Relieve Power Point Completo
Transcript of Relieve Power Point Completo
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EL RELIEVE TERRESTRE
RELIEVE CONTINENTAL, COSTERO Y OCEÁNICO
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La Tierra se divide en tres grandes capas concéntricas:La cortezacorteza es la capa más externa. Es una capa sólida y delgada que ocupa el 1% del planeta.El mantomanto es la capa intermedia y representa le 85% del planeta. Parte de los materiales del manto están fundidos y forma el magma.El núcleonúcleo es la capa más profunda y esta formada por materiales solidos y líquidos que soportan grandes temperaturas. Supone el 14% del volumen del planeta
LA ESTRUCTURA DE LA TIERRA
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LA SUPERFICIE TERRESTRE: CONTINENTES Y OCÉANOS
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Actividades
1. Dibuja o pega en tu cuaderno un mapamundi mudo y escribe en rojo el nombre de los continentes; y en azul, el de los océanos.
2. Escribe el nombre de cinco países que tengan costas en cada continente.
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LAS PLACAS TECTÓNICASLa corteza aparece fracturada en distintas partes denominadas placas tectónicas. Estas placas pueden contener tanto tierra emergida como océanos y se hallan en constante movimiento.
Videos 1A-B y 2A-B-C
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TEORÍA DE LA DERIVA DE LOS CONTINENTESHace 225 millones de años todas las tierras emergidas estaban unidas formando un supercontiente llamado Pangea, rodeado por un gran océano llamado Pantalasa. Con el paso del tiempo se este supercontinente se fue fracturando y las diversas partes separándose, hasta situarse en el lugar que ocupan en la actualidad y formar los continentes que hoy conocemos.
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Rift en IslandiaSeparación de las placas Euroasiática y Norteamericana
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EL RELIEVE CONTINENTAL
Formado por las fuerzas internas de la Tierra y
modelado por los agentes externos
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PRINCIPALES FORMAS DEL RELIEVE TERRESTRE
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MONTAÑA- Gran elevación del terreno
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SIERRA- Pequeña agrupación de montañas
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CORDILLERA- Agrupación de montañas muy extensa.
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CERRO O COLINA- Pequeña elevación del terreno, menor que una montaña.
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LLANURA- Amplia extensión de terreno, llana o ligeramente ondulada
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MESETA- Superficie de terreno llana, pero que está elevada respecto al terreno que la rodea.
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VALLE- Área de terreno hundida y rodeada de montañas. Casi siempre, por el fondo del valle transcurre un río.
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Actividades
3. Completa la siguiente tabla
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Nacimiento del Ebro
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Cuenca hidrográfica
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Garganta Barranco
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Cañón del río Lobos
Cañón del río Ebro
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Delta del Ebro
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Estuario del Miño
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Actividades
4. Completa la siguiente tabla:
5. Escribe el nombre de los principales ríos españoles, dónde nacen y dónde desembocan y cuál es su longitud.
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LAS AGUAS CONTINENTALES: RÍOS, GLACIARES Y AGUAS
SUBTERRÁNEAS
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Partes de un glaciar
http://www.youtube.com/watch?v=_DWl4AxfRto
Paseo por el glaciar Perito Moreno- YouTube
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Circo glaciar
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Circo glaciar de Fuente Dé- Cantabria
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B
A
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LAS AGUAS SUBTERRÁNEAS
En las zonas de rocas permeables, el agua de la lluvia, ríos y arroyos, se filtra hacia el interior de la tierra y , al encontrarse con una capa de rocas impermeables , se forman depósitos subterráneos de agua llamados acuíferos.
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En las zonas de rocas calizas, las aguas subterráneas disuelven la roca y crean un tipo de relieve llamado kárstico, que se caracteriza por la formación en el exterior de simas, cuevas, dolinas... , y en el interior de la tierra, de galerías subterráneas, estalactitas y estalagmitas, lagos subterráneos…
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Dolinas
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Simas
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Cueva
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Estalactitas y estalagmitas
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Lagos subterráneos
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LAGOS Y MARES INTERIORES
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LAGO – Acumulación de agua en un terreno hundido
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LAGUNA – Lago de pequeño tamaño
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MAR INTERIOR- Lago de gran tamaño y con el agua salada
Mar Caspio
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Actividades
5. Completa la siguiente tabla:
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EL RELIEVE costero
Formado por la acción del mar sobre las costas de los
continentes
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PLAYA- Forma del relieve costero creada por la acumulación de arenas y gravas.
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ACANTILADO- Pared rocosa, alta y escarpada, que da al mar.
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CABO- Zona de costa que se adentra en el mar.
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GOLFO- Entrada del mar en la tierra.
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BAHÍA- Golfo de pequeño tamaño.
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ALBUFERA- Laguna litoral de agua salada, separada del mar por un cordón de arena.
Repasamos el relieve continental: VIDEO 3
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ISLA- Porción de tierra rodeada de agua por todos sus lados.ARCHIPIÉLAGO- Conjunto de islas
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PENÍNSULA- Porción de tierra rodeada de agua por todos sus lados, menos por uno, llamado istmo.
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EL RELIEVE oceánico
ES EL RELIEVE TERRESTRE SUMERGIDO BAJO LAS AGUAS
DE LOS OCÉANOS
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PLATAFORMA CONTINENTAL- Prolongación de los continentes bajo el mar, que constituye una meseta submarina y alcanza los 200 metros de profundidad.TALUD CONTINENTAL- Es la inclinación de la plataforma continental hasta la llanura abisal; puede llegar a tener hasta 3600 metros de profundidad.
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LLANURA ABISAL- Gran extensión de tierra situada en el fondo del océano, a unos 5500 metro de profundidad; en ella se localizan las fosas y las dorsales oceánicas.
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DORSAL OCEÁNICA- Cordillera submarina que recorre la llanura abisal y que puede salir a la superficie en algún punto, dando lugar a islas.
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FOSA OCEÁNICA- Profunda cavidad situada en los fondos de los océanos, pudiendo alcanzar hasta los 11.000 metros de profundidad.
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LOS RIESGOS NATURALES
TERREMOTOS Y VOLCANES
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http://www.youtube.com/watch?NR=1&feature=fvwp&v=duoS7hwJlrU
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http://www.youtube.com/watch?v=sy6NY30rn_g&feature=related
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MAREMOTO O TERREMOTO SUBMARINO
OLA GIGANTESCA O TSUNAMI
(CONSECUENCIA DEL MAREMOTO)
MAREMOTO Y TSUNAMI(NO ES LO MISMO)
http://www.youtube.com/watch?v=fdwFWSWNt6o&feature=related
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Tsunami en Talilandia, 2004 http://www.youtube.com/watch?v=fdwFWSWNt6o&feature=related
http://www.youtube.com/watch?v=L3Pe8vFEKJg&feature=related – TERREMOTO Y TSUNAMI JAPÓN 2011 aprox. Minuto 19
Cómo se formó el terremoto y el tsunami de Japón, 2011http://www.youtube.com/watch?v=L3Pe8vFEKJg&feature=related
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Tsunami sobre Japón, 2011.
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Etna (Sicilia). Erupción en mayo de 2011
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Volcanes en la comarca de la Garrotxa- Olot (Gerona)
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Laguna volcánica de Cervera – Campo de Calatrava (Ciudad Real)
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Actividades
6.Busca información en Internet sobre el terremoto en Lorca (Murcia) y el terremoto y posterior tsunami en Japón, y elabora un breve trabajo sobre uno de ellos.
Datos que deben aparecer:- Fecha en que se produjeron- Causa del fenómeno- Magnitud- Consecuencias (materiales, personales…)- Movimientos sociales de ayuda a los damnificados.- Lorca y Japón, hoy.
Uno o dos trabajos de cada uno de ellos será expuesto en la clase por su autor/a.