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Bahasa antarmuka
Olhos de Água do Alviela

Olhos de Água do Alviela

Foto: GualdimG · CC BY-SA 4.0
Status akses belum terverifikasi · sesuai yang dipublikasikan 2002 The expedition's Portuguese partners obtained the necessary authorisations; no current public access rule for diving was found. Aturan akses bisa berubah: konfirmasikan dengan pemilik lahan atau otoritas pengelola sebelum Anda berangkat.
Terdokumentasi Juga dikenal sebagai: Alviela spring, Nascente do Alviela, Olhos d'Água do Alviela, Alviela
Panjang yang telah disurvei
Tidak diterbitkan
Kedalaman terdokumentasi
125 m (410 ft)
Pintu masuk yang tercantum
0
Suhu air
17 °C
Survei dan eksplorasi
FFESSM Commission nationale de plongée souterraine (CNPS), Portuguese cavers (Filipe Worsdell, Olímpio Martins, Piotr Gajek, José António Crispim)

1,370 m surveyed during the CNPS-FFESSM expedition; total cave length not stated. Reached during the CNPS-FFESSM expedition, more than 700 m from the entrance.

The main karst spring of the river Alviela at the foot of the Monsanto syncline in central Portugal, once tapped for Lisbon's water supply. A French-Portuguese expedition surveyed 1,370 m and reached 125 m depth.

The Olhos de Água do Alviela rise at the foot of the Monsanto syncline and drain most of the Planalto de Santo António karst plateau, with part of the water thought to come from the Mira-Minde polje to the north-east. In the early twentieth century the spring was captured and linked by aqueduct to Lisbon, though it was later replaced by other sources.

The flooded cave descends as a sizeable gallery, 4 to 8 m across in places, with side branches. Patrick Jolivet reached about 580 m and 98 m depth in 1988. A national cave-diving commission (CNPS) expedition of the FFESSM, organised with Portuguese cavers who handled accommodation, re-lining and authorisations, re-equipped the line, surveyed 1,370 m including about 200 m of new passage, and stopped at 125 m depth more than 700 m from the entrance.

The account notes a water temperature of about 17 °C and a depigmented crayfish seen 140 m into a side passage.

Air, arus, dan banjir

The spring drains the Planalto de Santo António; tracing work cited by the expedition indicates that part of the water comes from the Mira-Minde polje.

Mengapa ini penting

A major Portuguese karst spring, historically part of Lisbon's water supply, and the deepest documented cave dive in the sources found for Portugal.

Kondisi

Visibility on some dives in side passages dropped to 0.5-1.5 m on the return.

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

Sejarah survei dan eksplorasi

1988Patrick Jolivet reaches about 580 m from the entrance at -98 m. [1]
2002A CNPS-FFESSM expedition with Portuguese cavers re-lines and surveys 1,370 m and reaches -125 m. [1]

Pintu masuk dan lokasi selam

One entrance, the spring pool; the expedition rigged a tyrolean to move equipment to the pool edge and a rope deviation for the last pitch.

Belum ada pintu masuk individual yang terdaftar untuk sistem ini.

Sumber: [1] plongeesout.ffspeleo.fr ↗[2] plongeesout.ffspeleo.fr ↗ · telah diperiksa 2026-10-14
Setiap fakta di halaman ini, beserta sumbernya (7)
FaktaStatusSumber
The expedition's deepest dive stopped at -125 m more than 700 m from the entrance. Terverifikasi [1]
The expedition produced 1,370 m of survey and about 200 m of new passage with a maximum depth of -125 m. Terverifikasi [1]
Patrick Jolivet's 1988 terminus was at about 580 m and -98 m. Terverifikasi [1]
The expedition is filed on the FFS site as the 2002 FFESSM account; the text says the CNPS adopted the project in September 2002.Exact expedition dates are not stated in the account. Dilaporkan [1]
The account mentions water at about 17 °C. Terverifikasi [1]
The spring drains most of the Planalto de Santo António, with part of the water coming from the Mira-Minde polje; it was captured for Lisbon's water supply by an aqueduct built early in the twentieth century. Terverifikasi [1]
Portuguese partners handled accommodation, re-equipping the cave and the authorisations for the expedition. Mungkin sudah tidak mutakhir [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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