| Badilloa | |
|---|---|
 | |
| Badilloa salicina | |
Scientific classification  | |
| Kingdom: | Plantae |
| Clade: | Tracheophytes |
| Clade: | Angiosperms |
| Clade: | Eudicots |
| Clade: | Asterids |
| Order: | Asterales |
| Family: | Asteraceae |
| Subfamily: | Asteroideae |
| Tribe: | Eupatorieae |
| Genus: | Badilloa R.M.King & H.Rob. |
Badilloa is a genus of shrubs and small trees in the family Asteraceae. [1]
Badilloa is native to the Andes of northwestern South America, from Venezuela to Peru. [1]
Pichincha is a stratovolcano in Ecuador. The capital Quito wraps around its eastern slopes.
Villeta is a municipality and town in Cundinamarca (Colombia), located in Gualivá Province, approximately 84 kilometres (52 mi) northwest of Bogota, considered the capital of the province. Its name means "Little Village". The municipality borders Quebradanegra and Nimaima in the north, Nocaima and Sasaima in the east, Albán and Vianí in the south and Guaduas in the west. It is situated at an altitude of 850 metres (2,790 ft) in the Eastern Ranges of the Colombian Andes
Badilloa atrescens is a species of flowering plant in the family Asteraceae. It is endemic to Ecuador, where it is known from only two locations in the central Andes. It grows in forest habitat between 2000 and 3000 meters in elevation.
Cronquistianthus is a genus of shrubs native to the Andes in Colombia, Ecuador, and Peru.
Grosvenoria is a genus of South American shrubs and small trees in the family Asteraceae. They are native to the Andes, from central Ecuador to northern Peru at elevations of 2,700 to 3,700 metres.
Joseanthus is a genus of South American flowering plants in the family Asteraceae.
Kaunia is a genus of South American shrubs or small trees in the family Asteraceae. Its range is centered in Bolivia but it is also found in Argentina, southern Brazil, Peru and Ecuador.
Brachyotum is a genus of flowering plants in the family Melastomataceae. There are about 58 species native to the Andes of South America.
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.
Apodanthera herrerae, known as ckoto-ckoto, is grown for its edible tuber. It originates in the Andes.
Trichoceros is a genus of flowering plants from the orchid family, Orchidaceae. The genus is endemic to South America.
Columellia is a group of plant species in the Columelliaceae described as a genus in 1794.
The La Frontera Formation (Spanish: Formación La Frontera, K2F, Ksf) is a geological formation, part of the Villeta Group, of the Altiplano Cundiboyacense and neighbouring areas of the Eastern Ranges of the Colombian Andes. The sequence of limestones and lydites dates to the Late Cretaceous period; Turonian epoch and has a maximum thickness of 206 metres (676 ft).
The Hiló Formation is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly shale formation dates to the Middle Cretaceous period; Late Albian to Early Cenomanian epochs and has a measured thickness at its type section of 470 metres (1,540 ft). The fossiliferous formation has provided a great abundance of ammonites and other marine species.
The Socotá Formation is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consisting of a lower unit of calcareous sandstones and an upper sequence of shales dates to the Early Cretaceous period; Late Aptian epoch and in Quipile has a measured thickness of 255 metres (837 ft) with large regional variations. The formation hosts ammonite fossils.
The Pacho Formation is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consisting of alternating siltstones and shales with siderite concretions dates to the Middle Cretaceous period; Late Albian to Cenomanian epochs and has an approximate thickness of 1,050 metres (3,440 ft).
The Guavio Formation is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of conglomerates, shales and limestones, dates to the Late Jurassic and Early Cretaceous periods; Tithonian to Berriasian epochs and has a maximum thickness of 1,000 metres (3,300 ft).
The Vianí Fault is a dextral oblique thrust fault in the department of Cundinamarca in central Colombia. The fault has a total length of 38.3 kilometres (23.8 mi) and runs along an average northwest to southeast strike of 055.5 ± 15 in the Eastern Ranges of the Colombian Andes.
The Villeta Group is a geological group of the Eastern Ranges of the Colombian Andes, to the west of the Altiplano Cundiboyacense. The group, a sequence of shales, limestones and sandstones, is subdivided into various formations; Conejo, La Frontera, Simijaca, Hiló, Pacho, Chiquinquirá, Capotes, Socotá, El Peñón, and Trincheras, and dates to the Cretaceous period; Aptian-Coniacian epochs. The group stretches out across four departments, from Huila in the south, through Cundinamarca and Boyacá to southern Santander in the north. The upper part of the Villeta Group is time-equivalent with the La Luna Formation of the Middle Magdalena Valley (VMM) and Sierra Nevada del Cocuy, the Oliní and Güagüaquí Groups of the Guaduas-Vélez synclinal and the Chipaque Formation of the Altiplano Cundiboyacense. The lower part has been correlated with the Simití, Tablazo and Paja Formations of the VMM, the upper Tibasosa, Une and Fómeque Formations of the Altiplano Cundiboyacense and the Capacho, Aguardiente, Tibú-Mercedes and upper Río Negro Formations of the Sierra Nevada del Cocuy.
The Oliní Group (Spanish: Grupo Oliní, K3k5o, K2ol, Kso) is a fossiliferous geological group of the VMM, VSM and the eastern flanks of the Central and western flanks of the Eastern Ranges of the Colombian Andes. The regional group stretches from north to south across approximately 700 kilometres (430 mi) and dates to the Late Cretaceous period; Coniacian, Santonian and Campanian epochs, and has a maximum thickness of 287 metres (942 ft). Fossils of Eonatator coellensis have been found in the unit, near Coello, Tolima.
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