Mendoza, officially Province of Mendoza, is a province of Argentina, in the western central part of the country in the Cuyo region. It borders San Juan to the north, La Pampa and Neuquén to the south, San Luis to the east, and the republic of Chile to the west; the international limit is marked by the Andes mountain range. Its capital city is the homonymous city of Mendoza.
Jinotega is a department of Nicaragua. Its departmental head is Jinotega. It is located in the north of the country, on the border with Honduras.
San Rafael is one of the departments of Mendoza Province, Argentina. The seat of the department is in the city of San Rafael.
Malvinas Argentinas Stadium is a stadium in the city of Mendoza in the homonymous province of Argentina. With a seating capacity of 42,000 spectators, the stadium is the largest in Mendoza. Built for the 1978 FIFA World Cup, It is owned and administered by the Provincial Government.
LRA Radio Nacional, also known as Radio Nacional Argentina, is the Argentine national radio station, and part of the national public media system. It started transmitting in 1937 as LRA Radio del Estado and changed its name to the current one in 1957. Since 1949, National Radio is also in charge of the Radiodifusión Argentina al Exterior, an international service that broadcasts in numerous languages.
San Rafael is a city in the southern region of the Mendoza Province, Argentina. With more than 118,000 inhabitants, it is the largest city in and the seat of San Rafael Department.
The Paso Internacional Los Libertadores, also called Cristo Redentor, is a mountain pass in the Andes between Argentina and Chile. It is the main transport route out of the Chilean capital city Santiago into Mendoza Province in Argentina and so carries quite heavy traffic.
The University of Mendoza is an Argentine non-profit private university in the city of Mendoza with a branch in the city of San Rafael.
Ernesto Sanz is a former Argentine politician of the Radical Civic Union and one of the founders of Cambiemos. He served in the Argentine Senate representing Mendoza Province from 2003 to 2015.
The Precordillera Terrane or Cuyania was an ancient microcontinent or terrane whose history affected many of the older rocks of Cuyo in Argentina. It was separated by oceanic crust from the Chilenia terrane which accreted into it at ~420-390 Ma when Cuyania was already amalgamated with Gondwana. The hypothesized Mejillonia Terrane in the coast of northern Chile is considered by some geologists to be a single block with Cuyania.
Precordillera is a Spanish geographical term for hills and mountains lying before a greater range, similar to foothills. The term is derived from cordillera —literally "pre-mountain range"—and applied usually to the Andes.
Las Paredes is a 3.293 km (2.046 mi) Argentine motorsport circuit located near San Rafael, Mendoza Province. The circuit was opened in October 1968.
The Famatinian orogeny is an orogeny that predates the rise of the Andes and that took place in what is now western South America during the Paleozoic, leading to the formation of the Famatinian orogen also known as the Famatinian belt. The Famatinian orogeny lasted from the Late Cambrian to at least the Late Devonian and possibly the Early Carboniferous, with orogenic activity peaking about 490 to 460 million years ago. The orogeny involved metamorphism and deformation in the crust and the eruption and intrusion of magma along a Famatinian magmatic arc that formed a chain of volcanoes. The igneous rocks of the Famatinian magmatic arc are of calc-alkaline character and include gabbros, tonalites, granodiorites and trondhjemites. The youngest igneous rocks of the arc are granites.
The San Rafael orogeny was an orogeny that affected parts of western Argentina and Chile during the Late Paleozoic. The resulting orogenic belt has a NW-NNW curved form. The San Rafael orogeny might have been linked with the roughly contemporary Gondwanide orogeny of eastern Argentina. Parts of the Choiyoi Group sediments were deformed by the San Rafael orogeny. During the Neogene ancient faults related to the San Rafael orogeny conditioned the geometry of the blocks affected by the Andean orogeny.
The Gondwanide orogeny was an orogeny active in the Permian that affected parts of Gondwana that are by current geography now located in southern South America, South Africa, Antarctica, Australia and New Guinea. The zone of deformation in Argentina extends as a belt south and west of the cratonic nucleus of Río de la Plata–Pampia. The deformation of the orogeny is visible in the Sierra de la Ventana mountains in Argentina and the Cape Fold Belt in South Africa. The Gondwanide orogeny might have been linked with the roughly contemporary San Rafael orogeny of western Argentina.
Choiyoi Group is a Permian and Triassic-aged group of volcano-sedimentary formations in Argentina and Chile. The group bears evidence of bimodal-style volcanism related to an ancient subduction zone that existed along the western margin of the supercontinent Gondwana.
The Precordillera terrane of western Argentina is a large mountain range located southeast of the main Andes mountain range. The evolution of the Precordillera is noted for its unique formation history compared to the region nearby. The Cambrian-Ordovian sedimentology in the Precordillera terrane has its source neither from old Andes nor nearby country rock, but shares similar characteristics with the Grenville orogeny of eastern North America. This indicates a rift-drift history of the Precordillera in the early Paleozoic. The Precordillera is a moving micro-continent which started from the southeast part of the ancient continent Laurentia. The separation of the Precordillera started around the early Cambrian. The mass collided with Gondwana around Late Ordovician period. Different models and thinking of rift-drift process and the time of occurrence have been proposed. This page focuses on the evidence of drifting found in the stratigraphical record of the Precordillera, as well as exhibiting models of how the Precordillera drifted to Gondwana.
The Bucaramanga-Santa Marta Fault or Bucaramanga-Santa Marta Fault System is a major oblique transpressional sinistral strike-slip fault in the departments of Magdalena, Cesar, Norte de Santander and Santander in northern Colombia. The fault system is composed of two main outcropping segments, named Santa Marta and Bucaramanga Faults, and an intermediate Algarrobo Fault segment in the subsurface. The system has a total length of 674 kilometres (419 mi) and runs along an average north-northwest to south-southeast strike of 341 ± 23 from the Caribbean coast west of Santa Marta to the northern area of the Eastern Ranges of the Colombian Andes.
