Ngaba iSiriya, iLebhanon, nommandla waseLevant zikufuphi nenyikima etshabalalisayo?

Kwingcaciso yezi nyikima, ezinye zazo zafikelela kumlinganiselo we-4.8 kwisikali seRichter, umlawuli weZiko leSizwe leSeismic, u-Abdul Muttalib Al-Shalabi, uxelele i-RT ukuba ukungcangcazela yinto yendalo, njengoko uMhlaba liqela leenyikima. amacwecwe e-tectonic ahamba ngokuqhubekayo, kwaye ngenxa yale ntshukumo, ukuqokelelwa koxinzelelo lwenzeka, kwaye olu xinzelelo lukhululwa kwindlela yokuthuthumela, kodwa uhlobo lolo nyikima, nokuba lukhulu, luphakathi, okanye luncinci, luyinto engenako. kuxelwe kwangaphambili.”
Ngokuphathelele iinyikima ezitshabalalisayo ezibonwa ngummandla ngamaxesha athile, uAl-Shalabi uthi ngokwembali inyikima irekhodwa rhoqo emva kweminyaka engama-250 ukuya kwengama-300.
-Yayinini inyikima yokugqibela?
-Inyikima yokugqibela etshabalalisayo yabhalwa ngo-1759.
-Oko kukuthi, ngaba singaphakathi kwendawo yengozi?
Kuyenzeka ukuba inyikima yenzeke rhoqo emva kwama-250 ukuya kwangama-300, kodwa ngokwenzululwazi, uxinezeleko (olubangelwa kukushukuma kwamacwecwe eMhlabeni) lushukunyiswa kukungcangcazela okusenokuba kuncinane, okuphakathi, okanye okukhulu, yaye le yinto ekungekho bani unokuyenza. xela kwangaphambili, nakumazwe ahambele phambili kwezoqoqosho aneenyikima ezininzi, njengeJapan. .
Akunakwenzeka ukwazi ubunzulu benyikima, okanye ukuyiyeka, kwaye ukuhlalisana kunye neziganeko zendalo kufuna kugxininise kumbandela wolwakhiwo olukwaziyo ukumelana neenyikima.Kule meko, inyikima iba njengayo nayiphi na into yendalo, kwaye ilahleko yayo iba kancinci kangangoko.
* Kukho abo baye baqalisa ukuphakamisa uloyiko “lwetsunami,” ngokukodwa ekubeni iinyikima ezilinganiselweyo okanye iinyikima zomhlaba ebudeni bexesha lakutshanje bezigqugqisile elunxwemeni.” Lunokuba sengqiqweni ukusa kuwuphi umkhamo olu loyiko?
-Oku kunokwenzeka, kwaye kukho izifundo ezithi kunokwenzeka ukuba kwenzeke, kwaye i-tsunami yenzeke ngaphambili, kodwa ukuba ikude nonxweme kunoko, ubukhulu bayo bukhulu.
-Ngaba iinyikima ezilandelelanayo ngokwenene zisisilumkiso senyikima enkulu?
Akunakwenzeka ukuxela kwangaphambili oku, kwaye kukho ukungcangcazela rhoqo, enoba abantu bayaziva okanye akunjalo.

Iintaka zixela kwangaphambili phambi kwabantu:
Intloko yeSebe leTectonics kwiziko, uSamer Zayzoun, uthe ukubikezela iinyikima kuyinkqubo enzima, kwaye akunakwenzeka ukucacisa indawo yenyikima kunye nexesha lokwenzeka kwayo. Wongezelela kwiingxelo ezichazwe ngendawo Kwirediyo ye-“Ninar FM” kukho uhlolisiso olubonisa ukuba iintaka ziyaziva iintanda ezisemhlabeni, ngaloo ndlela zixela kwangaphambili ukuba kuya kubakho inyikima phambi kwabantu.

Ukungcangcazela okulandelelanayo

Ukususela ngomhla wesithathu kule nyanga, lo mmandla uye wabona inyikima (inyikima ephakathi) kunye nokuqina kwe-4.8, kumgama weekhilomitha ezingama-41 ukusuka kwisixeko saseLatakia, kwaye yavakala ngabahlali besixeko ngaphezu kweTartous, eHama, Homs, kunye neAleppo.

Ukususela ngentsasa yayizolo, ngoLwesibini, iqela leenyikima liqalile, elokuqala libe kukushukuma okungephi okumalunga ne-3.3, 115 km kumntla-ntshona wekomkhulu, iDamasko, kunye neekhilomitha ezingama-31 kumntla-ntshona weBeirut.

Kwalandelwa yinyikima emva kwasezinzulwini zobusuku (inyikima elinganiselweyo enomlinganiselo we-4.2), kufuphi nonxweme lwaseSiriya, ilandelwa ziinyikima ezincinane ezimbini, emva koko iqela leenyikima zomhlaba “ezincinane”.
NgoLwesithathu ekuseni, inyikima ye-4.7-magnitude yabhalwa kufuphi nonxweme lwaseSiriya, i-40 km enyakatho yesixeko saseLatakia.

Oku kwalandelwa yi-4.6 magnitude aftershock kunxweme lwaseSiriya, i-38 km kumntla-ntshona weLatakia.