Download - Eolski reljef
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EOLSKA EROZIJA
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Eolska erozija predstavlja proces formiranja oblika u reljefu pod uticajem vetra.
Rad vetra je najizrazitiji u suvim pustinjskim i polupustinjskim oblastima bez vegetacije.
Eol je u grčkoj mitologiji bio bog i gospodar vetrova.
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Pustinje su područja na Zemlji koja godišnje primaju manje od 250mm padavina.
Čine 22% površine svetskog kopna. Osim vjetra, na formiranje reljefa u
pustinjama utiču i velika dnevna kolebanja temperature, zbog kojih dolazi do pucanja, drobljenja i usitnjavanja stjenovite mase.
Pustinje mogu biti pjeskovite, kamenite, šljunkovite, glinovite i slane.
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PJESKOVITA PUSTINJA
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KAMENITA PUSTINJA
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ŠLJUNKOVITA PUSTINJA
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GLINOVITA PUSTINJA
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SLANA PUSTINJA
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SNIMAK IZ SVEMIRA SLANE PUSTINJE
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Eolski oblici reljefa dele se na erozivne i akumulativne.
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EOLSKI EROZIVNI OBLICI
Stvaraju se uglavnom u kamenitim pustinjama, ravnim i golim stjenovitim predjelima bez vegetacije i vode pokriveni komadima stjena nastali temperaturnim razaranjem.
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EOLSKI EROZIVNI OBLICI SU
Pustinjsko saće Pustinjski prozotac Pečurkasti ostenjak (Gur) Igličasti ostenjak Jardang Uade
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PUSTINJSKO SAĆE
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PUSTINJSKI LUK/PROZORAC
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PEČURKASTI OSTENJAK (GUR)
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Pečurkasti ostenjak (Gur)
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IGLIČASTI OSTENJAK
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JARDANG
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UADA
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UADA
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EOLSKI AKUMULATIVNI OBLICI
Javljaju se u pjeskovitim pustinjama .Imaju zatalasan brežuljkast reljef koji se dinamično mjenja pod uticajem vjetra.
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EOLSKI AKUMULATIVNI OBLICI SE
Dine Barhani
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DINE
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DINE
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BARHANI
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PUSTINJSKI PEJZAŽ IZ ALŽIRA
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ARABIJSKA PUSTINJA – ARABIJSKI POLUOTOK
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ATACAMA – NAJSUŠNIJI PROSTOR NA ZEMLJI
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PUSTINJSKI PEJZAŽ IZ AUSTRALIJE
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PEJZAŽ IZ AUSTRALIJE
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ULURU (AYERS ROCK) – AUSTRALIJA...
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I NJEGOVA BUDUĆNOST...
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PJEŠČANA OLUJA - IRAK
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PJEŠČANA OLUJA U AUSTRALIJI
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PUSTINJSKA RUŽA
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HVALA!1-2
MAŠA MIRILOVIĆMARIJA TODOROVIĆ
JULIJANA ĐUROVIĆMINA MILOVIĆ