Ukuzamazama komhlaba eMorocco kubangela ukuthi umhlaba uhlukane phakathi

Ukuzamazama komhlaba eMorocco kubangela ukuthi umhlaba uhlukane phakathi

Umhlaba uwonke usubone irekhodi lokuzamazama komhlaba kanye nokuzamazama komhlaba kusukela ekuqaleni konyaka.

Okokugcina kwalokhu kuzamazama komhlaba kwaba wudlame olwagadla eMorocco ekuseni namuhla ngesilinganiso esingu-7 esikalini sikaRichter, futhi kwalandelwa amakhulu okuzamazama okwenzeka ngemva kwalokho. UMnyango Wezangaphakathi WaseMoroccan umemezele ukuthi ukuzamazama komhlaba, okungumsuka wayo owawusesifundeni sase-Iguil esifundazweni i-Al Haousi, kubangele ukuwa kwenani lezakhiwo e-Al Haous, Marrakesh, Ouarzazate, Azilal, Chichaoua naseTaroudant. Abezindaba baseMoroccan bachaze ukuzamazama komhlaba njengokuzamazama komhlaba okuqine kakhulu uMbuso, kuyilapho ukukhala kosizo kukhuphuka ngaphansi kwemfucumfucu emadolobheni amaningana aseMorocco. Ukuzamazama komhlaba okunamandla kucekele phansi izakhiwo kusukela emadolobhaneni ase-Atlas Mountains kuya edolobheni lomlando lase-Marrakesh. Ukuzamazama komhlaba kudale umonakalo omkhulu wezinto ezibonakalayo, ngokusho kwezithombe nezigcawu ezibikwe abezindaba zendawo kanye nezinkundla zokuxhumana.

Ngokuvamile, ngokusho kososayensi, ukuzamazama komhlaba kwenzeka eduze kwemingcele yamapuleti e-lithospheric kanye namaphutha asebenzayo.

Ukuzamazama komhlaba kwenzeka kaningi kunalokho esikwaziyo, okulinganiselwa ku-100 XNUMX ngonyaka! Kodwa ezinye zazo ziphenduka zibe ukuzamazama komhlaba okubhubhisayo okuba usongo ekuphileni kwabantu nezakhiwo, okwavela ngemuva kokunyakaza okukhulu koqweqwe lomhlaba ekujuleni okungashoni, kuyilapho inani lokuzamazama komhlaba okuphawuliwe lingeqi ngaphezu kwekhulu noma ngaphansi. ngonyaka.

Njengoba ngaphambili kwachazwa uProfesa Nikolai Shestakov, uProfesa woMnyango Wokuqapha Nokuthuthukiswa Kwemithombo Yendawo e-Polytechnic Institute yaseRussian Far Eastern Federal University, wachaza indlela ukuzamazama komhlaba okwenzeka ngayo ngendlela elula ngokuthi: “Masicabange ukuthi uMhlaba isangweji ehlanganisa izingqimba ezahlukene. Ingxenye yawo engaphezulu, uqweqwe loMhlaba, inogqinsi oluncane olungamakhilomitha ayi-10 kuya kwayi-100, oluncane uma luqhathaniswa nobubanzi boMhlaba, obulingana namakhilomitha ayi-6371. Uqweqwe loMhlaba luhlukaniswe ngamapuleti, futhi lawa mapuleti ahlala enyakaza ngokuhlobene. Kunezinhlobo eziningana zokusabela kweplatelet. “Ndaweni ethile lapho zishayisana khona futhi kulezo zindawo ezishayisanayo, izintaba zivame ukuphakama, isibonelo esivelele kuyizintaba zaseHimalaya.”

Ngokwalokho okwabikwa yimithombo yezindaba yaseRussia, lesi sikhungo semfundo saseRussia saqhubeka, sichaza ukuziphatha kokuzamazama komhlaba, ngokuthi: “Endaweni ethile amapuleti ahlukana phakathi... nokunye, kanjalo ukuzamazama komhlaba kuba khona ngaso sonke isikhathi.” Amanye amapuleti ahamba ngokuhambisana. Ukuzamazama komhlaba kwenzeka eduze kwemingcele yamapuleti. “Ngaphakathi kwezingcwecwe, uma ukuzamazama komhlaba kwenzeka, akubalulekile futhi kuyivelakancane.”

Uveze ukuthi ukuzamazama komhlaba okujule kakhulu emlandweni kwenzeka ngo-2013 oLwandle lwase-Okhotsk, ogwini olusentshonalanga yeNhlonhlo yaseKamchatka, amakhilomitha angama-560 entshonalanga yePetropavlovsk-Kamchatsky. Isikhungo sawo sasisekujuleni okungamakhilomitha angaphezu kuka-600.

Nokho, okujabulisayo ukuthi ososayensi bathole ukuthi ukuzamazama komhlaba okukhulu, ikakhulukazi ukuzamazama komhlaba okujulile, kukhulula amandla ngenxa yokungqubuzana kwamapuleti e-lithosphere. Ngokwezibalo ezinembile zesayensi, kwatholakala ukuthi amandla angenza umhlaba “uqhekeke” angabangela ukuzamazama komhlaba okungaba namandla ngokuphindwe izikhathi ezingu-53 XNUMX kunokuzamazama komhlaba okunamandla kunakho konke okulotshwe isintu emlandweni waso. Lokhu kusho ukuthi sisekude nokuzamazama komhlaba okungadala ukucekelwa phansi komhlaba.

Ngokuqondene nokuzamazama komhlaba oku-5 okunamandla kakhulu okulotshwe isintu kuze kube manje, kungokulandelayo:

*Ukuzamazama komhlaba eKamchatka, okunesilinganiso esingu-9.0, kwenzeka ngo-November 1952. Ngenxa yalokhu kuzamazama, okwenzeka emngceleni ohlangene wezingcwecwe ezimbili oLwandlekazi iPacific, kwaba ne-tsunami enkulu ngenxa yokuzamazama komhlaba, kwacekela phansi. izindawo eziningi eziqhingini zaseKuril naseKamchatka.

*Ukuzamazama koMhlaba e-East Japan, okunesilinganiso esingu-9.1, kwenzeka ngo-2011 futhi kwabangela elinye lamagagasi e-tsunami acekela phansi kakhulu emlandweni wesintu, kwathatha ukuphila kwabantu abangu-20.

*Ukuzamazama komhlaba e-Alaska, okulinganiselwa ku-9.2, kwenzeka entwasahlobo ka-1964. Akuzange kube khona muntu owafa ngenxa yokuthi le ndawo yayingenabantu abaningi.

*Ukuzamazama komhlaba okungu-2004 magnitude kwagadla e-Indian Ocean ngo-9.3, futhi kwaba nomthelela omubi kakhulu e-Indonesia. I-tsunami eyaba umphumela yabulala abantu abangaba ingxenye yesine yesigidi.

*Ukuzamazama komhlaba okukhulu kwaseChile ngo-1960, okwakunobukhulu obungu-9.5, akuzange nje kubangele ukuzamazama komhlaba okunamandla nokubhubhisa kakhulu, kodwa futhi kwabangela i-tsunami enkulu eyakhukhula cishe lonke ugu lwasePacific.

Izibikezelo ze-horoscope zika-Maguy Farah zonyaka ka-2023