Aeropuerto las cruces | |||||||||||
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| Summary | |||||||||||
| Airport type | Publicó | ||||||||||
| Serves | Sabana de Torres, Colombia | ||||||||||
| Elevation AMSL | 440 ft / 134 m | ||||||||||
| Coordinates | 7°23′00″N73°30′20″W / 7.38333°N 73.50556°W Coordinates: 7°23′00″N73°30′20″W / 7.38333°N 73.50556°W | ||||||||||
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  SNT Location of the airport in Colombia | |||||||||||
| Runways | |||||||||||
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Las Cruces Airport( IATA : SNT, ICAO : SKRU) is an airport serving the town of Sabana de Torres in the Santander Department of Colombia.
The runway is on the southern edge of the town.
Carolina is a municipality located on the northeast coast of Puerto Rico. It lies immediately east of the capital San Juan and Trujillo Alto; north of Gurabo and Juncos; and west of Canóvanas and Loíza. Carolina is spread over 12 wards plus Carolina Pueblo. It is part of the San Juan-Caguas-Guaynabo Metropolitan Statistical Area, and home to Puerto Rico's main airport, the Luis Muñoz Marín International Airport.
Sabana Grande is a municipality of Puerto Rico located north of Lajas and Guánica; south of Maricao; east of San Germán; and west of Yauco. Sabana Grande is spread over seven wards and Sabana Grande Pueblo. It is part of the San Germán-Cabo Rojo Metropolitan Statistical Area.
Cruces is a municipality and town in Cienfuegos Province, Cuba. It is the home of the Mal Tiempo National Park which commemorates a battle in the 1895 War of Independence.
El Abra is the name given to an extensive archeological site, located in the valley of the same name. El Abra is situated in the east of the municipality Zipaquirá extending to the westernmost part of Tocancipá in the department of Cundinamarca, Colombia. The several hundred metres long series of rock shelters is in the north of the Bogotá savanna on the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes at an altitude of 2,570 metres (8,430 ft). The rock shelter and cave system is one of the first evidences of human settlement in the Americas, dated at 12,400 ± 160 years BP. The site was used by the hunter-gatherers of the Late Pleistocene epoch.
Piedras del Tunjo is an important archaeological park established on a natural rock shelter 40 kilometres (25 mi) west of Bogotá in the municipality of Facatativá.
Colonel Carlos Concha Torres Airport is an airport serving the Pacific coastal city of Esmeraldas, capital of the Esmeraldas Province of Ecuador. It is 3 kilometres (1.9 mi) east of the city, across the Esmeraldas River in the parish of Tachina. Established in 1940 as General Rivadeneira Airport, the airport was renovated between 2012 and 2013, receiving a new terminal and a lengthened runway.
The Las Brujas Airport is a domestic airport located in the town of Corozal, Sucre in Colombia. The airport is located 10 minutes from the capital of the department, the city of Sincelejo. In emergency situations, it serves as the alternate airport of the city of Montería. It has regional and national operations. Las Brujas operates regional and domestic flights to Barranquilla, Bogota and Medellin.
Jorge Enrique González Torres Airport is an airport serving San José del Guaviare, the capital of the Guaviare Department of Colombia. The runway is just north of the town and parallels the Guaviare River.
The North Andes Plate or North Andes Block is a small tectonic plate (microplate) located in the northern Andes. It is squeezed between the faster moving South American Plate and the Nazca Plate to the southwest. Due to the subduction of the Malpelo and Coiba Plates, this area is very prone to volcanic and seismic activity, with many historic earthquakes.
San Antonio de Areco Airport is an airport 3 kilometres (2 mi) northeast of San Antonio de Areco, a town in the Buenos Aires Province of Argentina.
Cruce a Nado Internacional is a yearly international swimming competition that takes place at Bahía de Ponce in Ponce, Puerto Rico. It is the oldest open water swimming event in the Caribbean. The event generally occurs on the first Sunday of September, to coincide with the Sunday of Labor Day Weekend every year. The event is sponsored by Club Cruce a Nado, Inc. Some 100 athletes compete. The event started in 1980.
Jaboque is a wetland, part of the Wetlands of Bogotá, located in the locality Engativá, Bogotá, Colombia. The wetland, close to the Bogotá River on the Bogotá savanna covers an area of 148 hectares. The wetland is close to El Dorado International Airport in the Juan Amarillo River basin.
The Tunjuelo or Tunjuelito River is a river on the Bogotá savanna and a left tributary of the Bogotá River. The river, with a length of 73 kilometres (45 mi) originates in the Sumapaz Páramo and flows northward through the Usme Synclinal to enter the Colombian capital Bogotá. There, the river is mostly canalised flowing westward into the Bogotá River. It is one of the three main rivers of the city, together with the Fucha and Juan Amarillo Rivers.
The Soacha River is a river on the Bogotá savanna and a left tributary of the Bogotá River.
The Chipaque Formation (Spanish: Formación Chipaque, K2cp, Kc) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation is also described as Gachetá Formation, named after Gachetá, in the area of the Llanos foothills of the Eastern Ranges. The predominantly organic shale formation dates to the Late Cretaceous period; Cenomanian-Turonian epochs and has a maximum thickness of 1,700 metres (5,600 ft). The formation, rich in TOC, is an important oil and gas generating unit for the giant oilfields Cupiagua and Cusiana of the Eastern Ranges as well as in the Llanos Orientales.
The Guadalupe Group (Spanish: Grupo Guadalupe, K2G, Ksg) is a geological group of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The group, a sequence of shales and sandstones, is subdivided into three formations; Arenisca Dura, Plaeners and Arenisca Labor-Tierna, and dates to the Late Cretaceous period; Campanian-Maastrichtian epochs and at its type section has a thickness of 750 metres (2,460 ft).
The Tunjuelo Formation, Río Tunjuelo or Río Tunjuelito Formation is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of conglomerates with intercalating shales and sandstones. The Tunjuelo Formation dates to the Quaternary period; covering the complete Pleistocene epoch, and has a maximum thickness of 150 metres (490 ft). It is a formation of the lacustrine and fluvio-glacial sediments of Lake Humboldt.
The Río Frío is a river on the Bogotá savanna and a right tributary of the Bogotá River. The river, in a basin of 6,008.69 hectares (23.1997 sq mi), originates on the Páramo de Guerrero in Zipaquirá at an altitude of 3,700 metres (12,100 ft). It flows through the municipalities Tabio and Cajicá and into the Bogotá River in the south of Chía, at 2,550 metres (8,370 ft) above sea level.
The Sabana Formation is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of shales with at the edges of the Bogotá savanna lignites and sandstones. The Sabana Formation dates to the Quaternary period; Middle to Late Pleistocene epoch, and has a maximum thickness of 320 metres (1,050 ft), varying greatly across the savanna. It is the uppermost formation of the lacustrine and fluvio-glacial sediments of paleolake Humboldt, that existed at the edge of the Eastern Hills until the latest Pleistocene.
The Bogotá Fault is a major inactive slightly dextral oblique thrust fault in the department of Cundinamarca in central Colombia. The fault has a total length of 79.3 kilometres (49.3 mi), while other authors designate a length of 107 kilometres (66 mi), and runs along an average north-northeast to south-southwest strike of 013.5 ± 7 across the Altiplano Cundiboyacense, central part of the Eastern Ranges of the Colombian Andes.
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