tag:blogger.com,1999:blog-52545240440895908072024-02-19T22:18:48.205-08:00New TectonicAnonymoushttp://www.blogger.com/profile/15158688228432621994noreply@blogger.comBlogger1125tag:blogger.com,1999:blog-5254524044089590807.post-79267925988530157702014-02-06T22:44:00.002-08:002014-02-06T22:44:23.822-08:00Valley includes<div dir="ltr" style="text-align: left;" trbidi="on">
Valley includes the Main Ethiopian Rift,[3]running eastward from the Afar Triple Junction, which continues south uplift has occurred within the last 30 Ma.[2] Using the environmental correlations and current topographic locations of the Jurassic Upper Limestone and Cretaceous Upper Sandstone, the net rock uplif a typical distance oceanic lithosphere must travel before being subducted, the thickness varies from about 6 km (4 mi) thick at mid-ocean ridges to greater than 100 km (62 mi) at subduction zones; for shorter or longer distances</div>
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