
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.
EspeleoWorld
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
长度: 45 m · 深度: 17 m
最新资料
https://espeleoworld.com/zh/c/cavita-di-monte-capoccia-pelata-spoleto-perugia
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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.
地形图
© Mauro Barbieri · CC BY-SA 4.0, https://creativecommons.org/licenses/by-sa/4.0/ · Federazione Umbra Gruppi Speleologici (FUGS), Catasto Speleologico dell'Umbria · https://catasto.fugs.it/index.php?mod=caves&op=view&id=1011
照片
© 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
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
附近洞穴
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




