Amagagasi Sea - inkohliso umbono womuntu

Namuhla kunzima ukucabanga ukuthi ngesikhathi esisodwa ku-Earth babengekho abantu nemizi lapho manje uhlala khona, kanye imigwaqo namasimu eshayisa. Kodwa iqiniso liwukuthi zonke izinkathi Geological ukuwo olwandle, futhi ngendlela efanayo njengoba namuhla, amagagasi iphuma phakathi kwabo namabhange. Ngempela, landscape eminingi yasendulo emhlabeni uhlobo igagasi kwamanzi, esehlanganise it ngokuthathu okukabili. izimbongi Bangaki liphefumulelwe amagagasi olwandle! Kodwa kungakhathaliseki ukuthi incazelo yabo ibonisa okushiwo lesi simanga kweqiniso?

Thina bayigqolozela isithombe: olwandle kubonakale kithi kubo ehamba ikholomu amanzi. Kodwa-ke kuvela ukuthi lokhu akunjalo. Uma ubheka kuya chips noma yimuphi omunye izinto ezisebusweni amanzi (isibonelo, waya esikebheni) siqaphela ukuthi amagagasi eligadulayo kolwandle musa ibenze, futhi kuphela ephakamisa ke eyehlisiwe. Ngokufanayo, benyuka amagagasi lapho ipheshulwa umoya yellowing cornfield emasimini. izindlebe zakhe futhi umoba musa ukushintsha isikhundla sabo futhi musa phenduka kusuka endaweni eyodwa kuya kwenye. Bathi nje iwe kancane phambili bese futhi ubuyele indawo yokuqala. Kodwa thina awuboni, ngokuba noma bebona, ababalekela ensimini ngemva kwenye 'azulise ", futhi bonke izindlebe zivulekile endaweni efanayo.

Isenzakalo esifanayo kuyabonakala temdzabu. Khumbula isisho uqhathanisa abantu amahemuhemu, ulwandle amagagasi. Kanjani ngokushesha basakaze izindaba komuzi. Kodwa ngenkathi akekho siphela kusukela komunye umkhawulo kuya komunye, proclaiming them. Nje amagagasi izindaba ngocansi ngomlomo, bayigubungele yoke imikhawulo.

Kodwa emuva kuncike yethu. Iyini imbangela lokuzalwa zale amagagasi amahle, iyashesha futhi inamandla kolwandle, izithombe ezingasetshenziswa shake umcabango wethu, ngisho into efana nayo ukuze uhambisane kanye nokumesaba? Kuyaziwa ngisho izingane "Umoya, umoya! Nawe! - onamandla". Ipheshulwa hit amanzi, futhi "flex" ubuso bayo. Ngenxa yalokho, ingxenye yayo uyagoba, kanti ezinye, akhuphuke. ' Kulokhu, injabulo idluliselwa kwamanye amaphuzu futhi ithumba izindawo ezinkulu. Futhi lapha esiyibonayo kakade umphumela ovundlile ezidluliselwa ngesivinini. It asakazeka ngokushesha namagagasi okwabangelwa ukuzamazama. Ngesikhathi esifanayo babe kuyagcinwa hhayi kuphela emanzini kodwa futhi phansi.

Inkohliso umthelela esinawo bezibona ukuphakama negagasi lolwandle noma olwandle. Izinganekwane yokuphakama igagasi yonke intaba babe kwamehlisa ngemva ososayensi kulinganiswa ngempela yabo. Iphuzu lapha liwukuthi ngesikhathi kunesiphepho izingqapheli ezisebusweni esemkhunjini, lelo, kanye emanzini ewela ngokucijile phansi, bese othukayo phezu Crest of igagasi phezulu. Nale ewa ngisho wave ongaphakeme kubonakale okuvimbezela omkhulu. Lokhu kungenxa yokuthi, ukuthi kokuba emphemeni of umgibeli oyigcinayo olungaqondile, futhi idayagonali ulingana nobude emthambekeni. Ngo yolwandle oluvulekile amandla umoya uhlale elinamandla kakhulu. Kodwa amanzi usawoti has a high density futhi ayikuvumeli ukuba kwakha amagagasi amakhulu. Ukuze amatilosi, lesi simanga ivame ukuhlotshaniswa nhlekelele. Kodwa ngenxa eziphilayo abahlala ukujula kwamanzi, amagagasi ulwandle (ezikulu nezincani) zinhle. Bona bazogcwalisa endaweni yazo umoya-mpilo.