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Voragine Pozzale

Voragine Pozzale

Bottle-shaped shaft about 30 m wide and 20 m deep, with the bottom occupied by a short gallery filled with debris.

Spoleto 48m 32m

Bottle-shaped shaft about 30 m wide and 20 m deep, with the bottom occupied by a short gallery filled with debris.

特征

  • 类型: 竖井
  • 市镇: Spoleto
  • 洞穴登记号: UM3
  • 长度: 48 米
  • 深度: 32 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 dirt road for about 1.5 km until crossing the ridge; from there proceed along the road to the right (not the left-hand track) that leads to Monte Capoccia Pelata. Proceed downhill parallel to the Fosso Pozzale for about 1.2 km where, to the left of the road, near the confluence of three streams, the wide and visible shaft opens.

Route: 2.8 km, 30 min. Route information: Walkable path, Dangerous access.

Entrance: Wide open-air shaft, the access rigging is to be verified. Entrance setting: Natural. Access: Fence. Location: Fosso di Pozzale, Monti Martani.

地图

洞口

出发前请务必核对坐标和通行条件。

  1. Voragine Pozzale

    海拔: 971 m

    42.775153, 12.582403
下载所有洞口的 GPX

照片

Voragine Pozzale - 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=3

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描述

形态

Bottle-shaped shaft about 30 m wide and 20 m deep. From the bottom a short gallery filled with debris branches off. Trend: Predominantly vertical.

Geology: MAI Maiolica - Upper Jurassic-Lower Cretaceous (Tithonian-Aptian); stratified micritic limestones; Stratified; See report by Famiani & Cardinali - 2018. This karst morphology is defined in the scientific literature as synkhole and is generated by the collapse of the ceiling of the pre-existing cavity, whose original structure is visible on the bottom of the shaft in the north-eastern portion of the cavity towards the Fosso di Pozzale.

水文

Hydrology and meteorology: no circulation; no airflow was detected at the entrance - 2018.

行进路线

Traversability: Experts only; recommended period All year round. Rigging: Temporary; use the fence posts for the first pitch from the surface. Progression difficulty: Pits. Hazards: Dangerous access, Rockfalls/collapses, Pits that discharge.

历史

Notes on the name: It takes its name from the Fosso Pozzale where it is located.

生物

Environmental and biological protections: No.

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参考文献

LOTTI B. (1902) Sulla costituzione geologica del gruppo montuoso di Amelia VINASSA DE REGNY P. (1906) Appunti di geologia Umbra PRINCIPI P. (1913) Secondo contributo allo studio dei fenomeni carsici dell'Umbria (Catena dei Monti Martani) LOTTI B. (1917) Il gruppo montuoso del Monte Martano LOTTI B. (1926) Descrizione geologica dell'Umbria MONTANARI R. (1940) I Monti Martani LIPPI BONCAMBI C. (1941) La pedologia della Catena Martana (Umbria) con alcune osservazioni sul fenomeno carsico di essa LIPPI BONCAMBI C. (1950) Sullo stato attuale del Catasto Speleologico dell'Umbria LEMMI G. (1958) Note di aggiornamento del Catasto Speleologico dell'Umbria LEMMI G. & COLETTI G. (1961) Elenco catastale delle grotte dell'Umbria VIVIANI C.G. (1971) L'attività del gruppo Speleologico C.A.I. Perugia nel 1970 TRIPPINI S. (2012) Cose de' pazzi, grotte e vedute dei dintorni dell'antica Civitella 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=3 · 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