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Transcript of Pptresumen age
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CLASIFICACIÓN DE LOS AGENTES GEOLÓGICOS
Evaporación
condensación precipitacionesEnergía solar
Gravedad
1
2
3
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5
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EL CICLO DEL AGUA
Glaciares Ríos Aguas subterránea
s
Viento oleaje
Calentamiento de la Tierra
EL SOL
EROSIÓN-TRANSPORTE-SEDIMENTACIÓN
MODELADO DE LA SUPERFICIE TERRESTRE
A. Salvajes
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LOS RÍOS
Tramo alto
Tramo medio
Tramo bajo
Son cursos de agua permanente que discurre por un cauce (sitio) fijo y que, generalmente, desemboca en el mar o en otro río.
VOLVER
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Acción geológica de los ríos
Domina la erosión de fondo
Domina el transporte y erosión lateral
Domina la sedimentación
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Tramo alto
Tramo alto
Erosión de fondo
Valle en forma de VDesfiladero
En terrenos blandosEn terrenos duros
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Tramo medio
Erosión lateral
Valle en forma de artesa
Deposita o sedimenta
Orilla convexaOrilla cóncava
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Valle en artesa
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Otras formas de relieve debido a los ríos
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Tramo inferior
Sedimentos
Llanura de inundación
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Llanura de inundación
Llanura de inundación
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Penillanura
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Delta
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AGUAS SALVAJES
Río
Las aguas salvajes son aquellas que discurren ladera abajo sin cauce fijo hasta el fondo de los valles donde se reúnen para formar torrentes o arroyos.
Torrente o arroyo
Aguas salvajes
Aguas salvajes
VOLVER
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Acción de las aguas salvajes
Cárcavas/barrancos/ramblas Chimeneas de hadas
En terrenos blandos originan En terrenos heterogéneos originan
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Cárcavas/barrancos y ramblas
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Chimeneas de hada
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Chimeneas de hada
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Partes de un torrente o arroyoCuenca de recepción
Canal de desagüe
Cono de deyección o abanico aluvial
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EL VIENTO
Erosión
Abrasión
BBBB
BBBB
A
Deflación
Roca en seta
Reg
Actúa en zonas costeras y en los desiertos
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DeflaciónEl viento arranca y levanta partículas finas que transporta en suspensión. Da lugar a campos de piedras llamados regs.
Abrasión Las partículas de arena desgasta o lija las rocas con las que choca. Da lugar a rocas en seta.
Erosión del viento
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transporte
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Sedimentación
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Loess
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EL MAR
Plataforma de abrasión
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Tómbolo Playa
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LOS GLACIARES
Los GLACIARES se dan en
Zonas polares Zonas de alta montaña
Casquetes polares Glaciares alpinos
Circo Lengua Zona de ablación o fusión
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Glaciares alpinos
Circo
Lengua
Zona de ablación o fusiónVOLVER
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Erosión
Erosión de fondo Erosión lateral
Valle en forma de Uibón
La erosión de los glaciares origina valles en forma de U y sobreexcavaciones que originan lagos llamados ibones
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Transporte
Morrena central
Morrena lateral
Morrena frontal
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M. lateral M. centrales
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Sedimentación
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Formas de modelado
1
2
3
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LAS AGUAS SUBTERRÁNEAS
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Modelado kárstico
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VOLVER
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IES Miguel Crespo2015
Este montaje es una adaptación de otros encontrados en la web. Nuestro agradecimiento al profesorado que
ha recopilado estas diapositivas y que nos ha permitido, de forma desinteresada y desconocida, su
adaptación a nuestras clases.