You are right. A braided river landform is generally the main river having its sub-branches flowing along its side. These sub branches are temporary and they emerge when the sediment carrying capacity, velocity and transporting capacity of a river Is decreased due to it being in its late old stage (as the river clears all the relief features around it in old age and form a peneplain having no reliefs at all and due to this) , the slope gradient is diminished and it results into difficulty to carry the heavy sediments further and as a result they get deposited along the bed of river as well as it may happen due to failure to erode the hard rock lying it its way, this forces the river to develop a sub-branch of its own ,more like a rivulet. This is temporary , when the river gets passed through it and reaches a position of equilibrium again, it does join back the main river but a distributary is opposite of tributary.
map reading በካርታ ብትሰራልን ደስ ይለናል entranc exam question
Ok.
Waaaw thank you teacher 👍👋👋
You welcome
thanks a lot❤❤❤
👍👍🙏🙏🙏🙏
wow arif new ketlibet
👍👍👍👍✨
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🍏
thanks Thatcher
You welcome
tebarek ymr betammm new yetekemegn
10Q God blessing you.
Thank you so much ❤️❤️
, 👍👍👍
መልሱ መጀመርያ አታቀልም ምክንያቱም ማብራሪያ ሳይስጥ መልሱ አወኩት ማለት ለእንትራንስ ጥያቄ ተፈተንኩት ማለት ነው ።
👍👍👍👍👍🙏🙏🙏🙏
Thx!!!
You welcome.
Barsiisaa qaalii dadhabbiike rabbi siifan baasuuf jabaadha gaaffii bars 2015 gaaffii 09_100 sana map irratti nuuf hojjadhu
👍👍👍👍👍Coming soon.
Tnxs gn teyakewm sertn sanchres lemn ante tengrenale malt egna sensera ante ne key kelm tadergwale esu demo legna.teru ayedelm
Ok kibron kasshun I will be edit it.
@@bridgeeducation4771 tnx🙏
Zandro entrance taftagj Nani ebki tolo tolo lekaklni bxm gobzi nk 😍😊😘
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Please history grade11 and 12🙏🙏🙏🙏
History grade 11 and 12 questions 🙏🙏🙏🙏🙏
If it is possible ok.
ok It is good but if and only if megemeria melsun batasayen yimeretal
Ok.
Wow thank you 🙏🙏🙏🙏👏👏👏 but braide stream is middle course not lower course ??
You are right.
A braided river landform is generally the main river having its sub-branches flowing along its side. These sub branches are temporary and they emerge when the sediment carrying capacity, velocity and transporting capacity of a river Is decreased due to it being in its late old stage (as the river clears all the relief features around it in old age and form a peneplain having no reliefs at all and due to this) , the slope gradient is diminished and it results into difficulty to carry the heavy sediments further and as a result they get deposited along the bed of river as well as it may happen due to failure to erode the hard rock lying it its way, this forces the river to develop a sub-branch of its own ,more like a rivulet. This is temporary , when the river gets passed through it and reaches a position of equilibrium again, it does join back the main river but a distributary is opposite of tributary.
@@bridgeeducation4771 ok thank
Ansewer bayserabet arif ymeslegnal endene mokrenew tesasten bnawkew aytefam so endeza bihon Elalehu ende hasab
ok.
betam arf nw ketilibet gin melisun endenmokir mecereshalaye bihone mitimelisehu arf nw
Yishalale ok.
@@bridgeeducation4771
Are
Me mehal sile mitabrara indiwu bihon yishalaal
Arife nbere gen melsun endenmokre giza alsetehenem melsu ketyakew ekule eygeba techegerku pls
🙏🙏🙏👍👍👍👍👍
betam arif nw gen melsu baykdem berasachen endnmoker plz
Ok.
Afaan.oromoottin nu ergi kaa way
Ok.