As catedrais c
Transcript of As catedrais c
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Fotos cedidas por Adela Leiro
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Ten unha lonxitude media de 1.500 metros, aínda que coa marea alta pode quedar reducida a 320 m, xa que está illada en varias porcións consideradas ás veces independentes. Ten un largo moi variable debido a que a preamar tapa toda a area en moitas partes dela, mentres noutras a baixa se descobre ata 100 m.
A praia é aberta con area branca e fina, bañada por unha ondada moderada.
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O maior interese do espazo reside nos cantís traballados polo mar nos xistos e areiscas da rasa de Ribadeo. A intensa erosión e a disposición dos estratos dá lugar a formacións moi curiosas e espectaculares: arcos, furnas, illotes, columnas, buratos (bocas do inferno)...
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A rasa de Ribadeo forma parte da rasa Cantábrica que se extende desde San Vicente de la Barquera (Cantabria) ata Burela. É unha superficie elevada sobre o nivel da auga, moi chan, cunha pendente suave cara ao mar que se corta bruscamente terra adentro. Estas formacións tiveron a súa orixe nun proceso tectónico de fallas e levantamento da costa no final da Oroxenia Hercínica.
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O que máis resalta desta praia son os 300 metros de cantís furados pola marea que forman uns arcos semellantes aos das catedrais góticas, e que só se poden ver coa marea baixa.
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14disposición horizontal das rochas
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16base do cantl puído polo mar
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17lousa verde
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20cuarcitas, mais resistentes que os xistos e as lousas
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22anacos le lousas e cuarcitas redondeadas pola forza das ondas
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PROTECCIÓN:LIC (Lugar de Importancia ComunitariaMonumento Natural
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Entre os arcos das Catedrais agóchanse gran cantidade de especies de algas, moluscos, aves e vexetais.
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