Olhos de Água do Alviela
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.
पानी, प्रवाह और बाढ़
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.
यह क्यों मायने रखता है
A major Portuguese karst spring, historically part of Lisbon's water supply, and the deepest documented cave dive in the sources found for Portugal.
परिस्थितियाँ
Visibility on some dives in side passages dropped to 0.5-1.5 m on the return.
प्रकाशित स्रोतों से सामान्य अनुमानित दायरे, वर्तमान परिस्थितियाँ नहीं।
सर्वे और एक्सप्लोरेशन इतिहास
| 1988 | Patrick Jolivet reaches about 580 m from the entrance at -98 m. [1] |
| 2002 | A CNPS-FFESSM expedition with Portuguese cavers re-lines and surveys 1,370 m and reaches -125 m. [1] |
प्रवेश द्वार और डाइव साइटें
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.
इस system के लिए अभी तक कोई individual entrance सूचीबद्ध नहीं है।
इस पृष्ठ का हर तथ्य, अपने source के साथ (7)
| तथ्य | स्थिति | स्रोत |
|---|---|---|
| The expedition's deepest dive stopped at -125 m more than 700 m from the entrance. | सत्यापित | [1] |
| The expedition produced 1,370 m of survey and about 200 m of new passage with a maximum depth of -125 m. | सत्यापित | [1] |
| Patrick Jolivet's 1988 terminus was at about 580 m and -98 m. | सत्यापित | [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. | रिपोर्ट किया गया | [1] |
| The account mentions water at about 17 °C. | सत्यापित | [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. | सत्यापित | [1] |
| Portuguese partners handled accommodation, re-equipping the cave and the authorisations for the expedition. | पुराना हो सकता है | [1] |
सत्यापित: किसी आधिकारिक या प्राथमिक स्रोत से पुष्टि हुई जिसे हमने खोला। रिपोर्ट किया गया: केवल द्वितीयक स्रोत से। स्रोतों में मतभेद: नोट में दोनों संस्करण दिए गए हैं। पुराना हो सकता है: हमें मिला सबसे नया स्रोत भी पुराना है।
ऊपर दिए गए sources से हमारे अपने शब्दों में लिखा गया। सुधार की रिपोर्ट करें