Search results
Results From The WOW.Com Content Network
The Late Miocene (also known as Upper Miocene) is a sub-epoch of the Miocene Epoch made up of two stages. The Tortonian and Messinian stages comprise the Late Miocene sub-epoch, which lasted from 11.63 Ma ( million years ago ) to 5.333 Ma.
Late Miocene (Huayquerian) South America: Argentina: Mammals, birds, reptiles, fish, bivalves, foraminifera, ichnofossils and flora: Jaguel Formation: Late Cretaceous/Early Paleocene (Maastrichtian – Danian) South America: Argentina: Cerro Cuadrado Petrified Forest: La Matilde Formation: Middle to Late Jurassic (Bathonian – Oxfordian) South ...
Manus Island is volcanic in origin and probably broke through the ocean's surface in the late Miocene, 8 to 10 million years ago. The substrate of the island is either directly volcanic or from uplifted coral limestone. Lorengau, the capital of Manus Province, is located on the island.
The Miocene (/ ˈ m aɪ. ə s iː n,-oʊ-/ MY-ə-seen, -oh-) [6] [7] is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words μείων (meíōn, "less") and καινός (kainós, "new") [8] [9] and means "less recent" because it has 18% fewer modern marine invertebrates ...
Cliffs of Upper Coralline Limestone Formation on islands at the western end of Comino. The top layer, the Upper Coralline Limestone (Maltese: Qawwi ta' Fuq), is the youngest formation of Messinian age (~7–5 million years old) and is around 140 m thick. [1] It is mainly present on the islands of Malta, Comino and in the east of Gozo. The ...
During the Late Miocene-Early Pleistocene, a massive basaltic volcanic activity occurred. After the emission of alkali basalts during the Late Miocene, major volcanic activity occurred during the Late Pliocene, in which large volumes of tholeiitic basalts were emitted and the foredeep north of the Hyblean foreland collapsed.
The Cycladic Massif is a Miocene high-pressure orogenic segment located in the Aegean Sea underlying the Cyclades. [1] Initially, the Massif was a single island which began to break apart due to the tectonic activities of the subduction of the African Plate under the Eurasian Plate during the late Miocene Epoch.
Their remains were preserved in locations such as the Alaska Peninsula, Awik, the Cook Inlet's shoreline, Eagle City, Unga Island. [8] Alaska's late Miocene fossil record also documents the state's ancient invertebrates. [6] From the Miocene to the Pliocene, Alaska's land area just about reached its full modern extent. [3]