-pavilion, noma amahholo okudlala, iziqondiso zifaka phakathi vikela ikhanda nomzimba ubambe izingalo noma ucashe ngaphansi kwezihlalo nefenisha elungisiwe, ugweme ukugijimela ezindaweni zokuphuma ngendlela engahlelekile ukuze ungabangeli ukuqhekeka kweqhwa noma ukuwa.
Uma ukuzamazama sekuphelile, i-IGN iyancoma Vala ompompi bamanzi, igesi, nogesi. Ukuze uvimbele imililo noma ukuvuza, gwema ukusebenzisa ama-lifti (njengoba angavinjelwa) futhi usebenzise izitebhisi njalo. Kunconywa futhi ukucima noma yimiphi imililo, futhi uma kudingeka ukukhanya, sebenzisa amathoshi esikhundleni samakhandlela noma izibani ukuze unciphise ingozi yokuqhuma.
Ngaphezu kwalokho, ukubaluleka Ungangeni ezakhiweni ezibonisa umonakalo obonakalayo kuze kube yilapho behlolwa ochwepheshe abanekhono, naka ukuthuthumela okungenzeka futhi ulandele imiyalelo yezinsizakalo eziphuthumayo nezokuvikela umphakathi ngaso sonke isikhathi.
Kuleli gagasi lakamuva lokuzamazama komhlaba eMalaga, kusukela Ukuzamazama komhlaba okuncane okuhlanu ngempelasonto Ngisho nokuzamazama okungu-3,1 magnitude eduze kwaseMarbella kugqamisa isimo sokuzamazama komhlaba sesifundazwe, kodwa futhi kukhombisa ukuthi, ezimweni eziningi, lokhu kuyizinyathelo ezilinganiselwe ezingabangeli ingozi enkulu. Ukuqapha okuqhubekayo yi-National Geographic Institute, ukubamba iqhaza kwezakhamuzi ngemibuzo, kanye nokusatshalaliswa kweziqondiso ezicacile zokuzivikela kuyizinto ezinhle kakhulu zokuphila naleli qiniso le-geological kanye nokunciphisa izingozi ezihlobene nalo.
