Zobrazeno 1 - 10
of 30
pro vyhledávání: '"Speleogenesi"'
Autor:
giuliana madonia, giuseppe riolo, cipriano di maggio, rosario di pietro, ilenia m d'angeli, jo de waele, marco vattano
Flank margin caves form in coastal regions by mixing dissolution. Their development is controlled by the position of the freshsalt water mixing boundary, which in turn, is related to sea-level position. They are characterized by a typical cave patter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::11fe92daf516ebbb42a22e375c06645a
https://hdl.handle.net/10447/590778
https://hdl.handle.net/10447/590778
Autor:
Cesareo Saiz-Jimenez, Jo De Waele, Ana Z. Miller, Daniele Ghezzi, Sergio Sanchez-Moral, Jose L. Gonzalez-Pimentel, Martina Cappelletti, Tamara Martin-Pozas, Soledad Cuezva, Angel Fernandez-Cortes, Ilenia M. D’Angeli, Valme Jurado
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
The thermal spring of Fetida Cave, a still active sulfuric acid cave opening at sea level and located in Santa Cesarea Terme, southeastern Salento (Apulia region, Southern Italy) hosts abundant floating white filaments. The white filaments were mainl
Autor:
Ilenia M. D’Angeli, Fernando Gázquez, Philippe Audra, Gabriella Koltai, Hsun-Ming Hu, Tsai-Luen Yu, Jean-Claude Nobécourt, Cristina Carbone, Andrea Columbu, Roberto Chiesa, Jean-Yves Bigot, Chuan-Chou Shen, Vasile Heresanu, Jo De Waele
The Toirano karst system is located in the Ligurian Alps (north Italy), around 4.5 km inland from the coastline and carved in Middle Triassic dolostone. It comprises five cave levels over a 154 m altitudinal range, specifically Ulivo (340 m a.s.l.),
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a2dba0b3efb26c1e1458afe2dabfb997
https://hdl.handle.net/11585/784100
https://hdl.handle.net/11585/784100
Autor:
Ilenia M. D’Angeli, Sandro Galdenzi, Jo De Waele, Giuliana Madonia, Mario Parise, Marco Vattano
In Italy, especially along the Apennine Chain, numerous active and inactive sulfuric acid speleogenetic (SAS) caves have been documented in the last two decades. Here we present an overview of these peculiar hypogene systems, illustrating their main
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e10bf3c481137e9214d366a925fab65f
http://hdl.handle.net/10447/345665
http://hdl.handle.net/10447/345665
Italy is a country hosting a large number of hypogenic sulfuric acid (SAS) speleogenesis caves, mostly located along the Apennine chain, but also in Campania (along the coastline of Capo Palinuro), Apulia (along the coastline of Santa Cesarea Terme)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::44b1c9e0217d029f72507341191550b5
http://hdl.handle.net/10447/238907
http://hdl.handle.net/10447/238907
Autor:
Philippe Audra, Lukas Plan, Jean Claude Nobécourt, Ilenia M. D’Angeli, Marco Vattano, Giuliana Madonia, Jean-Yves Bigot, Jo De Waele
Publikováno v:
Geomorphology
Geomorphology, Elsevier, 2016, 253, pp.452-467. ⟨10.1016/j.geomorph.2015.10.019⟩
Geomorphology, Elsevier, 2016, 253, pp.452-467. ⟨10.1016/j.geomorph.2015.10.019⟩
Caves formed by rising sulfuric waters have been described from all over the world in a wide variety of climate settings, from arid regions to mid-latitude and alpine areas. H2S is generally formed at depth by reduction of sulfates in the presence of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f665bd7610ddb378c47c44b0ad41fdbf
https://hal.archives-ouvertes.fr/hal-01527924
https://hal.archives-ouvertes.fr/hal-01527924
Publikováno v:
Memorie dell’Istituto Italiano di Speleologia
Memorie dell’Istituto Italiano di Speleologia, 2015, I Gessi di Brisighella e Rontana: studio multidisciplinare di un’area carsica nella Vena del Gesso Romagnola, II (28), pp. 113-118
Memorie dell’Istituto Italiano di Speleologia, 2015, I Gessi di Brisighella e Rontana: studio multidisciplinare di un’area carsica nella Vena del Gesso Romagnola, II (28), pp. 113-118
International audience; In questa breve nota vengono illustrati i processi e meccanismi che hanno portato alla formazione dei sistemi carsici nelle aree gessose di Brisighella e Rontana. La morfologia delle grotte indica una loro forte influenza stru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b7bf824567dc5df410be90bd5009a511
https://hal.archives-ouvertes.fr/hal-01895461
https://hal.archives-ouvertes.fr/hal-01895461
In questa breve nota vengono illustrati i processi e meccanismi che hanno portato alla formazione dei sistemi carsici nelle aree gessose di Brisighella e Rontana. La morfologia delle grotte indica una loro forte influenza strutturale ed una loro form
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::da2787a0bccbcc01bb11bd9a710cc49e
http://hdl.handle.net/11585/524795
http://hdl.handle.net/11585/524795
Caratteristiche minero-petrografiche di alcuni particolari speleotemi delle grotte di Matanzas, Cuba
Autor:
D'ANGELI, ILENIA MARIA, DE WAELE, JO HILAIRE AGNES, Bontognali Tomaso Renzo Rezio, Tisato Nicola
Durante la spedizione organizzata da La Salle 3D – International Team, Photo, Video and Documentation nel Dicembre 2012 sono state studiate diverse grotte nei pressi di Matanzas, sulla costa settentrionale dell’Isola di Cuba a circa 90 km ad E de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::7cb486b5b42acc16893e043952a4751e
http://hdl.handle.net/11585/496786
http://hdl.handle.net/11585/496786
Autor:
COLUMBU, ANDREA, Drysdale Russell, CHIARINI, VERONICA, DE WAELE, JO HILAIRE AGNES, FORTI, PAOLO
Publikováno v:
Conference: XXII Congresso Nazionale di Speleologia – Euro Speleo Forum 2015 “Condividere i dati”
Conference: XXII Congresso Nazionale di Speleologia – Euro Speleo Forum 2015 “Condividere i dati”, May 2015, Pertosa-Auletta, Italy. pp. 227-282
Conference: XXII Congresso Nazionale di Speleologia – Euro Speleo Forum 2015 “Condividere i dati”, May 2015, Pertosa-Auletta, Italy. pp. 227-282
In Emilia-Romagna la stragrande maggioranza delle grotte si sviluppa nei gessi, sia triassici che messiniani. Tali rocce evaporitiche, pur rappresentando solo l’1% delle superfici affioranti, ospitano oltre 600 grotte, tra cui la grotta epigenica n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::202fb35ce1926951e8fb48ea53cb1364
https://hal-sde.archives-ouvertes.fr/hal-01895406
https://hal-sde.archives-ouvertes.fr/hal-01895406