Distribution and historic evolution of the fluvial terraces from Santa Teresa valley Guanajuato

The present work reports the fluvial terraces originated during historical floods throughout the fluvial plain of the Guanajuato river. Six different terraces levels were identified and mapped that correspond to T1 (1,8 m), T2 (3,0 m), T3 (4,2 m), T4 (5,2 m), T5 (6,0 m), T6 (+6,8 m). A sequence anal...

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Detalles Bibliográficos
Autores: Miranda-Avilés, Raúl, Puy-Alquiza, María Jesús, Navarre-Barrera, Yann Rene, Navarro-Barrera, Ricardo
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2012
País:México
Institución:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
Repositorio:Investigaciones Geográficas
Idioma:español
OAI Identifier:oai:ojs.pkp.sfu.ca:article/29912
Acceso en línea:https://www.investigacionesgeograficas.unam.mx/index.php/rig/article/view/29912
Access Level:acceso abierto
Palabra clave:Fluvial terraces
Guanajuato
anthropogenic sediments
fluvial terraces evolution
Mesa Central Mexico
Terrazas fluviales
sedimentos antropogénicos
evolución de terrazas fluviales
Mesa Central México
Río Guanajuato
Descripción
Sumario:The present work reports the fluvial terraces originated during historical floods throughout the fluvial plain of the Guanajuato river. Six different terraces levels were identified and mapped that correspond to T1 (1,8 m), T2 (3,0 m), T3 (4,2 m), T4 (5,2 m), T5 (6,0 m), T6 (+6,8 m). A sequence analysis of terraces was supported by 2 isotopic C14 dating. The T1 corresponds to the present floodplain, the T2, T3, T4 was formed during periods of extreme floods, between 10 to 100 years in relation to the present. The T5 morphology corresponds to 1905 historical flood. The T6 deposit was followed by a degradation process that was interrupted by a period of increasing sediment budget between 1660 +/-40 to 1905 (T5), during the great mining activity of the Guanajuato Mining District. After 1905 the sediments budget to the Guanajuato River, diminishes substantially, generating a gradual degradation by pulses conforming the T4 to T1 terraces.