Kutup b\u00f6lgeleri ile y\u00fcksek da\u011flar\u0131n \u00fcst k\u0131s\u0131mlar\u0131nda b\u00fct\u00fcn y\u0131l hi\u00e7 erimeden kalan karlara Tokta\u011fan kar (daimi) denir. Enlemin etkisiyle tokta\u011fan kar s\u0131n\u0131r\u0131 Ekvatordan Kutuplara do\u011fru azal\u0131r.
\nBug\u00fcn d\u00fcnyan\u0131n yakla\u015f\u0131k %10 \u2018u (15 milyon km2\u2019si) buzullarla kapl\u0131d\u0131r. Buzullar\u0131n etki alan\u0131 daha \u00e7ok kutuplara yak\u0131n yerlerdir. <\/p>\n
Buzul \u00c7e\u015fitleri
\n1) Sirk Buzulu: Y\u00fcksek da\u011fl\u0131k alanlardaki k\u00fc\u00e7\u00fck \u00e7ukurluklar\u0131 dolduran buzullard\u0131r. Yurdumuzda baz\u0131 y\u00fcksek da\u011fl\u0131k b\u00f6lgelerde vard\u0131r. \u00d6r: Cilo. Sat, A\u011fr\u0131, Tend\u00fcrek, S\u00fcphan , Ka\u00e7kar, Erciyes, Beyda\u011flar\u0131, Geyik Da\u011flar\u0131, Bolkar, Binbo\u011fa da\u011flar\u0131 gibi. <\/p>\n
2) Vadi Buzulu: Buzul a\u015f\u0131nd\u0131rmas\u0131 ile olu\u015fan vadilerin i\u00e7ini dolduran buzullard\u0131r. \u00d6r: Cilo da\u011f\u0131nda oldu\u011fu gibi.<\/p>\n
3) \u00d6rt\u00fc Buzulu: Kutup b\u00f6lgelerinde g\u00f6r\u00fcl\u00fcr. Antartika ve Gr\u00f6nland\u2019da oldu\u011fu gibi. Kutup b\u00f6lgelerinde denizde y\u00fczen buz da\u011flar\u0131na Aysberg denir.<\/p>\n
4) Takke Buzulu: volkan da\u011flar\u0131n\u0131n \u00fcst k\u0131sm\u0131nda olu\u015fan buzullard\u0131r. \u00d6r: A\u011fr\u0131 da\u011f\u0131nda oldu\u011fu gibi.<\/p>\n
Buzul a\u015f\u0131nd\u0131rmas\u0131 \u015funlara ba\u011fl\u0131d\u0131r:
\n1) Buzulun kal\u0131nl\u0131\u011f\u0131na: Kal\u0131nl\u0131k fazla ise a\u015f\u0131nd\u0131rma oyma \u015feklinde , az ise t\u00f6rp\u00fcleme \u015feklinde olur.
\n2) Yatak E\u011fimine: Yatak e\u011fimi fazla ise a\u015f\u0131nd\u0131rma t\u00f6rp\u00fcleme \u015feklinde , az ise oyma \u015feklindedir.
\n3) Kayalar\u0131n \u00d6zelli\u011fine: Zemin sert kayalardan olu\u015fmu\u015f ise a\u015f\u0131nd\u0131rma t\u00f6rp\u00fcleme \u015feklinde , yumu\u015fak ise oyma \u015feklinde olur.<\/p>\n
Buzul A\u015f\u0131n\u0131m \u015eekilleri
\n1) Buzul Vadisi: Buzul a\u015f\u0131nd\u0131rmas\u0131 sonucu olu\u015fan “U” \u015feklindeki vadilerdir. Akarsu vadilerine g\u00f6re boylar\u0131 k\u0131sad\u0131r ve s\u00fcrekli ini\u015f g\u00f6stermezler (ini\u015fli \u2013\u00e7\u0131k\u0131\u015fl\u0131d\u0131r)<\/p>\n
2) H\u00f6rg\u00fc\u00e7 Kaya: Farkl\u0131 a\u015f\u0131nma sonucu olu\u015fan ve deve h\u00f6rg\u00fcc\u00fcne benzeyen kayalard\u0131r.
\n3) Sirk (buz yala\u011f\u0131) \u00e7ukurlu\u011fu: Da\u011flar\u0131n \u00fcst k\u0131sm\u0131nda a\u015f\u0131nd\u0131rma ile olu\u015fan k\u00fc\u00e7\u00fck \u00e7ukurluklad\u0131r.
\nBuzul Biriktirme \u015eekilleri
\n1) Moren setti: Buzullar\u0131n a\u015f\u0131nd\u0131rarak ta\u015f\u0131d\u0131\u011f\u0131 kum \u00e7ak\u0131l gibi maddelere moren denir. Bunlar\u0131 eridi\u011fi yerde biriktirmesi ile olu\u015fan sette denir.
\n2) Drumlin: Buzul biriktirmesi ile olu\u015fan al\u00e7ak tepelere denir.
\n3) Sander Ovas\u0131: Buzullar\u0131n eridi\u011fi yerde ortaya \u00e7\u0131kan akarsular\u0131n ta\u015f\u0131d\u0131\u011f\u0131 malzemeleri biriktirmesi ile olu\u015fan d\u00fczl\u00fcklerdir.<\/p>\n
T\u00fcrkiye\u2019nin bug\u00fcnk\u00fc yer \u015fekillerinin olu\u015fmas\u0131nda en az etkili olan d\u0131\u015f kuvvet buzullard\u0131r. <\/p>\n
Kutup b\u00f6lgeleri ile y\u00fcksek da\u011flar\u0131n \u00fcst k\u0131s\u0131mlar\u0131nda b\u00fct\u00fcn y\u0131l hi\u00e7 erimeden kalan karlara Tokta\u011fan kar (daimi) denir. Enlemin etkisiyle tokta\u011fan kar s\u0131n\u0131r\u0131 Ekvatordan Kutuplara do\u011fru azal\u0131r.
\nBug\u00fcn d\u00fcnyan\u0131n yakla\u015f\u0131k %10 \u2018u (15 milyon km2\u2019si) buzullarla kapl\u0131d\u0131r. Buzullar\u0131n etki alan\u0131 daha \u00e7ok kutuplara yak\u0131n yerlerdir. <\/p>\n
Buzul \u00c7e\u015fitleri
\n1) Sirk Buzulu: Y\u00fcksek da\u011fl\u0131k alanlardaki k\u00fc\u00e7\u00fck \u00e7ukurluklar\u0131 dolduran buzullard\u0131r. Yurdumuzda baz\u0131 y\u00fcksek da\u011fl\u0131k b\u00f6lgelerde vard\u0131r. \u00d6r: Cilo. Sat, A\u011fr\u0131, Tend\u00fcrek, S\u00fcphan , Ka\u00e7kar, Erciyes, Beyda\u011flar\u0131, Geyik Da\u011flar\u0131, Bolkar, Binbo\u011fa da\u011flar\u0131 gibi. <\/p>\n
2) Vadi Buzulu: Buzul a\u015f\u0131nd\u0131rmas\u0131 ile olu\u015fan vadilerin i\u00e7ini dolduran buzullard\u0131r. \u00d6r: Cilo da\u011f\u0131nda oldu\u011fu gibi.<\/p>\n
3) \u00d6rt\u00fc Buzulu: Kutup b\u00f6lgelerinde g\u00f6r\u00fcl\u00fcr. Antartika ve Gr\u00f6nland\u2019da oldu\u011fu gibi. Kutup b\u00f6lgelerinde denizde y\u00fczen buz da\u011flar\u0131na Aysberg denir.<\/p>\n
4) Takke Buzulu: volkan da\u011flar\u0131n\u0131n \u00fcst k\u0131sm\u0131nda olu\u015fan buzullard\u0131r. \u00d6r: A\u011fr\u0131 da\u011f\u0131nda oldu\u011fu gibi.<\/p>\n
Buzul a\u015f\u0131nd\u0131rmas\u0131 \u015funlara ba\u011fl\u0131d\u0131r:
\n1) Buzulun kal\u0131nl\u0131\u011f\u0131na: Kal\u0131nl\u0131k fazla ise a\u015f\u0131nd\u0131rma oyma \u015feklinde , az ise t\u00f6rp\u00fcleme \u015feklinde olur.
\n2) Yatak E\u011fimine: Yatak e\u011fimi fazla ise a\u015f\u0131nd\u0131rma t\u00f6rp\u00fcleme \u015feklinde , az ise oyma \u015feklindedir.
\n3) Kayalar\u0131n \u00d6zelli\u011fine: Zemin sert kayalardan olu\u015fmu\u015f ise a\u015f\u0131nd\u0131rma t\u00f6rp\u00fcleme \u015feklinde , yumu\u015fak ise oyma \u015feklinde olur.<\/p>\n
Buzul A\u015f\u0131n\u0131m \u015eekilleri
\n1) Buzul Vadisi: Buzul a\u015f\u0131nd\u0131rmas\u0131 sonucu olu\u015fan “U” \u015feklindeki vadilerdir. Akarsu vadilerine g\u00f6re boylar\u0131 k\u0131sad\u0131r ve s\u00fcrekli ini\u015f g\u00f6stermezler (ini\u015fli \u2013\u00e7\u0131k\u0131\u015fl\u0131d\u0131r)<\/p>\n
2) H\u00f6rg\u00fc\u00e7 Kaya: Farkl\u0131 a\u015f\u0131nma sonucu olu\u015fan ve deve h\u00f6rg\u00fcc\u00fcne benzeyen kayalard\u0131r.
\n3) Sirk (buz yala\u011f\u0131) \u00e7ukurlu\u011fu: Da\u011flar\u0131n \u00fcst k\u0131sm\u0131nda a\u015f\u0131nd\u0131rma ile olu\u015fan k\u00fc\u00e7\u00fck \u00e7ukurluklad\u0131r.
\nBuzul Biriktirme \u015eekilleri
\n1) Moren setti: Buzullar\u0131n a\u015f\u0131nd\u0131rarak ta\u015f\u0131d\u0131\u011f\u0131 kum \u00e7ak\u0131l gibi maddelere moren denir. Bunlar\u0131 eridi\u011fi yerde biriktirmesi ile olu\u015fan sette denir.
\n2) Drumlin: Buzul biriktirmesi ile olu\u015fan al\u00e7ak tepelere denir.
\n3) Sander Ovas\u0131: Buzullar\u0131n eridi\u011fi yerde ortaya \u00e7\u0131kan akarsular\u0131n ta\u015f\u0131d\u0131\u011f\u0131 malzemeleri biriktirmesi ile olu\u015fan d\u00fczl\u00fcklerdir.<\/p>\n
T\u00fcrkiye\u2019nin bug\u00fcnk\u00fc yer \u015fekillerinin olu\u015fmas\u0131nda en az etkili olan d\u0131\u015f kuvvet buzullard\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"
Kutup b\u00f6lgeleri ile y\u00fcksek da\u011flar\u0131n \u00fcst k\u0131s\u0131mlar\u0131nda b\u00fct\u00fcn y\u0131l hi\u00e7 erimeden kalan karlara Tokta\u011fan kar (daimi) denir. Enlemin etkisiyle tokta\u011fan kar s\u0131n\u0131r\u0131 Ekvatordan Kutuplara do\u011fru azal\u0131r. Bug\u00fcn d\u00fcnyan\u0131n yakla\u015f\u0131k %10 \u2018u (15 milyon km2\u2019si) buzullarla kapl\u0131d\u0131r. Buzullar\u0131n etki alan\u0131 daha \u00e7ok kutuplara yak\u0131n yerlerdir. Buzul \u00c7e\u015fitleri 1) Sirk Buzulu: Y\u00fcksek da\u011fl\u0131k alanlardaki k\u00fc\u00e7\u00fck \u00e7ukurluklar\u0131 dolduran …<\/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":[3167,3166,2887,3168,3170,3169],"class_list":["post-1073","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-buzul-cesitleri","tag-buzullar","tag-ekvator","tag-sirk-buzulu","tag-takke-buzulu","tag-vadi-buzulu"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1073","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=1073"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1073\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1073"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1073"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1073"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}