AGNESE LIVIA FISCHETTI and PETER ATTEMA (EDS), ALLE PENDICI DEI COLLI ALBANI: DINAMICHE INSEDIATIVE E CULTURA MATERIALE AI CONFINI CON ROMA (Groningen Archaeological Studies 35). Groningen: Barkhuis, 2019. Pp. 276. isbn 9789492444837. €54.95.

2021 ◽  
Vol 111 ◽  
pp. 271-273
Author(s):  
Eoin O'Donoghue
Keyword(s):  
2007 ◽  
Vol 7 (1) ◽  
pp. 269-276
Author(s):  
R. Drusiani ◽  
P. Bersani ◽  
P. Penta

A brief description of the geomorphological, historical, and archaeological aspects of the Colli Albani area, where the volcanic lakes of Albano and Nemi are situated, is followed by an examination on the problem of the policies of lake Albano regulation, by means of an ancient tunnel dating at least to the 5th century BC. In particular, it is investigated how, in the presence of even severe atmospheric phenomena, it was possible to control fluctuations in the level of the lake on the banks of which there were large settlements. Mathematical model simulations indicate the effectiveness of the ancient tunnel in achieving these objectives.


2017 ◽  
Vol 478 ◽  
pp. 179-191 ◽  
Author(s):  
Matteo Trolese ◽  
Guido Giordano ◽  
Francesca Cifelli ◽  
Aldo Winkler ◽  
Massimo Mattei

2018 ◽  
Vol 30 (1) ◽  
pp. 125-133 ◽  
Author(s):  
Alessandro Fabbrizio ◽  
Mario Gaeta ◽  
Michael R. Carroll ◽  
Maurizio Petrelli
Keyword(s):  

2021 ◽  
Author(s):  
Corin Jorgenson ◽  
Luca Caricchi ◽  
Michael Stueckelberger ◽  
Giovanni Fevola ◽  
Gregor Weber

<p>Melt inclusions provide a window into the inner workings of magmatic systems. Both mineral chemistry and volatile distributions within melt inclusions can provide valuable information about the processes modulating magma ascent and preceding volcanic eruptions. Many melt inclusions host vapour bubbles which can be rich in CO<sub>2</sub> and H<sub>2</sub>O and must be taken into consideration when assessing the volatile budget of magmatic reservoirs. These vapour bubbles can be the product of differential volumetric contraction between the melt inclusion and host phase during an eruption or indicate an excess fluid phase in the magma reservoir. Thus, determining the distribution of volatiles between melt and vapour bubbles is integral to our fundamental understanding of melt inclusions, and by extension the evolution of volatiles within magmatic systems.</p><p>A large dataset of 79 high-resolution tomographic scans of clinopyroxene and leucite phenocrysts from the Colli Albani Caldera Complex (Italy) was recently acquired at the German Electron Synchrotron (DESY). These tomograms allow us to quantify the volume of melt inclusions and associated vapour bubble both glassy and microcrystalline melt inclusions. Notably, in the glassy melt inclusions the vapour bubbles exist either as a single large vapour bubble in the middle of the melt inclusion or as several smaller vapour bubbles distributed around the edge of the melt inclusion. These two types of melt inclusions can coexist within a single crystal. We suggest that the occurrence of these rim- bubbles is caused by one of two exsolution pathways, either pre-entrapment and bubble migration or post entrapment with preferential exsolution at the rims. By combining the analysis of hundreds of melt inclusions with the chemistry of the host phase we aim to unveil magma ascent rates and distribution of excess fluids within the magmatic system of Colli Albani, which produced several mafic-alkaline large volume ignimbrites.</p>


Author(s):  
Alfredo Di Domenicantonio ◽  
Manuela Ruisi ◽  
Paolo Traversa
Keyword(s):  

2008 ◽  
Vol 176 (2) ◽  
pp. 225-240 ◽  
Author(s):  
M. Teresa Mariucci ◽  
Simona Pierdominici ◽  
Luca Pizzino ◽  
Fabrizio Marra ◽  
Paola Montone

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