Me yasa taimakon duniya ya bambanta? Babban hanyoyin tafiyar da taimako

Akwai hanyoyi masu yawa waɗanda aka nazari dalla-dalla ta hanyar yanayin duniya. Taimako yana ɗaya daga cikinsu. Duniya duniyarmu kyakkyawa ce ta musamman! Sakamakonta na waje shine sakamakon aikin ƙwayar maɗamban tsari daban-daban.

Me yasa taimakon duniya ya bambanta? Za mu yi kokarin amsa wannan tambaya a matsayin mai sauƙi a wannan labarin.

Me yasa yanayin ya bambanta? Dalilin dalili

Gorges mai zurfi a ƙarƙashin ruwa kuma mafi girma sun haɗu da kololuwa, babban filin jiragen ruwa da wuraren kwalliya, ƙananan filayen sararin samaniya da ƙananan tsaunuka - dukkan wannan za'a iya samuwa akan yanayin mu mai ban mamaki. Bari mu yi kokarin amsa mai sauki tambaya: me ya sa da taimako na Duniya ne sosai bambancin?

Babban dalilin wannan bambancin - shi ne mai juna tasiri a duniyar tamu ta surface ciki (na ciki) da kuma waje (exogenous) matakai. Hakanan, haɗakar waɗannan matakai, kyakkyawan shine, makamashin Sun.

Jigon tafiyar matakai na ƙarshe sun ƙunshi ƙungiyoyi na ɓawon ƙwayar ƙasa, wanda zai iya kasancewa a tsaye da kuma kwance. Wadannan gwagwarmayoyi ba kawai canza overall tsarin da Duniya ta ɓawon burodi, amma kuma haifar da sabon siffofin taimako.

Duk da yake na ciki matakai samar da topography na duniya (aiki a matsayin magina), exogenous Hone da kuma ado da shi, kamar yadda wasu "sculptors" duniya siffofin. Suna shafi farfajiya na duniya daga waje, ta hanyar yanayin duwatsu, aikin farfajiyar da ruwan sama, iska da nauyi. Yana da muhimmanci a lura cewa waɗannan matakai sun faru kuma suna faruwa a duniyarmu a duk lokacin.

Rarraba da haɗuwa su ne mahimman hanyoyin tafiyar da taimako

Yanzu da ka riga san me Duniya ta topography ne sosai bambancin, zai yiwu a bayyana su daki-daki da matakai da suke da laifin wannan. Zai kasance game da ƙyama da haɗuwa, waɗanda suke da alaka da su.

Ta hanyar ƙaryatawa an fahimci cikakkiyar dukkanin matakan da ake nufi da halakar duwatsu. Babban tuki da karfi a baya da denudation ne nauyi (karfi na nauyi). Gudun tuddai na ƙasa, lakaran ruwa, motsi na manyan glaciers da kwarara na koguna - duk wannan, hanyar daya ko wani, an haɗa shi da shi. Sakamakon yana nufin inganta ƙasa.

Haɗuwa shine kishiyar tsari, wanda ya ƙunshi jigilar nau'ikan dutse a wasu sassan duniya. Duk da haka, ƙin yarda da haɗuwa suna da hankali kuma suna danganta su. A sakamakon sakamakon haɗuwa a kan duniya, filayen, tuddai, deltas, barkhans, yankunan bakin teku da sauransu.

Dabbobi na halitta masu sauƙi na duniya

A sakamakon matakai na ƙarshe, wadannan nau'o'in taimako sun samo asali:

• Tectonic;
• Volcanic.

Daga cikin manyan nau'o'in asali na asalin halitta (tsari) ya kamata a bambanta:

• Saurin taimako (kwari na kogin, gullies, ravines, gullies, da dai sauransu);
• Glacial (kogin, kogi na moraine da filayen, kams, "goshin tumaki," da sauransu);
• Coastal ko abrasive (tafiya, tsagi, abrasion rairayin bakin teku masu, rairayin bakin teku, da dai sauransu);
• Gravitational (ragowar ƙasa, ragowar ƙasa, shararru);
• Eolian (barkans, dunes);
• Karst (caves, funnels, karst mines);
• Suffosion (pods, "steppe saucers");
• Anthropogenic (taimako da aka halicce ta daga aikin ɗan Adam: aiki, mine, mound, heap, dam, da sauransu).

Duk waɗannan nau'o'in kayan taimako masu yawa sun haifar da zane-zanen mu na musamman na duniya.

A ƙarshe

Bayan karatun labarinmu, tambayar da yasa taimakon duniya bai zama wanda zai iya motsa ku cikin mutuwar ba. Bayyanar waje, zane na duniya, an halicce mu ga miliyoyin shekaru. Dangane da samuwar babban nau'i na sauƙaƙan duniya shine matakai daban-daban, kamar su na ciki (na ciki) da kuma tsofaffi (waje).