This article relies largely or entirely on a single source .(April 2016) |
No tengo madre | |
---|---|
Also known as | Ya tengo madre Ya valió madre |
Genre | Telenovela Comedy |
Created by | Eugenio Derbez |
Written by | Carlos Aguilar |
Directed by | Eugenio Derbez Gustavo Rodríguez José Acosta Navas |
Starring | Eugenio Derbez Natalia Esperón Saby Kamalich Susana Alexander Norma Lazareno |
Opening theme | Yo quiero a mi mamá by Eugenio Derbez & Luis Ernesto Cano |
Country of origin | Mexico |
Original language | Spanish |
No. of episodes | 40 |
Production | |
Executive producer | Carlos Sotomayor |
Producer | Rafael Urióstegui |
Production locations | Filming Televisa San Ángel Mexico City, Mexico Locations Mexico City, D.F., Mexico |
Cinematography | Armando Zafra Carlos Sánchez Ross |
Running time | 21–22 minutes |
Production company | Televisa |
Original release | |
Network | Canal de las Estrellas |
Release | March 10 – May 2, 1997 |
No tengo madre (English title: I have no mother) is a Mexican comedy telenovela produced by Carlos Sotomayor for Televisa in 1997. [1]
On March 10, 1997, Canal de las Estrellas started broadcasting No tengo madre weekdays at 8:00pm, replacing Alguna vez tendremos alas. The last episode was broadcast on May 2, 1997, with Esmeralda replacing it the following Monday.
Natalia Esperón and Eugenio Derbez starred as protagonists.
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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 Subachoque Formation is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of sandy shales and lignite with sandstone beds. The Subachoque Formation dates to the Quaternary period; Early to Middle Pleistocene epoch, and has a maximum thickness of 150 metres (490 ft). It is the lowermost formation of the lacustrine and fluvio-glacial sediments of Lake Humboldt.
The Guaduas Formation (Spanish: Formación Guaduas, K2P1G, K2E1G, KPgg, KTg, TKg, Ktg) is a geological formation of the Middle Magdalena Basin and the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly shale with coalbed formation dates to the Late Cretaceous and Paleogene periods; Maastrichtian-Paleocene epochs, and has a maximum thickness of 1,090 metres (3,580 ft). Fossils of Coussapoa camargoi, Ficus andrewsi, Berhamniphyllum sp. and Archaeopaliurus boyacensis have been found in coalbeds in Zipaquirá and Tasco, Boyacá.
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