Wilson, Lionel; Head, James W. (1983). "A comparison of volcanic eruption processes on Earth, Moon, Mars, Io and Venus". Nature. 302 (5910): 663–669. Bibcode:1983Natur.302..663W. doi:10.1038/302663a0.
Burgisser, Alain; Bergantz, George W. (September 2002). "Reconciling pyroclastic flow and surge: the multiphase physics of pyroclastic density currents". Earth and Planetary Science Letters. 202 (2): 405–418. Bibcode:2002E&PSL.202..405B. doi:10.1016/S0012-821X(02)00789-6.
Jukes, Joseph Beete (1862). The Student's Manual of Geology (2nded.). Edinburgh, Scotland, U.K.: Adam and Charles Black. p.68. From p. 68: "The word 'ash' is not a very good one to include all the mechanical accompaniments of a subaerial or subaqueous eruption, since ash seems to be restricted to a fine powder, the residuum of combustion. A word is wanting to express all such accompaniments, no matter what their size or condition may be, when they are accumulated in such mass as to form beds of 'rock.' We might call them perhaps 'pyroclastic materials,' [...] "
Lacroix, A. (1904) La Montagne Pelée et ses Eruptions, Paris, Masson (in French) From vol. 1, p. 38: After describing on p. 37 the eruption of a "dense, black cloud" (nuée noire), Lacroix coins the term nuée ardente: "Peu après l'éruption de ce que j'appellerai désormais la nuée ardente, un immense nuage de cendres couvrait l'ile tout entière, la saupoudrant d'une mince couche de débris volcaniques." (Shortly after the eruption of what I will call henceforth the dense, glowing cloud [nuée ardente], an immense cloud of cinders covered the entire island, sprinkling it with a thin layer of volcanic debris.)
Weller, Roger (2005). Mount Vesuvius, Italy. Cochise College Department of Geology. Archived from the original on 23 October 2010. Retrieved 15 October 2010.
Giordano, Guido; Cas, Ray; Wright, John V. (2024). "Subaerial Pyroclastic Density Currents (Pyroclastic Flows and Surges): Origins, Types, and Deposit Characteristics". Volcanology. Springer Textbooks in Earth Sciences, Geography and Environment. pp.693–889. doi:10.1007/978-3-319-66613-6_10. ISBN978-3-319-66612-9.
Cas, Ray; Wright, John V.; Giordano, Guido (2024). "Subaqueous Flows of Pyroclastic Debris and Their Deposits: Origins, and Distinguishing Hot Gas-Supported Flows and Deposits from Water-Supported Ones". Volcanology. Springer Textbooks in Earth Sciences, Geography and Environment. pp.891–981. doi:10.1007/978-3-319-66613-6_11. ISBN978-3-319-66612-9.
Wilson, Lionel; Head, James W. (1983). "A comparison of volcanic eruption processes on Earth, Moon, Mars, Io and Venus". Nature. 302 (5910): 663–669. Bibcode:1983Natur.302..663W. doi:10.1038/302663a0.
Although the coining of the term nuée ardente in 1904 is attributed to the French geologist Antoine Lacroix, according to:
Hooker, Marjorie (1965). "The origin of the volcanological concept nuée ardente". Isis. 56 (4): 401–407. doi:10.1086/350041.
Burgisser, Alain; Bergantz, George W. (September 2002). "Reconciling pyroclastic flow and surge: the multiphase physics of pyroclastic density currents". Earth and Planetary Science Letters. 202 (2): 405–418. Bibcode:2002E&PSL.202..405B. doi:10.1016/S0012-821X(02)00789-6.
Camp, Vic. "KRAKATAU, INDONESIA (1883)". How Volcanoes Work. Department of Geological Sciences, San Diego State University, 31 Mar. 2006. Web. 15 Oct. 2010. Archived 2014-12-16 at the Wayback Machine.
Weller, Roger (2005). Mount Vesuvius, Italy. Cochise College Department of Geology. Archived from the original on 23 October 2010. Retrieved 15 October 2010.
Camp, Vic. "KRAKATAU, INDONESIA (1883)". How Volcanoes Work. Department of Geological Sciences, San Diego State University, 31 Mar. 2006. Web. 15 Oct. 2010. Archived 2014-12-16 at the Wayback Machine.
