{"id":7518,"date":"2023-08-07T15:18:07","date_gmt":"2023-08-07T13:18:07","guid":{"rendered":"https:\/\/geoparquemolina-altotajo.com\/?page_id=7518"},"modified":"2023-08-10T15:20:19","modified_gmt":"2023-08-10T13:20:19","slug":"galeria-de-geodiversidad","status":"publish","type":"page","link":"https:\/\/geoparquemolina-altotajo.com\/en\/galeria-de-geodiversidad\/","title":{"rendered":"Geodiversity Gallery"},"content":{"rendered":"
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Gallery of
Geodiversity<\/h1> <\/div>\r\n \n\n\n
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The extensive geodiversity is one of the most notable features of this geopark, we have numerous deposits corresponding to a wide range of geological eras, some very young such as the numerous Quaternary tuffs, rocks affected by the Alpine orogeny such as conglomerates, sands, marls and clays; from prolific periods in prehistoric animals such as the Jurassic and much older remains corresponding to the primary era.<\/p>\n<\/div>\n\n\n\n

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Quaternary<\/strong><\/h2>\n\n\n\n
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Tuffaceous Formations of the San Pedro Bridge<\/figcaption><\/figure>\n\n\n\n
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Tuffaceous building in formation at La Aguaspe\u00f1a, Czech<\/figcaption><\/figure>\n\n\n\n
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Quaternary tuffaceous formations. Mesa River Valley<\/figcaption><\/figure>\n<\/figure>\n<\/div><\/div>\n\n\n\n
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 Tertiary or Cenozoic<\/strong><\/h2>\n\n\n\n
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Lacustrine sediments from the Tertiary period in Molina de Arag\u00f3n <\/figcaption><\/figure>\n\n\n\n
\"Sedimentos<\/a>
Tertiary sediments from Zaorejas<\/figcaption><\/figure>\n\n\n\n
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Progressive unconformity in Alustante\n<\/figcaption><\/figure>\n<\/figure>\n<\/div><\/div>\n\n\n\n
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Secondary or<\/strong> Mesozoic<\/strong><\/h2>\n\n\n\n

Cretaceous<\/strong><\/em><\/h2>\n\n\n\n
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Limestone rocks from the Cretaceous period of the Enchanted City of Hoya del Espino de Pe\u00f1al\u00e9n.<\/figcaption><\/figure>\n\n\n\n
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Cretaceous limestones in Peralejos de las Truchas<\/figcaption><\/figure>\n\n\n\n
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Sands from the Cretaceous period, C\u00e1rcava de Peralejos de las Truchas\n<\/figcaption><\/figure>\n<\/figure>\n<\/div><\/div>\n\n\n\n
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Secondary or<\/strong> Mesozoic<\/strong><\/h2>\n\n\n\n

Jurassic<\/strong><\/em><\/h2>\n\n\n\n
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Fuentelsaz stratotype. Alternation of limestone and marl from the Jurassic in Fuentelsaz.<\/figcaption><\/figure>\n\n\n\n
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Bechified limestones from the Lower Jurassic in the vicinity of Molina de Arag\u00f3n<\/figcaption><\/figure>\n\n\n\n
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Sands from the Cretaceous period, C\u00e1rcava de Peralejos de las Truchas\n<\/figcaption><\/figure>\n\n\n\n
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Jurassic Limestone in Carved Caves\n<\/figcaption><\/figure>\n\n\n\n
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Jurassic marls in Pe\u00f1al\u00e9n.\n<\/figcaption><\/figure>\n<\/figure>\n<\/div><\/div>\n\n\n\n
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Secondary or Mesozoic<\/strong><\/h2>\n\n\n\n

Triassic<\/strong><\/em><\/h2>\n\n\n\n
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Intercalation of conglomerates and sandstones from the Lower Triassic. Barranco de la Hoz del R\u00edo Gallo.<\/figcaption><\/figure>\n\n\n\n
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Detail of sandstones from the Lower Triassic. Check<\/figcaption><\/figure>\n\n\n\n
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Clays and sandstones from the Lower Triassic \u2013 Middle Triassic transition. Rooster Rillo\n<\/figcaption><\/figure>\n\n\n\n
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Limestone of marine origin from the Middle Triassic. Rooster Rillo<\/figcaption><\/figure>\n\n\n\n
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Lacustrine sediments, clays with salts, from the Upper Triassic. Cobeta<\/figcaption><\/figure>\n\n\n\n
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Sandstones from the Lower Triassic. Rooster Rillo<\/figcaption><\/figure>\n<\/figure>\n<\/div><\/div>\n\n\n\n
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Primary or Paleozoic<\/strong><\/h2>\n\n\n\n

Permian<\/strong><\/em><\/h2>\n\n\n\n
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Clays from the Upper Permian period. Barranco de la Hoz of the Gallo River<\/figcaption><\/figure>\n\n\n\n
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Clays with sandstones and limestones. Lacustrine sediments from the Lower Permian period. Rooster Rillo<\/figcaption><\/figure>\n\n\n\n
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Rhyolitic volcanic rocks, Lower Permian period. Rooster Rillo.<\/figcaption><\/figure>\n\n\n\n
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Dacitic type volcanic rocks with columnar disjunction. Corks<\/figcaption><\/figure>\n\n\n\n
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Pe\u00f1a del Huevo, Tormo in volcanic rocks, Lower Permian period. Rooster Rillo.<\/figcaption><\/figure>\n<\/figure>\n<\/div><\/div>\n\n\n\n
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Primary or Paleozoic<\/strong><\/h2>\n\n\n\n

Silurian and Ordovician<\/strong><\/em><\/h2>\n\n\n\n
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Silurian black slates. Czech<\/figcaption><\/figure>\n\n\n\n
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Cretaceous limestones in Peralejos de las Truchas<\/figcaption><\/figure>\n\n\n\n
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Dacitic type volcanic rocks with columnar disjunction. Corks\n<\/figcaption><\/figure>\n\n\n
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\"Arenas<\/a>
Limestone from the Ordovician period. Setiles Mines<\/figcaption><\/figure>\n<\/div><\/figure>\n<\/div><\/div>\n\n\n\n
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