Namhlanje siza kuthetha ngohlobo lolwandle oluneempawu ezizodwa noluthathwa njengeqela elikhulu lamanzi. Imalunga nayo UMzantsi woLwandle lwase China. Luhlobo lolwandle olusecaleni olukuLwandlekazi lwePasifiki kwaye igama livela ekubeni kumazantsi eTshayina. Indawo ekulo lwandle imalunga ne-3.6 yezigidi zeekhilomitha. Ime emazantsi e-China.
Kweli nqaku siza kukuxelela ngazo zonke iimpawu, ukubunjwa nokubaluleka koLwandle lwase China lwase China.
Iimpawu eziphambili
Luhlobo lolwandle olunqamleza iPhilippines, iTaiwan, iMalaysia, iSingapore, iIndonesia, iThailand, iBrunei, iCambodia kunye neVietnam. Emantla mpuma yiTaiwan Strait, empuma ye-Malay Peninsula kunye nasezantsi yi-Borneo. Kuthathelwa ingqalelo isiqu esikhulu samanzi kwaye sinesitya esiphakathi esine-elliptical shape kwaye sineziqithi ezingaphezu kwe-250 ezincinci, iibhanki, iingqaqa, iitolls kunye nezitshixo. Kukho amaqela aliqela eziqithi ezikhulu apho uninzi lwazo kunye nokhenketho lwenziwa. Inani elikhulu lemilambo lingena emanzini olwandle, anje ngeMekong, iPearl River, iMin, iJiulong, iRajang, iPajang, iRed, iRio Grande de la Pampanga kunye nePásig.
ULwandle lwase China lwaseTshayina alunzulu kangako. Ngokungafaniyo nolunye ulwandle oluncinci, olunzulu, olu lwandle lunobunzulu obuphakathi kwe-1.212 yeemitha. Ithafa elumkisa lowo uphantsi kwamanzi kwaye inobunzulu beemitha ezingama-4.300. Ukutshintshiselana kwabo ngamanzi kunye nolwandle kwenzeka kakhulu kwindawo eyaziwa ngokuba yiStraits of Luzon. Le ndawo inoxanduva lokudibanisa olu lwandle kunye neePhilippines ukuze zibe yinxalenye ye-Pacific eseMpuma.
Amaqondo obushushu oLwandle lwaseMzantsi China
Ukuba sihlalutya umphezulu kunye neendawo ezikufuphi nabo siyabona ukuba amanzi afudumele ngokubanzi. Ubushushu ngokomyinge zijikeleze iidigri ezingama-29 ngeenyanga zehlobo. Kuyinyani ukuba ngexesha lobusika amaqondo obushushu ayahluka, kodwa akwenza oko ngamaqondo ambalwa. Isathathwa njengenye yezona zilwandle zifudumeleyo. Iqondo lobushushu kwiinyanga zobusika liyehla liye kuma-21 degrees, kodwa lihlala phantse lihlala linamaxabiso angama-27 degrees kwezinye iindawo. Inxalenye esemantla yeyona ibanda kakhulu.
Iimonons zinempembelelo enkulu kolu lwandle. Kwaye kukuba ezi monsoons zezo zilawula imisinga yomphezulu wolwandle kunye nemimoya evuthuzayo kule nxalenye. Kuqhelekile ukuba iichotho ezininzi zenzeke ngexesha lehlobo. Ithathwa njengenye ye Olona lwandle lukhulu ekumda emhlabeni kwaye lolona lukhulu kulwandle lonke lwasentshona yePasifiki.
Ubume kunye nemvelaphi
Njengenxalenye yoLwandlekazi lwePasifiki, uLwandle lwase China lwaseTshayina lwenziwa lwaselwandle olukhulu lwaze lwenziwa ngaphezulu kwesigidi se-750 seminyaka eyadlulayo. Ngelo xesha, kwakukho ilizwekazi eliphambili elaziwa ngegama likaRodinia. Kufuneka kukhunjulwe ukuba olu lwandle lumalunga neminyaka engama-45 ezigidi ubudala, nangona lwalusenziwa ngaphambili. Ivela ngenxa yeziganeko ezahlukeneyo zetectonic emva kokuba indawo ihambile ukusuka kumazantsi eTshayina.
Kukho ezinye izazinzulu ezijonga ukuba ukuhamba kwe Amacwecwe etektoni ukuba loluphi ulwandle olunike isiqabu malunga neminyaka engama-55 ezigidi eyadlulayo. Le ntshukumo yaqina xa i-Indian tectonic plates kunye ne-Eurasian tectonic plate zangqubana.
Isitya sokudibanisa esivelise olu lwandle nangona sasisemncinci ngexesha le-Miocene. Olu lwandle lwalukhula lude luye kufikelela ekwandeni komgangatho wolwandle ukuze lwenze uqweqwe olutsha emva kokuqhekeka kwelizwekazi laseRodinia. Kuthathe malunga neminyaka engama-30 ezigidi ukwenza le fomu. Ulwandle lwalutshonile kancinci ngexesha le- imiyaka yomkence oko kwenzeka ngexesha lika Ipleistocene.
Iintlobo ngeentlobo zoLwandle lwase China lwase China
Olu lwandle lutyebe kakhulu kubomi baselwandle. Zininzi iintlobo zeentlanzi eziyinxalenye ebalulekileyo yokutya kwezi dolophu zikufuphi nolwandle. Phakathi kwezilwanyana zaselwandle zoLwandle lwase China lwase China sifumana ityhuna, isardadi, isherring, imackerel kunye necorvina. Nangona kunjalo, Abantu babangela umsebenzi wokuloba ngokugqithileyo kwezi ndawo kwaye kukho iintlobo ezithile ezisendleleni yokuba ziphele ngokupheleleyo. Kukho iintlobo zezinto ezisemngciphekweni wokuphela ekungekho kuzo kuphela iintlobo zeentlanzi ezityiwayo. Sifumene kunye ne-turtle yolwandle eluhlaza kunye ne-Hawksbill turtle. Ezi ntlanzi zimbini zazininzi kakhulu ngaphambili, nangona namhlanje amanani asezantsi. Basenokubonakala kwezinye kodwa kwiindawo ezithile.
Iindidi ezininzi zookrebe zenza amakhaya kula manzi. Ezinye zazo zezona ziyinyani ezinje ngookrebe abamhlophe, ookrebe kunye nookrebe basendle. Ngaselunxwemeni, ngakumbi ezo zikumazantsi olwandle, zinokubonwa kwiingqaqa ezininzi zekorale. Kweminye imimandla kukho ingca yolwandle kunye neziqithi ezininzi ezinokuthi zibonelele ngendawo yokuhlala efanelekileyo yezinye iintlobo zeentaka ezinje nge-brown gannet, i-red-billed tern kunye ne-white tern.
Enye yeenzuzo ezibonelelwa lolu lwandle kwaye esinye sezizathu zokuba sisityebi kwindalo ephilayo kukuba uLwandle lwase China lwase China ityebe kakhulu kubutyebi bendalo. Inovimba wegesi yendalo enokuba sesona sibonelelo sikhulu sehydrocarbon kwingingqi iphela. Oku kwenza ukuba olu lwandle lubaluleke kakhulu kuqoqosho. Ambalwa kuphela amaqela esiqithi esiwakhankanye ngentla apha ayinyani ioyile kunye negesi yendalo eninzi. Ngokubanzi, ulwandle olwandle kucingelwa ukuba lunovimba omkhulu. Amanzi yindlela ebalulekileyo yaselwandle eye yahanjiswa ngenkulungwane ezininzi.
Olu lwandle lusongelwa zizinto ezininzi. Phakathi kwazo sifumana ukuloba ngokugqithileyo kunye nezinye iindawo ezibanjisiweyo ezibangela ukuhla kweentlanzi. Njengokuba Iindawo zokuhlala iindlwana zofudo ezininzi zichaphazeleka kukuphulukana nendawo ezihlala kuyo kunye nokuloba kakhulu. Ungcoliseko yenye yeengxaki ezinkulu ezichaphazela iyantlukwano.
Ndiyathemba ukuba ngolu lwazi unokufunda ngakumbi malunga noLwandle lwase China lwase China.