Ulwandle lwaseJapan yizwe elihle ngokumangalisayo. Ingxenye yayo eseningizimu ihluke ngokusobala ukusuka enyakatho zombili esimweni sezulu nasosogwini. Naphezu kweqiniso lokuthi iSakhalin neziqhingi zaseJapan zihlukanisa ulwandle nolwandle, izivunguvungu zivame ukubangisana lapha, ziphakamisa amaza amakhulu, okwenza uLwandle lwaseJapan lungazolile kakhulu ngokuhambisa. Azikho izindawo zokungcebeleka ezidumile lapha, kepha lolu lwandle lubaluleke kakhulu emnothweni nasekuhwebeni kwamazwe amaningana, kubandakanya neRussia.
1. Iziphepho nezivunguvungu zivame ukudlula ngaphezu koLwandle lwaseJapan. Ikakhulu inani labo likhulu ekwindla.
2. Amagagasi amamitha ayishumi ukuphakama akuyona into engjwayelekile, futhi phakathi nezivunguvungu ezinkulu kakhulu ukuphakama kwawo kungaba phezulu kakhulu.
3. Ingxenye esenyakatho yoLwandle lwaseJapan ebusika ivame ukubanda futhi imbozwe yiqhwa.
4. Ulwandle lwaseJapan lunamagama amaningana. Ngakho-ke, izakhamizi zaseNingizimu Korea zilibiza ngokuthi i-East Sea, kanti kwi-DPRK zibizwa ngokuthi yi-East Korea Sea. Amabalazwe amazwe amaningi afanayo akhombisa amagama amabili okuqala.
5. Ezinye izakhamizi ezingaphansi kwamanzi oLwandle lwaseJapan zifudukela engxenyeni yayo eseningizimu efudumele ebusika.
6. Kuzo zonke izinto zasolwandle ezihlanza iRussia, yiJapan ecebile kakhulu ngokuchichima kwezidalwa eziphilayo ezihlala kuyo.
7. Kwezinhlobo ezingamakhulu ayisishiyagalolunye kwezinhlanzi. abahlala oLwandle lwaseJapan, cishe abangamakhulu amabili bayadoba.
I-8.Also, izinhlobo eziyishumi zaboshaka zihlala oLwandle lwaseJapan. Ngenhlanhla, akekho noyedwa kubo obeka ingozi enkulu kumuntu. Kepha bese kunama-jellyfish amancane angabulala ngokuthinta okukodwa kwesikhumba.
I-geology kanye ne-geology
Ulwandle lwaseJapan lwakhiwa ngesikhathi se-orogeneissi endaweni yesiqhingi saseJapan eMiocene.
Njengamanje, uLwandle lwaseJapan lunqunyelwe ezweni elingaseningizimu iRussia nesiqhingi saseSakhalin enyakatho, iPeninsula yaseKorea entshonalanga neziqhingi zaseJapan iHokkaido, Honshu neKyushu empumalanga naseningizimu. Ixhunyaniswe nolunye ulwandle ngezigaba ezinhlanu: iTraar Strait phakathi kwe-Asia kanye neSakhalin, iTraffit Strait phakathi kweSakhalin neHokkaido, iTsugaru Strait phakathi kweHokkaido neHonshu, iKingmon Strait phakathi kweHonshu neKyushu, kanye neKorea Strait phakathi kweNhlonhlo yeKorea neKyushu.
I-Korea Strait iqukethe i-West Channel kanye ne-Tsushima Strait ezinhlangothini zombili ze-Tsushima Island. Imizila yakhiwa ezikhathini zakamuva zejology. Omdala kubo nguTsugaru noTsushima. Okwakamuva yiLaperouse Strait, eyakhiwe eminyakeni engaba ngu-60,000-11,000 edlule. Zonke izinhlobo zingashonile ngokujula okuphezulu okungamamitha ayi-100 noma ngaphansi. Lokhu kuphazamisa ukushintshana kwamanzi nolwandle, ngaleyo ndlela kuhlukanise uLwandle lwaseJapan ezilwandle nasemalwandle angomakhelwane.
Ulwandle luhlukaniswe izingxenye ezintathu: iSamato basin eningizimu-mpumalanga, isisekelo saseJapan enyakatho nesisekelo saseTsushima (isisekelo sase-Ullung) eningizimu-ntshonalanga Isizinda saseJapan sivela olwandle futhi siyindawo ejulile yolwandle, kuyilapho isisekelo saseTsushima sisendaweni engezansi. ngokujulile ngaphansi kwe-2300 m. Amashalofu ezwekazi lonke abanzi asogwini olusempumalanga, kodwa ogwini olusentshonalanga, ikakhulukazi ogwini lwaseKorea, aluncane, ngokwesilinganiso cishe amakhilomitha angama-30.
Engxenyeni esenyakatho kunamashalofu amathathu ahlukene ezwekazini (ngaphezulu kuka-44 ° N). Bakha izinyathelo ezithambekele kancane eningizimu, futhi bacwiliswa ngokulandelana ekujuleni kwe-900-1400, 1700-2000 ne-2300-2600 m. Isinyathelo sokugcina sehlela ngokujulile ekujuleni okungamamitha ayi-3 500 ukuya enkabeni (ekujuleni) kwengxenye yolwandle. Ngaphansi kwale ngxenye kucishe kufane, kepha kunamapuleti amaningana. Ngaphezu kwalokho, ama-ridges angaphansi kwamanzi akhuphuka afinyelela ku-3 500 m; ugijima usuka enyakatho uye eningizimu phakathi nendawo engaphakathi.
Indawo yolwandle yaseJapan yolwandle iqukethe umgibeli we-Okudziri, umgibeli weSado, amabhange aseHakusan, umgibeli waseWakas kanye ne-Oka ridge. I-Yamato Ridge isuka ezwenikazi futhi iqukethe i-granite, i-rhyolite, i-andesite ne-basalt. Ingaphansi layo elingalingani limbozwe ngamatshe odwala lwentaba-mlilo. Ezinye izindawo eziningi zolwandle zivela olwandle. Amanzi asolwandle afinyelela kuma-300 m ahlala ezweni lonke futhi ambozwe ngengxube yodaka, isihlabathi, amatshe amatshe amatshe kanye nezingcezu zamatshe. Amadiphozi aphakathi kuka-300 kuye ku-800 m ambozwe yimfucumfucu ye-hemipelagic (okungukuthi, yemvelaphi yolwandle olwandle); lezi zidalwa zakhiwe ngodaka oluhlaza okwesibhakabhaka olugcwele izinto eziphilayo. Ukudonswa okubucayi kodaka obomvu kubusa ezindaweni ezijulile.
Azikho iziqhingi ezinkulu olwandle. Iningi lazo elincanyana zitholakala ngasogwini olusempumalanga, ngaphandle kwe-Ullyndo (South Korea). Iziqhingi ezibaluleke kakhulu yilezi: iMoneron, iRubun, iRisiri, i-Okushiri, i-Oshima, iSado, i-Okinoshima, i-Askold, isiRussia, nePutyatin. Ugu lolwandle luqondile futhi alunamabhawu amakhulu noma izimbambo ezinkulu, amafomu asogwini alula eduzane naseSakhalin futhi anomoya omningi eziqhingini zaseJapan.
Amabheshu amakhulu kunawo wonke: uPeter the Great Bay, uSoetskaya Gavan, uVladimir Bay, u-Olga, uPostyet Bay eRussia, i-East Korea Bay eseNyakatho Korea, u-Ishikari (Hokkaido), Toyama (Honshu) noWakasa (Honshu) eJapan. Izinduna ezivelele zibandakanya iLazarev, Gromov, eRussia, Krillon on Sakhalin, Nosappu, Tappi, Rebun, Rishiri, Okushiri, Daso no-Oka eJapan, noMusa Dan eNorth Korea.
Njengoba izinga lolwandle lomhlaba lehla lapho kuqala unyaka wokugcina weqhwa, ubunzima bezinto eziphumayo zoLwandle lwaseJapan bomile futhi bavala ngakunye. Okujulile futhi, ngenxa yalokho, okugcina kuvaliwe kuyisiteshi esentshonalanga seKorea Strait. Kunempikiswano yokuthi lokhu kwenzeke noma kungenjalo, ukuguqula ulwandle lwaseJapan lube ichibi elikhulu elibandayo lasenkabeni.
Isimo sezulu
Isimo sezulu soLwandle lwaseJapan sinesimo sezulu esijabulisayo. Izingxenye zolwandle zasenyakatho nezasentshonalanga zibanda kakhulu kunaseningizimu nasempumalanga. Ezinyangeni ezibandayo kakhulu (ngoJanuwari - uFebhuwari), izinga lokushisa lomoya engxenyeni esenyakatho yolwandle licishe libe ngu-−20 ° C, kuthi eningizimu kube ngu-+5 ° C. I-monsoon ehlobo iletha umoya ofudumele nowomswakama. Izinga lokushisa eliphakathi nenyanga elifudumele kakhulu (Agasti) engxenyeni esenyakatho icishe ibe ngu-+15 ° C, ezifundeni eziseningizimu cishe ngo-+25 ° C. Ekwindla, inani lezivunguvungu ezibangelwa imimoya yesivunguvungu liyanda. Amagagasi amakhulu kunobude be-8-10 m, futhi ngezivunguvungu amaza aphezulu afinyelela ekuphakameni kwamamitha ayi-13.
Ama-Currents
Amasondo angaphezulu komhlaba enza umjikelezo oqukethe i-Tsushima efudumele yamanje empumalanga nokubanda kwe Primorsky entshonalanga. Ebusika, izinga lokushisa lamanzi angaphezulu komhlaba ukusuka ku-−1-0 ° C enyakatho nasenyakatho-ntshonalanga kukhuphukela ku-10 - + 14 ° C eningizimu naseningizimu mpumalanga. Ukushisa kwentwasahlobo kufaka phakathi ukwanda okushesha kwamazinga okushisa kwamanzi olwandle. Ehlobo, izinga lokushisa lamanzi angaphezulu likhuphuka lisuka ku-18-20 ° C enyakatho lize liye ku-25-27 ° C eningizimu yolwandle. Ukusatshalaliswa kwezinga lokushisa mpo akufani kumasizini ahlukene ezindaweni ezahlukahlukene zolwandle. Ehlobo, ezingxenyeni ezisenyakatho zolwandle, izinga lokushisa le-18-10 ° C lihlala ungqimba we-10-15 m, bese lehla kakhulu ku-+4 ° C endaweni ephakeme ngamamitha angama-50, futhi ukusuka ekujuleni kwama-250 m, izinga lokushisa lihlala njalo cishe cishe ngo-1 ° C. Ezingxenyeni eziphakathi neziseningizimu zolwandle, izinga lokushisa lamanzi lehla ngokushelela ngokujula futhi lifinyelela ku-+6 ° C ngokujula kwamamitha angama-200, kusukela ekujuleni okungama-250 m, izinga lokushisa libamba cishe ngu-0 ° C.
Amaza
Amaza oLwandle lwaseJapan avezwe ngokusobala, ngezinga elikhulu noma elincane, ezifundeni ezahlukahlukene. Ukushintshashintsha kwezinga eliphakeme kakhulu kuyabonakala ezifundeni ezisenyakatho neziseningizimu ngokweqile. Ukuguquguquka kwezinga lolwandle lwesizini kwenzeka ngasikhathi sinye phezu kobuso bonke bolwandle; ukukhuphuka kwezinga okuphezulu kuyabonakala ehlobo.
Isembozo seqhwa
Ngokuya ngezimo zeqhwa, uLwandle lwaseJapan lungahlukaniswa lwaba izifunda ezintathu: iTatar Strait, indawo esogwini lwePrimorye isuka eCape Povorotny iye eCape Belkin kanye noPeter the Great Bay. Ebusika, iqhwa lihlala ligcinwa kuphela eTatar Strait nasePeter the Great Bay, kuwo wonke amanye amanzi, ngaphandle kwama-bays avaliwe kanye namakhethini engxenyeni esenyakatho nentshonalanga yolwandle, akuhlali kwakha njalo. Isifunda esibandayo kakhulu yi-Tatar Strait, lapho ebusika ngaphezulu kwama-90% awo wonke amaqhwa abonwa olwandle ayakhiwa. Ngokusho kwedatha yesikhathi eside, isikhathi sesikhathi esineqhwa ePeter the Great Bay siyizinsuku ezingama-120, kanti eTatar Strait - kusuka ezinsukwini ezingama-40-80 engxenyeni eseningizimu ye-strait, kuze kube yizinsuku eziyi-140-170 engxenyeni yayo esenyakatho.
Ukubonakala kokuqala kweqhwa kwenzeka eziqongweni zama-bays and bays, kuvalwe umoya, amaza nokuba nesendlalelo esingaphezulu sakhiwe ngodonga. Kusebusika obuthambile ePeter the Great Bay, iqhwa lokuqala lenziwa eminyakeni eyishumi kaNovemba, kanti naseTatar Strait, ezinhlokodolobha zeSovetskaya Gavan, Chikhacheva neNevelsky Strait, amafomu ayisisekelo eqhwa ayabonakala kakade ekuqaleni kukaNovemba. Ukwakhiwa kweqhwa kwasekuqaleni ePeter the Great Bay (Amur Bay) kwenzeka ekuqaleni kukaNovemba, eTatar Strait - engxenyeni yesibili ka-Okthoba. Ukuhamba kwesikhathi - ekupheleni kukaNovemba. Ekuqaleni kukaDisemba, ukukhula kwesembozo seqhwa ogwini lweSakhalin Island kushesha kakhulu kunokuba kuseduze nogu lolwandle. Ngokuvumelana nalokho, engxenyeni esempumalanga yeTatar Strait ngalesi sikhathi kuneqhwa eliningi kunasentshonalanga. Ekupheleni kukaDisemba, inani leqhwa ezingxenyeni ezisempumalanga nezasentshonalanga lilinganiswa, futhi ngemuva kokufika kufana neCape Surkum, indlela eya emaphethelweni iyaguquka: ukususwa kwawo ogwini lweSakhalin kuyancipha, kuthi lapho kugudlwa i-mainland kusebenze.
Olwandle lwaseJapan, ikhava leqhwa lifinyelela ekukhuleni kwalo okukhulu maphakathi noFebhuwari. Ngokwesilinganiso, ama-52% amaTatar Strait no-56% wePeter the Great Bay ambozwe yiqhwa.
Ukucibilika kweqhwa kuqala engxenyeni yokuqala kaMashi. Maphakathi noMashi, amanzi avulekile kaPeter the Great Bay nawo wonke ugu olusogwini oluya eCape Zolotoy acwengulwa yiqhwa. Umngcele wesembozo seqhwa eTraar Strait wehla usiya enyakatho-nentshonalanga, futhi engxenyeni esempumalanga yeqhwa elithintekayo liyacwilisa ngaleso sikhathi. Ukuhlanza kuqala ulwandle kusuka eqhweni kwenzeka eminyakeni eyishumi yesibili ka-Ephreli, kamuva - ngasekupheleni kukaMeyi - ekuqaleni kukaJuni.
Izimbali nezilwane
Umhlaba ongaphansi kwamanzi ezifundeni ezisenyakatho naseningizimu yoLwandle lwaseJapan uhlukile kakhulu. Ezifundeni ezisenyakatho ezisenyakatho nasenyakatho-ntshonalanga, kwaqalwa izitshalo nezilwane zezinhliziyo ezifudumele, futhi engxenyeni eseningizimu yolwandle, eningizimu yeVladivostok, inkundla yemvelo efudumele enamanzi afudumele. Ngasogwini lwaseMpumalanga Ekude, kuhlangana ingxube yamanzi afudumele namanzi athambile. Lapha ungathola ama-octopus nama-squid - abamele ejwayelekile yolwandle olufudumele. Ngasikhathi sinye, izindonga zibheke phezulu zimbozwe ama-anemone olwandle, izingadi ze-kelp - i-kelp - konke lokhu kufana nokuma komhlaba oLwandle Olumhlophe nolweBarents. Olwandle lwaseJapan, kunenqwaba yama-starfish nama-urchins olwandle, anemibala ehlukene namasayizi ahlukahlukene, kukhona ama-ophiuras, ama-shrimps, ama-crabs amancane (ama-Kamchatka crabs atholakala lapha ngoMeyi kuphela, abese eya olwandle). Emadwaleni nasematsheni kuhlala i-ascidia ebomvu ekhanyayo. Kuma-mollusks, ama-scallops yiwona ajwayelekile. Kwezinhlanzi, izinja zasolwandle, ama-ruffs olwandle, i-pollock, i-flounder, i-sim, i-salmon ye-chum itholakala kakhulu.
Ezokuzijabulisa nezokuvakasha
Kusukela ngawo-1990s, ugu loLwandle lwaseJapan ngasogwini lwePrimorye luqala ukuthuthukiswa ngenkuthalo ngabavakashi bendawo nabavakashi. Umfutho bekuyizinto ezinjengokukhanselwa noma ukwenziwa lula kokuhambela umngcele, ukukhuphuka kwezindleko zokuhamba kwabagibeli ezweni lonke, okwenza iholide laseFar East ogwini lweBlack Sea libiza kakhulu, futhi nokwanda kakhulu kwezimoto zomuntu siqu okwenze ukuthi ugu lwasePrimorye lufinyeleleke kubahlali baseKhabarovsk kanye nesifunda se-Amur.
Isimo sezomthetho samazwe omhlaba
Ngokuka-Article 122 we-UN Convention on the Law of the Sea, uLwandle lwaseJapan ulwandle oluvalekile ngaphakathi. Isigaba 123 seNgqungquthela sihlinzeka ngesibopho sezifundazwe ukuthi zibambisane futhi zixhumanise imisebenzi yazo ekuphathweni kwezinsiza zasolwandle, kepha, ngenxa yokushayisana phakathi kwe-DPRK, iRiphabhuliki yaseKorea kanye neJapan, ukuxhumanisa akwenzeki njengamanje.
Umbuzo wokuqamba amagama olwandle
ENingizimu Korea, uLwandle lwaseJapan lubizwa ngokuthi "i-East Sea" (i-cor. 동해), kanti eNyakatho - nolwandle oluseKorea East (cor. 조선 동해). Uhlangothi lwaseKorea luthi igama elithi "Ulwandle lwaseJapan" labekwa emhlabeni womhlaba nguMbuso waseJapan, ngoba ngonyaka we-1910 kuya ku-1945 i-Korea yathathwa futhi uhulumeni akakwazanga ukukhuluma ngesikhathi sokushicilelwa “Imingcele ye-Oceans kanye olwandle, ”umbono waseKorea awuzange unakwe.
Njengamanje, iKorea ayiphindeli ngohlobo olulodwa lwegama elithi "i-East Sea", kepha incoma kuphela ukuthi abashicileli bamakhadi basebenzise bobabili amagama ngokufana kuze kuxazululwe impikiswano. Lokhu kuholele ekutheni isibalo samazwe asebenzisa womabili amagama kumamephu abo ngasikhathi sinye sikhula njalo.
Uhlangothi lwaseJapan nalo lukhombisa ukuthi igama elithi "uLwandle waseJapan" litholakala kumamephu amaningi futhi liyamukelwa ngokuvamile, futhi ligcizelela ukusetshenziswa kwegama elithi "Ulwandle lwaseJapan" kuphela.
Amaqiniso abalulekile ngoLwandle lwaseJapan
- Ulwandle lwaseJapan ludumile izimo zezulu ezingalindelekilengakho-ke kubhekwa njengengozi. Imvamisa amaza afinyelela ekuphakameni kwamamitha ayi-10, kuthi ngesikhathi sesiphepho esinamandla aphakeme kakhulu.
- Njengoba amanzi ayo egezwa ngasogwini lwezifundazwe eziningana, igama olwandle alufani. ENingizimu Korea, ibizwa Empumalanga, futhi izakhamizi ze-DPRK ziyamfonela I-Korean Oriental. Okwe-Russia, kungumJapan ngokwemvelo. Emazweni amaningi, amagama ama-2 akhonjisiwe kumamephu.
- Njengoba kushiwo ngaphambili, ingxenye esenyakatho yesikebhe embozwe yiqhwa ebusika, okumangaza kakhulu izivakashi. Impela, ingxenye yendawo yayo ihlala ingenamakhaza ngenxa yokushisa okuhlukanisa kakhulu amanzi. I-Ice ancibilikisa kuphela maphakathi noJuni.
- Kuwo wonke unyaka, ngaphezulu komhlaba wokudlula kwamanzi izivunguvungu ezinamandla neziphepho. Kepha ikakhulukazi ikakhulukazi le nto yemvelo ihlasela ekwindla.
- Ngokungafani nolunye ulwandle, usawoti ungaphansi kwesilinganiso. Lokhu kwavumela ubheshu lwePacific ukuhlalisa inani elikhulu lezakhamizi nezimila ezingaphansi kwamanzi.
- Ensimini yogu lwaseRussia ehlobo amabhishi avulekilelapho abantu bendawo bekujabulela ukuphumula. Kepha ngeshwa, isikhathi esifushane sibekelwe isikhathi sokubhukuda.
- Kuyaziwa ukuthi ekujuleni okungaphezulu kwama-250 m okushisa kwamanzi akakhuphuki ngaphezulu kwe-0.
- Ukusuka olwandle lwaseJapan, ungaphuma ulwandle oluya ePacific ngokusebenzisa ubunzima obungu-4: AmaSangari, I-Nevelsky, IsiKorea futhi Larepuza.
- Amanzi emifula eminingi yezintaba aqondiswa emanzini ayo, futhi phakathi nonyaka ukugeleza komfula okuphelele ngaphezu kwama-200 cubic metres.
- Ukushintshana kwamanzi phakathi koLwandle i-East kanye nolwandle iPacific kuvunyelwe kuphela ezingxenyeni ezingaphezulu zamanzi. Ekujuleni okukhulu, lokhu akunakwenzeka ngenxa yamazinga okushisa aphansi.
- Yize kunethuba lokuphumula ogwini ehlobo, isimo sezulu phakathi nezinyanga ezifudumele kule ndawo inkungu futhi enamafu. Futhi futhi lenyuka kakhulu umswakama.
- Ukugcotshwa Kogu OluseMpumalanga Ekude Ngasolwandle lwaseJapan igolide, isiliva, itini kanye ne-tungsten. Amanye amaminerali amaningi akhanywa kule ndawo ecebile.
Amaqiniso athakazelisayo ngomhlaba ongaphansi kwamanzi oLwandle lwaseJapan
- Kuzo zonke izilwandle ezigeza ugu lwaseRussia, amaJapan abhekwa njengothile ngobuningi nezinhlobonhlobo zezidalwa eziphilayo nezitshalo ezihlala kuwo.
- Kuyatholakala lapha izinhlobo zezinhlanzi ezingaphezu kuka-900 futhi izinhlobo ezingaphezu kuka-10 zoshaka. Cishe izinhlobo ezingama-200 zabantu ngamunye zingaphansi kokudoba.
- Ngenkathi ebandayo, ezinye izinhlobo zezinhlanzi ziya ebusika engxenyeni eseningizimu yesikebhe, okufudumele nokuthandwa kakhulu yizo.
- Phezu kokuba khona kwezinhlobo eziningana zikashaka kula manzi, kubantu bona ungasongeli. Ingozi ekhethekile imelelwa yi-jellyfish encane, ukuthinta kwayo esikhunjeni somuntu omdala kungabulala.
- Isikhathi esithile e-East Sea bekuvinjelwe ukukhalisa. Kepha manje izinhlobo eziningana zemikhomo, izihlambi zasolwandle ngisho namahlengethwa zihlala emanzini alo. Ama-Minke whales, imikhomo yokubulala kanye nemikhomo yesidoda kubhekwa njengomunye wabantu abathandwa kakhulu.
- Futhi uhlala lapha lenqwaba zama-molluskezisebenza njengezihlungi zamanzi zemvelo. Zibekezelela kalula isikhathi sobusika futhi ziyakwazi ukukhula zize zibe ngu-70 cm ubude.
- Indima enkulu idlalwa ukutholakala imbaza emanzini olwandle. Ngemuva kwakho konke, aziyona kuphela injongo yokudoba, kodwa futhi nokudla okusebenzayo kwezinhlanzi ngokwazo nezinye izakhamizi. Zihlala kakhulu, yize zingakwazi ukuhamba, futhi lokhu kuyabasindisa ekuqothulweni okuphelele. Ngezinye izikhathi ukusetshenziswa kwabo ukudla kungaba ngisho nayingozi. Uma behlala ezindaweni ezinezimo ezingezinhle, khona-ke konke ukuphuma okulimazayo kwama-mollusks kuyadlula kubo uqobo. Ngakho-ke, kungcono ukuqala ukuthola indawo yabo.
- AbakwaShrimp abahlala oLwandle lwaseJapan bayakwazi ukukhula kufika ku-18 cm, futhi isibalo sabo asinqunyelwe nhlobo. Futhi kula manzi ukhukhamba olwandle bukhoma - izilwane zasolwandle eziwusizo kakhulu ezingenasici ezisetshenziswa kabanzi kwezokwelapha kanye ne-cosmetology.
- Lawa manzi awacebile nje ezintweni eziphilayo, kodwa futhi isitshalo ukwehluka. I-Algae kuphela inezinhlobo ezingaphezu kwama-220, kanti izinhlobo ezidumile kunazo zonke yi-kelp. Sekuyisikhathi eside isetshenziswa hhayi ekuphekeni kuphela, kepha naku-cosmetology. Kwezinye izindawo selivele selitshalwe emasimini.
Njengoba kwenzeka, uLwandle lwaseJapan luyindaba ekhangayo ngokukhethekile yocwaningo nokubuka. Kuyavela ukuthi ayigcini nje ngokungahlelekile, kodwa futhi icebile ngokulandela izakhamizi zomhlaba ongaphansi kwamanzi, uma uqhathanisa nolwandle Olumnyama. Izinsizakusebenza zalo zikhulu kakhulu, kepha ukuphuthuma kwenkinga yemvelo kusekhona. Ngaphandle kokuthi lezi zifunda kazilungelanga impela uhambo oluya eholidini, umhambi ngamunye kufanele aqhubeke nokuzivakashela ukubona ubuhle bePrimorsky Territory futhi ezwe amandla angenakuphikwa olwandle olugcwele ulaka.