1. O RELEVO ESPAÑOL DIVERSIDADE XEOMORFOLÓXICA
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1 1. O RELEVO ESPAÑOL DIVERSIDADE XEOMORFOLÓXICA
2 O relevo español e a súa diversidade xeomorfolóxica DEFINICIÓNS Aluvión / Foz / Litosfera / Meseta / Penechaira / Somonte / Tectónica de placas / Esteiro / Ría / Tómbolo TEMA: Formación e evolución xeomorfolóxica da Península Ibérica e das Illas Canarias e Baleares. Tipos de unidades morfoestruturais. PRÁCTICOS: - Comentario guiado dun fragmento de mapa topográfico. - Comentario de perfís topográficos: N-S - Mapa litolóxico de España. - Debuxos e gráficos con tipos de modelado: granítico, cárstico, glaciar ou volcánico.
3 O espazo xeográfico español 1.1 Características 1.2 Estrutura da Terra e tectónica de placas 1.3 Evolución xeolóxica da Península 1.4 Tipos de unidades morfoestructurais 1.5 Litoloxía e modelaxe 1.6 Principais unidades do relevo
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8 1.2 Estrutura da Terra e tectónica de placas
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11 POZO SUPERPROFUNDO DE KOLA
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16 Animación: placas diverxentes e converxentes
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18 1.1 Espazo xeográfico español Composición: España peninsular Arquipélagos Ceuta e Melilla Trazos principais Posición de encrucillada Forma maciza Elevada altitude media Disposición periférica do relevo Diversidade de paisaxes
19 1.3 Evolución xeolóxica da Península Panxea 0/dpbg/2bch-ctma/tema7/moviePan gaea.swf
20 Tempos xeolóxicos
21 Evolución xeolóxica da Península: arcaica (ou precámbrica) e primaria (paleozoico)
22 Evolución xeolóxica da Península: principios do secundario
23 Evolución xeolóxica da Península: mediados do terciario
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25 Evolución xeolóxica da Península: glaciarismo no cuaternario
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27 Canal Roya. Pirineo, Huesca
28 Ibón e circo glaciar
29 Glaciarismo: erosión e circo (Gredos, Sistema Central)
30 Outro fenómeno do cuaternario: terrazas fluviais
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32 1.4 Tipos de unidades morfoestructurais ZÓCOLOS CORDILLEIRAS DE PREGAMENTO MACIZOS ANTIGOS CONCAS SEDIMENTARIAS
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35 1.4 Tipos de unidades morfoestructurais
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37 1.4 Tipos de unidades morfoestructurais ZÓCOLOS
38 A Meseta Penechaira zamorano-salmantina e cacereña
39 MACIZOS ANTIGOS
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41 CORDILLEIRAS DE PREGAMENTO
42 CONCAS SEDIMENTARIAS
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44 PRÁCTICOS - Comentario guiado dun fragmento de mapa topográfico. - Comentario de perfís topográficos: N-S - Mapa litolóxico de España. - Debuxos e gráficos con tipos de modelado: granítico, cárstico, glaciar ou volcánico.
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46 1.5 Litoloxía e tipos de modelaxe España silícea España calcaria España arxilosa España volcánica m/apps/viewer/index.html?appid=f0 6b b42b58a1bf36d28686f3 4
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48 Área silícea
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51 Alta montaña: galaios e pedregais (canchales)
52 Área calcaria
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56 Dolina
57 Área arxilosa
58 Campiñas e badlands
59 Área volcánica
60 Conos e caldeiras
61 Malpaís
62 Dique e roque
63 Barranco
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65 Relevo causado pola erosión diferencial A. HORIZONTAL B. EN COSTA C. PREGADO
66 A. HORIZONTAL / ACLINAL
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68 B. EN COSTA / MONOCLINAL
69 C. PREGADO: apalachense Montes de Toledo: as Villuercas
70 Relevo de crestas e vales paralelos, aliñados
71 C. PREGADO: xurásico
72 DEFINICIÓNS Aluvión / Foz / Litosfera / Meseta / Penechaira / Somonte / Tectónica de placas / Esteiro / Ría / Tómbolo
73 Tectónica de placas
74 Litosfera
75 Meseta
76 Penechaira
77 Somonte
78 Aluvión
79 Foz
80 Esteiro
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82 Ría
83 Tómbolo
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85 1.6 As principais unidades de relevo
86 1.6.1 A Meseta Penechaira zamorano-salmantina e cacereña
87 1.6.2 Concas interiores da Meseta
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90 1.6.3 Serras interiores da Meseta a) Antigo zócolo b) Serras interiores i) SISTEMA CENTRAL ii) MONTES DE TOLEDO Macizos antigos de rochas primarias, silíceas. Cumios erosionados. Serras destacadas do sistema Central: Somosierra, Guadarrama, Gredos, Gata Serra destacada dos Montes de Toledo (máis baixos): Guadalupe. c) Concas interiores
91 Montes de Toledo. Relevo apalachense
92 1.6.3 Rebordos montañosos da Meseta a) Macizo Galaico-Leonés b) Cordilleira Cantábrica c) Sistema Ibérico d) Serra Morena Macizo antigo, materiais paleozoicos, silíceos (granito, gneis, lousa). Sistema de serras moi complexo pola falta de alineacións definidas e pola acción erosiva dos ríos. Serras: Caurel, Ancares, Xurés, Queixa, San Mamede...
93 1.6.3 Rebordos montañosos da Meseta a) Macizo Galaico-Leonés b) Cordilleira Cantábrica c) Sistema Ibérico d) Serra Morena Cordilleira de pregamento intermedia. Divídese en dous sectores: 1. Leste: macizo Asturiano. Materiais paleozoicos (lousas, cuarcitas, calcarias). Maiores alturas nos Picos de Europa. 2. Oeste: Montaña Cantábrica. Materiais secundarios (calcarias)
94 Unidades morfoestructurais: rebordos montañosos da Meseta a) Macizo Galaico-Leonés b) Cordilleira Cantábrica c) Sistema Ibérico d) Serra Morena Cordilleira de pregamento intermedia. Materiais principalmente calcarios, pero tamén sectores paleozoicos (zócolo) e arxilosos (fosas). Estrutura en dúas partes: 1. Terzo norte: maiores alturas (Moncayo, Picos de Urbión e Demanda, paleozoica) 2. Sueste: bifúrcase en dúas ramas a. Rama castelá: Albarracín, serra de Cuenca b. Fosa de Calatayud c. Rama aragonesa: Javalambre
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96 Unidades morfoestructurais: rebordos montañosos da Meseta a) Macizo Galaico-Leonés b) Cordilleira Cantábrica c) Sistema Ibérico d) Serra Morena Gran flexión fracturada en moitos puntos. Formouse na terciaria pola presión desde o sur (formación das Béticas). Rochas paleozoicas de cor escura. Serras de Madrona, Pedroches e Aracena.
97 Unidades morfoestructurais: depresións exteriores da Meseta a) Depresión do Ebro b) Depresión do Guadalquivir Depresión do Guadalquivir: paralela as cordilleiras Béticas. Estivo primeiro aberta ao mar, pasou a convertirse nun lago litoral e despois, en marismas. Encheuse con arxilas, calcarias e margas mariñas. Relevo: campiñas e mesas.
98 Unidades morfoestructurais: depresións exteriores da Meseta a) Depresión do Ebro b) Depresión do Guadalquivir Ambas son depresións prealpinas formadas na era terciaria, recheas con sedimentos terciarios e cuaternarios. Depresión do Ebro: primeiro ocupada polo mar, pechouse e se transformou nun gran lago ata finais do terciario, cando o Ebro se abre paso. Relevos: somontano, mallos, mesas e badlands.
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100 Derrubios de piedemonte
101 Unidades morfoestructurais: cordilleiras exteriores a) Pireneos b) Montes Vascos c) Cordilleira Costeira-catalá d) Béticas Formáronse na oroxenia alpina polo pregamento de sedimentos secundarios acumulados nas fosas coeánicas. Predominio de calcáreas. Pireneos: estrutura a) Eixe ou Pireneo axial: materiais paleozoicos do antigo macizo. Relevo abrupto e grandes alturas b) Prepireneos: ao sur do eixe. Formados por pregamento na terciaria. Calcareas. Dúas aliñacións: serras interiores e exteriores c) Depresión media: separa as serras prepirenaicas. Margas.
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104 Unidades morfoestructurais: cordilleiras exteriores a) Pireneos b) Montes Vascos c) Cordilleira Costeira-catalá d) Béticas Na súa maior parte, prolongan os Prepirineos (materiais calcáreos, altitude moderada, formas suaves) Máximas alturas: Aralar e Pena Gorbea
105 Unidades morfoestructurais: cordilleiras exteriores a) Pireneos b) Montes Vascos c) Cordilleira Costeira-catalá d) Béticas Transformación da zona oriental dos Pireneos. Materiais: - Metade norte: paleozoicos - Metade sur: calcarios Estrutura: - Cordilleira. litoral: aliñación paralela á costa, de menor altura (Altos do Garraf) - Depresión prelitoral (materiais terciarios e cuaternarios) - Cordilleira prelitoral: aliñación interior, máis alta (Montserrat, Montseny)
106 - Cordilleira Penibética: bordea a costa. Rexuvenecemento na terciaraia do antigo macizo Bético-Rifeño. Materiais paleozoicos. Relevo moi elevado: Serra Nevada. - Depresión intrabética: entre as aliñacións. Fragmentada en depresións pequenas. Materiais terciarios, relevo de badlands. - Cordilleira Subbética:: aliñación interior. Materiais secundarios depositados na fosa bética e pregados na oroxenia altpina. Margas e calcarias. Serras destacadas: Grazalema, Ubrique, Cazorla. Unidades morfoestructurais: cordilleiras exteriores a) Pireneos b) Montes Vascos c) Cordilleira Costeira-catalá d) Béticas Estrutura:
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108 Relevo costeiro: as costas atlánticas a) Costa Cantábrica b) Rías galegas c) Costa andaluza
109 Acantilados, arcos e farallóns
110 Rasas
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112 Relevo costeiro: as costas atlánticas a) Costa Cantábrica b) Rías galegas c) Costa andaluza
113 Rías galegas
114 Relevo costeiro: as costas atlánticas a) Costa Cantábrica b) Rías galegas c) Costa andaluza
115 Marismas
116 Frechas/dunas
117 Relevo costeiro: as costas mediterráneas a) Costa Penibética: b) Costa Levantina c) Costa Catalá
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119 Relevo costeiro: as costas mediterráneas
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124 Liña de falla
125 Relevo de Galicia Costa Rías e franxa litoral Fractura Carballo-Tui Dorsal: Faro Faladoira Cova da Serpe Meseta central Penechaira de Chantada Fosas de Monforte, Sarria, Verín... Serras orientais e surorientais Lourenzá, Meira, Cabrera, Segundera Ancares, Courel
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