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Cavità di Monte Capoccia Pelata

Cavità di Monte Capoccia Pelata

Cave formed on a fault in the Monti Martani, with horizontal development and deepening along the fracture, whose entrance, about 50 cm in diameter, opens in the flat meadow.

Spoleto 45m 17m

Cave formed on a fault in the Monti Martani, with horizontal development and deepening along the fracture, whose entrance, about 50 cm in diameter, opens in the flat meadow.

特征

  • 类型: 洞穴
  • 市镇: Spoleto
  • 洞穴登记号: UM1011
  • 长度: 45 米
  • 深度: 17 米
  • 记录更新:

位置

Coming from Massa Martana or Giano dell’Umbria via the SP 445 towards the Monti Martani, park the vehicle at Passo di Acqua Canale. Continue on foot towards Monte Forzano following the path heading SOUTH that starts from the wooden gate. Continue along the uphill track for about 1.6 km until crossing the ridge. At the junction keep left on the track leading to Monte Capoccia Pelata, where after about 800 m at the top you leave the path to the left, reaching after 30-40 m the entrance that opens in the middle of the meadow among some small depressions. Route: 2.4 km, 25 min on foot. Path passable.

Location: Monti Martani, Monte Capoccia Pelata. Entrance about 50 cm in diameter that opens in the flat meadow; natural entrance setting. Free access; the access is located at a small doline.

地图

洞口

出发前请务必核对坐标和通行条件。

  1. Cavità di Monte Capoccia Pelata

    海拔: 1055 m

    42.778800, 12.585180
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照片

Cavità di Monte Capoccia Pelata - 照片, Spoleto查看图片
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© Mauro Barbieri · LicenseRef-FUGS-media-per-item · Federazione Umbra Gruppi Speleologici (FUGS), Catasto Speleologico dell'Umbria · https://catasto.fugs.it/index.php?mod=caves&op=view&id=1011

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描述

形态

Fissure formed on a fault with horizontal development but with deepening that follows the fracture, currently impassable but with the possibility of clearing and widening. Trend: horizontal/vertical. The cave develops within the Maiolica formation (Upper Jurassic-Lower Cretaceous, Tithonian-Aptian), stratified micritic limestones, along a tectonic structure with a north-western trend (about 330°). The fault within which the cave develops is directly connected to the tectonic system that develops in the Fosso di Pozzale valley and that gave rise to the other caves (Pozzale, Pozzicola and Pozzicoletto).

洞穴次生沉积物

Abundant presence of moonmilk along the walls.

水文

No significant air flows were detected - 2018. Water difficulties: other water-related.

行进路线

Traversability: experts only; recommended period all year round. Progression difficulty: pits, narrow passages, traverses. Rigging: temporary; an aerial traverse must be rigged along the fracture since the cave is made slippery by the abundant presence of moonmilk on the walls. Hazards: dangerous access.

历史

Notes on the name: it takes its name from the mountain of the same name.

生物

Bats: certainly present given the presence of guano on 17/02/2025.

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参考文献

LOTTI B. (1917) Il gruppo montuoso del Monte Martano MONTANARI R. (1940) I Monti Martani FAMIANI F. & CARDINALI R. (2018) Esplorazioni Monti Martani Gennaio-Febbraio 2018

来源:Catasto Cavità Umbria (Federazione Umbra Gruppi Speleologici, FUGS)(catasto.fugs.it),已修改。 LicenseRef-FUGS-no-licence-stated Federazione Umbra Gruppi Speleologici (FUGS), Catasto Speleologico dell'Umbria · https://catasto.fugs.it/index.php?mod=caves&op=view&id=1011 · 2025年数据 · 来源:Catasto Cavità Umbria (Federazione Umbra Gruppi Speleologici, FUGS)(catasto.fugs.it),已修改。 LicenseRef-FUGS-media-per-item Federazione Umbra Gruppi Speleologici (FUGS), Catasto Speleologico dell'Umbria · 2025年数据