Système de grottes
Padre Nuestro Complex
A cluster of water-filled sinkholes and caverns just east of Bayahibe, used by the Taíno as a fresh-water source and today tapped to supply local hotels. Its Cueva de Chicho is visited on guided dives from Bayahibe.
The Padre Nuestro complex is a group of sinkholes and caverns holding fresh water in the karst of the south-east Dominican Republic, a short distance east of the coastal village of Bayahibe. Archaeologists from Indiana University list four named caverns in the complex: El Toro, Padre Nuestro, Cueva Brujo and Cueva de Chicho.
The caverns were sources of drinking and cooking water for Taíno communities before European contact. Divers working with the Indiana University team recovered pottery water bottles (potizas) from the Chicho pool, and petroglyphs have been recorded there. In 2002 the complex was reported to supply water to hotels in the Bayahibe-Dominicus resort area.
Cueva de Chicho is the cave offered for guided dives. A steep slope leads down into a large chamber lit by daylight from the entrance, ending at a clear fresh-water pool from which a flooded passage continues. A Bayahibe dive centre runs guided visits there.
Géologie
The complex lies in the limestone karst of the south-eastern Dominican Republic, a landscape of hundreds of caves and sinkholes formed by fresh water dissolving the bedrock.
Eau, courant et crues
Beeker and colleagues measured the Chicho pool as fresh water at a nearly constant 25 °C, with no measurable flow, little runoff and no oxygen-free layer.
Pourquoi c'est important
One of the two flooded cave sites used by Beeker, Conrad and Foster (2002) to compare everyday and ritual Taíno use of water-filled caverns: the Chicho finds are almost all simple water bottles, pointing to routine water collection.
Conditions
Clear fresh water at about 25 °C in the Chicho pool (measured for the 2002 study). The complex is a drinking-water source for local hotels.
Fourchettes indicatives issues de sources publiées, pas les conditions actuelles.
Historique du relevé topographique et de l'exploration
| 2002 | Beeker, Conrad and Foster published the archaeology of Cueva de Chicho and the Padre Nuestro complex in the Journal of Caribbean Archaeology. [1] |
Entrées et sites de plongée
Four named caverns (El Toro, Padre Nuestro, Cueva Brujo, Cueva de Chicho). Cueva de Chicho is the one offered for guided dives by a Bayahibe dive centre.
Pour s'orienter, pas pour naviguer. Les points creux sont approximatifs.
Chaque information de cette page, avec sa source (8)
| Information | Statut | Source |
|---|---|---|
| The Padre Nuestro complex is a series of water-containing sinkholes about 3.4 km east of Bayahibe, including El Toro, Padre Nuestro, Cueva Brujo and Cueva de Chicho.2002 paper. | Vérifié | [1] |
| The complex lies near, but not inside, the East National Park.Beeker et al. (2002) place it outside the park boundary; the dive centre (undated) and Wikipedia describe it as within the park, now named Parque Nacional Cotubanamá (renamed 2014). Boundaries may have changed. | Les sources se contredisent | [1] [2] [3] |
| The complex currently supplies water to hotels in the Bayahibe-Dominicus area.Stated in 2002; current status not checked. | Peut être obsolète | [1] |
| Thirty ceramic pieces, all from water-bottle forms, were recovered from Cueva de Chicho, indicating everyday water collection. | Vérifié | [1] |
| The Chicho pool is fresh water at a nearly constant 25 °C, with no measurable flow and no anoxic layer.Measured for the 2002 study. | Vérifié | [1] |
| Water temperature in the Chicho pool is about 25 °C.2002 measurement; typical, not current. | Vérifié | [1] |
| A Bayahibe dive centre runs guided dives in Cueva de Chicho and says park staff help with equipment on site.Provider claim, page checked 2026-10-14. | Signalé | [2] |
| Area coordinates are the GeoNames point for Padre Nuestro (18.376, -68.824), consistent with the 2002 paper's location 3.4 km east of Bayahibe.Area-level. | Signalé | [4] [1] |
Vérifié : indiqué par une source officielle ou primaire que nous avons consultée. Signalé : issu d'une source secondaire uniquement. Sources contradictoires : la note présente les deux versions. Peut être obsolète : la source la plus récente que nous avons trouvée est ancienne.
Rédigé dans nos propres mots à partir des sources ci-dessus. Signaler une correction