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Ocak programı 👉http://bit.ly/2KGR8ks UEP- Uzaktan Eğitim Programı için👉 https://www.tongucmagaza.com/satisnok... Ödevlerdeki kitaplar için👉https://www.tongucmagaza.com/tongucma...","preview":{"posterSrc":"//avatars.mds.yandex.net/get-vthumb/4083704/291b6ba0d9557bb4ecd6aaf22c19233e/564x318_1","videoSrc":"https://video-preview.s3.yandex.net/kwYbXgEAAAA.mp4","videoType":"video/mp4"},"target":"_self","position":"7","reqid":"1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL","summary":{"isFull":true,"fullTextUrl":"/video/result?ask_summarization=1&numdoc=1&noreask=1&nomisspell=1&parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=videoid:16244262769245772910","teaser":[{"list":{"type":"unordered","items":["Bu video, Tonguç Akademi tarafından sunulan bir coğrafya eğitim dersidir. Eğitmen, uzaktan eğitim formatında haritada yer şekillerini gösterme yöntemlerini ve izohips haritalarını anlatmaktadır.","Video, haritada yer şekillerini gösterme yöntemlerini üç ana başlık altında ele almaktadır: kabartma yöntemi, renklendirme yöntemi ve izohips (eş yükselti eğrileri) yöntemi. İzohips haritalarının nasıl okunacağı, yorumlanacağı ve farklı yeryüzü şekillerinin (vadi, sırt, kapalı çukur, falez, boyun, plato, delta ve haliç) nasıl tespit edileceği detaylı şekilde açıklanmaktadır.","Videoda ayrıca izohips aralık değeri, ekü distans gibi kavramlar örneklerle anlatılmakta, izohipslerin birbirine yaklaşması ve uzaklaşması durumunda eğim değişimi, akarsuların akış hızı ve aşındırma gücü, hidroelektrik potansiyeli, yol yapım maliyeti ve tarım makine kullanımı gibi konular ele alınmaktadır. Video, ÖSYM sınavlarında çıkabilecek soru tiplerini de içermekte ve öğrencilere ödevlendirme ile sonlanmaktadır."]},"endTime":1760,"title":"Haritada Yer Şekillerini Gösterme Yöntemleri ve İzohips Haritaları","beginTime":0}],"fullResult":[{"index":0,"title":"Haritada Yer Şekillerini Gösterme Yöntemleri","list":{"type":"unordered","items":["Uzaktan eğitimle haritada yer şekillerini gösterme yöntemleri işlenecek.","Bu bölümde kabartma yöntemi, renklendirme yöntemi, izohips yöntemi ve eğim hesaplama konuları ele alınacak."]},"beginTime":5,"endTime":57,"href":"/video/preview/16244262769245772910?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=5&ask_summarization=1"},{"index":1,"title":"Kabartma Yöntemi","list":{"type":"unordered","items":["Kabartma yöntemi, yer şekillerinin üç boyutlu kabartması yapılarak elde edilen haritadır.","Bu yöntem yer şekillerinin gerçeğe en yakın gösterildiği yöntemdir.","Kabartma haritaları 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arası yükseklik farkı (ekü distans) daha az olan harita daha ayrıntılı çizimle yapılmıştır ve büyük ölçeklidir.","İzohipsler arası yükseklik farkı daha fazla olan harita daha küçük ölçekli haritadır.","Hem izohipsin sayısı hem de izohipsler arası yükselti farkı haritanın ölçeğine göre değişir."]},"beginTime":1014,"endTime":1097,"href":"/video/preview/16244262769245772910?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1014&ask_summarization=1"},{"index":10,"title":"İzohips Haritalarında Yer Şekillerinin Gösterimi","list":{"type":"unordered","items":["Dağ ve tepe, iç içe kapalı eğriler şeklinde süreklilik arz eden bir alandır.","İzohipslerin birbirinden uzaklaştığı alanlarda eğimi az olan yamaç, birbirine yaklaştığı alanlarda eğimi fazla olan yamaç olur.","Dağ ve tepenin iç kısmına nokta ya da üçgen şeklinde ifade koyulabilir ve bu zirve ya da doruk olarak adlandırılır."]},"beginTime":1097,"endTime":1147,"href":"/video/preview/16244262769245772910?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1097&ask_summarization=1"},{"index":11,"title":"İzohips Haritalarında Yer Şekilleri","list":{"type":"unordered","items":["İzohipslerin yüksekliğin arttığı yöne doğru yaptığı büklümler vadileri gösterir.","Vadilerde süreklilik arz eden çizgiler daimi akarsu, kesik kesik çizgiler ise mevsimlik akarsuyu gösterir.","İzohipslerin yüksekliğin azaldığı yöne doğru yaptığı büklümler sırttır."]},"beginTime":1151,"endTime":1242,"href":"/video/preview/16244262769245772910?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1151&ask_summarization=1"},{"index":12,"title":"Diğer Yer Şekilleri","list":{"type":"unordered","items":["Kapalı çukur, çanak veya krater, eş yükselti eğrilerinin arasında içe doğru uzanan oklarla gösterilir ve 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konumundadır."]},"beginTime":1024,"endTime":1140,"href":"/video/preview/5456775098856299647?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1024&ask_summarization=1"},{"index":10,"title":"Türkiye'deki Kapalı Havzalar","list":{"type":"unordered","items":["Van Gölü, Tuz Gölü, Göller Yöresi, Konya Ovası ve Afyon Akarçay kapalı havzaları Türkiye'de bulunmaktadır.","Göller Yöresi kapalı havzasında Burdur Gölü ve Saldı Gölü gibi karstik oluşumlu göller yer almaktadır.","Seyfe Gölü, Kırşehir'de bulunan ve dışarıya çıkış olmayan önemli bir kapalı havzadır."]},"beginTime":1140,"endTime":1292,"href":"/video/preview/5456775098856299647?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1140&ask_summarization=1"},{"index":11,"title":"İç Anadolu Kapalı Havzası","list":{"type":"unordered","items":["Türkiye'nin en büyük kapalı havzası İç Anadolu Kapalı Havzası'dır ve Orta Anadolu Kapalı Havzaları olarak da bilinir.","İç Anadolu Kapalı Havzası içerisinde Beyşehir Gölü, Konya Ovası ve Tuz Gölü bulunur.","Göller Yöresi ayrı bir kapalı havza olup, İç Anadolu Kapalı Havzası içerisinde yer almaz."]},"beginTime":1292,"endTime":1366,"href":"/video/preview/5456775098856299647?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1292&ask_summarization=1"},{"index":12,"title":"Açık Havzalar","list":{"type":"unordered","items":["Açık havza, kaynağını karadan alıp bütün sularını toplayıp denize boşaltabilen havzalardır.","Türkiye'de Karadeniz, Akdeniz, Ege ve Marmara dört açık havzası bulunmaktadır.","Türkiye akarsularının döküldüğü açık havza, Irak'ın Basra Körfezi'ne dökülen Fırat ve Dicle nehirleriyle 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girer ve Batum'dan Karadeniz'e dökülür.","Çoruh Akarsuyu, akış hızı fazla ve hidro potansiyeli yüksek olan bir akarsudur; Türkiye'nin en yüksek setli barajı olan Yusufeli Barajı (eski adıyla Deriner Barajı) bu akarsuyun üzerinde bulunmaktadır.","Yeşil İrmak, Gümüşhane yakınlarından Kelkit Çayı olarak kaynağını alır, Yozgat'tan Çekerek Çayı gibi yan kollarla birleşerek Samsun Çarşamba'dan Çarşamba Deltası oluşturur ve denize dökülür."]},"beginTime":1565,"endTime":1704,"href":"/video/preview/5456775098856299647?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1565&ask_summarization=1"},{"index":15,"title":"Karadeniz Açık Havzası","list":{"type":"unordered","items":["Karadeniz Açık Havzası, Türkiye'nin en büyük açık havzasıdır ve en fazla tatlı su ile beslenen havzadır.","Havzada yer alan en büyük akarsular Kızılırmak, Yeşil İrmak, Sakarya ve Çoruh'dur.","Havzaya dökülen akarsular arasında Çoruh hariç, tüm akarsular Türkiye sınırları içinde dökülmektedir."]},"beginTime":1704,"endTime":1789,"href":"/video/preview/5456775098856299647?parent-reqid=1773734577397103-14873154737732092505-balancer-l7leveler-kubr-yp-vla-32-BAL&text=StudyGe+-+Geography&t=1704&ask_summarization=1"},{"index":16,"title":"Kızılırmak ve Diğer Akarsular","list":{"type":"unordered","items":["Kızılırmak, Sivas Kızıldağ'dan kaynağını alan, Türkiye sınırları içerisinde akan en uzun akarsudur ve Samsun Bafra'dan Bafra Deltası oluşturarak denize dökülür.","Kızılırmak'ın üç önemli kolu vardır: Yozgat'tan gelen Delice, Küre İlgaz Dağlarından kaynağını alan Gökırmak ve diğer bir kolu.","Bartın Çayı, küçük bir akarsu olmasına rağmen, Bartın'ın merkezinden denize döküldüğü yere kadar olan 5 km'lik bir yerde turistik ulaşım için 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