Radon migration into different building types at medium and low south-eastern flank of Mt Etna (Sicily): connection with the volcanic activity

2011 ◽  
Vol 66 (3) ◽  
pp. 923-931 ◽  
Author(s):  
Santo La Delfa ◽  
Fabio Vizzini ◽  
Giuseppe Patanè
2020 ◽  
Vol 8 ◽  
Author(s):  
Silvio De Angelis ◽  
Matthew M. Haney ◽  
John J. Lyons ◽  
Aaron Wech ◽  
David Fee ◽  
...  
Keyword(s):  

2019 ◽  
Vol 6 ◽  
Author(s):  
Raphael S. M. De Plaen ◽  
Andrea Cannata ◽  
Flavio Cannavo' ◽  
Corentin Caudron ◽  
Thomas Lecocq ◽  
...  

2018 ◽  
Vol 357 ◽  
pp. 418-424 ◽  
Author(s):  
Giorgio De Guidi ◽  
Fabio Brighenti ◽  
Francesco Carnemolla ◽  
Sebastiano Imposa ◽  
Salvatore Antonio Marchese ◽  
...  

2013 ◽  
Vol 14 (8) ◽  
pp. 2886-2899 ◽  
Author(s):  
Marco Liuzzo ◽  
Sergio Gurrieri ◽  
Gaetano Giudice ◽  
Giovanni Giuffrida

2006 ◽  
Vol 164 (3) ◽  
pp. 697-718 ◽  
Author(s):  
Nathalie Feuillet ◽  
Massimo Cocco ◽  
Carla Musumeci ◽  
Concetta Nostro
Keyword(s):  

1976 ◽  
Vol 17 (75) ◽  
pp. 73-77
Author(s):  
C. M. Clapperton ◽  
D. E. Sugden

AbstractAlthough it is known that cirque glaciers once existed in the Falkland Islands, it has remained in doubt whether or not the islands were ever covered by ice caps or an ice sheet during the Cainozoic. This paper scrutinizes geomorphological evigernce on the south-eastern flank of a high massif in West Falkland. It is suggested that, at the time of their maximum extent in the Cainozoic, the largest glaciers were no more than 2.7 km long.


Sign in / Sign up

Export Citation Format

Share Document