ARCHAEOLOGICAL SITES

The Geopark Viñales area contains an extensive and valuable archaeological heritage, where sites of historical, cultural, and natural relevance converge. In our inventory, over eighty places testify to the rich legacy of past communities.

Type Locality Ancón Formation

Schistose and clayey limestones, marls, calcareous breccias with fragments of limestones and cherts, well-stratified, ranging from violet to pink.

Type Locality Pan de Azúcar Member

Stratified limestones, shelly, coquinal, and silicified, typical with the microfossil Conicospirillina basiliensis, and ammonites and fragments of other microfossils can be observed.

Hypostratotype 2. San Cayetano Formation

Deltaic sediments, composed in this section of fine-grained shales and sandstones, laminated claystones with symmetrical ripples in some parts of the outcrop.

Type Locality, San Vicente Member

Bluish-gray limestones, hard, massive or very thickly stratified, where fragments of poorly preserved macrofossils can be observed, with significant development of conical karst.

La Legua Breccia Section

The section exhibits a cut of calcareous breccias composed of fragments of limestones and cherts. Toward the top of the section, the fine fraction predominates.

Type Locality, Zacarías Member

Clay schists ranging from gray to black and reddish on the surface due to weathering. Ammonites of the genera Ochetoceras, Vinalesphinctes, Perisphinctes, and Discosphinctes can be observed.

Type Locality, Jagua Vieja Member

Dark, almost black micrites, strongly bituminous, stratified, brown-gray schists with calcareous concretions, “cheeses” with ammonites, fish, reptiles, and other fossils that are indices of the Upper Jurassic (Middle Oxfordian).

Type Locality, Tumbadero Member

Micrites and calcilutites with intercalations of dark chert, with calpionellid microfauna, assigning it an age of Upper Jurassic (Tithonian)-Lower Cretaceous (Berriasian).

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