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    Süper yanardağ

    Volkan Türü
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    Genel bilgiler

    Süper yanardağlar bilinen en büyük volkanlar olup normal yanardağların hilâfına magma haznesinin büyüklüğünden dolayı patlamalardan sonra bir volkan konisi yerine yerde dev boyutlarda kalderalar (göçükler) oluştururlar.

    Süper yanardağlar, bölgelerinin altında bulunan fevkalâde büyük bir magma haznesiyle kendilerini belli ederler.

    Şu sıralar Dünya'da ancak birkaç süper yanardağ bilinmektedir. Yellowstone'un yanı sıra Toba gölü, Taupo gölü ve La Garita kalderası bilinenler arasındadır.

    tr.wikipedia.org

    İlgili gündem

    Dünyanın en aktif yanardağlarından biri olan Hawaii'deki Kilauea Yanardağı'nda 23 Aralık’tan bu yana yaşanan volkanik hareketlilik sürüyor. Yanardağ, Aralık ayından bu yana 25. kez patladı. Hawaii Yanardağı Gözlemevi, lav püskürmelerinin yaklaşık 100 metre yüksekliğe ulaştığını bildirdi.
    dunya.com12 Haziran
    Dünyanın farklı coğrafyalarında meydana gelen yanardağ patlamaları, yalnızca doğayı değil, insanlık tarihini de derinden etkiledi. Tarihte iz bırakan bazı felaketler, şehirleri haritadan silerken, bazıları iklimi dahi değiştirdi. İşte, yeryüzünün en yıkıcı 5 yanardağ felaketi!
    haberturk.com3 Haziran
    İtalya’daki Campi Flegrei volkanik kalderasının olduğu bölgede son altı ay içinde yaşanan sarsıntılar, yanardağ patlaması endişelerini de beraberinde getirdi.
    ntv.com.tr30 Mayıs
    İtalya'da bulunan Phlegraean Sahaları'nda süper yanardağ şiddetli depremlerle gündemde. Uzmanlar sarsıntıların magmada kabarcıklara neden olan basınç nedeniyle zeminin yükselmesinden kaynaklandığını belirtti.
    tgrthaber.com26 Nisan

    Volkanik yeryüzü şekilleri

    Yellowstone
    Kalderası
    Vezüv
    Yanardağı
    Toba
    felaket teorisi
    Karakatau
    Kilimanjaro
    Fuji Dağı
    Etna
    Yanardağı
    Volkanik
    patlama türleri
    Mauna Loa
    Dağı
    Tambora
    Dağı
    Kaynak veriler bazında Yandex nöral ağları tarafından oluşturuldu; yanlışlıklar olabilir. Lütfen önemli bilgileri kontrol ediniz
    tr.wikipedia.org
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