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Émergence de Lamerlie

A small spring whose natural entrance, choked with limestone blocks, opens beneath a road; a very low passage leads to a first small sump, then to flooded galleries and a clay-sand terminus.

Sauliac-sur-Célé 17m

A small spring whose natural entrance, choked with limestone blocks, opens beneath a road; a very low passage leads to a first small sump, then to flooded galleries and a clay-sand terminus.

特征

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洞口

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  1. Émergence de Lamerlie

    44.532377, 1.745454
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描述

形态

A small square-section tunnel, built of cut stone, crosses the road embankment beneath which opens the natural entrance of the spring, choked with limestone blocks detached from the surrounding rock. The passage immediately becomes very low, on the order of about twenty centimetres, and remains so for 4 metres. The roof, which had risen noticeably, drops again at 28 metres from the entrance. Beyond, the gallery takes on larger proportions and the depth varies from 1 to 6 metres. At 46 metres one lands in a sort of small chamber. The gallery, of elliptical emerged section, is oriented to the N.W. for 25 metres and ends in a duck-under followed by a clay-sand deposit. A clay coating covers the walls and the roof, which lowers steadily to the terminus. Just below the water surface a large joint is visible, whose inclined floor drops abruptly to -17 at the entrance of the flooded passage. The elliptical section over the first half of the route then becomes more stretched vertically; ledges and a small incised channel are sometimes visible and the direction of the passage bends twice.

洞穴次生沉积物

At 46 metres, the small chamber is occupied by a flowstone that descends from a section of upper passage heading due S. Developing 3 metres above the exit threshold of the spring, it is sheltered from floods, which explains a relatively abundant concretion. Perhaps this passage formerly opened to the outside, at the level of the road?

水文

The first small sump is very certainly unprimed by about ten centimetres during the annual low-water periods. Beyond, one must swim, the depth varying from 1 to 6 metres; at this depth and to the left of the outlet of the narrow sump passage, a flooded gallery descends toward the S.W.: is it a diversion toward an unknown spring in the bed of the Célé? Visibility is average (5 to 10 m.) and one ascends the flooded passage almost horizontally for about 70 metres to butt against a rocky slope. When the spring flows in the meadow bordering the Célé, the cavity is then submerged except for the upper passage. At low water it is not possible to detect the slightest current; only pumping would make it possible to verify whether there is a supply at that time.

行进路线

The very low passage continues for 4 metres, from which point progression continues over small gours oriented toward the interior and temporarily fed by a flowstone on the right. At the first small sump, immersion becomes obligatory and it may be prudent to have a mask with a snorkel in case the water reaches the surface over the 2 metres of length of this passage. A short opposition in a small meander allows one to avoid wedged blocks and the pool is found again at the foot of a sand bank.

历史

The summer of 77 having been rather wet, a quick survey, in August, of the right bank of the Célé, downstream of Marcilhac, allows Péjout to note a recent flow of water at the small spring of émergence de Lamerlie, along the D 41, whose name could be the contraction of “la mère Lie”. This spring, opening in the limestones of the Middle Bathonian, was known only to a few rare initiates; a brief glance at the first ten metres suggests that a continuation is possible. On 1 September, Péjout and Coustou slip into the masonry passage that passes under the road and emerge in front of the natural porch of the cavity; Péjout forces a low passage, a former known terminus, crawls up a few gours and stops in front of a sumping pool occupying the entire width of the small gallery. A second attempt is launched on 18 September: the objective, to dive the small sump. Coustou, Héreil and Péjout bring diving equipment but find that it will not be necessary, the sump being slightly unprimed following a late low-water period. They pass the duck-under, a few metres long, and swim for about twenty metres in a more spacious gallery, twice bent at a right angle. A landing and a short opposition in a meander, and the water is found again at the foot of a sand bank. The gallery continues straight for more than twenty metres and the ceiling gradually approaches the pool to disappear entirely at 83 m. from the entrance opening. On the other hand, a short descent, free-diving and using a snorkel, reveals a large flooded joint directly beneath the gallery; Péjout, who had geared up in the meantime, dives and descends to -15 m. where he glimpses a gallery toward the N.N. Having no guide line, he ascends. On the return, an upper, concretion-covered passage is traversed near the first pool. On 2 October, Coustou, Dagès and Péjout are again at work, the last two being equipped to explore the flooded passage glimpsed at the bottom of the joint; the equipment is painfully carried into the terminal gallery. The two divers can then sink into the calm, green-clear water, Péjout in the lead with the Ariadne's thread held by Coustou wedged in opposition near the bottom of the emerged part of the joint. An elliptical-section gallery is traversed for 70 m. to a rise in the ceiling, without any continuation being visible. The return nearly turned dramatic: Dagès, having cylinder problems, had gone back up when Péjout found himself completely entangled and tied up in the Ariadne's thread in the very middle of the flooded passage; a prisoner, and on a single cylinder, he could no longer fin. His air reserve running out, he owed his salvation only to his dagger, which allowed him to free himself and reach the surface in extremis. Then Coustou and Péjout carry out the topographic survey (compass, clinometer and tape) of the cavity while Dagès spots a flooded start at 6 m. depth beneath the first pool. The natural lowering of the pool inside the cavity, even at low water, will never be significant enough to clear the two flooded galleries; the continuation of explorations can only be done by diving or by carrying out serious pumping in the terminal joint. This last solution, easily achievable with a good pump, would offer the advantage of verifying whether a connection exists between the two basins and moreover of possibly evaluating the supply flow rate. The easy clearing of a clay-sand mass at the current terminus also seems worthy of attention.

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包含来自 Grottocenter (Wikicaves)(grottocenter.org)的信息,依据开放数据库许可协议(Open Database License,ODbL 1.0, https://opendatacommons.org/licenses/odbl/1-0/)提供,已修改。 · https://grottocenter.org/ui/entrances/9132 · 衍生数据可应要求依据 ODbL 提供: [email protected] · 2026年数据 · 来源:Grottocenter (Association Wikicaves), worldwide collaborative cave database(grottocenter.org),已修改。 CC BY-SA 3.0, https://creativecommons.org/licenses/by-sa/3.0/ Grottocenter (Wikicaves) · 文本作者:CDS 46 · 由 Espeleoworld 改编(规范化、翻译);改编内容依据 CC BY-SA 3.0, https://creativecommons.org/licenses/by-sa/3.0/ 许可 · https://grottocenter.org/ui/entrances/9132 · 2026年数据