¿De que parte geológica es la Gallina de Palo?

Biology

1 answer:

Karo-lina-s [1.5K]2 years ago

6 0

Answer:

Nombrado como la formación media del grupo La Plata para Todilto Park, T20N, R20W, McKinley Co, NM en la cuenca de San Juan. No se ha designado ninguna localidad tipo. Tapas de piedra arenisca Wingate. Es más antiguo que la piedra arenisca de Navajo. Varía de 2 a 200 pies de espesor. Dos secciones medidas. Mapa geológico. Mapeado en Apache contiguo y Navajo Cos, AZ en la cuenca de Black Mesa. Consiste en piedra caliza azul grisácea, densa y resistente cubierta y sustentada por arenisca calcárea blanca en una localidad de Apache Co, y de conglomerado de piedra caliza separada por lutitas calcáreas y lechos de arenisca en Navajo Co. El contacto de Navajo-Todilto suele conformarse. Fragmentos bien gastados de sílex negro, gris y blanco que se encuentran cerca de la parte superior en cantidades suficientes para formar bandas irregulares incrustadas en la piedra caliza. La parte media de La Plata (¿Todilto?) Se engrosa hacia el norte y se encuentran cambios en esa más arenisca y pizarra. Huellas de dinosaurios encontradas en dos localidades. Asignado a Jurassic.

Explanation:

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¿De que parte geológica es la Gallina de Palo?​

¿De que parte geológica es la Gallina de Palo?