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Southern Alps (geology) : ウィキペディア英語版 | Southern Alps (Europe)
The Southern Alps are a geological subdivision of Alps that are found south of the Periadriatic Seam, a major geological faultzone across the Alps. The southern Alps contain almost the same area as the Southern Limestone Alps. The rocks of the southern Alps gradually go over in the ''Dinarides'' or Dinaric Alps to the south-east. In the south-west they disappear below recent sediments of the Po basin that are lying discordant on top of them. ==Lithology== The Southern Alps are composed of material from the Adriatic or Apulian tectonic plate, the area is a part of this plate. These are mainly Mesozoic sedimentary rocks, most of them limestones.
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