pedro farias has made this presentation and has it rights reserved
TRANSCRIPT
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Universidad de Oviedo Pedro Farias Arquer
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El origen del relieve: las cordilleras
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Mosaico de placas litosféricas
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Velocidad y dirección de movimiento de las placas
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Dentro de 50 millones de años
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Edades de las rocas de los fondos oceánicos
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Apertura del Golfo de Vizcaya y elevación de los PirineosTriásico-Jurásico-Cretácico (200-55 m.a.)
Reproducido de: Geología de Asturias (1996)
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Apertura del Golfo de Vizcaya:
Estructura del margen continental pasivo cantábrico
Eoceno inferior (55 m.a.)
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Empuje de la placa africana
contra la placa ibérica
Eoceno superior (35 m.a.)
Boillot y Mallod [1988].
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Levantamiento de la Cordillera Cantábrica
(55-10 M.a.)
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El Relieve Alpino de la Cordillera Cantábrica(55-10 m.a.)
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La Cordillera Cantábrica emerge desde la planicie formada por los materiales detríticos procedentes de su propia erosión.
Fotografía tomada desde el Area de Servicio de Rioseco de Tapia, en la autopista A-66
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Actividad sísmica desde 1960
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FACTORES DEL MODELADO DEL RELIEVE Y DEL PAISAJE
• Geología del sustratoLitologíaEstructura
• Clima
• Actividades humanas
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Geología y Paisaje en Asturias
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El Clima como factor del Relieve y del Paisaje
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Lenguas glaciares del glaciar de “La Mer de Glace”.
Macizo del Mont Blanc. Francia
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Formas de erosión glaciar en la Cordillera Cantábrica: Circo glaciar del Lago del Valle (Somiedo)
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Formas de erosión glaciar en la Cordillera Cantábrica: Circo glaciar de Cembaviella (Peña Santa de Enol, Picos de Europa)
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Formas de erosión glaciar en la Cordillera Cantábrica: Valle glaciar de Valle del Lago (Somiedo)
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Formas de depósito glaciar en la Cordillera Cantábrica: Morrena de Casares de Arbás (León)
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Formas de erosión glaciar en la Cordillera Cantábrica: Valle glaciar de la Vega de Enol (Picos de Europa)
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Paisaje de dolinas en las calizas de la Sierra de La Sobia (Quirós)
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Los ríos de Asturias
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El sustrato como condicionante de la red hidrográfica
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¿Cómo se encajan
los ríos?
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Deslizamientos
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Explotación de oro de Boinás
2007
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