Akarsular\u0131n biriktirme yapabilmesi i\u00e7in;
\n\u2013 E\u011fimin azalmas\u0131
\n\u2013 Suyun azalmas\u0131,
\n\u2013 Akarsu h\u0131z\u0131n\u0131n azalmas\u0131,
\n\u2013 Akarsu y\u00fck\u00fcn\u00fcn artmas\u0131,
\ngereklidir. Bu fakt\u00f6rler bir arada olunca, akarsuyun g\u00fcc\u00fc azal\u0131r ve biriktirme ba\u015flar.
\nAKARSU B\u0130R\u0130K\u0130M \u015eEK\u0130LLER\u0130
\n1. Birikinti Konileri ve Yelpazeleri
\nDa\u011f yama\u00e7lar\u0131ndan d\u00fczl\u00fc\u011fe inen akarsular, ta\u015f\u0131d\u0131klar\u0131 materyalleri e\u011fimin azald\u0131\u011f\u0131 yerlerde yar\u0131m koni \u015feklinde biriktirirler. Bunlara birikinti konisi denir. <\/p>\n
Akarsular\u0131n ta\u015f\u0131d\u0131klar\u0131 maddeler ince ise, geni\u015f bir alana yelpaze gibi yay\u0131l\u0131rlar. Bunlara da birikinti yelpazesi denir. \u00dclkemizde da\u011f eteklerinde, bu tip \u015fekillere s\u0131k\u00e7a rastlan\u0131r.
\n2. Da\u011f Ete\u011fi Ovalar\u0131
\nDa\u011f ete\u011finde, e\u011fimin azald\u0131\u011f\u0131 yerlerde meydana gelen birikinti konileri ve yelpazelerinin zamanla yanlara do\u011fru b\u00fcy\u00fcyerek birle\u015fmeleri sonucu olu\u015fan ovalard\u0131r. <\/p>\n
Bursa ovas\u0131, Uluda\u011f\u2019\u0131n ete\u011finde olu\u015fmu\u015f bir da\u011f ete\u011fi ovas\u0131d\u0131r.
\n3. Da\u011f \u0130\u00e7i Ovalar\u0131
\nDa\u011f i\u00e7lerinde, e\u011fimin azald\u0131\u011f\u0131 yerlerde, akarsuyun ta\u015f\u0131d\u0131\u011f\u0131 malzemeleri biriktirmesi sonucu olu\u015fan d\u00fczl\u00fcklerdir. Engebeli \u00fclkelerde daha fazla olu\u015fur. <\/p>\n
Malatya, Mu\u015f, Elaz\u0131\u011f ovalar\u0131 bu \u015fekilde olu\u015fmu\u015flard\u0131r.
\n4. Taban Seviyesi Ovalar\u0131
\nAkarsular\u0131n denize yakla\u015ft\u0131klar\u0131 yerlerde ta\u015f\u0131ma g\u00fcc\u00fc azd\u0131r. B\u00f6yle yerlerde akarsular, ta\u015f\u0131d\u0131klar\u0131 malzemeleri biriktirirler ve ova y\u00fczeyini al\u00fcvyal dolgu alan\u0131 haline getirirler. B\u00f6yle olu\u015fan d\u00fczl\u00fcklere taban seviyesi ovas\u0131 veya al\u00fcvyal ta\u015fk\u0131n ovas\u0131 denir.
\n5. Delta Ovalar\u0131
\nAkarsular\u0131n ta\u015f\u0131d\u0131klar\u0131 malzemeleri, deniz i\u00e7erisinde biriktirmesi sonucu, \u00fc\u00e7gene benzeyen d\u00fczl\u00fckler meydana gelir. Bunlara delta ovas\u0131 ad\u0131 verilir.
\nDelta ovalar\u0131n\u0131n olu\u015fabilmesi i\u00e7in,
\n\u2022 Ak\u0131nt\u0131lar\u0131n olmamas\u0131,
\n\u2022 Akarsu y\u00fck\u00fcn\u00fcn fazla olmas\u0131,
\n\u2022 Gel – git genli\u011finin az olmas\u0131,
\n\u2022 K\u0131y\u0131n\u0131n s\u0131\u011f olmas\u0131, gereklidir.
\nT\u00fcrkiye\u2019de bir\u00e7ok delta ovas\u0131 vard\u0131r. Ba\u015fl\u0131calar\u0131 \u00c7ukurova, Bafra ve \u00c7ar\u015famba ovalar\u0131d\u0131r.
\n6. Tara\u00e7alar (Sekiler)
\nAl\u00fcvyal tabanl\u0131 vadi \u00fczerindeki akarsular\u0131n, yeniden canlanarak, yata\u011f\u0131n\u0131 kazmas\u0131 sonucunda olu\u015fan y\u00fcksekte kalm\u0131\u015f eski vadi tabanlar\u0131d\u0131r.
\nT\u00fcrkiye\u2019de, \u00e7e\u015fitli zamanlarda epirojenik hareketler g\u00f6r\u00fcld\u00fc\u011f\u00fc i\u00e7in, vadiler boyunca tara\u00e7alar g\u00f6r\u00fcl\u00fcr.
\nTara\u00e7alar birikim \u015fekilleri olmakla birlikte, olu\u015fumunda akarsu a\u015f\u0131nd\u0131rmas\u0131 da etkili olmu\u015ftur.
\n7. Kum Adac\u0131klar\u0131
\nAkarsu e\u011fiminin azald\u0131\u011f\u0131 ve yata\u011f\u0131n geni\u015fledi\u011fi yerlerde, ta\u015f\u0131nan al\u00fcvyonlar ve kumlar k\u00fc\u00e7\u00fck adac\u0131klar \u015feklinde biriktirilir. Bunlara kum adac\u0131klar\u0131 denir<\/p>\n","protected":false},"excerpt":{"rendered":"
Akarsular\u0131n biriktirme yapabilmesi i\u00e7in; \u2013 E\u011fimin azalmas\u0131 \u2013 Suyun azalmas\u0131, \u2013 Akarsu h\u0131z\u0131n\u0131n azalmas\u0131, \u2013 Akarsu y\u00fck\u00fcn\u00fcn artmas\u0131, gereklidir. Bu fakt\u00f6rler bir arada olunca, akarsuyun g\u00fcc\u00fc azal\u0131r ve biriktirme ba\u015flar. AKARSU B\u0130R\u0130K\u0130M \u015eEK\u0130LLER\u0130 1. Birikinti Konileri ve Yelpazeleri Da\u011f yama\u00e7lar\u0131ndan d\u00fczl\u00fc\u011fe inen akarsular, ta\u015f\u0131d\u0131klar\u0131 materyalleri e\u011fimin azald\u0131\u011f\u0131 yerlerde yar\u0131m koni \u015feklinde biriktirirler. Bunlara birikinti konisi …<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1403,1406],"tags":[3275,3277,3278,3279,3281,3276,3280],"class_list":["post-1109","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-akarsularda-biriktirme","tag-birikinti-konileri","tag-dag-etegi-ovalari","tag-dag-ici-ovalari","tag-delta-ovalari","tag-egim","tag-taban-seviyesi-ovalari"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1109","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/comments?post=1109"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1109\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1109"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1109"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1109"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}