Los Llanos Formation
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Los Llanos Formation
Los Llanos Formation is a geological Formation (geology), formation in the in La Rioja Province, Argentina, La Rioja Province, northwestern Argentina whose strata date back to the Campanian stage of the Late Cretaceous. Los Llanos Formation over the years has been controversially described as ranging from Late Cretaceous to Miocene, but the Miocene succession was assigned to Las Mulitas Formation in 2019. The formation rests on top of the Early Permian Los Sauces Formation, Los Sauces and Patquía Formations and in parts on Ordovician crystalline basement. The maximum thickness is estimated at . The sandstones and conglomerate (geology), conglomerates of the formation were deposited ij a fluvial depositional environment, environment. The formation outcrop, crops out in the , where more than 90 titanosaurid nesting sites were discovered in Los Llanos Formation. The sites were encountered on top of areas characterized by hydrothermal activity as geysers and other vents, suggesting ...
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Geological Formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by Abraham Gottlob Wer ...
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