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Paleogeography of the Campanian Outcrops of the Cerro del Pueblo Formation at the type locality of Cerro del Pueblo, on the edge of Saltillo, Coahuila. The Cerro del Pueblo Formation is a geological formation in Coahuila, Mexico, whose strata date back to the latest Campanian of the Late Cretaceous, just before the Campanian-Maastrichtian boundary.
Extent of the formation in the Ischigualasto-Villa Unión Basin. Los Colorados Formation is a unit with an approximate thickness of 600 metres (2,000 ft) of the Agua de la Peña Group in the Ischigualasto-Villa Unión Basin, where it is exposed in the Ischigualasto Provincial Park, a World Heritage Site in Argentina.
Rinderknecht, Andrés (2011), Estudio sobre los roedores gigantes del Uruguay, Departamento de San José (Mioceno tardío-Pliocene) y sus implicancias para la sistemática y taxonomía de la familia Dinomyidae (Mammalia, Rodentia) (PDF), Universidad de la República, pp. 1–101
A soil scientist examining horizons within a soil profile. Soil science is the study of soil as a natural resource on the surface of the Earth including soil formation, classification and mapping; physical, chemical, biological, and fertility properties of soils; and these properties in relation to the use and management of soils.
Soil structure describes the arrangement of the solid parts of the soil and of the pore spaces located between them (Marshall & Holmes, 1979). [1] Aggregation is the result of the interaction of soil particles through rearrangement, flocculation and cementation.
Robert De Niro tells Savannah Guthrie what he thought of her 'Zero Day' cameos. Entertainment. Harper's Bazaar. Here’s how you can score tickets to the 2025 Blackpink world tour. Finance.
U.S. Treasury Secretary Scott Bessent has been ordered to cease production of the one-cent coin known as the penny, President Donald Trump said in a posting on his Truth Social media account on ...
The Dakota is a sedimentary geologic unit name of formation and group rank in Midwestern North America. The Dakota units are generally composed of sandstones, mudstones, clays, and shales deposited in the Mid-Cretaceous opening of the Western Interior Seaway. [7]