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      <title>10.sınıf by Özge Koçak</title>
      <link>https://padlet.com/ozgk/10</link>
      <description>Dersimizle ilgili bilgi, belge vb. paylaşımı için kullanacağız.</description>
      <language>en-us</language>
      <pubDate>2020-06-13 19:13:18 UTC</pubDate>
      <lastBuildDate>2023-12-25 09:04:29 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625277493</link>
         <description><![CDATA[]]></description>
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         <pubDate>2020-06-13 19:19:23 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625277493</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625305215</link>
         <description><![CDATA[<div>*Geniş yer kabuğu parçalarının yükselip alçalmasına denir.</div><blockquote>Farklı yoğunluk ve kalınlıktaki yer kabuğu parçaları manto üzerinde yüzer durumdadır.Bu<br>parçalar, yoğunluk ve kalınlıklarına göre mantoya az ya da çok gömülerek dengede durur. Bu dengeye izostatik<br>denge adı verilir.</blockquote><div>*İzostatik dengenin bozulması sonucunda <strong><em>transgresyon</em></strong> ve <strong><em>regresyon</em></strong> oluşur.</div>]]></description>
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         <pubDate>2020-06-13 20:09:41 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625305215</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625344505</link>
         <description><![CDATA[]]></description>
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         <pubDate>2020-06-13 21:30:04 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625344505</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625344634</link>
         <description><![CDATA[]]></description>
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         <pubDate>2020-06-13 21:30:21 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625344634</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625344963</link>
         <description><![CDATA[]]></description>
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         <pubDate>2020-06-13 21:30:36 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625344963</guid>
      </item>
      <item>
         <title>Transgresyoon</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625345377</link>
         <description><![CDATA[<div>Kara kütlesinin ağırlaşıp alçalmasıyla denizin karaya doğru<br>ilerlemesidir.Bu olay şunlar sonucunda oluşur:<br><a href="https://i.pinimg.com/736x/76/a8/35/76a8350a9d7c7c24e4a2ca0c9b16ff2b.jpg"><strong><em>*Buzul oluşumu,<br>*Aşınan toprakların birikmesi,<br>*Volkanik faaliyetler sonucunda çıkan malzeme birikmesi.</em></strong></a></div>]]></description>
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         <pubDate>2020-06-13 21:31:45 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625345377</guid>
      </item>
      <item>
         <title>Regresyon</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625354055</link>
         <description><![CDATA[<div>Kara kütlesinin hafifleyip yükselmesiyle deniz seviyesinin<br>geri çekilmesidir.Bu olay şunlar sonucunda oluşur:<br><a href="https://pbs.twimg.com/media/DwyoCOqX0AAXB3f.jpg"><strong><em>*Aşınma sonucunda,<br>*Buzulların erimesi.</em></strong></a></div>]]></description>
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         <pubDate>2020-06-13 21:52:28 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625354055</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625356759</link>
         <description><![CDATA[]]></description>
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         <pubDate>2020-06-13 21:59:04 UTC</pubDate>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625717557</link>
         <description><![CDATA[<div>*Geniş jeosenklinal alanlarda biriken tortul tabakaların yan basınçların etkisiyle yükselmesi sonucunda gerçekleşmesine denir.</div><blockquote>Yükselen tabakalar genç ise kıvrımlı dağlar, yaşlı ise kırıklı dağlar oluşur.</blockquote><div><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2020-06-14 09:49:47 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625717557</guid>
      </item>
      <item>
         <title>Kıvrımlı Dağlar</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625720989</link>
         <description><![CDATA[<div>*Esnek, genç tortul tabakaların yükselmesi sonucunda oluşur.<br>*Kıvrılan tabakaların yükselen  kısımlarına <strong><em>antiklinal,</em></strong> çukurlaştığı</div><div>kısımlarına da <strong><em>senklinal</em></strong> denir.<a href="https://tse3.mm.bing.net/th?id=OIP.Twh9xkEYZrq3jDFy0BRq-QHaDV&amp;pid=Api">Bknz?</a></div>]]></description>
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         <pubDate>2020-06-14 09:53:25 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625720989</guid>
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      <item>
         <title>Kırıklı Dağlar</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625730674</link>
         <description><![CDATA[<div>*Sert, yaşlı tortul tabakaların yükselmesi sonucunda oluşur.<br>*Kırılma sonucu tabakaların dikey yöndeki yükseltilere <strong><em>horst</em></strong>, alçalan<br>kısımlara da <strong><em>graben</em></strong> denir. <a href="https://tse2.mm.bing.net/th?id=OIP.qmy2vcOzX4IUN80AUfAsQwHaD1&amp;pid=Api">Bknz:?</a></div>]]></description>
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         <pubDate>2020-06-14 10:05:17 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625730674</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625738184</link>
         <description><![CDATA[]]></description>
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         <pubDate>2020-06-14 10:13:30 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625738184</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625758333</link>
         <description><![CDATA[<div>Dünya'nın oluşumundan bugüne kadar dört büyük orojenez olayı meydana gelmiştir.Bunlar sırasıyla <a href="https://i.hizliresim.com/cGRP5h.png"><strong><em>Huron, Kaledoniyen, Hersiyen ve Alp</em></strong></a> Kıvrımlarıdır.</div>]]></description>
         <enclosure url="" />
         <pubDate>2020-06-14 10:36:52 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625758333</guid>
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      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625763673</link>
         <description><![CDATA[<div>*Magmanın yeryüzüne çıkması veya yeryüzüne yakın yerlere kadar sokulması olarak adlandırılır.<br>*Oluşum yerlerine göre <strong><em>derinlik ve yüzey volkanizması</em></strong> olarak ikiye ayrılır.<br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2020-06-14 10:43:47 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625763673</guid>
      </item>
      <item>
         <title>Derinlik Volkanizması</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625765908</link>
         <description><![CDATA[<div>*Yer kabuğunun içerisindeki çatlak ve boşluklara<br>sokulan magmanın yüzeye ulaşamaması sonucu meydana gelir.<a href="https://i.hizliresim.com/hCukQt.png">Bknz:?</a><br>*Magmanın<br>bu alanlarda soğumasıyla</div><div><a href="https://opengeology.org/textbook/wp-content/uploads/2018/05/Half-Dome-a-granitic-batholith-in-Yosemite-300x257.jpg">batolit</a>, <a href="https://tse2.mm.bing.net/th?id=OIP.FpSr7ySeHOhEwzCWJDTa8wHaD2&amp;pid=Api">lakolit</a>, <a href="https://slideplayer.biz.tr/slide/2397165/8/images/19/sill.jpg">sill</a> ve <a href="https://lh3.googleusercontent.com/proxy/IHoNCIsC9Qr3-rqj1mk0ZMGhiE4SAm1ffMLUFd9hdtoYvOlYpX9Ue2z5Outj-BnW8SNStA4juLiA14FIHopQo8godMd-iE-22VFDummgEtBN92Lgxw">dayk</a> adı verilen yeryüzü şekilleri oluşur. *Bu şekiller üstteki tabakaların aşınması sonucu</div><div>yüzeye çıkabilir.</div>]]></description>
         <enclosure url="" />
         <pubDate>2020-06-14 10:46:30 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625765908</guid>
      </item>
      <item>
         <title>Yüzey Volkanizması</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625791925</link>
         <description><![CDATA[<div>*Magmanın yeryüzüne ulaşmasıyla oluşur.<a href="https://i.hizliresim.com/nkKYbn.png">Bknz:?</a><br>*Bu esnada yeryüzüne sıvı, katı ve gaz hâlde maddeler çıkar. <br>*Yüzey volkanizması sonucu oluşan yeryüzü şekillerine <a href="http://ogmmateryal.eba.gov.tr/panel/upload/etkilesimli/kitap/cografya/10/unite1/icerik/C10S133D01/C10S133D01.html"><strong><em>kaldera</em></strong></a>, <a href="https://www.google.com.tr/maps/place/Meke+Tuzlas%C4%B1+Krater+G%C3%B6l%C3%BC/@37.6849324,33.6314772,2296m/data=!3m1!1e3!4m13!1m7!3m6!1s0x14d772c9d105af39:0x853fc6da4fe69510!2zTWVrZSBHw7Zsw7w!3b1!8m2!3d37.6845143!4d33.6350612!3m4!1s0x14d772b571f1fc39:0x4d7f578508cf7720!8m2!3d37.6903027!4d33.6389512?hl=tr"><strong><em>krater</em></strong></a>, <a href="https://www.google.com.tr/maps/place/Ac%C4%B1+G%C3%B6l/@37.7135208,33.657291,2295m/data=!3m1!1e3!4m13!1m7!3m6!1s0x14d70cfced7f313f:0xc9cad81bf5843da9!2zQWPEsWfDtmw!3b1!8m2!3d37.7144254!4d33.6651265!3m4!1s0x14d70cfcb151fdf9:0x2c4e5a4ef91d2d0d!8m2!3d37.7118239!4d33.6668971?hl=tr"><strong><em>maar</em></strong></a> ve <a href="https://i.hizliresim.com/5Qb7kH.png"><strong><em>volkan<br>konileri</em></strong></a> örnek verilebilir. Ayrıca lavların ve volkanik küllerin birikmesi sonucu<a href="https://encrypted-tbn0.gstatic.com/images?q=tbn%3AANd9GcSOhYsElJa42yvU-ZN2rq4C1cNe_QyIMrFTNW5UnV5gRKoSgWZ_&amp;usqp=CAU"><strong><em> lav düzlükleri</em></strong></a>, bu düzlüklerin<br>akarsularla yarılması sonucu da <a href="https://lh3.googleusercontent.com/proxy/WJVLDD3UjV43uOvyyXVoP0w3z1SqrVlgn3v2YM-wLsPZhecMij6bJeXbc4C63j_79M5vlA0gcl28lWlHPIhSXt3qGk14VzPQ1JpFloksyR0F-TEtoBkShc1PJT1oadtAd5YXcbjDNn3NhOZDnR16kpg"><strong><em>volkanik platolar</em></strong></a> oluşur.</div>]]></description>
         <enclosure url="" />
         <pubDate>2020-06-14 11:19:11 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625791925</guid>
      </item>
      <item>
         <title>Volkanların Dağılışı</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625813202</link>
         <description><![CDATA[<div>*Yeryüzünde volkanların dağılışı ile levha sınırları birbirleriyle paralellik gösterir. Dünyadaki<br>volkanların yaklaşık %75'i Pasifik Levhası'nın çevresinde yer aldığından bu alana <a href="https://www.arcgis.com/apps/MapTour/index.html?appid=696a67cce70e43888929f302b05992b0"><strong><em>Ateş Çemberi </em></strong></a>adı verilir.<br>* Ülkemizde geçmiş zamanlarda aktifleşmiş ve sönmüş volkanlar genellikle  İç Anadolu ve Doğu Anadolu çevresinde görülmektedir.<a href="https://1.bp.blogspot.com/-llPtWQfzpxQ/WEaH0o5q34I/AAAAAAAAAVE/PEAdIgXcClgrkopth5VFQHAmphhtL9clwCLcB/s1600/klkl.jpeg"><strong><em>Bknz:?</em></strong></a></div>]]></description>
         <enclosure url="" />
         <pubDate>2020-06-14 11:46:32 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625813202</guid>
      </item>
      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/625857152</link>
         <description><![CDATA[<div>*Yer kabuğunda çeşitli nedenlerle meydana gelen kısa süreli sarsıntılar olarak tanımlanır.<br>*Yer kabuğu içerisinde meydana gelen depremin başladığı noktaya<br><em>iç merkez (hiposantır)</em> denir.<br>İç merkezden başlayıp çevreye doğru yayılan deprem dalgalarının yeryüzüne ulaştığı ilk noktaya da <em>dış merkez (episantır)</em> adı<br>verilir.<a href="https://o.quizlet.com/k9zn3ilRecMIlXYpYvtGig.jpg"><strong><em>Bknz:?</em></strong></a><strong><em><br>*</em></strong>Depremin merkezinden başlayan deprem dalgaları, genel olarak çevreye üç farklı şekilde yayılır. Bunlar boyuna (P) dalgalar, enine<br>(S) dalgalar ve yüzey (L) dalgalarıdır.<br>*Oluşum nedenlerine göre depremler; çöküntü, volkanik ve tektonik depremler olmak üzere üç gruba ayrılır.<br>*Yer kabuğu hareketleri sırasında meydana gelen kırıklara <a href="https://docplayer.biz.tr/docs-images/48/24560629/images/1-0.jpg"><strong><em>fay</em></strong></a> denir.Faylar; hareket yönlerine<br>göre <a href="https://giphy.com/gifs/fault-THuGplEQoQ2xq"><strong><em>ters</em></strong></a>, <a href="https://commons.wikimedia.org/wiki/File:Fault3.gif"><strong><em>doğrultu atımlı</em></strong></a> ve <a href="https://giphy.com/gifs/earthquake-iris-normal-fault-1zgOYLsKZpj2cONhdZ"><strong><em>normal</em></strong></a> olmak üzere üç gruba ayrılır.Fay hatları boyunca<br>yeryüzünde çatlaklar, yarıklar, çukurluklar oluşur ve<br>heyelanlar meydana gelir. Fay hatlarının bulunduğu<br>alanlarda genellikle deprem riski fazladır.</div>]]></description>
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         <pubDate>2020-06-14 12:40:20 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/625857152</guid>
      </item>
      <item>
         <title>Deprem Kuşakları</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/628680227</link>
         <description><![CDATA[<div><a href="https://depremonlemleri.com/wp-content/uploads/2020/01/yeryuzundeki-buyuk-deprem-kusaklari.jpg"><strong><em>Dünya Deprem Kuşakları</em></strong></a><strong><br></strong>- Pasifik Deprem Kuşağı<br>- Alp- Himalaya Deprem Kuşağı<br>- Atlantik Deprem Kuşağı<br><br><a href="https://deprem.afad.gov.tr/deprem-tehlike-haritasi"><strong><em>Türkiye'deki Deprem Kuşakları</em></strong></a><strong><br></strong>- Kuzey Anadolu Fay Hattı<br>- Doğu Anadolu Fay Hattı<br>- Batı Anadolu Fay Hattı</div>]]></description>
         <enclosure url="" />
         <pubDate>2020-06-16 09:55:09 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/628680227</guid>
      </item>
      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/869274952</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://padlet.com/padlets/m7pkbgtpgjh430vu" />
         <pubDate>2020-10-28 12:23:20 UTC</pubDate>
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      </item>
      <item>
         <title></title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/869309719</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://ogmmateryal.eba.gov.tr/panel/panel/EKitapUniteOnizle.aspx?Id=194" />
         <pubDate>2020-10-28 12:35:14 UTC</pubDate>
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      <item>
         <title>Dünya; yoğunluk ve sıcaklık bakımından yer kabuğu, manto ve çekirdek olmak üzere üç katmandan oluşur. </title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/869338909</link>
         <description><![CDATA[<div><a href="https://i.pinimg.com/originals/b0/5b/7e/b05b7e979e84ac0d1557f5665216e92f.jpg">Bknz.?</a></div>]]></description>
         <pubDate>2020-10-28 12:44:01 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/869338909</guid>
      </item>
      <item>
         <title> Yer Kabuğu </title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/869342278</link>
         <description><![CDATA[<div>* Farklı özellikteki kayaçlardan oluşan yer kabuğuna litosfer ya da taş küre adı verilir. <br>* En dıştaki katmandır</div>]]></description>
         <enclosure url="" />
         <pubDate>2020-10-28 12:45:00 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/869342278</guid>
      </item>
      <item>
         <title>Manto</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/869345609</link>
         <description><![CDATA[<div> *Yer kabuğunun altından başlayıp yaklaşık 2900 km derinliğe kadar uzanır. <br>*Dünya’nın toplam hacminin yaklaşık %84’lük kısmını oluşturur. </div>]]></description>
         <enclosure url="" />
         <pubDate>2020-10-28 12:45:56 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/869345609</guid>
      </item>
      <item>
         <title>Çekirdek</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/869348328</link>
         <description><![CDATA[<div> *Mantodan sonra yer alan ve Dünya’nın merkezinde bulunan katmandır. <br>*Yoğunluğu, sıcaklığı ve kalınlığı en fazla olan katmandır. </div>]]></description>
         <enclosure url="" />
         <pubDate>2020-10-28 12:46:45 UTC</pubDate>
         <guid>https://padlet.com/ozgk/10/wish/869348328</guid>
      </item>
      <item>
         <title>Levha Tektoniği</title>
         <author>ozgk</author>
         <link>https://padlet.com/ozgk/10/wish/869361932</link>
         <description><![CDATA[<div> *Üzerinde yaşadığımız yer kabuğu, uzaydan bakıldığında tek bir parçadan oluşmuş gibi görünür. Ancak son yüzyılda yapılan araştırmalar, yer kabuğunun yapboz gibi parçalardan oluştuğunu göstermektedir .<br>* Yer kabuğunu oluşturan bu parçalara <a href="https://kurious.ku.edu.tr/wp-content/uploads/2017/02/istock-522470764-1170x779.jpg"><strong><em>levha</em></strong></a> adı verilir. Levhalar tıpkı suyun üzerinde yüzen bir sal gibi manto üzerinde hareket hâlindedir. <br>* Levhaları hareket ettiren güç mantodan gelir. Örneğin suyla dolu bir tencere ısıtıldığında ısınan su yukarı, üstte soğuyan su ise aşağı doğru hareket eder. Burada olduğu gibi çekirdeğin sıcaklığından dolayı manto içerisinde ergimiş hâlde bulunan maddelerde benzer bir hareket başlar. Bu harekete konveksiyonel akımlar denir. Levhalar, bu akımların etkisiyle hareket eder. <br>*Levhalar; birbirlerine yakınlaşma, uzaklaşma ve çarpışma hareketi vardır.</div>]]></description>
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         <description><![CDATA[<div>*Günümüzde Türkiye sınırları içerisinde aktif volkana rastlanmamaktadır. <br>* II. Jeolojik Zaman'da ülkemizin<br>bulunduğu alanda su altı volkanları görülmekteydi. Su altı volkanlarına ait kalıntılar, bugünkü <a href="https://i.sozcu.com.tr/wp-content/uploads/2016/09/basliksiz-1-395.jpg">Toroslar</a> ve<br>Kuzey Anadolu Dağları ile Doğu Anadolu’nun büyük bir kısmını kapsayan alanda yer almaktadır. Bu dağların zamanla aşınması sonucu ortaya çıkan derinlik kayaçları bunun bir göstergesidir.<br>*Doğu Anadolu'da yer alan Nemrut, Tendürek, Süphan, Büyük ve Küçük Ağrı dağları ile İç<br>Anadolu'da yer alan Erciyes , Melendiz, Hasan dağları, Karadağ ve Karacadağ önceden aktif olan volkanizmalara örnek verilebilir.</div>]]></description>
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         <description><![CDATA[<div>*Ülkemiz arazisinin %67'sinin genç oluşumlu olmasından dolayı depreme elverişli bir coğrafyamız vardır.<br>*Deprem alanlarının beş bölgeye ayrıldığı Türkiye'de fay hatlarına yaklaştıkça deprem riski artmakta,<br>fay hatlarından uzaklaştıkça da bu risk azalmaktadır.<br>*Türkiye'de Yaşanan Bazı Büyük Depremler<br><strong><em>26 Aralık 1939: Erzincan, depremin büyüklüğü 7,9<br>1 Şubat 1944: Gerede (Bolu), depremin büyüklüğü 7,2<br>30 Kasım 1983: Erzurum ve Kars, depremin büyüklüğü 6,8<br>17 Ağustos 1999: Gölcük (Kocaeli), depremin büyüklüğü 7,4<br>23 Ekim 2011: Erciş (Van), depremin büyüklüğü 7,2</em></strong></div>]]></description>
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