GEOLOGY - Holocene

Jun 28th, 2015
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The Holocene is a geological epoch which began approximately 11,700 years ago [ 1 ] (10 000 14 C years ago). The Holocene adalah geologi zaman yang dimulai sekitar 11.700 tahun yang lalu [1] (10 000 14 P tahun lalu). According to traditional geological thinking, the Holocene continues to the present.

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HoloceneFrom Wikipedia, the free encyclopedia Dari Wikipedia, ensiklopedia bebasJump to: navigation , search Langsung ke: navigasi, cariSubdivisions of the Quaternary period Pembagian administratif Kuarter periodeSystem Sistem Series Seri Stage Tahap Age ( Ma ) Umur (Ma)Quaternary Kuarter Holocene Holocene 00.0117 0-0.0117Pleistocene Pleistosen Tarantian (Upper) Tarantian (Upper) 0.01170.126 0.0117-0.126Ionian (Middle) Ionia (Tengah) 0.1260.781 0.126-0.781Calabrian (Lower) Calabria (Lower) 0.7811.806 0.781-1.806Gelasian (Lower) Gelasian (Lower) 1.8062.588 1.806-2.588Neogene Neogen Pliocene Pliosen Piacenzian Piacenzian older tuaIn Europe and North America, the Holocene is subdivided into Preboreal , Boreal , Atlantic , Subboreal and Subatlantic stages of the Blytt-Sernander time scale . Di Eropa dan Amerika Utara, Holocene dibagi menjadi Preboreal, Boreal, Atlantik, Subboreal dan Subatlantic tahap Blytt-Sernander skala waktu. There are many regional subdivisions for the Upper or Late Pleistocene, usually these represent locally recognized cold ( glacial ) and warm ( interglacial ) periods. Ada banyak subdivisi regional untuk Upper atau akhir Pleistosen, biasanya ini diakui secara lokal mewakili dingin (glasial) dan hangat (interglacial) periode. The last glacial period ends with the cold Younger Dryas substage. Yang zaman es terakhir berakhir dengan dingin Dyas Muda substage.Holocene epoch Holocene epochThis box: view talk

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