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Andrade, Mary J. Day of the Dead A Passion for Life – Día de los Muertos Pasión por la Vida. La Oferta Publishing, 2007. ISBN 978-0-9791624-04; Anguiano, Mariana, et al. Las tradiciones de Día de Muertos en México. Mexico City 1987. Brandes, Stanley (1997). "Sugar, Colonialism, and Death: On the Origins of Mexico's Day of the Dead".
The Loma Gorda Formation (Spanish: Formación Loma Gorda, Kl, Kslg) is a fossiliferous geological formation of the Upper Magdalena Valley (VSM) and surrounding Central and Eastern Ranges of the Colombian Andes, extending from Cundinamarca in the north to Huila and easternmost Tolima in the south.
In 1966, Uruguayan geologists Héctor Goso and Jorge Bossi defined the Raigón Formation, which they subdivided into the San José Member (the same as Francis and Mones' San José Formation) below and the San Bautista Member above. [2]
Olivier de Serres, considered the father of French agronomy, was the first to suggest the abandonment of fallowing and its replacement by hay meadows within crop rotations. He also highlighted the importance of soil (the French terroir) in the management of vineyards.
The Formaciones de Tepuyes Natural Monument also known as tepui [1] (Spanish: Monumento Natural Formaciones de Tepuyes) [2] Also Formaciones de Tepuyes Is a protected natural space since 1991, located in Venezuela [3] more specifically in the states of Amazonas and Bolívar. [4]
Hilgard was born at Zweibrücken, Kingdom of Bavaria, January 5, 1833, the son of Theodore Erasmus and Margaretha (Pauli) Hilgard. His father was a successful lawyer, holding the position of chief justice of the court of appeals of the province of Rhenish Bavaria.
"El día que me quieras" (English: The day that you love me) is an Argentine tango with music by Carlos Gardel and lyrics by Alfredo Le Pera. It is considered one of the most popular songs of the 20th century and one of the best Latin songs of all time. [ 1 ]
Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.