Download - EL MAR. 3ºA-1
![Page 1: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/1.jpg)
EL MAR
Pedro Madueño Rodríguez 3º A Mayo 2009
![Page 2: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/2.jpg)
![Page 3: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/3.jpg)
EROSIÓN TRANSPORTE Y SEDIMENTACIÓN
![Page 4: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/4.jpg)
FORMAS LITORALES ORIGINADAS POR LA EROSIÓN
• ACANTILADOS
• PROMONTORIOS Y ENSENADAS
• ISLOTES COSTEROS
• ARCOS NATURALES
![Page 5: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/5.jpg)
ACANTILADOS
![Page 6: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/6.jpg)
![Page 7: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/7.jpg)
![Page 8: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/8.jpg)
DESPLOME DE ROCAS SOBRE LA PLATAFORMA DE ABRASIÓN
![Page 9: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/9.jpg)
![Page 10: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/10.jpg)
ACANTILADO CON VOLADURA EN EL CABO DE GATA
![Page 11: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/11.jpg)
![Page 12: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/12.jpg)
PROMONTORIOS Y ENSENADAS. CABO DE GATA
![Page 13: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/13.jpg)
![Page 14: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/14.jpg)
ISLOTES COSTEROS
![Page 15: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/15.jpg)
ARCOS NATURALES EN NORMANDÍA
![Page 16: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/16.jpg)
![Page 17: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/17.jpg)
FORMAS LITORLALES ORIGINADAS POR LA SEDIMENTACIÓN
• PLAYAS• DELTAS• BARRAS• TÓMBOLOS• ALBUFERAS Y MARISMAS
![Page 18: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/18.jpg)
PLAYAS
![Page 19: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/19.jpg)
EL MAR TRANSPORTA. Cuando el oleaje incide oblicuo a la costa los materiales avanzan en zigzag.
![Page 20: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/20.jpg)
![Page 21: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/21.jpg)
![Page 22: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/22.jpg)
![Page 23: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/23.jpg)
![Page 24: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/24.jpg)
DELTA DEL EBRO
![Page 25: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/25.jpg)
Barras de arena que se forman por las corrientes que circulan por el litoral. Barra de San Fernando y Cádiz
![Page 26: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/26.jpg)
Su formación a lo largo del tiempo
![Page 27: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/27.jpg)
Tómbolos son depósitos de arena que conectan un islote con la tierrra firme. Tómbolo de Peñíscola
![Page 28: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/28.jpg)
Los depósitos de arena acabarán conectando el islote al continente
![Page 29: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/29.jpg)
ALBUFERAS Y MARISMAS
![Page 30: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/30.jpg)
Marismas de Sancti Petri y Chiclana en la bahía de Cádiz
![Page 31: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/31.jpg)
Dunas costeras
![Page 32: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/32.jpg)
![Page 33: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/33.jpg)
DUNA
![Page 34: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/34.jpg)
Dirección del viento
Sotavento Barlovento
![Page 35: EL MAR. 3ºA-1](https://reader033.vdocuments.co/reader033/viewer/2022050921/55624eddd8b42a1b4b8b4b4a/html5/thumbnails/35.jpg)
Recursos empleados
• Fotos de álbum familiar, Cabo de Gata y Bahía de Cádiz.
• Dibujos explicativos del libro de texto “biología y geología, proyecto ecosfera.
• Vistas aéreas de “google earth”.
• Alguna foto de catálogos turísticos.