Ukudilika kwenhlabathi kungenye yezinhlekelele zemvelo eziningi ezidala ukucekelwa phansi nokulahlekelwa ukuphila emhlabeni wonke. Ihambisana nohlobo lwenhlabathi, ukuthambekela, indawo yezindawo zabantu kanye nokuba khona kokuzamazama komhlaba kanye/noma iziphepho ezinamandla. Kunezimbangela nemiphumela eminingi eholela ekwehlukeni imiphumela yokudilika komhlaba.
Kulesi sihloko sizokutshela ukuthi iyini imiphumela ehlukene yokudilika komhlaba nokuthi yiziphi izimbangela nemiphumela yako.
Imiphumela yokudilika komhlaba
Ngokocwaningo olwenziwe yi-International Centre for Landslides eNyuvesi yaseDurham e-UK, kube nokubihlika komhlaba okuyingozi okungu-2.620 phakathi kuka-2004 no-2010. Lokhu kubihlika komhlaba kwabulala abantu abangaphezu kuka-32,322. Lesi sibalo asifaki ukudilika komhlaba okudalwe ukuzamazama komhlaba. Kuyamangaza okutholakele uma kubhekwa isibalo sabantu abashona ngenxa yokubihlika komhlaba. Ngakho-ke, kubalulekile ukuqonda izimbangela nezimpawu eziyisixwayiso zokudilika komhlaba okungaba khona ukuze kuncishiswe ukulahlekelwa.
Ukudilika kwenhlabathi, ngezinye izikhathi okubizwa ngokuthi ukudilika komhlaba, ukuhluleka kweslope, noma ukudilika komhlaba, ukugeleza okungalawuleki kwamatshe, ukungcola, udoti, noma inhlanganisela yakho konke kokuthathu. Ukudilika komhlaba kuwumphumela wokwehluleka kwezinto ezakha umthambeka futhi ziqiniswa amandla adonsela phansi.. Lapho inhlabathi igcwala, iyantengantenga futhi ingalingani isikhathi eside. Kulapho-ke kwaqubuka khona ukudilika komhlaba. Lapho abantu behlala kula magquma noma ezintabeni, ngokuvamile kuba yindaba yesikhathi nje ngaphambi kokuba kugadle inhlekelele.
Izimbangela zemvelo zokudilika komhlaba
Nakuba ukudilika komhlaba kubhekwa njengezinhlekelele zemvelo, izinguquko zemvelo ezibangelwa abantu ziye zabangela ukuba zibuye muva nje. Nakuba ukudilika kwenhlabathi kunezimbangela ezihlukahlukene, kunezinto ezimbili ezifanayo: zinikwa amandla amandla adonsela phansi futhi ziwumphumela wokucekelwa phansi kwenhlabathi namadwala akha igquma.
Isimo sezulu
Ukushintsha kwesimo sezulu isikhathi eside kungathinta kakhulu ukuzinza kwenhlabathi. Ukuncipha kwemvula sekukonke kuphumela emazingeni aphansi angaphansi komhlaba kanye nesisindo senhlabathi esiphelele, ukuncibilika okuncane kwezinto kanye nomsebenzi omncane wokuqandisa nokuncibilika. Ukwenyuka okukhulu kwemvula noma ukugcwala komhlabathi kuzokwandisa kakhulu amazinga amanzi angaphansi komhlaba. Ukudilika komhlaba kwenzeka lapho indawo eyehlelayo igcwala amanzi ngokuphelele. Ngaphandle kokusekelwa ngomshini kwezimpande, inhlabathi izoqala ukulahlekelwa yiyo.
Ukuzamazama komhlaba
Umsebenzi wokuzamazama komhlaba kudala kudala ukudilika kwenhlabathi emhlabeni jikelele. Njalo lapho amapuleti e-tectonic ehamba, kanjalo nomhlabathi obasibekele. Uma ukuzamazama komhlaba kushaya umqansa, ezikhathini eziningi ukudilika komhlaba nokudilika kwenhlabathi kwenzeka. Ukwengeza, umlotha wentaba-mlilo nokudilika komhlaba okubangelwa ukuzamazama komhlaba nakho kungabangela ukunyakaza komhlaba ngezinga elikhulu.
Isimo sezulu
Isimo sezulu yinqubo yemvelo yokuwohloka kwamadwala, okwenza izinto zibe buthaka futhi zithambekele ekubhidlikeni komhlaba. Isimo sezulu sikhiqizwa isenzo samakhemikhali samanzi, umoya, izitshalo kanye namagciwane. Uma amatshe ephuka ngokwanele, angashelela futhi abangele ukudilika komhlaba.
Ukuguguleka kwenhlabathi
Ukuguguleka kwemisinga yamanzi engavamile njenge imifula, imifula, umoya, imisinga, iqhwa, amagagasi, njll., kubangela ukuthi ukusekela okucashile kanye neseceleni komthambeka kunyamalale, nokudilika komhlaba kwenzeke.
Izintaba-mlilo
Ukuqhuma kwentaba-mlilo kungabangela ukudilika komhlaba. Uma ukuqhuma kwenzeka ezimweni ezimanzi, umhlabathi uzoqala ukwehla, okubangela ukudilika komhlaba. I-Stratovolcano iyisibonelo sakudala sentaba-mlilo ebangela ukudilika komhlaba okuningi.
Umlilo wehlathi
Imililo yamahlathi idala ukuguguleka kwenhlabathi futhi iholele ezikhukhuleni, okuthi bese kubanga ukudilika komhlaba
Ukunciphisa amandla
Imithambeka emikhulu ehlangene namandla adonsela phansi ingabangela ukudilika komhlaba okukhulu.
Izimbangela Zabantu Zokudilika Komhlaba
Ukumayini
I-Las imisebenzi yezimayini ngamasu okuqhumisa yiyona imbangela enkulu yokudilika kwenhlabathi. Ukudlidliza okuvela ekuqhumeni kungenza umhlabathi ube buthaka kwezinye izindawo ezijwayele ukudilika. Ukuba buthaka komhlaba kusho ukuthi ukudilika komhlaba kungenzeka noma nini.
ukusika okuhlanzekile
Ukugawula imithi kuyindlela yokugawula izingodo esusa zonke izihlahla ezindala endaweni. Le nqubo iyingozi ngoba ishintsha ukwakheka kwemishini yezimpande endaweni.
Imiphumela emibi yokudilika komhlaba
Ukudilika
Ukudilika komhlaba kukhonjiswe ukuthi kudala umonakalo wempahla. Uma ukwehla kubaluleke kakhulu, kungase kucekele phansi umnotho wesifunda noma wezwe. Ngemva kokuwa, indawo ethintekile ngokuvamile iyalungiswa. Ukulungiswa okunjalo kuhilela izindleko ezinkulu zezimali. Ngokwesibonelo, ukudilika kwenhlabathi ngo-1983 e-Utah, eU.SA, kwabiza cishe amaRandi ayizigidi ezingu-500 ukulungisa. Ukulahlekelwa okuvela ekubhidlikeni komhlaba e-United States kulinganiselwa ku-$1.5 billion ngonyaka.
Ingqalasizinda
Ukugeleza okuphoqelekile kodaka, amatshe namatshe okubangelwa ukudilika kwenhlabathi kungabangela umonakalo omkhulu wempahla. Ingqalasizinda efana nemigwaqo, izitimela, izindawo zokungcebeleka, izakhiwo kanye nezinhlelo zokuxhumana zingacekelwa phansi yinhlabathi eyodwa.
Izimpilo ezilahlekile
Imiphakathi ehlala ngaphansi kwentaba isengozini enkulu yokufa ngenxa yokubihlika kwenhlabathi. Ukudilika kwenhlabathi okukhulu kuletha amatshe amakhulu, imfucumfucu enzima, nenhlabathi ewugqinsi. Lolu hlobo lwama-slide lunamandla okubulala abantu abaningi ngomthelela. Ngokwesibonelo, ukudilika kwenhlabathi e-UK eminyakeni embalwa edlule kwabangela imfucumfucu enyakazayo kwacekela phansi isikole kwashona abantu abangaphezu kuka-144, okuhlanganisa nezingane ezifunda isikole ezingu-116 ezineminyaka engu-7 kuya kweyishumi. Kwesinye isigameko, i-NBC News ibike ukuthi abantu abangu-10 babulawa endaweni yodaka e-Oso, eWashington ngoMashi 21, 22.
Kuthinta ubuhle bendawo
Ukuguguleka kokubihlika kwenhlabathi kushiye indawo emagebhugebhu futhi engabukeki. Izinqwaba zomhlaba, amatshe nemfucumfucu etholakala emithambekeni Bangakwazi ukukhava umhlaba osetshenziswa imiphakathi ngezinhloso zezolimo noma zomphakathi.
Umthelela ku-ecosystem yomfula
Ukungcola, imfucumfucu, namadwala ashibilika ezansi emithambekeni kungangena emifuleni futhi kuvimbele ukugeleza kwawo okungokwemvelo. Izindawo eziningi ezihlala eduze nomfula, njengezinhlanzi, zingafa ngenxa yokuphazamiseka kokugeleza kwamanzi okungokwemvelo. Imiphakathi encike emfuleni ukwenza imisebenzi yasekhaya kanye nokunisela izothinteka uma ukugeleza kwamanzi kuvimbekile.
Ngithemba ukuthi ngalolu lwazi ungafunda kabanzi mayelana nemiphumela yokudilika komhlaba kanye nezici zabo.