. . . . . . . . . . . . . "Between 29 and 27 million years ago, the extrusion of Ethiopia\u2019s flood basalts was interrupted and deposition of continental sediments occurred. Inter-trappean beds outcrop in many places of the Ethiopian highlands. They consist of fluvio-lacustrine deposits, that are generally a few tens of metres thick. Often, these interbedded fluvio-lacustrine deposits are very visible because their bright colours strongly contrast with the basalt environment."@en . . . . ":It:Giovanni Merla"@en . "Intra-volcanic sedimentary rock"@en . . . . . "Northern Ethiopian Highlands"@en . . . "Oligocene"@en . . . . . . . . "7562"^^ . . . . . . . . . . . "61376569"^^ . . "13.6552 39.1731" . . . "Intra-volcanic sedimentary rock in North Ethiopia"@en . "937593782"^^ . . . . . "13.65520000457764"^^ . . . "Ksad Addi Amyuq near Hagere Selam"@en . . . . "POINT(39.173099517822 13.655200004578)"^^ . "39.17309951782227"^^ . "Between 29 and 27 million years ago, the extrusion of Ethiopia\u2019s flood basalts was interrupted and deposition of continental sediments occurred. Inter-trappean beds outcrop in many places of the Ethiopian highlands. They consist of fluvio-lacustrine deposits, that are generally a few tens of metres thick. Often, these interbedded fluvio-lacustrine deposits are very visible because their bright colours strongly contrast with the basalt environment."@en . . . . . . . . . .