Me ne Duniya ta topography ne sosai bambancin. tasiri ƙarfi

Akwai biyu main abubuwan da tasiri da samuwar siffofin daban-daban na surface, misali, daga daban-daban sasanninta, Duniya ta ɓawon burodi. Saboda haka, shared da yawa effects, wanda bayyana dalilin da ya sa da taimako na Duniya ne sosai bambancin. Amma da farko, za mu ga, abin da take ɗauke da ra'ayi na "taimako."

Kalmar "taimako", kuma ta muhimmanci

Wannan kalma ne na Faransa asalin, ko wasu kafofin bayyana shi da fassara cikin litattafansu na Latin, da kuma shi ne amfani da dama sassa - yi, art. Amma a kowane ji shi ne daya darajar - a sa na magudi. Domin da sassaka, wadannan magudi tsari na wucin gadi ta mutum, a yi kamar yadda a hannun mutum yin kokari don ƙirƙirar daya ko wani nau'i. Amma mutane a duniya daukan uku wuri na girmamawa tsakanin sojoji da tasiri a kan me ya sa da taimako na Duniya ne sosai bambancin.

taimako kungiyoyin, ko wanda Categories ne waɗanda ko wasu ilimi

Don fara da za mu tuna abin da su ne siffofin a cikin ƙasa ta surface. Duk wani nau'i na ƙasar sauƙi ne zuwa kashi tabbatacce kuma korau. A kan m gefe ne da wani dagagge wuri sama da hasashen kwance jirgin sama, da kuma mummunan - a kan m, a karkashin ta. Wannan shi ne, na farko da kungiyar hada da tsaunuka, duwãtsu, tsaunuka, plateaus. Na biyu kungiyar - depressions, crevices, kwaruruka, gullies. Kuma yanzu mafi game da bambancin da duniya ta sauƙi, wato cewa shi halitta.

A farko wuri - ciki da karfi na duniya

Wadannan sojojin da kimiyya sunan - na ciki. Mene ne tasiri?

Da farko, da dukan duniya ta surface topography aka hõre m ciki sojojin. Girgizar asa, volcanic eruptions - shi ne mafi bayyane bayyana cewa, idan ka bincika a hankali da bincike na binciken burbushin, baya maida canza da Duniya ta faɗi, kuma yanzu sukan yi wa rushewar Duniya ta ɓawon burodi, ya kuma inganta neoplastic surface. Bugu da kari, da lithosphere faranti ne a akai jinkirin motsi, wanda kuma rinjayar da halittar wani sauƙi. Me ne Duniya ta topography ne bambancin cikin sharuddan da ciki dakarun? Saboda dangane da duk matakai gudana daga ƙarƙashinsu ɓawon burodi na canji a waje. Saboda haka akwai duwatsu, teku ramuka, filayen da tuddai. Lithospheric faranti (bakwai da manyan mutane da dama ne karami su) tafi, yi karo, motsa baya, kafa mafi girma duwãtsu (Alps, Himalayas, da dai sauransu), ko zurfin depressions a cikin ƙasa da a karkashin ruwa (Mariana tare mahara - mafi daukan hankali misali).

Abin da muke gani yanzu, shi ne sakamakon yunkuri na faranti a kan miliyoyin ko biliyoyin shekaru, to gyara da wadannan ra'ayoyi a kan tasirin da taimako.

Na biyu wuri - external askarawan ƙasa

A kimiyya sunan wadannan sojojin - exogenous. Me ne Duniya ta topography ne sosai bambancin saboda wadannan tsoma?

Sun, iska, ruwan sama - duk wadannan yau da kullum mamaki kai tsaye alaka da samuwar wasu nau'i na surface. All ilimi, wanda sun taso a ƙarƙashin rinjayar ciki sojojin, za a fara sake fasalin ko saboda su. Saboda haka, da rana heats da dutse kololuwa. Kwayoyin halitta, ma'adanai, wanda suna samuwa a matsayin wani ɓangare daga duwãtsu, da daban-daban thermal watsin da sauran jiki Properties. Saboda haka, unevenly fadada, suka rasa da karfi links tsakanin kansu, exfoliating, dismembered, kuma a karshe juya cikin yashi. Kuma idan muka ƙara da wannan tasiri na ruwa, wanda a cikin warmer ya kai a cikin kowane kankanin rata, da kuma yayin da ragewan da yawan zafin jiki ya jũya zuwa kankara, wanda, bi da bi, yana faɗaɗa da kuma Firaministan da crack, ƙara zuwa gare su, yana yiwuwa take kaiwa zuwa guda, halakarwa. Shi ya sa da Duniya ta topography ne sosai bambancin, saboda wadannan matakai faruwa yau da kullum a cikin ƙasa.

Kada ka manta game da mataki na koguna, da tabkuna da kuma teku a dab da yankin. Saboda haka, da tekun kowace shekara iya duka biyu karuwa kuma yana raguwa - dangane da shugabanci na ruwa. Wannan zai iya faruwa kusan imperceptibly, amma har yanzu faruwa.

Na uku wuri - mutane

Yana ake waje sojojin, amma son mu haskaka da wannan tasiri a raba category. A ci gaba da fasahar ya ba mutum wani m damar shiga cikin sararin samaniya da kuma hawa zurfi a cikin ƙasa ta ɓawon burodi (babban abu cewa kudade da aka kyau sarari a nan har vigryvaet). Mining albarkatun (mai, iskar gas, ores, rock gishiri da kuma wasu ma'adanai), kuma da canje-canje da zarar saba wuri mai faɗi. Bushewa da dausayi, deforestation, halittar ruwa kududdufai, da dai sauransu tasiri a kan bambancin da Duniya ta topography iya canja sauyin yanayi na mutum yankuna, tilasta dabbobi don nemi wani daban habitats. Kuma shi ke faruwa a ko'ina, kuma kiran amfani da wannan tasiri iya ba ko da yaushe. Idan a cikin yanayin iska ba zai iya haqqinta a gare shi - yana da kashi, sa'an nan da mutum a matsayin m kasancewarsa, zai ze, shi ne su fahimci destructiveness na ayyuka, da kuma yin hankali yanke shawara. Zai ze.

Kuma abin da shi ne sakamakon

A sakamakon haka, ta bayyana cewa zamani taimako na Duniya - sakamakon da hulda da duk wadannan sojojin, kuma sun ci gaba da kullum, ci gaba, har ma a yanzu, kamar yadda idan dai ka idanu suna karanta wannan dogon jumla, aiki sannu a hankali, amma lalle canza contours na duniya tamu. Kuma mai yiwuwa ne zuriyar 'yan daruruwan shekaru, sosai mamakin ganin wani tsohon taswirar sauƙi, misali, a 1995, da yadda duniya take a lokacin.