banner

The Chicama Moche intervalley canal: social explanations and physical paradigms. Charles R. Ortloff

Por: Ortloff, Charles RColaborador(es): Moseley, Michael E | Feldman, Robert ATipo de material: ArtículoArtículoIdioma: Inglés Series no.1Detalles de publicación: Estados Unidos-US : Society for American Archaeology, 1983Descripción: 375-389 páginas: ilustraciones blanco y negroTema(s): ARQUEOLOGIA | GEOLOGIA En: Society for American Archaeology American Antiquity. Journal of the Society for American ArchaeologyResumen: Antithetical premises of a static versus dynamic Andean landscape, inoperable canal gradients must be explained by social parameters such as poor surveying or construction techniques. The paradigm of Plate Tectonics and evidence of ongoing crustal convergence support an anternative premise of continuos, gradual landscape alteration and ground slope change. This premise provides a physical explanation for why abandoned canals often exhibit uphill gradients and ancient monuments are frequently not level. However, this premise also requires that complex methods in the engineering analysis of slope altered structures be made explicit.Existencias: 1
Etiquetas de esta biblioteca: No hay etiquetas de esta biblioteca para este título. Ingresar para agregar etiquetas.
    Valoración media: 0.0 (0 votos)
Tipo de ítem Biblioteca actual Colección Signatura Info Vol Copia número Estado Fecha de vencimiento Código de barras
Publicaciones Periodicas Extranjeras Publicaciones Periodicas Extranjeras Museo Nacional de Etnografía y Folklore
Centro de procesamiento
Revistas E/ AMER-ANT/ vol.48(2)/ Apr.1983 no. 2 1 Disponible HEMREV012694

Antithetical premises of a static versus dynamic Andean landscape, inoperable canal gradients must be explained by social parameters such as poor surveying or construction techniques. The paradigm of Plate Tectonics and evidence of ongoing crustal convergence support an anternative premise of continuos, gradual landscape alteration and ground slope change. This premise provides a physical explanation for why abandoned canals often exhibit uphill gradients and ancient monuments are frequently not level. However, this premise also requires that complex methods in the engineering analysis of slope altered structures be made explicit.

No hay comentarios en este titulo.

para colocar un comentario.

Haga clic en una imagen para verla en el visor de imágenes


MUSEO NACIONAL DE ETNOGRAFÍA Y FOLKLORE        
La Paz N° 916 Calle Ingavi (591-2) 2408640- 2406030 Fax (591-2) 2406642
E-mail: musef@musef.org.bo   Casilla postal 5817   www.musef.org.bo
Sucre 74 calle España (591-4) 6455293
Pie de página
© Copyright 2023 · MUSEF