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Sistem cave

Manantial de la Aleta

Sinkhole73 m dalamDominican Republic, La Altagracia
Status akses belum terverifikasi · sesuai yang dipublikasikan 2002 An underwater archaeological site inside Parque Nacional Cotubanamá, studied by research teams with Dominican government and park support. No recreational diving access or current rules are published. Aturan akses bisa berubah: konfirmasikan dengan pemilik lahan atau otoritas pengelola sebelum Anda berangkat.
Terdokumentasi Juga dikenal sebagai: La Aleta, Spring of the Fin, Manantial La Aleta, La Aleta sinkhole
Panjang yang telah disurvei
Tidak diterbitkan
Kedalaman terdokumentasi
73 m (239 ft)
Pintu masuk yang tercantum
1
Suhu air
24 °C
Survei dan eksplorasi
Indiana University Office of Underwater Science, Museo del Hombre Dominicano

Maximum depth of the debris-mound slopes below the water surface, as measured for the 2002 study.

A deep flooded sinkhole inside Parque Nacional Cotubanamá that was a Taíno ritual site. Its oxygen-free deep water preserved wooden objects and pottery recovered by archaeological divers from 40-71 m. It is an archaeological research site.

Manantial de la Aleta, the 'Spring of the Fin', lies inside the national park about 5 km inland from the nearest coast. Several small openings in the ground lead into a chamber that drops 16 m to a roughly circular pool about 40 m across. Under water, a mound of collapsed rubble rises to within 34 m of the surface, and its slopes descend to 73 m.

The water is clear in the top 10 m, then passes through a milky layer charged with hydrogen sulfide before clearing again below about 20 m. Below about 11 m the water has no oxygen and no light, conditions that preserved organic Taíno artefacts for centuries.

Indiana University archaeologists, working with Dominican partners, mapped and recovered 245 artefacts from the slopes at 40 to 71 m, including a small carved wooden seat (duho), a vomiting spatula, a small wooden vessel tentatively linked to the cohoba ritual, and decorated pottery. Four ceremonial plazas lie within about 75 m of the sinkhole, and the researchers interpret it as a regional ritual centre linked to ancestor worship. A description by the 16th-century chronicler Bartolomé de las Casas has been argued to refer to this spring.

The site is an underwater archaeological site in a national park. No public diving access is published.

Geologi

A collapse sinkhole in the karst of the south-east Dominican Republic: rubble fallen from the roof forms a submerged mound whose top is at 34 m and whose flanks reach 73 m.

Air, arus, dan banjir

The study reports no measurable flow and little runoff, a sulfide-laden layer from about 10 m that clears below 20 m, oxygen-free water below about 11 m, and a nearly constant water temperature of about 24 °C.

Mengapa ini penting

Its investigators interpret it as a regional Taíno ritual centre connected with ancestor worship. Because the deep water is dark and oxygen-free, it preserved wooden artefacts that did not survive at comparable sites such as Cueva de Chicho.

Kondisi

Hydrogen sulfide layer from about 10 m; oxygen-free water below about 11 m (2002 study).

Rentang tipikal dari sumber yang dipublikasikan, bukan kondisi saat ini.

Sejarah survei dan eksplorasi

1981José Guerrero identified the Manantial de la Aleta during a brief survey sponsored by the Museo del Hombre Dominicano. [1]
2002Beeker, Conrad and Foster reported 245 artefacts recovered from depths of 40 to 71 m. [1]

Pintu masuk dan lokasi selam

Several small openings in the ground surface lead to one chamber. Archaeological site; no public access point is published.

Sumber: [1] Journal of Caribbean Archaeology (hosted by Florida Museum of Natural History) ↗[2] Wikipedia ↗ · telah diperiksa 2026-10-14
Setiap fakta di halaman ini, beserta sumbernya (9)
FaktaStatusSumber
The site is within the East National Park, 20 km from the Padre Nuestro complex and 5 km inland from the nearest shoreline.The park was renamed Parque Nacional Cotubanamá in 2014 (Wikipedia, orientation). Terverifikasi [1]
The chamber drops 16 m to a roughly circular pool about 40 m across. Terverifikasi [1]
A rubble mound reaches to 34 m below the water surface and its slopes reach a maximum depth of 73 m.2002. Terverifikasi [1]
Water is clear to 10 m, then a milky sulfide layer blurs visibility until it clears below 20 m; water is anoxic below about 11 m and about 24.2 °C. Terverifikasi [1]
The water column is a fairly constant 24.2 °C.2002 measurement. Terverifikasi [1]
245 artefacts were recovered from slopes at 40-71 m, including organic items such as a small duho and a vomiting spatula; four ceremonial plazas lie within 75 m. Terverifikasi [1]
José Guerrero identified the site in a 1981 survey for the Museo del Hombre Dominicano. Terverifikasi [1]
The 2002 study acknowledges support from Dominican government officials and the park's staff; no public diving access is described.No current rule text was found, so access status is left as unknown; the site is documented only as a research site. Dilaporkan [1]
No coordinates are given; the site is inside the national park about 5 km inland and 20 km from Padre Nuestro.Archaeological site; location withheld. Terverifikasi [1]

Terverifikasi: dinyatakan oleh sumber resmi atau sumber primer yang kami buka langsung. Dilaporkan: hanya dari sumber sekunder. Sumber berbeda pendapat: catatan menyajikan kedua versi. Mungkin sudah kedaluwarsa: sumber terbaru yang kami temukan sudah lama.

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