Njengoba sibonile esihlokweni ku izingqimba zangaphakathi zomhlaba, kunezinhlelo ezine zasemhlabeni: Umkhathi, i-biosphere, i-hydrosphere ne-geosphere. Ngaphakathi kwe-geosphere sithola izingqimba ezahlukahlukene lapho iplanethi yethu yakhiwe khona. Umuntu uzamile ukujula esebenzisa izindlela zokuhlola ukuze akwazi ukutadisha okungaphansi kwezinyawo zethu. Kodwa-ke, sikwazile ukungena kuphela amakhilomitha ambalwa. Kwe-apula, sidabule isikhumba salo esihle kuphela

Ukuze sifunde konke okungaphakathi komhlaba kumele sisebenzise izindlela ezingaqondile. Ngale ndlela, kuye kwenzeka ukuthi kutholakale amamodeli amabili achaza ukwakheka kwezendlalelo zomhlaba ngokuya kokwakhiwa kwezinto nezinto eziguqukayo ezilandelayo. Ngakolunye uhlangothi, sinemodeli emile lapho izingqimba zomhlaba zakhiwa khona: Isikhumba, ingubo kanye nomongo. Ngakolunye uhlangothi, sinemodeli enamandla lapho izingqimba zomhlaba zingu: I-Lithosphere, i-asthenosphere, i-mesosphere ne-endosphere.

Imodeli emile

Ukubuyekeza imodeli emile kancane, sithola ukuthi uqweqwe lomhlaba lwehlukaniswe phakathi uqweqwe lwamazwekazi kanye noqweqwe lwasolwandle. I-continental crust iqukethe izinto zokwakheka okuhlukahlukene nobudala, kuyilapho uqweqwe lwasolwandle lufana kakhulu futhi luncane. Ukuze ufunde kabanzi mayelana nokuthi izintaba zakhiwe kanjani, ungathintana ukwakheka kwezintaba.

Siphinde sibe nengubo yasemhlabeni efane kakhulu lapho zikhona imibukiso ye-convection. Ekugcineni, umnyombo woMhlaba, owakhiwe ngensimbi ne-nickel futhi ubonakala ngokuminyana kwawo okuphezulu kanye nezinga lokushisa.

Imodeli yeDynamic

Sizogxila kumodeli eguqukayo. Njengoba sesishilo ngaphambili, ngokwemodeli eguquguqukayo izingqimba zoMhlaba ziyi-lithosphere, i-asthenosphere, i-mesosphere ne-endosphere. Namuhla sizokhuluma ngokuningiliziwe mayelana ne- lithosphere.

Umthombo: https://tectonicadeplacasprimeroc.wikispaces.com/02.+MODEL+EST%C3%81TICO+DEL+INTERIOR+DEL+INTERIOR+DE+LA+TIERRA

I-Lithosphere

I-lithosphere yakhiwa yilokho okuzoba kumodeli ye-static uqweqwe loMhlaba nengubo yangaphandle yoMhlaba. Isakhiwo sawo siqinile futhi sinokujiya okungaba ngu-100 km. Ukuqina kwayo ekujuleni okunjalo kuyaziwa ngoba ijubane lamagagasi azamazama komhlaba lilokhu likhuphuka ngokujula. Ukuze uqonde kangcono ukwakheka kwayo, ungathintana isostasy kanye nokuncipha.

Ku-lithosphere, izinga lokushisa nokucindezela kufinyelela amanani avumela amadwala ukuba ancibilike ezindaweni ezithile. Ukwengeza, ungafunda ngezingxenye zokuzamazama komhlaba izingxenye zokuzamazama komhlaba.

Ngokuya ngohlobo lwe-crust oluqukethe i-lithosphere, silihlukanisa libe yizinhlobo ezimbili:

• I-lithosphere yezwekazi: Yi-lithosphere eyakhiwa uqweqwe lwamazwekazi kanye nengxenye yangaphandle yengubo yomhlaba. Kuwo kukhona amazwekazi, izinhlelo zezintaba, njll. Ubukhulu bucishe bube amakhilomitha ayi-120 kuphela futhi budala beminyaka yobudala njengoba kukhona amatshe okuthi engaphezu kweminyaka engu-3.800 XNUMX ubudala.
• I-Oceanic lithosphere: Yakhiwa uqweqwe lwasolwandle nengubo yangaphandle yomhlaba. Zakha phansi olwandle futhi zincane kune-lithosphere yezwekazi. Ubukhulu bayo bungu-65 km. Yakhiwe ikakhulukazi ngamabhasalthi futhi kuyo kukhona izingqimba ze-oceanic. Lezi yizintaba ezingaphansi kolwandle lapho ubukhulu bungu-7 km kuphela.

Umthombo: http://www.aula2005.com/html/cn1eso/04lalitosfera/04lalitosferaes.htm

I-lithosphere ihlezi phezu kwe-asthenosphere equkethe yonke isambatho sangaphandle soMhlaba. I-lithosphere ihlukaniswe yaba amapuleti ahlukene e-lithospheric noma e-tectonic ahamba ngokuqhubekayo. Ukuze ufunde kabanzi mayelana namapuleti, ungafunda mayelana imiphetho yepuleti le-tectonic.

Umbono wokukhukhuleka kwezwekazi

Kuze kube sekuqaleni kwekhulu lama-1910, izinto zasemhlabeni ezinjengezintaba-mlilo, ukuzamazama komhlaba nama-folds kwakungamaqiniso ayengenayo incazelo. Kwakungekho ndlela yokuchaza ukwakheka kwamazwekazi, ukwakheka kwamabanga nezintaba, njll. Kusukela ngo-XNUMX sibonga isazi sokuma komhlaba saseJalimane U-Alfred Wegener, eyayiphakamisa iTheory of drift yezwekazi, kungenzeka ukuthi inikeze incazelo futhi ikwazi ukuhlobanisa yonke le mibono nemibono.

Lo mbono waphakanyiswa ngo-1912 futhi wamukelwa ngo-1915. U-Wegener waqagela ukuthi amazwekazi ayahamba ngokuya ngezivivinyo ezahlukahlukene.

• Ukuhlolwa kwe-Geological. Zazisekelwe ebudlelwaneni phakathi kwezakhiwo ze-geological ezinhlangothini zombili zoLwandlekazi i-Atlantic. Okusho ukuthi, ukwakheka kwamazwekazi kubonakala kufanelana njengoba ake andawonye. Izwekazi lomhlaba wonke elake lahlanganiswa futhi elaligcina zonke izinhlobo zezitshalo nezilwane kule planethi laqanjwa ngokuthi iPangea. Ungafunda kabanzi mayelana nalesi simo ngokubonisana.

Amazwekazi ahlangana ndawonye. Umthombo: http://recursos.cnice.mec.es/biosfera/alumno/4ESO/MedioNatural1I/contente2.htm

• Ubufakazi bePaleontological. Lezi zivivinyo zahlaziya ukuba khona kwezitshalo nezilwane ezisafufusa ezifanayo kakhulu ezindaweni zasezwekazini okwamanje ezihlukaniswa ulwandle Ukwengeza, kunomehluko phakathi kweziqhingi zentaba-mlilo neziqhingi okungaxhunyanwa nazo. lapha.

Umthombo :: http://www.geologia.unam.mx:8080/igl/index.php/difusion-y-divulgacion/temas-selectos/568-la-teoria-de-la-tectonica-de-placas-y -ukuqhubeka kwezwekazi

• Ubufakazi bePaleoclimatic. Lezi zivivinyo zifundise ukutholakala kwamatshe okwethula izimo zezulu ezihlukile endaweni abahlala kuyo njengamanje.

Ekuqaleni, le ndlela yokukhukhuleka kwezwekazi yenqatshwa ngumphakathi wesayensi ngoba yayingenayo indlela okuchazwa ngayo ukuhamba kwamazwekazi. Yimaphi amandla ahambisa amazwekazi? UWegener uzame ukuchaza lokhu ngokuthi amazwekazi ahamba ngokwehlukana kwabantu nokuthi amazwekazi, njengoba eminyene, ashibilika njengokhaphethi phansi ekamelweni. Lokhu kwenqatshelwe yisikhulu amandla okulwa lokho kukhona.

Plate tectonics theory

Ithiyori yePlate Tectonics yaphakanyiswa kanye nayo yonke idatha ngo-1968 ngumphakathi wesayensi. Kuyo, i-lithosphere ungqimba oluqinile olungaphezulu loMhlaba (uqweqwe nengubo yangaphandle) futhi ihlukaniswe yaba izingcezu ezibizwa amapuleti lokho kuhamba. Amapuleti ayashintsha ngosayizi nangokuma kwawo futhi anganyamalala. Amazwekazi akulezi zingcwephe futhi ashukunyiswa ngu imisinga yombukiso yesembatho somhlaba. Ukuze uqonde ukuthi izintaba zakhiwe kanjani, ungavakashela isihloko esithi.

Imingcele ye-plate yilapho ukunyakaza kokuzamazama komhlaba kanye nezinqubo ze-geological zenzeka. Umkhawulo ophansi wepuleti uyashisa. Ukushayisana kwamapuleti yikho okudala ukugoqa, amaphutha nokuzamazama komhlaba. Ukuze uthole ulwazi olwengeziwe mayelana nokuzamazama komhlaba, ungabheka isihloko esithi ukuzamazama komhlaba eNaples. Ukunyakaza okuhlukene kuye kwahlongozwa ukuchaza ukunyakaza kwamapuleti. Lapho amapuleti enyakaza, izinhlobo ezintathu zokucindezeleka zingenzeka emingceleni ephakathi kwawo, okubangela izinhlobo ezintathu ezihlukene zamachopho.

• Imiphetho ehlukanisayo noma imikhawulo yokwakha: Yizindawo lapho kunezingcindezi zokuqina ezijwayele ukwehlukanisa amapuleti. Indawo yemikhawulo yokwakha yimifula yolwandle. Iphansi lolwandle landa phakathi kuka-5 no-20 cm ngonyaka futhi kunokugeleza kokushisa kwangaphakathi. Umsebenzi wokuzamazama komhlaba kwenzeka ekujuleni okungaba ngamakhilomitha angama-70.
• Iguqula imiphetho noma imingcele eyonakalisayo: Zenzeka phakathi kwamapuleti zibhekane ngamandla okucindezelwa. Ipuleti elincanyana nelicinene licwilisa ngaphansi kwelinye bese lingena engubeni. Zibizwa ngama-subduction zones. Ngenxa yalokhu, ama-orogens nama-arches eziqhingi akhiwa. Kunezinhlobo eziningana zamaphethelo aguqukayo ngokuya ngomsebenzi wamapuleti:
  • Ukushayisana phakathi kwe-lithosphere yolwandle nezwekazi: Ipuleti lasolwandle yilona elihlula ngaphansi kwezwekazi. Lapho lokhu kwenzeka, ukwakheka komsele wasolwandle kwenzeka, umsebenzi omkhulu wokuzamazama komhlaba, umsebenzi omkhulu oshisayo nokwakhiwa kwamaketanga amasha we-orogenic.
  • Ukushayisana phakathi kwe-oceanic ne-oceanic lithosphere: Lapho kwenzeka lesi simo, kwenziwa umsele wasolwandle kanye nomsebenzi wentaba-mlilo ongaphansi kwamanzi.
  • Ukushayisana phakathi kwe-lithosphere yezwekazi nelizwekazi: Lokhu kubangela ukuvala kolwandle olwabahlukanisa kanye nokwakheka kwezintaba ezinkulu ze-orogenic. Zakhiwa kanje izintaba ze-Himalaya. Ukuze uthole okwengeziwe ngale nqubo, vakashela ukuthi izintaba zaseHimalaya zaqala kanjani.

• Imiphetho engathathi hlangothi noma izingcindezi ze-shear: Yizindawo lapho ubudlelwano phakathi kwamapuleti amabili benzeka khona ngenxa yengcindezi yokushefa ngenxa yokufuduka ngemuva kwabo phakathi kwabo. Ngakho-ke alikho i-lithosphere elenzelwe noma elonakaliswe. Ukuguqula amaphutha kuhlobene nengcindezi ye-shear lapho amapuleti ahamba khona ngezindlela ezihlukile futhi akhiqize uchungechunge olukhulu lokuzamazama komhlaba.

Umthombo: http://www.slideshare.net/aimorales/lmites-12537872?smtNoRedir=1

Kukhona amandla okushayela okubangwa ukushisa okugcinwe ngaphakathi eMhlabeni. Amandla ashisayo alokhu kushisa okugciniwe aguqulwa abe amandla asetshenziswa yi-convection currents ku-mantle. I-mantle inamandla okugeleza ngesivinini esincane (1 cm / ngonyaka). Kungakho umnyakazo wamazwekazi ungabonakali ngesilinganiso somuntu.

Amapuleti weLithospheric eMhlabeni

Ipuleti lase-Eurasia

Isifunda empumalanga ye-Atlantic Ridge. Ihlanganisa ulwandle olusempumalanga ye-Atlantic Ridge, iYurophu kanye ne-Asia eningi kuze kufike eziqhingini zaseJapan. Endaweni yayo yolwandle inokuxhumana okwehlukile nocwecwe lwaseNyakatho Melika, kuthi ngaseningizimu kushayisane nocwecwe lwase-Afrika (ngenxa yalokho, kwakhiwa ama-Alps), nasempumalanga, namapuleti asePacific nasePhilippines. Le ndawo, ngenxa yomsebenzi wayo omkhulu, iyingxenye yomlilo wasePacific.

Ukhukhunathi nama-Plates aseCaribbean

Lezi zingcwecwe ezimbili zasolwandle ziphakathi kweNyakatho Melika neNingizimu Melika.

Ipuleti elinokuthula

Liyipuleti elikhulu lasolwandle elixhumana nabanye abayisishiyagalombili. Imingcele ebhubhisayo itholakala emaphethelweni ayo akha indandatho yomlilo yasePacific.

Ipuleti le-Indica

Kufaka phakathi i-India, iNew Zealand, i-Australia nengxenye yolwandle ehambelana nayo. Ukushayisana kwayo nocwecwe lwase-Eurasia kukhiqize ukukhuphuka kwezintaba zaseHimalaya.

Ipuleti lase-Antarctic

Ipuleti elikhulu elenza imingcele ehlukile elixhumana nayo.

Ipuleti laseNingizimu Melika

Ipuleti elikhulu elinomkhawulo oguqukayo endaweni yalo esentshonalanga, lisebenza kakhulu ngokuzamazama komhlaba nangokusebenzisa izintaba-mlilo.

I-Nazca plate

I-Oceanic. Ukushayisana kwayo nepuleti laseNingizimu Melika kwavela e-Andes.

Ipuleti lelayisense lasePhilippine

Isolwandle futhi ingenye emincane kakhulu. Izungezwe imingcele eguquguqukayo, ehlotshaniswa namagagasi okunciphisa, anemisele yolwandle kanye nama-arcs esiqhingi.

Ipuleti laseNyakatho Melika

Endaweni yayo esentshonalanga ithinta ipuleti lasePacific. Kuhlobene nephutha elidumile laseSan Andrés (California), iphutha eliguqulayo futhi elibhekwa njengengxenye yebhande lomlilo.

Ipuleti lase-Afrika

Ipuleti elixutshiwe. Emngceleni walo osentshonalanga ukwanda kolwandle kwenzeka. Ngasenyakatho yakha iMedithera ne-Alps ngokushayisana nocwecwe lwase-Eurasia. Kuwo kuvulwa kancane kancane uqhekeko oluzohlukanisa i-Afrika izigaba ezimbili.

Ipuleti lesi-Arabhu

Ipuleti elincane emngceleni osentshonalanga lapho kuvulwa khona ulwandle lwakamuva kakhulu, uLwandle Olubomvu.

Umthombo: https://biogeo-entretodos.wikispaces.com/Tect%C3%B3nica+de+placas