Pozzicola
Bell-shaped pit about 8 m deep, with a predominantly vertical trend, bounded by a fence at its entrance.
EspeleoWorld
Pozzicola
Bell-shaped pit about 8 m deep, with a predominantly vertical trend, bounded by a fence at its entrance.
Spoleto
الطول: 11 m · العمق: 8 m
السجل المحدّث
https://espeleoworld.com/ar/c/pozzicola-spoleto-perugia
قد تتغير المعلومات. تحقق دائمًا من الإحداثيات والوصول والطقس وظروف الكهف قبل الانطلاق.
Bell-shaped pit about 8 m deep, with a predominantly vertical trend, bounded by a fence at its entrance.
الصور
© 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=4
الوصف
الشكل
Bell-shaped pit about 8 m deep. Trend: predominantly vertical. Entrance: cavity bounded by a fence at its entrance, about 2 metres in diameter, with a tree usable for the descent.
المياه
Hydrology and meteorology: no circulation; no airflow was detected at the entrance - 2018.
التقدم
Traversability: demanding; recommended period all year round. Rigging: temporary. Progression difficulty: shafts. Hazards: dangerous access.
تفاصيل أخرى
Geology: MAI Maiolica - Upper Jurassic-Lower Cretaceous (Tithonian-Aptian); stratified micritic limestones; stratified; see report by Famiani & Cardinali - 2018. The cavity formed through the combined effect of the tectonic system that guided the displacements and primary fractures in the limestone formation on which the karst action was established, followed by a gravitational collapse of the vaults with the related accumulation of debris on the bottom.
التاريخ
Notes on the name: referred to by Lippi Boncambi as Voragine Pozzicula in the 1950 Cadastral List.
الأحياء
Other hypogean fauna: troglobitic Carabid beetle: Duvalius consortii Magrini & Degiovanni, 2006; troglobitic Carabid beetle: Duvalius andreuccii Magrini & Vanni, 1984. Bait trapping revealed the presence of two specialized troglobitic species. Studies and monitoring: entomological.
تعليقات المستخدمين (0)
لا توجد تعليقات بعد.
كن أول من يشارك تجربته!
الاستكشافات المسجلة (0)
لا توجد استكشافات مسجلة بعد.
سجل زيارتك لهذا الكهف!
المراجع
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 FAMIANI F. & CARDINALI R. (2018) Esplorazioni Monti Martani Gennaio-Febbraio 2018
الكهوف القريبة
المصدر: Catasto Cavità Umbria (Federazione Umbra Gruppi Speleologici, FUGS) (catasto.fugs.it)، مع تعديلات. 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=4 · بيانات عام 2025 · المصدر: Catasto Cavità Umbria (Federazione Umbra Gruppi Speleologici, FUGS) (catasto.fugs.it)، مع تعديلات. LicenseRef-FUGS-media-per-item Federazione Umbra Gruppi Speleologici (FUGS), Catasto Speleologico dell'Umbria · بيانات عام 2025