Yerkabu\u011fundaki herhangi bir sars\u0131nt\u0131n\u0131n \u00e7evreye do\u011fru yay\u0131lan titre\u015fim bi\u00e7imindeki hareketine deprem denir.<\/p>\n
1. Volkanik depremler<\/p>\n
Volkanik p\u00fcsk\u00fcrmeler esnas\u0131nda g\u00f6r\u00fclen ve etki alanlar\u0131 dar olan depremlerdir.<\/p>\n
2. \u00c7\u00f6k\u00fcnt\u00fc (G\u00f6\u00e7me) depremleri<\/p>\n
Kayatuzu jips kalker gibi kolay eriyebilen karstik sahalarda zamanla yer alt\u0131nda b\u00fcy\u00fck bo\u015fluklar olu\u015fur. Bu bo\u015fluklar\u0131n \u00fcst\u00fc bir m\u00fcddet sonra \u00e7\u00f6kerse sars\u0131nt\u0131lar olu\u015fur. Etki alanlar\u0131 en dar olan depremler bunlard\u0131r.<\/p>\n
3. Tektonik (Dislokasyon) depremler<\/p>\n
Yer kabu\u011funun derinliklerinde bas\u0131n\u00e7 ve gerilimler sonucu katmanlar\u0131n yer de\u011fi\u015ftirme oynama ve k\u0131r\u0131lma gibi hareketlerinin ortaya \u00e7\u0131kard\u0131\u011f\u0131 sars\u0131nt\u0131lard\u0131r. Etki alanlar\u0131 en geni\u015f olan ve en \u00e7ok hasara neden olan depremler bunlard\u0131r.<\/p>\n
Depremin yerin i\u00e7inde olu\u015ftu\u011fu k\u0131sm\u0131na i\u00e7 merkez (hiposantr) denir. Depremin yery\u00fcz\u00fcne en k\u0131sa yoldan ula\u015ft\u0131\u011f\u0131 yere de d\u0131\u015f merkez (episantr) denir. Deprem bilimi sismoloji deprem \u015fiddetini \u00f6l\u00e7en alet de sismograf olarak adland\u0131r\u0131l\u0131r. <\/p>\n
Depremlerin ne kadar kuvvetli oldu\u011funu belirlemek i\u00e7in iki t\u00fcrl\u00fc \u00f6l\u00e7ek kullan\u0131l\u0131r.
\nRichter (Rihter) \u00f6l\u00e7e\u011fi
\nMercalli – Sieberg \u00f6l\u00e7e\u011fi (\u015eiddet Iskalas\u0131)
\nMercalli – Sieberg \u00f6l\u00e7e\u011fi sars\u0131nt\u0131n\u0131n yol a\u00e7t\u0131\u011f\u0131 zarar ve de\u011fi\u015fikliklere g\u00f6re d\u00fczenlenmi\u015ftir. Richter \u00f6l\u00e7e\u011fi ise i\u00e7 merkezde depremle bo\u015falan enerjinin \u00f6l\u00e7\u00fclmesi esas\u0131na dayan\u0131r. Deprem s\u0131ras\u0131nda bo\u015falan bu enerjiye depremin b\u00fcy\u00fckl\u00fc\u011f\u00fc (magnit\u00fcd\u00fc) denir.
\n Pasifik Okyanusu Japonya \u00e7evresi Antil Adalar\u0131 Do\u011fu Hint Adalar\u0131 Akdeniz \u00e7evresi ve Amerika k\u0131talar\u0131n\u0131n bat\u0131 kesimleri yery\u00fcz\u00fcnde depremlerin en \u00e7ok oldu\u011fu alanlard\u0131r.
\n Buna kar\u015f\u0131l\u0131k eski jeolojik devirlerde olu\u015fan Do\u011fu Avrupa Kanada Sibirya Gr\u00f6nland Adas\u0131 Avustralya ve \u0130skandinav Yar\u0131madas\u0131\u2019nda hemen hemen hi\u00e7 deprem olmamaktad\u0131r.<\/p>\n
T\u00fcrkiye\u2019deki Deprem Alanlar\u0131<\/p>\n
T\u00fcrkiye n\u00fcfusunun % 60’a yak\u0131n\u0131 faal olan ve zarar verebilen deprem alanlar\u0131 \u00fczerinde yerle\u015fmi\u015ftir.
\n Daha \u00f6nce g\u00f6r\u00fclen Erzurum Erzincan Van Bolu \u00e7ank\u0131r\u0131 Tokat Adapazar\u0131 K\u00fctahya Burdur Lice Bing\u00f6l Dinar Ceyhan G\u00f6lc\u00fck ve D\u00fczce depremlerinin b\u00fcy\u00fck oranda can ve mal kayb\u0131na neden olmas\u0131nda bu kentlerin fay hatlar\u0131 \u00fczerinde yer almalar\u0131n\u0131n \u00f6nemli rol\u00fc olmu\u015ftur.
\n Konya Ovas\u0131 Karaman Mersin (Ta\u015feli PlAtosu \u00e7evresi) Ergene Havzas\u0131 ve Mardin E\u015fi\u011fi deprem bak\u0131m\u0131ndan tehlikesi az olan yerlerdir.<\/p>\n","protected":false},"excerpt":{"rendered":"
Yerkabu\u011fundaki herhangi bir sars\u0131nt\u0131n\u0131n \u00e7evreye do\u011fru yay\u0131lan titre\u015fim bi\u00e7imindeki hareketine deprem denir. 1. Volkanik depremler Volkanik p\u00fcsk\u00fcrmeler esnas\u0131nda g\u00f6r\u00fclen ve etki alanlar\u0131 dar olan depremlerdir. 2. \u00c7\u00f6k\u00fcnt\u00fc (G\u00f6\u00e7me) depremleri Kayatuzu jips kalker gibi kolay eriyebilen karstik sahalarda zamanla yer alt\u0131nda b\u00fcy\u00fck bo\u015fluklar olu\u015fur. Bu bo\u015fluklar\u0131n \u00fcst\u00fc bir m\u00fcddet sonra \u00e7\u00f6kerse sars\u0131nt\u0131lar olu\u015fur. Etki alanlar\u0131 en …<\/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":[3204,10350,2917,2875,10352,3468,10351],"class_list":["post-4797","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-pasifik-okyanusu","tag-seizma-hareketleri","tag-taseli-platosu","tag-tektonik","tag-turkiyedeki-deprem-alanlari","tag-volkanik-depremler","tag-volkanik-puskurmeler"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4797","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=4797"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4797\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=4797"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=4797"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=4797"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}