TsimSecondary kev kawm ntawv thiab cov tsev kawm ntawv

Lub continental nqes hav - nws ... Nta ntawm ib tug qauv thiab cov hom ntawm tus continental nqes hav

Dej hiav txwv muaj ob peb yam ntxwv hais. Lub continental nqes hav - qhov no yog ib tug ntawm lawv. Yuav ua li cas nws yog thiab qhov twg yog? Qhov no koj yuav kawm tau los ntawm qhov tsab xov xwm.

Lub continental nqes hav - nws yog ...

Geography kev tshawb fawb tsis tau tsuas yog av, tab sis kuj lub fact tias yog nyob rau hauv cov dej. Nyob rau hauv kev, txoj kev tshawb ntawm underwater topography ntawm lub hiav txwv los ntawm ib tug tshwj xeeb kev qhuab qhia - oceanography.

Dej hiav txwv pem teb muaj ob peb yam ntxwv xeem. Lub continental nqes hav - qhov no yog ib txoj kev hloov cheeb tsam ntawm lub txee nyob saum toj no, thiab lub thiaj li hu ua txaj ntawm lub hiav txwv, nyob rau hauv qab. Nyob rau nruab nrab, nws yog nyob rau ntawm depths xws li los ntawm 200 mus rau 2000 meters.

Geologically, lub continental nqes hav - ib tug zwj ceeb txuas ntxiv rau cov continental av. Qhov no daim ntawv ntawm underwater struts txawv considerably ntxhab qhov chaw siab tshaj, uas yuav ncav cuag 30-40 degrees. Heev feem ntau nws yog nyuab los ntawm cov loj loj mob rocky cov kauj ruam, canyons, ridges thiab cliffs. Feem ntau pom nyob rau hauv continental nqes hav thiab underwater landslides uas tshwm sim nyob rau hauv qhov kev txiav txim ntawm lub ntiajteb txawj nqus.

Lub continental nqes hav - qhov no yog ib tug kuj nqaim feem ntawm lub seabed uas, li cas los xij, yog hais txog 12% ntawm lub ntiaj teb no tus dej hiav txwv.

Nta ntawm cov qauv ntawm cov continental nqes hav

Rau lub continental slopes yog tsis cov yam ntxwv ntawm ib tug du nto. Conversely, hauv qab lub caij no txawv tuab thiab haum sib sib zog nqus tawg nyem. Nws yog ib yam rau saib sib sib zog nqus ravines thiab nram hav. Nrog rau sab sauv toj feem ntau xaub loj masses ntawm pob zeb, txoj kev ua turbid fluxes thiab currents.

Lub continental nqes hav nyob rau hauv ntau qhov chaw ntawm lub ntiaj teb no tsis yog tib yam thiab txawv nyob rau hauv qhov tob, ntev thiab nqes hav. Piv txwv li, tawm ntug dej hiav txwv ntawm teb chaws Australia tob continental nqes hav yuav tau tsib kilometers thiab ib tug dav ntawm 150-200 km. Tab sis nyob ze ntawm lub continental nqes hav ntawm South Africa txawv cov lus hais tshaj cov qauv.

Lossis loj underwater theem thiab oceanographers sab nyob rau outskirts ntawm lub Arctic hiav txwv. Ntawm no, nyob deb hauv qab cov dej mus Chukchi Cap, qhov twg nws yog abut haib underwater ridges.

Lub ntsiab yam ntawm continental slopes

Zaum conventionally muab faib tag nrho cov continental nqes hav rau hauv peb caj hom:

  • denudation;
  • accumulative;
  • denudation-accumulative.

Nyob rau hauv continental slopes denudation dab predominate hom pob zeb puas tsuaj. Lub accumulative tooj, tus thawj hauv tus txheej txheem ntawm tsub zuj zuj ntawm geological khoom. Lub continental nqes hav ntawm no hom no muaj xws li clastic sediments los yog xuab zeb. Denudation-accumulative continental slopes sawv cev rau ib txoj kev hloov hom ntawm cov saum toj no embodiments slopes.

Nyob rau hauv dav dav, lub ntsiab "pub" geological sedimentary cov khoom siv rau ib yam ntawm cov continental nqes hav yog lub txee. Pob zeb ntxuav nrog underwater currents nws thiab khom hauv qab no raws li khaubncaws sab nraud povtseg ntawm txawv thicknesses.

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